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            [post_title] => 5beavers
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            [post_content] => 
            [post_title] => 1beavers
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            [post_title] => 2beavers
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            [post_author] => 12
            [post_date] => 2022-10-01 13:18:04
            [post_date_gmt] => 2022-10-01 11:18:04
            [post_content] => Photograph by Inge Dekker © All rights reserved
            [post_title] => 6.DSCF4142
            [post_excerpt] => The steel frame needs regular clearing; beavers aren’t easily deceived. August 23, 2022.
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            [post_author] => 12
            [post_date] => 2022-10-01 13:17:36
            [post_date_gmt] => 2022-10-01 11:17:36
            [post_content] => Photograph by Inge Dekker © All rights reserved
            [post_title] => 5. DSCF4139
            [post_excerpt] => The dam appears to have been repaired, August 23, 2022. 
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            [post_date] => 2022-10-01 13:17:11
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            [post_content] => Photograph by Inge Dekker © All rights reserved
            [post_title] => 4._3MD3489
            [post_excerpt] => A worrying sight—has the beaver given up the dam? April 15, 2022. 
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            [post_content] => Photograph by Inge Dekker © All rights reserved
            [post_title] => 3. FFA71286-7D6D-4AAC-82FE-B80B9C5D7DAF
            [post_excerpt] => Beaver dam with beaver deceiver pipe installed, January 19, 2022. 
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            [post_content] => Photograph by Inge Dekker © All rights reserved
            [post_title] => 2. DSCF4149
            [post_excerpt] => Traces of tree felling by beavers along the Keersop river. 
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            [post_content] => Photograph by Pieter van der Braak © All rights reserved
            [post_title] => 1. image00003
            [post_excerpt] => Beaver in the Dome River, July 23, 2022. 
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            [post_date] => 2022-10-01 12:53:49
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            [post_title] => 4beavers
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            [post_title] => 3beavers
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            [ID] => 50903
            [post_author] => 12
            [post_date] => 2022-09-30 15:09:33
            [post_date_gmt] => 2022-09-30 13:09:33
            [post_content] => 

Where is the Planetary? curatorial statement

Where is the Planetary? curatorial statement

[post_title] => A Planetary Praxis in the Anthropocene [post_excerpt] => [post_status] => publish [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => a-planetary-praxis-in-the-anthropocene [to_ping] => [pinged] => [post_modified] => 2022-09-30 15:12:22 [post_modified_gmt] => 2022-09-30 13:12:22 [post_content_filtered] => [post_parent] => 0 [guid] => https://www.anthropocene-curriculum.org/?post_type=contribution&p=50903 [menu_order] => 0 [post_type] => contribution [post_mime_type] => [comment_count] => 0 [filter] => raw ) [12] => Array ( [ID] => 50902 [post_author] => 12 [post_date] => 2022-09-30 14:58:46 [post_date_gmt] => 2022-09-30 12:58:46 [post_content] => Image by Koki Tanika © All rights reserved [post_title] => where_is_the_planetary_key_visual [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => where_is_the_planetary_key_visual [to_ping] => [pinged] => [post_modified] => 2022-09-30 15:09:23 [post_modified_gmt] => 2022-09-30 13:09:23 [post_content_filtered] => [post_parent] => 50903 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/09/where_is_the_planetary_key_visual.jpeg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [13] => Array ( [ID] => 50877 [post_author] => 99 [post_date] => 2022-09-29 13:43:07 [post_date_gmt] => 2022-09-29 11:43:07 [post_content] => [post_title] => Collaborative Practice on a Changing Planet [post_excerpt] => [post_status] => publish [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => collaborative-practice-on-a-changing-planet [to_ping] => [pinged] => [post_modified] => 2022-09-29 14:24:57 [post_modified_gmt] => 2022-09-29 12:24:57 [post_content_filtered] => [post_parent] => 0 [guid] => https://www.anthropocene-curriculum.org/?post_type=event&p=50877 [menu_order] => 0 [post_type] => event [post_mime_type] => [comment_count] => 0 [filter] => raw ) [14] => Array ( [ID] => 50870 [post_author] => 99 [post_date] => 2022-09-29 13:23:52 [post_date_gmt] => 2022-09-29 11:23:52 [post_content] => [post_title] => Where is the Planetary? Day 3 [post_excerpt] => [post_status] => publish [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => where-is-the-planetary-day-3 [to_ping] => [pinged] => [post_modified] => 2022-09-29 13:45:36 [post_modified_gmt] => 2022-09-29 11:45:36 [post_content_filtered] => [post_parent] => 0 [guid] => https://www.anthropocene-curriculum.org/?post_type=event&p=50870 [menu_order] => 0 [post_type] => event [post_mime_type] => [comment_count] => 0 [filter] => raw ) [15] => Array ( [ID] => 50867 [post_author] => 99 [post_date] => 2022-09-29 13:12:58 [post_date_gmt] => 2022-09-29 11:12:58 [post_content] => [post_title] => Where is the Planetary? Day 2 [post_excerpt] => [post_status] => publish [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => where-is-the-planetary-day-2 [to_ping] => [pinged] => [post_modified] => 2022-09-29 13:46:18 [post_modified_gmt] => 2022-09-29 11:46:18 [post_content_filtered] => [post_parent] => 0 [guid] => https://www.anthropocene-curriculum.org/?post_type=event&p=50867 [menu_order] => 0 [post_type] => event [post_mime_type] => [comment_count] => 0 [filter] => raw ) [16] => Array ( [ID] => 50864 [post_author] => 99 [post_date] => 2022-09-29 13:00:16 [post_date_gmt] => 2022-09-29 11:00:16 [post_content] => [post_title] => Where is the Planetary? Day 1 [post_excerpt] => [post_status] => publish [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => where-is-the-planetary-day-1 [to_ping] => [pinged] => [post_modified] => 2022-09-29 13:46:45 [post_modified_gmt] => 2022-09-29 11:46:45 [post_content_filtered] => [post_parent] => 0 [guid] => https://www.anthropocene-curriculum.org/?post_type=event&p=50864 [menu_order] => 0 [post_type] => event [post_mime_type] => [comment_count] => 0 [filter] => raw ) [17] => Array ( [ID] => 50842 [post_author] => 99 [post_date] => 2022-09-29 12:10:03 [post_date_gmt] => 2022-09-29 10:10:03 [post_content] => Photograph courtesy Maya Marshak © All rights reserved [post_title] => motheaten Sasha 3 [post_excerpt] => Maya Marshak, Moth-eaten, 2016. Archival agricultural entomology collection [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => motheaten-sasha-3 [to_ping] => [pinged] => [post_modified] => 2022-09-29 17:12:30 [post_modified_gmt] => 2022-09-29 15:12:30 [post_content_filtered] => [post_parent] => 49814 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/09/motheaten-Sasha-3.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [18] => Array ( [ID] => 50841 [post_author] => 12 [post_date] => 2022-09-29 12:02:50 [post_date_gmt] => 2022-09-29 10:02:50 [post_content] => Photograph by Jeremias Herberg [post_title] => Zur Deutschen Einigkeit [post_excerpt] => Impressions of Lusatia. The former coal mining region has been described as a "wounded landscape," bearing the scars of its industrial past. Today, it is not just the area’s physical environment that is in need of repair but also its social fabric. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => zur-deutschen-einigkeit [to_ping] => [pinged] => [post_modified] => 2022-10-03 14:28:10 [post_modified_gmt] => 2022-10-03 12:28:10 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/09/Zur-Deutschen-Einigkeit.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [19] => Array ( [ID] => 50840 [post_author] => 12 [post_date] => 2022-09-29 12:02:49 [post_date_gmt] => 2022-09-29 10:02:49 [post_content] => Photograph by Jeremias Herberg [post_title] => Love Wut Freiheit [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => love-wut-freiheit [to_ping] => [pinged] => [post_modified] => 2022-09-29 14:59:48 [post_modified_gmt] => 2022-09-29 12:59:48 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/09/Love-Wut-Freiheit.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [20] => Array ( [ID] => 50839 [post_author] => 12 [post_date] => 2022-09-29 12:02:48 [post_date_gmt] => 2022-09-29 10:02:48 [post_content] => Photograph by Jeremias Herberg [post_title] => forst - auf staat sein nacken [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => forst-auf-staat-sein-nacken [to_ping] => [pinged] => [post_modified] => 2022-09-29 14:59:45 [post_modified_gmt] => 2022-09-29 12:59:45 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/09/forst-auf-staat-sein-nacken.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [21] => Array ( [ID] => 50838 [post_author] => 12 [post_date] => 2022-09-29 12:02:39 [post_date_gmt] => 2022-09-29 10:02:39 [post_content] => Photograph by George Hallett, CC BY-SA 3.0 [post_title] => Jann_Turner_with_Eugene_de_Kock,_TRC_Headquarters_in1997 [post_excerpt] => Jann Turner with Eugene de Kock, Truth Reconciliation Commission Headquarters, 1997. Kock was a South African Police colonel and assassin during the apartheid regime. Turner is the daughter of the prominent 1970s anti-Apartheid activist Dr Rick Turner, who was assassinated in 1978. 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In this audio episode, we hear from various participants of the Unearthing the Present event and discuss the science and sociopolitical implications of the Anthropocene.

An Audio Reflection on the Science and Sociopolitical Implications of the Anthropocene. [post_title] => The Geology and Culture of the Anthropocene [post_excerpt] => [post_status] => publish [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => the-geology-and-culture-of-the-anthropocene [to_ping] => [pinged] => [post_modified] => 2022-09-29 09:43:27 [post_modified_gmt] => 2022-09-29 07:43:27 [post_content_filtered] => [post_parent] => 0 [guid] => https://www.anthropocene-curriculum.org/?post_type=contribution&p=50374 [menu_order] => 0 [post_type] => contribution [post_mime_type] => [comment_count] => 0 [filter] => raw ) [24] => Array ( [ID] => 50387 [post_author] => 129 [post_date] => 2022-09-29 09:43:13 [post_date_gmt] => 2022-09-29 07:43:13 [post_content] =>

As part of the Unearthing the Present events in May 2022, the public were given the opportunity to ask questions members of the AWG questions about their work.

The AWG Answer Questions About Their Work

During the program Unearthing the Present, the Anthropocene Working Group (AWG) presented findings from their twelve research sites. On May 20, 2022, the public were given the unique opportunity to pose questions to the AWG in an open forum. You can find out more about the AWG’s work in the publication The Geological Anthropocene, which provides an in-depth introduction to each of the research sites and the geological ratification process.

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A conversation between Dr. Catherine Russell, Anthropocene sedimentologist and Dr. Jamie Allen, an artist and media researcher.

Being a Sedimentologist in the Anthropocene

The generous discussion presented here began as a conversation between Dr. Catherine Russell, Anthropocene sedimentologist and now a US-UK Fulbright-Lloyd’s Visiting Scholar at the University of New Orleans, and Dr. Jamie Allen, an artist and media researcher. Catherine’s interests in Anthropocene research began through its elaborations in geoscience, through the work of people like Jan Zalasiewicz, with whom she worked at the University of Leicester. Jamie works on issues related to the scientific mastery of nature, systems sciences like ecology, and the distance and intimacies between “pure” and “applied” science. Their discussion started on a walk, continued on a bus trip, and proceeded through online calls, messaging, and email, including during a pandemic and its lockdowns, for quite a long time—almost three years of intermittent check-ins paying witness to changing perspectives, sometimes difficult realizations, and the generative magic of discussion between people with rather different perspectives.

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See Red Woman’s Workshops was a feminist a collective screen-printing studio operating in London between 1974-1990. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => fig-3-wages-for-housework [to_ping] => [pinged] => [post_modified] => 2022-09-13 19:58:18 [post_modified_gmt] => 2022-09-13 17:58:18 [post_content_filtered] => [post_parent] => 50212 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/09/Fig-3-Wages-for-Housework.jpeg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [70] => Array ( [ID] => 50215 [post_author] => 12 [post_date] => 2022-09-13 19:47:24 [post_date_gmt] => 2022-09-13 17:47:24 [post_content] => Image by Louise Carver and Jamie Allen, from Strange Exchanges in an Almanac for the Beyond. Published by Tropic Editions © All rights reserved [post_title] => Fig 1 Strange Exchanges [post_excerpt] => Historical dynamics and strange exchanges within machinic processions converging logics towards the reparative modes of capitalist production. 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What alliances and common questions can help to work toward a science of partnerships, especially in processes that include more-than-human entities?

Stratigraphic analyses of the Anthropocene’s geology and debates on the decolonization of nature (in the arts and humanities) have pursued radically different paths in zooming in on the human histories left in soils, rocks and sediments. Yet, a shared sense of urgency underpins these different interests. In this session recorded during Unearthing the Present, professor of anthropology Lesley Green and professor of earth sciences Francine M. G. McCarthy consider the ways scientists and humanities scholars need to weigh the politics of their own work in very different ways. What alliances and common questions can help to work toward a science of partnerships, especially in processes that include more-than-human entities?

[post_title] => Exchange on Geo-Inheritance [post_excerpt] => [post_status] => publish [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => exchange-on-geo-inheritance [to_ping] => [pinged] => [post_modified] => 2022-09-13 16:33:17 [post_modified_gmt] => 2022-09-13 14:33:17 [post_content_filtered] => [post_parent] => 0 [guid] => https://www.anthropocene-curriculum.org/?post_type=contribution&p=50145 [menu_order] => 0 [post_type] => contribution [post_mime_type] => [comment_count] => 0 [filter] => raw ) [84] => Array ( [ID] => 50142 [post_author] => 12 [post_date] => 2022-09-13 16:32:33 [post_date_gmt] => 2022-09-13 14:32:33 [post_content] =>

What are the prospects of living among radioactive substances as military spending on atomic weapons increases and some countries invest in and maintain nuclear power on their paths to “net zero” CO₂ emissions?

The presence of critical radioactivity in environments everywhere on the planet is owed to mid-twentieth-century atomic weapon tests as well as to the ongoing use of nuclear energy and concomitant accidents. While the notion of the “Nuclear Age” evoked the idea of a legacy from the past only a few years ago, we currently face a much different nuclear situation amid ongoing geopolitical shifts and ruptures. In this session recorded during Unearthing the Present, professor of environmental radioactivity Andy Cundy and artist-writer Brian Holmes ask: What are the prospects of living among radioactive substances as military spending on atomic weapons increases and some countries invest in and maintain nuclear power on their paths to “net zero” CO₂ emissions?

[post_title] => Exchange on the Half Life of the Nuclear Age [post_excerpt] => [post_status] => publish [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => exchange-on-the-half-life-of-the-nuclear-age [to_ping] => [pinged] => [post_modified] => 2022-09-13 16:32:33 [post_modified_gmt] => 2022-09-13 14:32:33 [post_content_filtered] => [post_parent] => 0 [guid] => https://www.anthropocene-curriculum.org/?post_type=contribution&p=50142 [menu_order] => 0 [post_type] => contribution [post_mime_type] => [comment_count] => 0 [filter] => raw ) [85] => Array ( [ID] => 50139 [post_author] => 12 [post_date] => 2022-09-13 16:32:26 [post_date_gmt] => 2022-09-13 14:32:26 [post_content] =>

How can we mediate and embed scientific findings into new narrations? And what contingency, what order, will these narrations have?

How can we mediate and embed scientific findings into new narrations? And what contingency, what order, will these narrations have? In this session recorded during Unearthing the Present, artist Susan Schuppli and paleoclimatologist Liz Thomas draw upon their extensive research on ice cores to reflect on the processification of ice and its situated material condition in evidence-based research. They discuss the procedures of “continuous flow analysis” as well as their practical and epistemic preconditions that help to read climate developments into the past and future.

[post_title] => Exchange on Melting Narrations [post_excerpt] => [post_status] => publish [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => exchange-on-melting-narrations [to_ping] => [pinged] => [post_modified] => 2022-09-13 16:32:26 [post_modified_gmt] => 2022-09-13 14:32:26 [post_content_filtered] => [post_parent] => 0 [guid] => https://www.anthropocene-curriculum.org/?post_type=contribution&p=50139 [menu_order] => 0 [post_type] => contribution [post_mime_type] => [comment_count] => 0 [filter] => raw ) [86] => Array ( [ID] => 50135 [post_author] => 12 [post_date] => 2022-09-13 16:32:20 [post_date_gmt] => 2022-09-13 14:32:20 [post_content] =>

How do the geochronologists and geohistorians understand their response-ability to material signals from the past?

Determining the age of materials—a seemingly objective act—is, in fact, one of multiple significations evoking cosmic hopes and political resonances. Radionuclide and radiocarbon signals offer humankind understanding of more than just chronometric measures—they attach human history and activities to material processes. The laboratory practice of geochronology is one of both scientific fact and fiction that relies on climate research, environmental studies, archaeology and forensics. In this session recorded during Unearthing the Present, artist and researcher Jamie Allen and geochronologist Irka Hajdas ask: How can we imagine the intimacy that geochronology creates with abstracted, distanced events? And how do the geochronologists and geohistorians interpreting these events understand their response-ability to material signals from the past?

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How best can organizations reconcile alliance building, promote public discussions on environmental crises and nurture cultural shifts?

Different institutions have been involved in the formalizing process of the Anthropocene, among them the Anthropocene Working Group (AWG) alongside the cultural institution Haus der Kulturen der Welt and the scientific research institute Max Planck Institute for the History of Science. In this session recorded during Unearthing the Present, Simon Turner, the scientific coordinator of the AWG project, and Victor Galaz, a scholar of complex systems, governance and global sustainability, focused on the difficulties and affordances of such an undertaking. While scientifically studying the concurrence between transformations in social, financial and environmental systems remains challenging, at the institutional level we may ask: How best can organizations reconcile alliance building, promote public discussions on environmental crises and nurture cultural shifts?

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49921 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/09/image6.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [103] => Array ( [ID] => 49926 [post_author] => 12 [post_date] => 2022-09-02 13:44:43 [post_date_gmt] => 2022-09-02 11:44:43 [post_content] => [post_title] => image5 [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => image5-2 [to_ping] => [pinged] => [post_modified] => 2022-09-02 13:44:43 [post_modified_gmt] => 2022-09-02 11:44:43 [post_content_filtered] => [post_parent] => 49921 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/09/image5.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [104] => Array ( [ID] => 49925 [post_author] => 12 [post_date] => 2022-09-02 13:43:26 [post_date_gmt] => 2022-09-02 11:43:26 [post_content] => Photograph by Jamie Allen [post_title] => image3 [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => image3 [to_ping] => [pinged] => [post_modified] => 2022-09-07 13:42:40 [post_modified_gmt] => 2022-09-07 11:42:40 [post_content_filtered] => [post_parent] => 49921 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/09/image3.jpeg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [105] => Array ( [ID] => 49923 [post_author] => 12 [post_date] => 2022-09-02 13:39:44 [post_date_gmt] => 2022-09-02 11:39:44 [post_content] => "heap of salt ursula". [post_title] => heap of salt ursula [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => heap-of-salt-ursula-2 [to_ping] => [pinged] => [post_modified] => 2022-09-02 13:39:47 [post_modified_gmt] => 2022-09-02 11:39:47 [post_content_filtered] => [post_parent] => 49921 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/09/heap-of-salt-ursula.mp3 [menu_order] => 0 [post_type] => attachment [post_mime_type] => audio/mpeg [comment_count] => 0 [filter] => raw ) [106] => Array ( [ID] => 49908 [post_author] => 12 [post_date] => 2022-08-31 11:49:37 [post_date_gmt] => 2022-08-31 09:49:37 [post_content] => Image courtesy of Catherine Russell [post_title] => Screenshot 2022-08-31 at 11.46.50 [post_excerpt] => The logo for the Anthropocene Sediment Network, which Catherine established in 2020. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => screenshot-2022-08-31-at-11-46-50-2 [to_ping] => [pinged] => [post_modified] => 2022-08-31 11:50:28 [post_modified_gmt] => 2022-08-31 09:50:28 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/08/Screenshot-2022-08-31-at-11.46.50-1.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [107] => Array ( [ID] => 49898 [post_author] => 12 [post_date] => 2022-08-31 11:18:20 [post_date_gmt] => 2022-08-31 09:18:20 [post_content] => Drawing by Catherine Russell [post_title] => Screenshot 2022-08-31 at 11.18.02 [post_excerpt] => A collection of drawings of graptolites, small plankton now long extinct. Their shapes are used to unravel mysteries about stratigraphy and ancient ocean currents. For scale, B, C, F, G, I, and J are all to the same scale and B is 13 mm long. A, D, E, H, K, L, and M are all twice the scale. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => screenshot-2022-08-31-at-11-18-02 [to_ping] => [pinged] => [post_modified] => 2022-09-02 14:07:56 [post_modified_gmt] => 2022-09-02 12:07:56 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/08/Screenshot-2022-08-31-at-11.18.02.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [108] => Array ( [ID] => 49885 [post_author] => 12 [post_date] => 2022-08-31 10:43:57 [post_date_gmt] => 2022-08-31 08:43:57 [post_content] => [post_title] => Photo 28-02-2019, 18 18 06 [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => photo-28-02-2019-18-18-06 [to_ping] => [pinged] => [post_modified] => 2022-08-31 10:43:57 [post_modified_gmt] => 2022-08-31 08:43:57 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/08/Photo-28-02-2019-18-18-06.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [109] => Array ( [ID] => 49884 [post_author] => 12 [post_date] => 2022-08-31 10:43:46 [post_date_gmt] => 2022-08-31 08:43:46 [post_content] => Photograph by Catherine Russell [post_title] => Photo 27-02-2019, 16 18 23 [post_excerpt] => The vast of model of the Mississippi River structure engraved in polymer at Louisiana State University's Center for River Studies, which Catherine first encountered during a trip to LSU in February 2019. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => photo-27-02-2019-16-18-23 [to_ping] => [pinged] => [post_modified] => 2022-08-31 11:36:24 [post_modified_gmt] => 2022-08-31 09:36:24 [post_content_filtered] => [post_parent] => 49852 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/08/Photo-27-02-2019-16-18-23.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [110] => Array ( [ID] => 49883 [post_author] => 12 [post_date] => 2022-08-31 10:43:36 [post_date_gmt] => 2022-08-31 08:43:36 [post_content] => Photograph by Catherine Russell [post_title] => Photo 26-02-2019, 10 55 47 [post_excerpt] => The river deposits have many layers—seen here is a layer of brown clay at the bottom of the image, with layers of sand and silt above. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => photo-26-02-2019-10-55-47 [to_ping] => [pinged] => [post_modified] => 2022-08-31 11:31:37 [post_modified_gmt] => 2022-08-31 09:31:37 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/08/Photo-26-02-2019-10-55-47.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [111] => Array ( [ID] => 49882 [post_author] => 12 [post_date] => 2022-08-31 10:43:23 [post_date_gmt] => 2022-08-31 08:43:23 [post_content] => [post_title] => Photo 25-02-2019, 17 21 10 [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => photo-25-02-2019-17-21-10 [to_ping] => [pinged] => [post_modified] => 2022-08-31 10:43:23 [post_modified_gmt] => 2022-08-31 08:43:23 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/08/Photo-25-02-2019-17-21-10.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [112] => Array ( [ID] => 49881 [post_author] => 12 [post_date] => 2022-08-31 10:43:13 [post_date_gmt] => 2022-08-31 08:43:13 [post_content] => Photograph by Catherine Russell [post_title] => Photo 24-02-2019, 17 05 11 [post_excerpt] => The swamp landscape of southern Louisiana. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => photo-24-02-2019-17-05-11 [to_ping] => [pinged] => [post_modified] => 2022-08-31 11:30:35 [post_modified_gmt] => 2022-08-31 09:30:35 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/08/Photo-24-02-2019-17-05-11.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [113] => Array ( [ID] => 49880 [post_author] => 12 [post_date] => 2022-08-31 10:43:01 [post_date_gmt] => 2022-08-31 08:43:01 [post_content] => Photograph by Catherine Russell [post_title] => Photo 24-02-2019, 16 01 52 [post_excerpt] => An alligator enjoying the sunny swamps of Louisiana. “I remember the sheer scale of the region once I was on the ground,” recalls Catherine. “It is so easy to think that you know a place from satellite photos and maps, but actually being there and connecting knowledge to reality is a different experience.” [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => photo-24-02-2019-16-01-52 [to_ping] => [pinged] => [post_modified] => 2022-08-31 11:28:28 [post_modified_gmt] => 2022-08-31 09:28:28 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/08/Photo-24-02-2019-16-01-52.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [114] => Array ( [ID] => 49879 [post_author] => 12 [post_date] => 2022-08-31 10:42:50 [post_date_gmt] => 2022-08-31 08:42:50 [post_content] => Photograph by Catherine Russell [post_title] => Photo 23-02-2019, 17 08 43 [post_excerpt] => A mosaic of the Mississippi River adorns the floor of the terminal building at Dallas/Fort Worth International Airport in Texas. “It showed me the importance of the river to the local community right away,” remarks Catherine. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => photo-23-02-2019-17-08-43 [to_ping] => [pinged] => [post_modified] => 2022-08-31 11:27:28 [post_modified_gmt] => 2022-08-31 09:27:28 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/08/Photo-23-02-2019-17-08-43.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [115] => Array ( [ID] => 49878 [post_author] => 12 [post_date] => 2022-08-31 10:42:37 [post_date_gmt] => 2022-08-31 08:42:37 [post_content] => [post_title] => Photo 03-04-2017, 14 04 05 [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => photo-03-04-2017-14-04-05 [to_ping] => [pinged] => [post_modified] => 2022-08-31 10:42:37 [post_modified_gmt] => 2022-08-31 08:42:37 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/08/Photo-03-04-2017-14-04-05.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [116] => Array ( [ID] => 49877 [post_author] => 12 [post_date] => 2022-08-31 10:42:25 [post_date_gmt] => 2022-08-31 08:42:25 [post_content] => Photograph by Catherine Russell [post_title] => Photo 03-04-2017, 12 13 37 [post_excerpt] => Catherine presents her PhD research findings at the American Association for Petroleum Geoscience in Houston, Texas, 2017. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => photo-03-04-2017-12-13-37 [to_ping] => [pinged] => [post_modified] => 2022-08-31 11:24:32 [post_modified_gmt] => 2022-08-31 09:24:32 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/08/Photo-03-04-2017-12-13-37.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [117] => Array ( [ID] => 49876 [post_author] => 12 [post_date] => 2022-08-31 10:42:15 [post_date_gmt] => 2022-08-31 08:42:15 [post_content] => Photograph by Catherine Russell [post_title] => Photo 02-03-2019, 13 24 22 [post_excerpt] => The clean-up begins. “The beads were so widespread, even in the trees, so it prompted me to see them as a part of this environment and include them in future studies,” recalls Catherine. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => photo-02-03-2019-13-24-22 [to_ping] => [pinged] => [post_modified] => 2022-08-31 11:45:30 [post_modified_gmt] => 2022-08-31 09:45:30 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/08/Photo-02-03-2019-13-24-22.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [118] => Array ( [ID] => 49875 [post_author] => 12 [post_date] => 2022-08-31 10:42:01 [post_date_gmt] => 2022-08-31 08:42:01 [post_content] => Photograph by Catherine Russell [post_title] => Photo 02-03-2019, 13 10 20 [post_excerpt] => Beaded necklaces are thrown from Mardi Gras parade floats into the crowd below. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => photo-02-03-2019-13-10-20 [to_ping] => [pinged] => [post_modified] => 2022-08-31 11:38:28 [post_modified_gmt] => 2022-08-31 09:38:28 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/08/Photo-02-03-2019-13-10-20.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [119] => Array ( [ID] => 49874 [post_author] => 12 [post_date] => 2022-08-31 10:41:54 [post_date_gmt] => 2022-08-31 08:41:54 [post_content] => Photograph by Catherine Russell [post_title] => Photo 01-03-2019, 20 05 03 [post_excerpt] => A nighttime parade as part of Mardi Gras celebrations in New Orleans, 2019. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => photo-01-03-2019-20-05-03 [to_ping] => [pinged] => [post_modified] => 2022-08-31 11:38:42 [post_modified_gmt] => 2022-08-31 09:38:42 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/08/Photo-01-03-2019-20-05-03.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [120] => Array ( [ID] => 49851 [post_author] => 12 [post_date] => 2022-08-30 15:53:38 [post_date_gmt] => 2022-08-30 13:53:38 [post_content] => [post_title] => Picture1 [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => picture1-8 [to_ping] => [pinged] => [post_modified] => 2022-08-30 15:59:33 [post_modified_gmt] => 2022-08-30 13:59:33 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/08/Picture1.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [121] => Array ( [ID] => 49840 [post_author] => 12 [post_date] => 2022-08-30 11:28:27 [post_date_gmt] => 2022-08-30 09:28:27 [post_content] => Photograph courtesy Kreismuseum Bitterfeld © All rights reserved [post_title] => LEAD Technologies Inc. V1.01 [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => lead-technologies-inc-v1-01 [to_ping] => [pinged] => [post_modified] => 2022-09-22 12:16:08 [post_modified_gmt] => 2022-09-22 10:16:08 [post_content_filtered] => [post_parent] => 49837 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/08/10489-Ballonplatz-25.09.1910.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [122] => Array ( [ID] => 49839 [post_author] => 12 [post_date] => 2022-08-30 11:28:22 [post_date_gmt] => 2022-08-30 09:28:22 [post_content] => Photograph courtesy Kreismuseum Bitterfeld © All rights reserved [post_title] => 01014 Ansichtskarte Bitterfeld total mit Industriegelände [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 01014-ansichtskarte-bitterfeld-total-mit-industriegela%cc%88nde [to_ping] => [pinged] => [post_modified] => 2022-09-22 12:16:19 [post_modified_gmt] => 2022-09-22 10:16:19 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/08/01014-Ansichtskarte-Bitterfeld-total-mit-Industriegelände-.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [123] => Array ( [ID] => 49813 [post_author] => 12 [post_date] => 2022-08-26 12:15:08 [post_date_gmt] => 2022-08-26 10:15:08 [post_content] => Photograph by Robb Hannawacker, from Wikicommons, public domain. [post_title] => Edwards_Glassy-wing_Moth_Pseudohemihyalea_edwarsii_-71649_det._R._Hannawacker_North_Rim_Grand_Canyon_Arizona_August_1948_Noel_Crickmer_49553271262-scaled [post_excerpt] => Edwards' Glassy-wing Moth (Pseudohemihyalea edwardsii). 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[post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => hkw-cloud-cloud [to_ping] => [pinged] => [post_modified] => 2022-08-26 11:57:31 [post_modified_gmt] => 2022-08-26 09:57:31 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/08/hkw-cloud-cloud.gif [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/gif [comment_count] => 0 [filter] => raw ) [126] => Array ( [ID] => 49802 [post_author] => 12 [post_date] => 2022-08-26 11:48:47 [post_date_gmt] => 2022-08-26 09:48:47 [post_content] => [post_title] => hkw-clean-test1 [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => hkw-clean-test1 [to_ping] => [pinged] => [post_modified] => 2022-09-29 17:03:25 [post_modified_gmt] => 2022-09-29 15:03:25 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/08/hkw-clean-test1.gif [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/gif [comment_count] => 0 [filter] => raw ) [127] => Array ( [ID] => 49795 [post_author] => 12 [post_date] => 2022-08-26 11:35:51 [post_date_gmt] => 2022-08-26 09:35:51 [post_content] => Photograph by Werner Bayer, CC0 1.0 [post_title] => 40505906613_cec2f2f9e5_k [post_excerpt] => A grid of metallic cars adorns the facade of a Museum Garage in Miami Design District. 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Held in Spring 2022 as the next iteration of State of Nature—a project initiated by Goethe-Institut and Max Mueller Bhavan Mumbai—the exhibition New Natures: A Terrible Beauty is Born was a proposition to rethink the world as we know it today.

A Terrible Beauty is Born

As the next iteration of State of Nature—a project initiated by Goethe-Institut and Max Mueller Bhavan Mumbai in 2018 that brings together multiple perspectives to understand and address our present ecological crisis—the exhibition New Natures: A Terrible Beauty is Born is a proposition to rethink the world as we know it today. Taking place in Spring 2022, the exhibition was curated by Ravi Agarwal and curator of literature Ranjit Hoskote, who conceptualised a complimentary programme consisting of prominent writers, poets, and essayists.

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A close reading of coral samples from the Caribbean Sea and Pacific Ocean—finding signals of ocean warming and the impacts of offshore oil extraction.

How do we conceive of coral as a life form? What does it mean to read in an archive signs of its impending destruction? During Unearthing the Present, scientists, researchers, and artists undertook a close reading of coral samples from the Caribbean Sea and Pacific Ocean. These samples—from West Flower Garden Bank Reef (Gulf of Mexico, USA) and Flinders Reef (Coral Sea, Australia)—have recorded a variety of anthropogenic signals, including ocean warming and the impacts of offshore oil extraction. The changing climate, which is so accurately recorded by coral reefs, increasingly leads to their demise. West Flower Garden Bank Reef and Flinders Reef are two of twelve sites across the globe explored by geologists looking for traces of human impact on the planet. Read our online guide The Geological Anthropocene for more information and to explore the other sites.

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Tracing socio-political upheavals and technological change in sediment samples from Sihailongwan Lake in northeastern China.

During Unearthing the Present, scientists, researchers, artists, and activists gathered to decipher stratigraphic samples taken from lake deposits in northeastern China—in an effort to jointly identify ways and means of responding to the signals of the Anthropocene. The sediment cores from Sihailongwan Lake are particularly marked by the history of Chinese industrialization, with both socio-political upheavals and technological change precisely traced in the sediment samples. Participants explored the chemical markers of Chinese environmental and industrial history and the different ways in which energy sources and usage have been conceptualized in northeastern China. Sihailongwan Lake is one of twelve sites across the globe explored by geologists looking for traces of human impact on the planet. Read our online guide The Geological Anthropocene for more information and to explore the other sites.

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How do different forms of societal organization and land use over the centuries affect the environment on local and planetary levels?

During Unearthing the Present, scientists, researchers, and artists discussed sediments of Canada’s Crawford Lake that record traces of the Anthropocene—and much more: changes in the sediment composition and color show that the area was inhabited as early as the thirteenth century. This raises the question of how different forms of societal organization and land use affect the environment on local and planetary levels. Reading this earth archive also brings the very practice of reading and the position of the reader to the fore. Who is looking for what and with which interests? And how do history and culture inscribe themselves into stratigraphic knowledge production? Crawford Lake is one of twelve sites across the globe explored by geologists looking for traces of human impact on the planet. Read our online guide The Geological Anthropocene for more information and to explore the other sites.

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Researchers study an ice core from one of the fastest-warming places on Earth—revealing key data on Antarctica’s environmental history.

The Antarctic Peninsula is the northernmost arm of the planet’s coldest, most remote continent. While the recent increase in heat waves indicates that the area is particularly sensitive to anthropogenic climate change, Antarctica as a landscape still seems to defy an anthropocentric gaze. During Unearthing the Present, scientists, researchers, artists, and activists studied an Antarctic ice core sample, which contains detailed data on Antarctica’s environmental history, from the amount of local snowfall to rising CO₂ concentrations in the atmosphere. The Antarctic Peninsula is one of twelve sites across the globe explored by geologists looking for traces of human impact on the planet. Read our online guide The Geological Anthropocene for more information and to explore the other sites.

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image/jpeg [comment_count] => 0 [filter] => raw ) [174] => Array ( [ID] => 49633 [post_author] => 12 [post_date] => 2022-08-16 16:24:48 [post_date_gmt] => 2022-08-16 14:24:48 [post_content] => [post_title] => SihailongwanMaarLake [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => sihailongwanmaarlake [to_ping] => [pinged] => [post_modified] => 2022-08-16 16:27:23 [post_modified_gmt] => 2022-08-16 14:27:23 [post_content_filtered] => [post_parent] => 49465 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/08/SihailongwanMaarLake.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [175] => Array ( [ID] => 49631 [post_author] => 12 [post_date] => 2022-08-16 16:24:45 [post_date_gmt] => 2022-08-16 14:24:45 [post_content] => [post_title] => Antarctica [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => antarctica [to_ping] => [pinged] => [post_modified] => 2022-08-16 16:25:32 [post_modified_gmt] => 2022-08-16 14:25:32 [post_content_filtered] => [post_parent] => 49462 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/08/Antarctica.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [176] => Array ( [ID] => 49595 [post_author] => 99 [post_date] => 2022-08-16 11:36:52 [post_date_gmt] => 2022-08-16 09:36:52 [post_content] =>

Recording of a live, read-along event presenting a collage of writing by climate fiction authors from all over the world.

This read-along event, held during Unearthing the Present in May 2022 and recorded in the images and film below, presented a collage of writing by climate fiction authors from all over the world. Short synopses of selected books were read in chronological order according to their fictive position in time. The artist duo Beate Geissler and Oliver Sann suggest that these fictional constructions have the potential to appear as trustworthy mirrors of current cultural atmospheres—and can serve as indices and symptoms of the present, or echoes of today. As archetypal vibrancies of deep time and a future imagined as pre-traumatic anticipation of catastrophe, they preempt the coming world in disarray.

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19:03:11 [post_modified_gmt] => 2022-08-14 17:03:11 [post_content_filtered] => [post_parent] => 49595 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/08/P958-174A0819-original-2.jpeg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [178] => Array ( [ID] => 49604 [post_author] => 99 [post_date] => 2022-08-14 18:59:57 [post_date_gmt] => 2022-08-14 16:59:57 [post_content] => Photograph by Katy Otto [post_title] => P958-174A0824-original [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => p958-174a0824-original [to_ping] => [pinged] => [post_modified] => 2022-08-14 19:02:29 [post_modified_gmt] => 2022-08-14 17:02:29 [post_content_filtered] => [post_parent] => 49595 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/08/P958-174A0824-original.jpeg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [179] => Array ( [ID] => 49603 [post_author] => 99 [post_date] => 2022-08-14 18:59:56 [post_date_gmt] => 2022-08-14 16:59:56 [post_content] => Photograph by Katy Otto [post_title] => P958-174A0837-original [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => p958-174a0837-original [to_ping] => [pinged] => [post_modified] => 2022-08-14 19:02:27 [post_modified_gmt] => 2022-08-14 17:02:27 [post_content_filtered] => [post_parent] => 49595 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/08/P958-174A0837-original.jpeg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [180] => Array ( [ID] => 49602 [post_author] => 99 [post_date] => 2022-08-14 18:59:55 [post_date_gmt] => 2022-08-14 16:59:55 [post_content] => Photograph by Katy Otto [post_title] => P958-174A0841-original [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => p958-174a0841-original [to_ping] => [pinged] => [post_modified] => 2022-08-14 19:02:24 [post_modified_gmt] => 2022-08-14 17:02:24 [post_content_filtered] => [post_parent] => 49595 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/08/P958-174A0841-original.jpeg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [181] => Array ( [ID] => 49601 [post_author] => 99 [post_date] => 2022-08-14 18:59:54 [post_date_gmt] => 2022-08-14 16:59:54 [post_content] => Photograph by Katy Otto [post_title] => P958-174A0862-original [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => p958-174a0862-original [to_ping] => [pinged] => [post_modified] => 2022-08-14 19:02:21 [post_modified_gmt] => 2022-08-14 17:02:21 [post_content_filtered] => [post_parent] => 49595 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/08/P958-174A0862-original.jpeg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [182] => Array ( [ID] => 49600 [post_author] => 99 [post_date] => 2022-08-14 18:59:53 [post_date_gmt] => 2022-08-14 16:59:53 [post_content] => Photograph by Katy Otto [post_title] => P958-174A0874-original [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => p958-174a0874-original [to_ping] => [pinged] => [post_modified] => 2022-08-14 19:02:19 [post_modified_gmt] => 2022-08-14 17:02:19 [post_content_filtered] => [post_parent] => 49595 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/08/P958-174A0874-original.jpeg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [183] => Array ( [ID] => 49599 [post_author] => 99 [post_date] => 2022-08-14 18:59:50 [post_date_gmt] => 2022-08-14 16:59:50 [post_content] => Photograph by Katy Otto [post_title] => P958-174A0884-original [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => p958-174a0884-original [to_ping] => [pinged] => [post_modified] => 2022-08-14 19:02:17 [post_modified_gmt] => 2022-08-14 17:02:17 [post_content_filtered] => [post_parent] => 49595 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/08/P958-174A0884-original.jpeg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [184] => Array ( [ID] => 49409 [post_author] => 105 [post_date] => 2022-08-04 16:10:36 [post_date_gmt] => 2022-08-04 14:10:36 [post_content] =>

What does the Baltic Sea drill core reveal about microplastics and the difficulty of defining their sources? Part of Unearthing the Present in May 2022.

A seminar held during Unearthing the Present

The rapid dissemination of plastics through the air and aquatic bodies has created microplastic-rich sediment layers over the last several decades. Which refined analytical techniques are necessary to measure this process? What does the Baltic Sea drill core reveal about microplastics and the difficulty of defining their sources? Taking into account their abundance, minuscule scale, and sociopolitical entanglements, the session will explore the imprints of microplastics, touching on ways of living with their ubiquity. The following is a recording of the seminar “What’s So Micro About Plastics?,” which was held during Unearthing the Present in May 2022.

[post_title] => What’s So Micro About Plastics? [post_excerpt] => [post_status] => publish [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => whats-so-micro-about-plastics [to_ping] => [pinged] => [post_modified] => 2022-08-05 12:38:36 [post_modified_gmt] => 2022-08-05 10:38:36 [post_content_filtered] => [post_parent] => 0 [guid] => https://www.anthropocene-curriculum.org/?post_type=contribution&p=49409 [menu_order] => 0 [post_type] => contribution [post_mime_type] => [comment_count] => 0 [filter] => raw ) [185] => Array ( [ID] => 49401 [post_author] => 103 [post_date] => 2022-07-22 15:19:58 [post_date_gmt] => 2022-07-22 13:19:58 [post_content] => [post_title] => ie_pdf_test [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => ie_pdf_test-2 [to_ping] => [pinged] => [post_modified] => 2022-07-22 15:20:37 [post_modified_gmt] => 2022-07-22 13:20:37 [post_content_filtered] => [post_parent] => 49196 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/07/ie_pdf_test-1.pdf [menu_order] => 0 [post_type] => attachment [post_mime_type] => application/pdf [comment_count] => 0 [filter] => raw ) [186] => Array ( [ID] => 49398 [post_author] => 103 [post_date] => 2022-07-22 15:04:39 [post_date_gmt] => 2022-07-22 13:04:39 [post_content] => [post_title] => ie_pdf_test [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => ie_pdf_test [to_ping] => [pinged] => [post_modified] => 2022-07-22 15:05:46 [post_modified_gmt] => 2022-07-22 13:05:46 [post_content_filtered] => [post_parent] => 49196 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/07/ie_pdf_test.pdf [menu_order] => 0 [post_type] => attachment [post_mime_type] => application/pdf [comment_count] => 0 [filter] => raw ) [187] => Array ( [ID] => 49388 [post_author] => 105 [post_date] => 2022-07-15 11:22:53 [post_date_gmt] => 2022-07-15 09:22:53 [post_content] => [post_title] => Bensaude-Vincent_radiation [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => bensaude-vincent_radiation-3 [to_ping] => [pinged] => [post_modified] => 2022-07-15 11:22:53 [post_modified_gmt] => 2022-07-15 09:22:53 [post_content_filtered] => [post_parent] => 49142 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/07/Bensaude-Vincent_radiation.pdf [menu_order] => 0 [post_type] => attachment [post_mime_type] => application/pdf [comment_count] => 0 [filter] => raw ) [188] => Array ( [ID] => 49386 [post_author] => 105 [post_date] => 2022-07-15 11:19:19 [post_date_gmt] => 2022-07-15 09:19:19 [post_content] => [post_title] => Bensaude-Vincent_radiation_final [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => bensaude-vincent_radiation_final [to_ping] => [pinged] => [post_modified] => 2022-07-15 11:19:19 [post_modified_gmt] => 2022-07-15 09:19:19 [post_content_filtered] => [post_parent] => 49142 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/07/Bensaude-Vincent_radiation_final.pdf [menu_order] => 0 [post_type] => attachment [post_mime_type] => application/pdf [comment_count] => 0 [filter] => raw ) [189] => Array ( [ID] => 49382 [post_author] => 105 [post_date] => 2022-07-15 11:02:32 [post_date_gmt] => 2022-07-15 09:02:32 [post_content] => [post_title] => Bensaude-Vincent_radiation-2 [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => bensaude-vincent_radiation-2 [to_ping] => [pinged] => [post_modified] => 2022-07-15 11:02:32 [post_modified_gmt] => 2022-07-15 09:02:32 [post_content_filtered] => [post_parent] => 49142 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/07/Bensaude-Vincent_radiation-2.pdf [menu_order] => 0 [post_type] => attachment [post_mime_type] => application/pdf [comment_count] => 0 [filter] => raw ) [190] => Array ( [ID] => 49293 [post_author] => 105 [post_date] => 2022-07-07 12:36:04 [post_date_gmt] => 2022-07-07 10:36:04 [post_content] => [post_title] => Bensaude-Vincent_Radiation [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => bensaude-vincent_radiation [to_ping] => [pinged] => [post_modified] => 2022-07-07 12:36:04 [post_modified_gmt] => 2022-07-07 10:36:04 [post_content_filtered] => [post_parent] => 49142 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/07/Bensaude-Vincent_Radiation.pdf [menu_order] => 0 [post_type] => attachment [post_mime_type] => application/pdf [comment_count] => 0 [filter] => raw ) [191] => Array ( [ID] => 49046 [post_author] => 99 [post_date] => 2022-06-30 14:16:59 [post_date_gmt] => 2022-06-30 12:16:59 [post_content] =>

Publication of processes and projects that build on and continue from six case studies of the Mississippi. An Anthropocene River project by design students at the University of Applied Sciences, Potsdam.

Building on six artistic and scientific case studies from the Mississippi. An Anthropocene River project, students from the University of Applied Sciences, Potsdam, documented the processes and visualizations explored in their related seminar, The Shape of a River: Mississippi, held during the winter of 2020/21.

[post_title] => The Shape of a River: Mississippi [post_excerpt] => [post_status] => publish [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => the-shape-of-a-river-mississippi [to_ping] => [pinged] => [post_modified] => 2022-07-01 10:53:50 [post_modified_gmt] => 2022-07-01 08:53:50 [post_content_filtered] => [post_parent] => 0 [guid] => https://www.anthropocene-curriculum.org/?post_type=contribution&p=49046 [menu_order] => 0 [post_type] => contribution [post_mime_type] => [comment_count] => 0 [filter] => raw ) [192] => Array ( [ID] => 49199 [post_author] => 103 [post_date] => 2022-06-29 12:17:53 [post_date_gmt] => 2022-06-29 10:17:53 [post_content] => [post_title] => ei_test_pdf [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => ei_test_pdf [to_ping] => [pinged] => [post_modified] => 2022-06-29 12:17:53 [post_modified_gmt] => 2022-06-29 10:17:53 [post_content_filtered] => [post_parent] => 49196 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/06/ei_test_pdf.pdf [menu_order] => 0 [post_type] => attachment [post_mime_type] => application/pdf [comment_count] => 0 [filter] => raw ) [193] => Array ( [ID] => 49169 [post_author] => 105 [post_date] => 2022-06-27 14:27:53 [post_date_gmt] => 2022-06-27 12:27:53 [post_content] => [post_title] => CloudChamber [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => cloudchamber [to_ping] => [pinged] => [post_modified] => 2022-07-27 12:53:49 [post_modified_gmt] => 2022-07-27 10:53:49 [post_content_filtered] => [post_parent] => 49105 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/06/CloudChamber.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [194] => Array ( [ID] => 49167 [post_author] => 105 [post_date] => 2022-06-27 14:25:38 [post_date_gmt] => 2022-06-27 12:25:38 [post_content] => [post_title] => Waters [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => waters [to_ping] => [pinged] => [post_modified] => 2022-06-27 14:25:38 [post_modified_gmt] => 2022-06-27 12:25:38 [post_content_filtered] => [post_parent] => 49135 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/06/Waters.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [195] => Array ( [ID] => 49164 [post_author] => 105 [post_date] => 2022-06-27 14:21:05 [post_date_gmt] => 2022-06-27 12:21:05 [post_content] => © All rights reserved Susan Schuppli [post_title] => Hydrology [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => hydrology [to_ping] => [pinged] => [post_modified] => 2022-06-27 14:21:40 [post_modified_gmt] => 2022-06-27 12:21:40 [post_content_filtered] => [post_parent] => 49137 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/06/Hydrology.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [196] => Array ( [ID] => 49162 [post_author] => 105 [post_date] => 2022-06-27 14:20:31 [post_date_gmt] => 2022-06-27 12:20:31 [post_content] => © All rights reserved Andy Cundy [post_title] => AlphaSpec [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => alphaspec [to_ping] => [pinged] => [post_modified] => 2022-06-27 14:20:47 [post_modified_gmt] => 2022-06-27 12:20:47 [post_content_filtered] => [post_parent] => 49103 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/06/AlphaSpec.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [197] => Array ( [ID] => 49131 [post_author] => 105 [post_date] => 2022-06-23 16:40:03 [post_date_gmt] => 2022-06-23 14:40:03 [post_content] => © All rights reserved Irka Hajdas [post_title] => Picture6 [post_excerpt] => Graphite samples are pressed into the Al cathodes and organized for accelerator mass spectrometry (AMS) analysis. A set of known samples (standards OXA at the position 2) is included for a calculation of ages. Samples of background (BL at position 3 to 6) are made of very old carbon (free of 14C) and work to monitor contamination introduced to the sample during the preparation process. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => picture6 [to_ping] => [pinged] => [post_modified] => 2022-07-07 12:06:27 [post_modified_gmt] => 2022-07-07 10:06:27 [post_content_filtered] => [post_parent] => 49122 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/06/Picture6.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [198] => Array ( [ID] => 49129 [post_author] => 105 [post_date] => 2022-06-23 16:31:03 [post_date_gmt] => 2022-06-23 14:31:03 [post_content] => © All rights reserved Irka Hajdas [post_title] => Picture8 [post_excerpt] => The MICADAS ion source. To see more pictures of the AMS system at the ETH Zurich facility, visit: https://ams.ethz.ch/. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => picture8 [to_ping] => [pinged] => [post_modified] => 2022-07-07 12:06:58 [post_modified_gmt] => 2022-07-07 10:06:58 [post_content_filtered] => [post_parent] => 49122 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/06/Picture8.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [199] => Array ( [ID] => 49128 [post_author] => 105 [post_date] => 2022-06-23 16:30:59 [post_date_gmt] => 2022-06-23 14:30:59 [post_content] => © All rights reserved Irka Hajdas [post_title] => Picture7 [post_excerpt] => Targets organized in a cassette are analyzed using AMS at the ETH Zurich facility (MICADAS). [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => picture7 [to_ping] => [pinged] => [post_modified] => 2022-06-23 16:40:55 [post_modified_gmt] => 2022-06-23 14:40:55 [post_content_filtered] => [post_parent] => 49122 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/06/Picture7.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [200] => Array ( [ID] => 49127 [post_author] => 105 [post_date] => 2022-06-23 16:30:54 [post_date_gmt] => 2022-06-23 14:30:54 [post_content] => © All rights reserved Irka Hajdas [post_title] => Picture5 [post_excerpt] => The elemental analyzer is connected to the graphitization line, where the CO2 of the sample is reduced to graphite. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => picture5-3 [to_ping] => [pinged] => [post_modified] => 2022-06-23 16:40:57 [post_modified_gmt] => 2022-06-23 14:40:57 [post_content_filtered] => [post_parent] => 49122 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/06/Picture5.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [201] => Array ( [ID] => 49126 [post_author] => 105 [post_date] => 2022-06-23 16:30:50 [post_date_gmt] => 2022-06-23 14:30:50 [post_content] => © All rights reserved Irka Hajdas [post_title] => Picture4 [post_excerpt] => Here, a set of samples is in place and ready for combustion in elemental analyzer. The samples in the carousel are organized according to the list, and will drop into the combustion system (the open hole below #1 near the bottom of the frame). [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => picture4-5 [to_ping] => [pinged] => [post_modified] => 2022-06-23 16:40:58 [post_modified_gmt] => 2022-06-23 14:40:58 [post_content_filtered] => [post_parent] => 49122 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/06/Picture4.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [202] => Array ( [ID] => 49125 [post_author] => 105 [post_date] => 2022-06-23 16:30:46 [post_date_gmt] => 2022-06-23 14:30:46 [post_content] => © All rights reserved Irka Hajdas [post_title] => Picture3 [post_excerpt] => Weighing the sample (in the glass tube, left) on the precise balance. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => picture3-5 [to_ping] => [pinged] => [post_modified] => 2022-07-07 12:07:18 [post_modified_gmt] => 2022-07-07 10:07:18 [post_content_filtered] => [post_parent] => 49122 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/06/Picture3.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [203] => Array ( [ID] => 49124 [post_author] => 105 [post_date] => 2022-06-23 16:30:43 [post_date_gmt] => 2022-06-23 14:30:43 [post_content] => © All rights reserved Irka Hajdas [post_title] => Picture2 [post_excerpt] => Clean samples are weighed and packed into Al cups for combustion in an elemental analyzer. The portion of sample contains an equivalent of 1 mg of carbon. That means that if sediment contains 10% of carbon by weight, a portion of 10 mg of clean powder will be placed in the cup and wrapped tight. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => picture2-5 [to_ping] => [pinged] => [post_modified] => 2022-06-23 16:41:02 [post_modified_gmt] => 2022-06-23 14:41:02 [post_content_filtered] => [post_parent] => 49122 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/06/Picture2.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [204] => Array ( [ID] => 49123 [post_author] => 105 [post_date] => 2022-06-23 16:30:39 [post_date_gmt] => 2022-06-23 14:30:39 [post_content] => © All rights reserved Irka Hajdas [post_title] => Picture1 [post_excerpt] => Samples of sediment from the cores are placed in glass tubes and washed in an acid and then a base to remove contamination. This is an essential step because old or young carbonates can change the 14C signal in the sample. Multiple washes are required before a clean sample can be frozen and dried in a freeze-drying system. 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https://content.anthropocene-curriculum.org/wp-content/uploads/2022/06/P958-174A0751-original.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [211] => Array ( [ID] => 49114 [post_author] => 105 [post_date] => 2022-06-23 16:24:46 [post_date_gmt] => 2022-06-23 14:24:46 [post_content] => © All rights reserved Katy Otto [post_title] => P958-174A0692-original [post_excerpt] => Photograph by Katy Otto [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => p958-174a0692-original [to_ping] => [pinged] => [post_modified] => 2022-07-11 12:17:28 [post_modified_gmt] => 2022-07-11 10:17:28 [post_content_filtered] => [post_parent] => 49107 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/06/P958-174A0692-original.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [212] => Array ( [ID] => 49112 [post_author] => 105 [post_date] => 2022-06-23 16:20:14 [post_date_gmt] => 2022-06-23 14:20:14 [post_content] => © All rights reserved Katy Otto [post_title] => P958-174A0659-original [post_excerpt] => Andy Cundy at the Fingerprints of the Nuclear Age seminar. Photo by Katy Otto [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => p958-174a0659-original [to_ping] => [pinged] => [post_modified] => 2022-07-11 14:50:47 [post_modified_gmt] => 2022-07-11 12:50:47 [post_content_filtered] => [post_parent] => 49107 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/06/P958-174A0659-original.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [213] => Array ( [ID] => 49110 [post_author] => 105 [post_date] => 2022-06-23 16:14:51 [post_date_gmt] => 2022-06-23 14:14:51 [post_content] => © All rights reserved Katy Otto [post_title] => P958-174A0586-original [post_excerpt] => Photograph by Katy Otto [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => p958-174a0586-original [to_ping] => [pinged] => [post_modified] => 2022-07-11 12:17:24 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All rights reserved Andy Cundy [post_title] => Banana [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => banana [to_ping] => [pinged] => [post_modified] => 2022-06-23 15:44:40 [post_modified_gmt] => 2022-06-23 13:44:40 [post_content_filtered] => [post_parent] => 49099 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/06/Banana.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [217] => Array ( [ID] => 49082 [post_author] => 99 [post_date] => 2022-06-23 13:51:29 [post_date_gmt] => 2022-06-23 11:51:29 [post_content] => [post_title] => Screen Shot 2022-06-23 at 13.50.50 [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => screen-shot-2022-06-23-at-13-50-50 [to_ping] => [pinged] => [post_modified] => 2022-06-23 13:51:29 [post_modified_gmt] => 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13:03:53 [post_content_filtered] => [post_parent] => 46376 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/Bolen-Holmes-–-Hourglass-River-Part-3.1-1.pdf [menu_order] => 0 [post_type] => attachment [post_mime_type] => application/pdf [comment_count] => 0 [filter] => raw ) [222] => Array ( [ID] => 48986 [post_author] => 105 [post_date] => 2022-06-07 15:01:58 [post_date_gmt] => 2022-06-07 13:01:58 [post_content] => [post_title] => Bolen Holmes – Hourglass River Part 3.1 [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => bolen-holmes-hourglass-river-part-3-1 [to_ping] => [pinged] => [post_modified] => 2022-06-07 15:01:58 [post_modified_gmt] => 2022-06-07 13:01:58 [post_content_filtered] => [post_parent] => 46376 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/Bolen-Holmes-–-Hourglass-River-Part-3.1.pdf [menu_order] => 0 [post_type] => attachment 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Artist talk with Giulia Bruno & Armin Linke [post_excerpt] => [post_status] => publish [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => artist-talk-with-giulia-bruno-armin-linke [to_ping] => [pinged] => [post_modified] => 2022-05-26 15:23:54 [post_modified_gmt] => 2022-05-26 13:23:54 [post_content_filtered] => [post_parent] => 0 [guid] => https://www.anthropocene-curriculum.org/?post_type=event&p=48860 [menu_order] => 0 [post_type] => event [post_mime_type] => [comment_count] => 0 [filter] => raw ) [225] => Array ( [ID] => 48857 [post_author] => 12 [post_date] => 2022-05-26 14:57:03 [post_date_gmt] => 2022-05-26 12:57:03 [post_content] => [post_title] => Screenshot 2022-05-26 at 14.56.51 [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => screenshot-2022-05-26-at-14-56-51 [to_ping] => [pinged] => [post_modified] => 2022-05-26 14:57:03 [post_modified_gmt] => 2022-05-26 12:57:03 [post_content_filtered] => [post_parent] => 48368 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/Screenshot-2022-05-26-at-14.56.51.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [226] => Array ( [ID] => 48368 [post_author] => 129 [post_date] => 2022-05-18 12:23:31 [post_date_gmt] => 2022-05-18 10:23:31 [post_content] =>

Frequently asked questions on the work to define the Anthropocene.

Frequently asked questions on the work to define a new geological epoch: the Anthropocene. They cover criteria that constrains the research, the novelties and traditional aspects of the scientific work being done, the stages of the ratification process, and geological naming conventions.

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The geological time scale and the work of the Anthropocene Working Group.

Putting the Anthropocene on the Chronostratigraphic Chart

The geological time scale is the product of centuries of careful study of Earth’s history. This text describes some of that research process and how it informs the designation of a new potential epoch: the Anthropocene. This is the job of the Anthropocene Working Group, an interdisciplinary research group who, since 2009, have been investigating human traces in the geological record.

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A conversation with Jan Zalasiewicz on the geological Anthropocene research.

This is a conversation with Jan Zalasiewicz on the geological Anthropocene. We discuss the differences between the Anthropocene concept in geology and in broader usage, the novel interdisciplinary work of the Anthropocene Working Group, the role of HKW in the research, and the implications of the potential ratification of a new geological epoch.

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The Geological Anthropocene
[post_title] => tga_landing [post_excerpt] =>
PUBLICATION
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Evidence & Experiment
[post_title] => ee_pre_landing [post_excerpt] =>
PROJECT
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Where is the Planetary? is a collective search for models of living together on Earth.

How could collaboration maintain a habitable planet? What concepts of the world underlie political and social approaches to a transforming Earth system? How can a variety of worldviews be transformed into shared planetary-scale practices that could address the current challenges? Where is the Planetary? is a collective search for models of living together on Earth.

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A project by artists Giulia Bruno and Armin Linke explores the scientific and social conditions producing the new geological epoch, the Anthropocene.

A project by artists Giulia Bruno and Armin Linke explores the scientific and social conditions producing the new geological epoch, the Anthropocene. The exhibition Earth Indices opens at Haus der Kulturen der Welt opens in May 2022, while a digital translation of the project will be published on anthropocene-curriculum.org in the following months.

How do we make sense of the transformations in the Earth system? Who is writing the chronicle of the planet? What are the tools and practices that allow us to read Earth’s changes? Over the past two years, Giulia Bruno and Armin Linke have closely followed the research of the Anthropocene Working Group on the geological evidence for the new Earth epoch. Earth Indices is the result of a close collaboration between the two artists and the many scientists involved. A visual structure designed by Linda van Deursen highlights the polyphonic nature of this artistic research project.

The exhibition portrays both the natural landscapes from which sediments are extracted and the complex laboratory processes employed to transform the evidence into data that can be interpreted. Earth Indices focuses on the social interaction in which this scientific research takes place, shedding light on the specific procedures and tasks required for the production of geological evidence. In this way, a multilayered archive of the demarcating process for the new geological epoch emerges.

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What is the new geological epoch made of? Unearthing the Present connects the geological analysis of the present with a discussion of the changing scope for social and political agency.

What is the new geological epoch made of? Unearthing the Present connects the geological analysis of the present with a discussion of the changing scope for social and political agency.

How does a new geological epoch take shape? What do the sediments of Earth tell us about the present and about the actions and decisions we have to take today? The planet has entered the first stage of the Anthropocene: a highly disruptive transitional period of “global weirding” within which ecological patterns and societal structures are changing radically. Over the past two years, the Anthropocene Working Group has been assembling stratigraphic evidence for the geological reality of the new Earth epoch. Unearthing the Present connects these analyses with a discussion of the changing scope for social and political agency. In collaborative Core Readings, scientists, researchers, artists and activists decipher stratigraphic samples from pacific corals, from lake deposits in northeastern China and from speleothems found in an Italian cave. They examine the microscopic traces left in Earth’s archives by the burning of fossil fuels, atmospheric nuclear bomb testing and the disruption of marine ecosystems to jointly identify ways and means of responding to these signals.

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Through a close reading and contextualization of material evidence of planetary upheaval, the yearlong program Evidence & Experiment gathers material testimonies of the Anthropocene stratum.

When in search of models for living in a transitioning Earth system, what sociopolitical considerations emerge through the geological evidence for the Anthropocene? How does the global fingerprint of humankind manifest itself in Earth’s sediments? In which way does this evidence influence decision-making in the face of planetary challenges? How is cohabitation on Earth possible amid conflicting assumptions and cosmologies?

Since 2019, the Anthropocene Working Group (AWG) has been searching for stratigraphic evidence indicating the geological onset of the Anthropocene at various sites around the world. Through a close reading and contextualization of this material evidence of planetary upheaval, the yearlong program Evidence & Experiment gathers material testimonies of the Anthropocene stratum. In the face of the urgent political challenges of this new epoch, finding the nexus between the production of evidence and the outlining of the scope for experimentation and social maneuvering is nothing less than essential. It is this uncharted space between the evident and the experimental, between what is “given” and the collective search for adequate responses, that the program strives to explore.

The planet has entered the first stage of the Anthropocene: a highly disruptive transitional period of “global weirding” within which ecological patterns and societal structures are changing radically. Over the past two years, the Anthropocene Working Group has been assembling stratigraphic evidence for the geological reality of this new Earth epoch.

Throughout 2022, Evidence & Experiment assesses the conditions, values, and scales that define the ongoing planetary transformation on the basis of the AWG’s stratigraphic research. A series of events, publications, and exhibitions provides a unique opportunity for a public engagement on the Anthropocene by thinking with and through the specific scientific undertaking that is set up to formally define its geologically distinct beginning. Anthropocene-curriculum.org offers a comprehensive repositorium for the geologic exploration of the Anthropocene and of the many program strands unfolding both on- and offline.

The Geological Anthropocene publication provides in-depth information on the AWG’s stratigraphic research to support the formalization of the Anthropocene and includes a detailed overview of the twelve sites that have been analyzed as possible stratigraphic references for the new epoch. Alongside these site guides, “Defining a New Earth Epoch” offers an introduction to the practicalities of establishing a new geologic time unit, while in an interview, Jan Zalasiewicz, former chair of the AWG, explains the interdisciplinary work of the of group and the challenges of defining the Anthropocene from a geologic standpoint. The FAQ and Glossary shed light on key terms and processes around the formal ratification of the new earth epoch.

The special publication Anthropogenic Markers: Stratigraphy and Context explores and contours some of the historical contexts and epistemic settings around the ongoing work of Anthropocene geology. In seven thematic dossiers, contributions from the fields of geochemistry and paleobiology, history and science studies, artistic research, archaeology, literary studies, and anthropology reflect on selected material markers of human impacts on earthly strata.

The events, publications, and exhibition taking place in the framework of Evidence & Experiment on site at HKW will be amply documented on anthropocene-curiculum.org: the multi-day event Unearthing the Present (May 19-22) connects the geological analysis of the present with a discussion of the changing scope for social and political agency. Where is the Planetary? (October 12-16) explores shared planetary-scale practices for an equitable cohabitation on Earth. The exhibition Earth Indices (May 19-Oct 17) by artists Giulia Bruno and Armin Linke addresses the scientific and social conditions producing the new geological epoch. At a concluding press conference in December, the final recommendations of the AWG on the geological reference point of the Anthropocene will be presented.

With this program, the HKW concludes a full decade of Anthropocene programming and research in which it has undertaken an experiment of its own. In a long-standing collaboration with the AWG and the Max Planck Institute for the History of Science (MPIWG), Berlin, the HKW set out to explore the shifting boundaries of knowledge production under the growing rumblings of the Anthropocene. Here, in this final program, this direct engagement with the geosciences and the humanities is prompted to look closer at the scientific evidence and its production and bring it into conversation with the promises and pitfalls of reacting to these findings through social, artistic, and epistemic experimentation.

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Peter dal Ferro, Daniel Powers and Jennifer McKee operate the vibracore winch system. 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Coral photo taken during diving trip to Flower Garden Banks. 2. Assigning the yearly growth bands on the Flinders Reef cores for sampling at the Australian Institute of Marine Science X-ray laboratory. 3. Image of an ice core section displayed at the British Antarctic Survey. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => ee220510_ee_bildcollagen_16_9_draft_s_7 [to_ping] => [pinged] => [post_modified] => 2022-05-14 12:49:26 [post_modified_gmt] => 2022-05-14 10:49:26 [post_content_filtered] => [post_parent] => 48171 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/EE220510_EE_Bildcollagen_16_9_draft_s_7.jpeg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [273] => Array ( [ID] => 48547 [post_author] => 12 [post_date] => 2022-05-14 12:47:15 [post_date_gmt] => 2022-05-14 10:47:15 [post_content] => 1. Photograph by Beata Smieja – Król 2. Photograph by Kristine DeLong © All Rights Reserved. Design: NODE Berlin Oslo [post_title] => CLASHING220510_EE_Bildcollagen_16_9_draft_s_18 [post_excerpt] => Collage including 1. Scanning microscopy workstation. 2. Coral photo taken during diving trip to Flower Garden Banks. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => clashing220510_ee_bildcollagen_16_9_draft_s_18 [to_ping] => [pinged] => [post_modified] => 2022-05-14 12:50:43 [post_modified_gmt] => 2022-05-14 10:50:43 [post_content_filtered] => [post_parent] => 47516 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/CLASHING220510_EE_Bildcollagen_16_9_draft_s_18.jpeg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [274] => Array ( [ID] => 48546 [post_author] => 12 [post_date] => 2022-05-14 12:45:28 [post_date_gmt] => 2022-05-14 10:45:28 [post_content] => 1. Photograph by NASA's Goddard Space Flight Center/USGS, www.stratigraphy.org, public domain [post_title] => ChronostratChart2022-02 [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => chronostratchart2022-02-2 [to_ping] => [pinged] => [post_modified] => 2022-05-12 13:11:34 [post_modified_gmt] => 2022-05-12 11:11:34 [post_content_filtered] => [post_parent] => 48379 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2011/05/ChronostratChart2022-02.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [290] => Array ( [ID] => 48414 [post_author] => 129 [post_date] => 2022-05-12 13:02:49 [post_date_gmt] => 2022-05-12 11:02:49 [post_content] => Photograph by Kent G. Budge, Wikimedia Commons, CC0 1.0 Universal [post_title] => OLYMPUS DIGITAL CAMERA [post_excerpt] => An outcrop of the Zuni Sandstone just outside El Malpais National Monument, New Mexico, US. The Zuni Sandstone is the light colored rock making up the lower and middle portion of the escarpment. Below rests the Wingate Sandstone or Chinle Group and above is the Dakota Formation. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => olympus-digital-camera-41 [to_ping] => [pinged] => [post_modified] => 2022-05-12 13:08:03 [post_modified_gmt] => 2022-05-12 11:08:03 [post_content_filtered] => [post_parent] => 48379 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2011/05/Zuni_Sandstone_El_Malpais.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [291] => Array ( [ID] => 48389 [post_author] => 12 [post_date] => 2022-05-12 11:48:26 [post_date_gmt] => 2022-05-12 09:48:26 [post_content] => Photograph by Sebastian Bolesch © All Rights Reserved [post_title] => jan_zalasiewicz_cat_anthropozaen [post_excerpt] => During the first in-person meeting of the Anthropocene Working Group (AWG) at HKW in October 2014, speakers were asked to have something on stage that could represent the Anthropocene. Jan Zalasiewicz, then Chair of the AWG, asked if he could have a cat—and HKW, somewhat to Jan's surprise—provided one. Jan remembers that Philou, a professional cat specially trained to work in public settings, remained admirably composed in front of an audience of 400 humans, demonstrating why its species is among the winners in the emerging Anthropocene biosphere. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => jan_zalasiewicz_cat_anthropozaen [to_ping] => [pinged] => [post_modified] => 2022-05-13 09:41:35 [post_modified_gmt] => 2022-05-13 07:41:35 [post_content_filtered] => [post_parent] => 48381 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2011/05/jan_zalasiewicz_cat_anthropozaen.jpeg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [292] => Array ( [ID] => 48380 [post_author] => 129 [post_date] => 2022-05-12 11:37:14 [post_date_gmt] => 2022-05-12 09:37:14 [post_content] => Photograph by Bahudhara, Wikimedia Commons, CC BY-SA 3.0 [post_title] => Ediacaran_GSSP_-_closeup [post_excerpt] => The golden spike marking the Global Boundary Stratotype Section and Point (GSSP) at the lower boundary of the Ediacaran Period. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => ediacaran_gssp_-_closeup [to_ping] => [pinged] => [post_modified] => 2022-05-12 11:39:26 [post_modified_gmt] => 2022-05-12 09:39:26 [post_content_filtered] => [post_parent] => 48379 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/Ediacaran_GSSP_-_closeup.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [293] => Array ( [ID] => 48326 [post_author] => 129 [post_date] => 2022-05-11 11:25:31 [post_date_gmt] => 2022-05-11 09:25:31 [post_content] => Photograph by Renza Miorandi © All Rights Reserved [post_title] => IMGP4628 [post_excerpt] => The forest road towards Grotta di Ernesto in winter. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => imgp4628 [to_ping] => [pinged] => [post_modified] => 2022-05-11 11:25:57 [post_modified_gmt] => 2022-05-11 09:25:57 [post_content_filtered] => [post_parent] => 47894 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/IMGP4628.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [294] => Array ( [ID] => 48325 [post_author] => 129 [post_date] => 2022-05-11 11:24:35 [post_date_gmt] => 2022-05-11 09:24:35 [post_content] => Photograph by Andrea Borsato © All Rights Reserved [post_title] => DSCN2566 [post_excerpt] => Silvia Frisia mounting a slice of stalagmite ER78 at beamline ID21 at the European Synchrotron Radiation Facility (Grenoble, France). [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => dscn2566 [to_ping] => [pinged] => [post_modified] => 2022-05-11 11:25:10 [post_modified_gmt] => 2022-05-11 09:25:10 [post_content_filtered] => [post_parent] => 47894 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/DSCN2566.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [295] => Array ( [ID] => 48315 [post_author] => 12 [post_date] => 2022-05-10 14:34:04 [post_date_gmt] => 2022-05-10 12:34:04 [post_content] => [post_title] => CARBON Summer School, Science Gallery Bengaluru [post_excerpt] => [post_status] => publish [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => carbon-summer-school-science-gallery-bengaluru [to_ping] => [pinged] => [post_modified] => 2022-05-10 14:34:42 [post_modified_gmt] => 2022-05-10 12:34:42 [post_content_filtered] => [post_parent] => 0 [guid] => https://www.anthropocene-curriculum.org/?post_type=event&p=48315 [menu_order] => 0 [post_type] => event [post_mime_type] => [comment_count] => 0 [filter] => raw ) [296] => Array ( [ID] => 48317 [post_author] => 129 [post_date] => 2022-05-10 14:32:32 [post_date_gmt] => 2022-05-10 12:32:32 [post_content] => Photograph by Silvia Frisia © All Rights Reserved [post_title] => Ernesto67 [post_excerpt] => Mixed conifer and deciduous forest above Grotta di Ernesto. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => ernesto67 [to_ping] => [pinged] => [post_modified] => 2022-05-10 14:32:59 [post_modified_gmt] => 2022-05-10 12:32:59 [post_content_filtered] => [post_parent] => 47894 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/Ernesto67.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [297] => Array ( [ID] => 48316 [post_author] => 12 [post_date] => 2022-05-10 14:29:46 [post_date_gmt] => 2022-05-10 12:29:46 [post_content] => [post_title] => Carbon_Summer+School [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => carbon_summerschool [to_ping] => [pinged] => [post_modified] => 2022-05-10 14:29:46 [post_modified_gmt] => 2022-05-10 12:29:46 [post_content_filtered] => [post_parent] => 48315 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/Carbon_SummerSchool.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [298] => Array ( [ID] => 48313 [post_author] => 12 [post_date] => 2022-05-10 14:17:16 [post_date_gmt] => 2022-05-10 12:17:16 [post_content] => [post_title] => jeju_island-1-edited [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => jeju_island-1-edited [to_ping] => [pinged] => [post_modified] => 2022-05-10 14:17:16 [post_modified_gmt] => 2022-05-10 12:17:16 [post_content_filtered] => [post_parent] => 47589 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/jeju_island-1-edited.jpeg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [299] => Array ( [ID] => 48311 [post_author] => 129 [post_date] => 2022-05-10 11:54:24 [post_date_gmt] => 2022-05-10 09:54:24 [post_content] =>
Image by Michael Wagreich © All Rights Reserved [post_title] => Bild2.corrected [post_excerpt] => The Karlsplatz excavation site with years of sediment layers labelled. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => bild2-corrected [to_ping] => [pinged] => [post_modified] => 2022-05-10 11:55:55 [post_modified_gmt] => 2022-05-10 09:55:55 [post_content_filtered] => [post_parent] => 47964 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/Bild2.corrected.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [300] => Array ( [ID] => 48299 [post_author] => 129 [post_date] => 2022-05-10 11:33:39 [post_date_gmt] => 2022-05-10 09:33:39 [post_content] =>
Photograph by Renza Miorandi © All Rights Reserved [post_title] => IMGP8014 [post_excerpt] => Active stalactites in Grotta di Ernesto. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => imgp8014 [to_ping] => [pinged] => [post_modified] => 2022-05-10 11:41:17 [post_modified_gmt] => 2022-05-10 09:41:17 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/IMGP8014.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [301] => Array ( [ID] => 48298 [post_author] => 129 [post_date] => 2022-05-10 11:33:36 [post_date_gmt] => 2022-05-10 09:33:36 [post_content] =>
Photograph by Andrea Borsato © All Rights Reserved [post_title] => Ernesto10cut [post_excerpt] => Active stalactites and stalagmites in Grotta di Ernesto. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => ernesto10cut [to_ping] => [pinged] => [post_modified] => 2022-05-10 14:31:26 [post_modified_gmt] => 2022-05-10 12:31:26 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/Ernesto10cut.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [302] => Array ( [ID] => 48297 [post_author] => 129 [post_date] => 2022-05-10 11:33:20 [post_date_gmt] => 2022-05-10 09:33:20 [post_content] =>
Image by Andrea Borsato © All Rights Reserved [post_title] => ER76_Fluo_30 [post_excerpt] => Thin section of the upper portion of stalagmite ER76 showing
the structure of annual laminae as observed in transmitted
polarized light (PPL) and fluorescent light (470 and 365
nanometer wavelengths) at different magnifications. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => er76_fluo_30 [to_ping] => [pinged] => [post_modified] => 2022-05-10 11:44:18 [post_modified_gmt] => 2022-05-10 09:44:18 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/ER76_Fluo_30.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [303] => Array ( [ID] => 48284 [post_author] => 129 [post_date] => 2022-05-10 09:07:50 [post_date_gmt] => 2022-05-10 07:07:50 [post_content] =>
Image by Andrea Borsato © All Rights Reserved [post_title] => Speleothem_formation_sketch_Ernesto [post_excerpt] => Model of speleothem formation in Ernesto Cave.
Meteoric water uptakes CO2 in the soil zone and
causes carbonate dissolution in the epikarst. The
water percolates through the aquifer via fissures and
porosity (fissure and matrix flow) of the rock. Once
the water enters the cave, most of the dissolved CO2
is released to the atmosphere, promoting carbonate
precipitation on the roof (stalactites) and floor
(flowstones and stalagmites). [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => speleothem_formation_sketch_ernesto [to_ping] => [pinged] => [post_modified] => 2022-05-10 09:09:24 [post_modified_gmt] => 2022-05-10 07:09:24 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/Speleothem_formation_sketch_Ernesto.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [304] => Array ( [ID] => 48283 [post_author] => 129 [post_date] => 2022-05-10 09:07:41 [post_date_gmt] => 2022-05-10 07:07:41 [post_content] => Image by Andrea Borsato © All Rights Reserved [post_title] => Figure-5 [post_excerpt] => Thin section image in transmitted light of the topmost section of ER77 stalagmite compared with the age model derived from annual layer counting, the oxygen and carbon isotope composition, and the 14C activity. Two time-markers are highlighted: 1) The passage between microcrystalline porous to compact columnar calcite at 13.1 mm dft (lamina age 1841±10 CE) marked by a steady increase in the growth rate and a sharp rise in δ13C; 2) The deflection point in the 14C activity curve. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => figure-5-2 [to_ping] => [pinged] => [post_modified] => 2022-05-10 11:51:43 [post_modified_gmt] => 2022-05-10 09:51:43 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/Figure-5.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [305] => Array ( [ID] => 48282 [post_author] => 129 [post_date] => 2022-05-10 09:07:34 [post_date_gmt] => 2022-05-10 07:07:34 [post_content] => Image by Andrea Borsato © All Rights Reserved [post_title] => Figure-4 [post_excerpt] => Thin section image in transmitted and fluorescent light (470 nm) of the topmost section of ER78 stalagmite compared with the annual growth rate and age model derived from layer counting, the fluorescence signal, the S concentration composition and the δ34S–SO4. Four time markers are highlighted: 1) The passage between microcrystalline porous to compact columnar calcite at 8.6 mm dft (age 1836±15 CE); 2) The peak in sulphur concentration at 8.4 mm dft (lamina age 1884±7 CE), possibly related to the Krakatoa volcanic eruption in August 1883; 3) The increase in the annual growth rate and S concentration, and the following shift towards depleted δ34S–SO4 that suggests an additional source of stalagmite sulphur originating from industrial pollution; 4) The sudden increase of growth rate along a thin micro-detrital layer that correspond to the opening of the cave entrance and archaeological excavation carried out in summer 1984. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => figure-4-2 [to_ping] => [pinged] => [post_modified] => 2022-05-10 11:51:32 [post_modified_gmt] => 2022-05-10 09:51:32 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/Figure-4.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [306] => Array ( [ID] => 48281 [post_author] => 129 [post_date] => 2022-05-10 09:07:21 [post_date_gmt] => 2022-05-10 07:07:21 [post_content] => Image by Andrea Borsato © All Rights Reserved [post_title] => Figure-2b [post_excerpt] => Projected cross section of Grotta di Ernesto in the Trento Province. The sampling sites of stalagmites ER76, 77 and 78 is shown. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => figure-2b [to_ping] => [pinged] => [post_modified] => 2022-05-10 09:10:44 [post_modified_gmt] => 2022-05-10 07:10:44 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/Figure-2b.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [307] => Array ( [ID] => 48280 [post_author] => 129 [post_date] => 2022-05-10 09:07:12 [post_date_gmt] => 2022-05-10 07:07:12 [post_content] =>
Image by Andrea Borsato © All Rights Reserved [post_title] => Figure-2a [post_excerpt] => Location map of Grotta di Ernesto in the Trento Province. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => figure-2a [to_ping] => [pinged] => [post_modified] => 2022-05-10 14:35:00 [post_modified_gmt] => 2022-05-10 12:35:00 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/Figure-2a.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [308] => Array ( [ID] => 48279 [post_author] => 129 [post_date] => 2022-05-10 09:07:06 [post_date_gmt] => 2022-05-10 07:07:06 [post_content] =>
Photograph by Silvia Frisia © All Rights Reserved [post_title] => Ernesto60 [post_excerpt] => Andrea Borsato installing lysimeters
and soil gas probes above Ernesto Cave. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => ernesto60 [to_ping] => [pinged] => [post_modified] => 2022-05-10 09:08:11 [post_modified_gmt] => 2022-05-10 07:08:11 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/Ernesto60.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [309] => Array ( [ID] => 48278 [post_author] => 129 [post_date] => 2022-05-10 09:06:58 [post_date_gmt] => 2022-05-10 07:06:58 [post_content] => Photograph by Andrea Borsato © All Rights Reserved [post_title] => ER77-insieme [post_excerpt] => The ER77 stalagmite cut along its growth axis. Note the characteristic translucent calcite layer at the top. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => er77-insieme-2 [to_ping] => [pinged] => [post_modified] => 2022-05-10 11:27:47 [post_modified_gmt] => 2022-05-10 09:27:47 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/ER77-insieme-1.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [310] => Array ( [ID] => 48273 [post_author] => 129 [post_date] => 2022-05-10 08:59:23 [post_date_gmt] => 2022-05-10 06:59:23 [post_content] => Photograph by Andrea Borsato © All Rights Reserved [post_title] => ER77-insieme [post_excerpt] => The ER77 stalagmite cut along its growth axis. Note the characteristic translucent calcite layer at the top. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => er77-insieme [to_ping] => [pinged] => [post_modified] => 2022-05-10 09:23:41 [post_modified_gmt] => 2022-05-10 07:23:41 [post_content_filtered] => [post_parent] => 47894 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/ER77-insieme.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [311] => Array ( [ID] => 48268 [post_author] => 129 [post_date] => 2022-05-10 08:41:15 [post_date_gmt] => 2022-05-10 06:41:15 [post_content] => Photograph courtesy Leibniz Institute for Baltic Sea Research Warnemünde (IOW) © All Rights Reserved [post_title] => Micha_Naumann_IMG_4145 [post_excerpt] => The research vessel Elisabeth Mann Borgese used to recover the sediment core from the East Gotland Basin. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => micha_naumann_img_4145 [to_ping] => [pinged] => [post_modified] => 2022-05-10 08:53:34 [post_modified_gmt] => 2022-05-10 06:53:34 [post_content_filtered] => [post_parent] => 47807 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/Micha_Naumann_IMG_4145.jpeg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [312] => Array ( [ID] => 48267 [post_author] => 129 [post_date] => 2022-05-10 08:40:53 [post_date_gmt] => 2022-05-10 06:40:53 [post_content] => Photograph by Jerome Kaiser © All Rights Reserved [post_title] => EMB201_1 [post_excerpt] => Heading to the coring site in the Baltic Sea onboard the research vessel Elisabeth Mann Borgese. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => emb201_1 [to_ping] => [pinged] => [post_modified] => 2022-05-10 08:44:03 [post_modified_gmt] => 2022-05-10 06:44:03 [post_content_filtered] => [post_parent] => 47807 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/EMB201_1.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [313] => Array ( [ID] => 48266 [post_author] => 129 [post_date] => 2022-05-10 08:40:48 [post_date_gmt] => 2022-05-10 06:40:48 [post_content] => Photograph by Patricia Roeser © All Rights Reserved [post_title] => IMG-20201019-WA0011 [post_excerpt] => Early morning on the Baltic Sea from the deck of the research vessel Elisabeth Mann Borgese. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => img-20201019-wa0011 [to_ping] => [pinged] => [post_modified] => 2022-05-10 08:53:42 [post_modified_gmt] => 2022-05-10 06:53:42 [post_content_filtered] => [post_parent] => 47807 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/IMG-20201019-WA0011.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [314] => Array ( [ID] => 48254 [post_author] => 103 [post_date] => 2022-05-09 16:13:18 [post_date_gmt] => 2022-05-09 14:13:18 [post_content] => [post_title] => hkw_logo [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => hkw_logo [to_ping] => [pinged] => [post_modified] => 2022-05-09 16:16:52 [post_modified_gmt] => 2022-05-09 14:16:52 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/hkw_logo.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [315] => Array ( [ID] => 48246 [post_author] => 129 [post_date] => 2022-05-09 14:51:38 [post_date_gmt] => 2022-05-09 12:51:38 [post_content] => Photograph by Petr Vodička, Wikimedia Commons [post_title] => TurowCoalMine [post_excerpt] => Turów coal mine and power station, Poland. The "Black Triangle" area has had a long history of extraction and industry. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => turowcoalmine [to_ping] => [pinged] => [post_modified] => 2022-05-09 14:52:05 [post_modified_gmt] => 2022-05-09 12:52:05 [post_content_filtered] => [post_parent] => 47764 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/TurowCoalMine.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [316] => Array ( [ID] => 48103 [post_author] => 129 [post_date] => 2022-05-05 16:56:18 [post_date_gmt] => 2022-05-05 14:56:18 [post_content] => Image by R. Scott Anderson, Northern Arizona University © All Rights Reserved [post_title] => Screenshot 2022-05-05 at 16.53.58 [post_excerpt] => Preliminary pollen record from Searsville Reservoir (data produced by R. Scott Anderson, Northern Arizona University). [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => screenshot-2022-05-05-at-16-53-58 [to_ping] => [pinged] => [post_modified] => 2022-05-05 16:59:23 [post_modified_gmt] => 2022-05-05 14:59:23 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/Screenshot-2022-05-05-at-16.53.58.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [317] => Array ( [ID] => 48102 [post_author] => 129 [post_date] => 2022-05-05 16:56:06 [post_date_gmt] => 2022-05-05 14:56:06 [post_content] => Photograph by Elizabeth A. Hadly, Stanford University © All Rights Reserved [post_title] => Screenshot 2022-05-05 at 16.54.12 [post_excerpt] => Anthony D. Barnosky and Sergio Redondo. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => screenshot-2022-05-05-at-16-54-12 [to_ping] => [pinged] => [post_modified] => 2022-05-05 17:01:57 [post_modified_gmt] => 2022-05-05 15:01:57 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/Screenshot-2022-05-05-at-16.54.12.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [318] => Array ( [ID] => 48101 [post_author] => 129 [post_date] => 2022-05-05 16:55:49 [post_date_gmt] => 2022-05-05 14:55:49 [post_content] =>
Photograph by Anthony D. Barnosky,
Stanford University © All Rights Reserved [post_title] => Screenshot 2022-05-05 at 16.54.26 [post_excerpt] => Elizabeth A. Hadly. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => screenshot-2022-05-05-at-16-54-26 [to_ping] => [pinged] => [post_modified] => 2022-05-06 09:44:35 [post_modified_gmt] => 2022-05-06 07:44:35 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/Screenshot-2022-05-05-at-16.54.26.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [319] => Array ( [ID] => 48100 [post_author] => 129 [post_date] => 2022-05-05 16:55:35 [post_date_gmt] => 2022-05-05 14:55:35 [post_content] => Photograph by Anthony D. Barnosky, Stanford University © All Rights Reserved [post_title] => Screenshot 2022-05-05 at 16.54.37 [post_excerpt] => Brian Sherrod, M. Allison Stegner, and SeanPaul La Selle. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => screenshot-2022-05-05-at-16-54-37 [to_ping] => [pinged] => [post_modified] => 2022-05-05 17:01:46 [post_modified_gmt] => 2022-05-05 15:01:46 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/Screenshot-2022-05-05-at-16.54.37.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [320] => Array ( [ID] => 48099 [post_author] => 129 [post_date] => 2022-05-05 16:55:05 [post_date_gmt] => 2022-05-05 14:55:05 [post_content] => Photograph by Anthony D. Barnosky, Stanford University © All Rights Reserved [post_title] => Screenshot 2022-05-05 at 16.54.48 [post_excerpt] => M. Allison Stegner and Maria Viteri. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => screenshot-2022-05-05-at-16-54-48 [to_ping] => [pinged] => [post_modified] => 2022-05-05 17:01:33 [post_modified_gmt] => 2022-05-05 15:01:33 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/Screenshot-2022-05-05-at-16.54.48.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [321] => Array ( [ID] => 48092 [post_author] => 129 [post_date] => 2022-05-05 16:40:06 [post_date_gmt] => 2022-05-05 14:40:06 [post_content] =>
Photograph by M. Allison Stegner, Stanford University
© All Rights Reserved [post_title] => 3_core2 [post_excerpt] => A section of the core in the lab, sampled for Mercury analysis. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 3_core2-5 [to_ping] => [pinged] => [post_modified] => 2022-05-06 09:41:29 [post_modified_gmt] => 2022-05-06 07:41:29 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/3_core2-2.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [322] => Array ( [ID] => 48088 [post_author] => 129 [post_date] => 2022-05-05 16:33:40 [post_date_gmt] => 2022-05-05 14:33:40 [post_content] =>
Image by SeanPaul La Selle,
United States Geological Survey
© All Rights Reserved [post_title] => 3_core searsville scans copy [post_excerpt] => Preliminary CT
scans of the core. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 3_core-searsville-scans-copy [to_ping] => [pinged] => [post_modified] => 2022-05-06 09:41:54 [post_modified_gmt] => 2022-05-06 07:41:54 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/3_core-searsville-scans-copy.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [323] => Array ( [ID] => 48086 [post_author] => 12 [post_date] => 2022-05-05 16:29:47 [post_date_gmt] => 2022-05-05 14:29:47 [post_content] => Photograph by Yongming Han © All Rights Reserved [post_title] => 3_corestrip [post_excerpt] => A frozen core strip, 20 cm long, 2 cm wide. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 3_corestrip-2 [to_ping] => [pinged] => [post_modified] => 2022-05-05 16:32:37 [post_modified_gmt] => 2022-05-05 14:32:37 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/3_corestrip-1.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [324] => Array ( [ID] => 48085 [post_author] => 12 [post_date] => 2022-05-05 16:29:43 [post_date_gmt] => 2022-05-05 14:29:43 [post_content] => Photographs by Dewen Lei © All Rights Reserved [post_title] => 3_core [post_excerpt] => The frozen core. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 3_core-11 [to_ping] => [pinged] => [post_modified] => 2022-05-05 16:33:34 [post_modified_gmt] => 2022-05-05 14:33:34 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/3_core-5.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [325] => Array ( [ID] => 48084 [post_author] => 129 [post_date] => 2022-05-05 16:29:29 [post_date_gmt] => 2022-05-05 14:29:29 [post_content] =>
Photograph by Nona Chiariello,
Stanford University © All Rights Reserved [post_title] => 2_upper lake copy [post_excerpt] => Aerial image of Upper Lake, 700 meters to
the southwest of Searsville Reservoir. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 2_upper-lake-copy [to_ping] => [pinged] => [post_modified] => 2022-05-06 09:36:28 [post_modified_gmt] => 2022-05-06 07:36:28 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/2_upper-lake-copy.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [326] => Array ( [ID] => 48079 [post_author] => 129 [post_date] => 2022-05-05 15:41:48 [post_date_gmt] => 2022-05-05 13:41:48 [post_content] => Image by M. Allison Stegner, Stanford University © All Rights Reserved [post_title] => 3_carbon copy [post_excerpt] => Preliminary carbon isotope record from Searsville Reservoir (data produced by M. Allison Stegner, Stanford University). [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 3_carbon-copy [to_ping] => [pinged] => [post_modified] => 2022-05-05 15:59:41 [post_modified_gmt] => 2022-05-05 13:59:41 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/3_carbon-copy.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [327] => Array ( [ID] => 48078 [post_author] => 129 [post_date] => 2022-05-05 15:41:47 [post_date_gmt] => 2022-05-05 13:41:47 [post_content] => Image by M. Allison Stegner, Stanford University © All Rights Reserved [post_title] => 3_caseium copy [post_excerpt] => Preliminary cesium record from Searsville Reservoir (data produced by the Rose Lab, University College London and the St. Croix Watershed Research Station). [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 3_caseium-copy [to_ping] => [pinged] => [post_modified] => 2022-05-05 15:59:46 [post_modified_gmt] => 2022-05-05 13:59:46 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/3_caseium-copy.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [328] => Array ( [ID] => 48077 [post_author] => 129 [post_date] => 2022-05-05 15:41:46 [post_date_gmt] => 2022-05-05 13:41:46 [post_content] => Image by M. Allison Stegner, Stanford University © All Rights Reserved [post_title] => 3_SCP copy [post_excerpt] => Preliminary spheroidal carbonaceous particle record from Searsville Reservoir (data produced by the Rose Lab, University College London). [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 3_scp-copy [to_ping] => [pinged] => [post_modified] => 2022-05-05 15:59:59 [post_modified_gmt] => 2022-05-05 13:59:59 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/3_SCP-copy.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [329] => Array ( [ID] => 48076 [post_author] => 129 [post_date] => 2022-05-05 15:37:32 [post_date_gmt] => 2022-05-05 13:37:32 [post_content] => Photograph by Nona Chiariello, Stanford University © All Rights Reserved [post_title] => 4_collection copy [post_excerpt] => Collecting the core. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 4_collection-copy [to_ping] => [pinged] => [post_modified] => 2022-05-05 15:59:01 [post_modified_gmt] => 2022-05-05 13:59:01 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/4_collection-copy.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [330] => Array ( [ID] => 48075 [post_author] => 129 [post_date] => 2022-05-05 15:37:13 [post_date_gmt] => 2022-05-05 13:37:13 [post_content] => Photograph by Nona Chiariello, Stanford University © All Rights Reserved [post_title] => 4_aerial collection copy [post_excerpt] => Aerial view of the core collection by Searsville Dam. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 4_aerial-collection-copy [to_ping] => [pinged] => [post_modified] => 2022-05-05 15:58:48 [post_modified_gmt] => 2022-05-05 13:58:48 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/4_aerial-collection-copy.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [331] => Array ( [ID] => 48074 [post_author] => 129 [post_date] => 2022-05-05 15:36:54 [post_date_gmt] => 2022-05-05 13:36:54 [post_content] => Photograph by M. Allison Stegner, Stanford University © All Rights Reserved [post_title] => 4_lab5 copy [post_excerpt] => Sediment core description using a Munsel color chart. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 4_lab5-copy [to_ping] => [pinged] => [post_modified] => 2022-05-05 16:44:29 [post_modified_gmt] => 2022-05-05 14:44:29 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/4_lab5-copy.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [332] => Array ( [ID] => 48073 [post_author] => 129 [post_date] => 2022-05-05 15:36:41 [post_date_gmt] => 2022-05-05 13:36:41 [post_content] =>
Photograph by M. Allison Stegner,
Stanford University © All Rights Reserved [post_title] => 4_lab6 copy [post_excerpt] => Sediment samples connected
to the freeze-drier. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 4_lab6-copy [to_ping] => [pinged] => [post_modified] => 2022-05-06 09:43:46 [post_modified_gmt] => 2022-05-06 07:43:46 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/4_lab6-copy.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [333] => Array ( [ID] => 48072 [post_author] => 129 [post_date] => 2022-05-05 15:36:30 [post_date_gmt] => 2022-05-05 13:36:30 [post_content] => Photograph by Anthony D. Barnosky, Stanford University © All Rights Reserved [post_title] => 5_Stegner Viteri [post_excerpt] => M. Allison Stegner and Maria Viteri. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 5_stegner-viteri [to_ping] => [pinged] => [post_modified] => 2022-05-05 15:58:06 [post_modified_gmt] => 2022-05-05 13:58:06 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/5_Stegner-Viteri.pdf [menu_order] => 0 [post_type] => attachment [post_mime_type] => application/pdf [comment_count] => 0 [filter] => raw ) [334] => Array ( [ID] => 48071 [post_author] => 129 [post_date] => 2022-05-05 15:36:11 [post_date_gmt] => 2022-05-05 13:36:11 [post_content] => Photograph by Anthony D. Barnosky, Stanford University © All Rights Reserved [post_title] => 5_Sherrod Stegner La Selle [post_excerpt] => Brian Sherrod, M. Allison Stegner, and SeanPaul La Selle. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 5_sherrod-stegner-la-selle [to_ping] => [pinged] => [post_modified] => 2022-05-05 15:57:52 [post_modified_gmt] => 2022-05-05 13:57:52 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/5_Sherrod-Stegner-La-Selle.pdf [menu_order] => 0 [post_type] => attachment [post_mime_type] => application/pdf [comment_count] => 0 [filter] => raw ) [335] => Array ( [ID] => 48070 [post_author] => 129 [post_date] => 2022-05-05 15:36:02 [post_date_gmt] => 2022-05-05 13:36:02 [post_content] => Photograph by Anthony D. Barnosky, Stanford University © All Rights Reserved [post_title] => 5_Hadly1 [post_excerpt] => Elizabeth A. Hadly. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 5_hadly1 [to_ping] => [pinged] => [post_modified] => 2022-05-05 15:57:40 [post_modified_gmt] => 2022-05-05 13:57:40 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/5_Hadly1.pdf [menu_order] => 0 [post_type] => attachment [post_mime_type] => application/pdf [comment_count] => 0 [filter] => raw ) [336] => Array ( [ID] => 48069 [post_author] => 129 [post_date] => 2022-05-05 15:35:46 [post_date_gmt] => 2022-05-05 13:35:46 [post_content] => Photograph by Will Struble © All Rights Reserved [post_title] => 5_Black [post_excerpt] => Bryan Black. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 5_black [to_ping] => [pinged] => [post_modified] => 2022-05-05 15:57:27 [post_modified_gmt] => 2022-05-05 13:57:27 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/5_Black.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [337] => Array ( [ID] => 48068 [post_author] => 129 [post_date] => 2022-05-05 15:35:32 [post_date_gmt] => 2022-05-05 13:35:32 [post_content] => Photograph by Elizabeth A. Hadly, Stanford University © All Rights Reserved [post_title] => 5_Barnosky Redondo [post_excerpt] => Anthony D. Barnosky and Sergio Redondo. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 5_barnosky-redondo [to_ping] => [pinged] => [post_modified] => 2022-05-05 15:57:14 [post_modified_gmt] => 2022-05-05 13:57:14 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/5_Barnosky-Redondo.pdf [menu_order] => 0 [post_type] => attachment [post_mime_type] => application/pdf [comment_count] => 0 [filter] => raw ) [338] => Array ( [ID] => 48067 [post_author] => 129 [post_date] => 2022-05-05 15:35:16 [post_date_gmt] => 2022-05-05 13:35:16 [post_content] => Photograph by Pamela Anderson © All Rights Reserved [post_title] => 5_Anderson [post_excerpt] => R. Scott Anderson. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 5_anderson [to_ping] => [pinged] => [post_modified] => 2022-05-05 17:01:58 [post_modified_gmt] => 2022-05-05 15:01:58 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/5_Anderson.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [339] => Array ( [ID] => 48064 [post_author] => 129 [post_date] => 2022-05-05 15:32:59 [post_date_gmt] => 2022-05-05 13:32:59 [post_content] => Photograph by M. Allison Stegner, Stanford University © All Rights Reserved [post_title] => 4_lab4 [post_excerpt] => Weighing tin capsules for Nitrogen isotope analysis. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 4_lab4-3 [to_ping] => [pinged] => [post_modified] => 2022-05-05 15:56:48 [post_modified_gmt] => 2022-05-05 13:56:48 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/4_lab4-2.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [340] => Array ( [ID] => 48063 [post_author] => 129 [post_date] => 2022-05-05 15:32:48 [post_date_gmt] => 2022-05-05 13:32:48 [post_content] => Photograph by M. Allison Stegner, Stanford University © All Rights Reserved [post_title] => 4_lab3 [post_excerpt] => Preparing samples for carbon and nitrogen isotope analysis. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 4_lab3-4 [to_ping] => [pinged] => [post_modified] => 2022-05-05 15:56:35 [post_modified_gmt] => 2022-05-05 13:56:35 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/4_lab3-3.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [341] => Array ( [ID] => 48062 [post_author] => 129 [post_date] => 2022-05-05 15:32:38 [post_date_gmt] => 2022-05-05 13:32:38 [post_content] => Photograph by M. Allison Stegner, Stanford University © All Rights Reserved [post_title] => 4_lab2 [post_excerpt] => Freeze-dried samples ready for further analysis. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 4_lab2-7 [to_ping] => [pinged] => [post_modified] => 2022-05-05 15:56:23 [post_modified_gmt] => 2022-05-05 13:56:23 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/4_lab2-5.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [342] => Array ( [ID] => 48061 [post_author] => 129 [post_date] => 2022-05-05 15:32:27 [post_date_gmt] => 2022-05-05 13:32:27 [post_content] => Photograph by Sergio Redondo © All Rights Reserved [post_title] => 4_lab1 [post_excerpt] => Sergio Redondo analysing mercury samples. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 4_lab1-4 [to_ping] => [pinged] => [post_modified] => 2022-05-05 15:56:13 [post_modified_gmt] => 2022-05-05 13:56:13 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/4_lab1-1.jpeg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [343] => Array ( [ID] => 48060 [post_author] => 129 [post_date] => 2022-05-05 15:32:11 [post_date_gmt] => 2022-05-05 13:32:11 [post_content] => Photograph by Anthony D. Barnosky, Stanford University © All Rights Reserved [post_title] => 4_collection6 [post_excerpt] => Collecting the core. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 4_collection6 [to_ping] => [pinged] => [post_modified] => 2022-05-05 15:55:28 [post_modified_gmt] => 2022-05-05 13:55:28 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/4_collection6.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [344] => Array ( [ID] => 48059 [post_author] => 129 [post_date] => 2022-05-05 15:31:54 [post_date_gmt] => 2022-05-05 13:31:54 [post_content] => Photograph by Elizabeth A. Hadly, Stanford University © All Rights Reserved [post_title] => 4_collection5 [post_excerpt] => Collecting the core. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 4_collection5 [to_ping] => [pinged] => [post_modified] => 2022-05-05 15:55:25 [post_modified_gmt] => 2022-05-05 13:55:25 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/4_collection5.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [345] => Array ( [ID] => 48058 [post_author] => 129 [post_date] => 2022-05-05 15:31:37 [post_date_gmt] => 2022-05-05 13:31:37 [post_content] => Photograph by Anthony D. Barnosky, Stanford University © All Rights Reserved [post_title] => 4_collection4 [post_excerpt] => Collecting the core. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 4_collection4 [to_ping] => [pinged] => [post_modified] => 2022-05-05 15:55:22 [post_modified_gmt] => 2022-05-05 13:55:22 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/4_collection4.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [346] => Array ( [ID] => 48057 [post_author] => 129 [post_date] => 2022-05-05 15:31:18 [post_date_gmt] => 2022-05-05 13:31:18 [post_content] => Photograph by Elizabeth A. Hadly, Stanford University © All Rights Reserved [post_title] => 4_collection3 [post_excerpt] => Collecting the core. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 4_collection3 [to_ping] => [pinged] => [post_modified] => 2022-05-05 15:55:20 [post_modified_gmt] => 2022-05-05 13:55:20 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/4_collection3.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [347] => Array ( [ID] => 48056 [post_author] => 129 [post_date] => 2022-05-05 15:31:00 [post_date_gmt] => 2022-05-05 13:31:00 [post_content] => Photograph by Anthony D. Barnosky, Stanford University © All Rights Reserved [post_title] => 4_collection2 [post_excerpt] => Collecting the core. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 4_collection2 [to_ping] => [pinged] => [post_modified] => 2022-05-05 15:55:17 [post_modified_gmt] => 2022-05-05 13:55:17 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/4_collection2.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [348] => Array ( [ID] => 48055 [post_author] => 129 [post_date] => 2022-05-05 15:30:43 [post_date_gmt] => 2022-05-05 13:30:43 [post_content] => Photograph by Elizabeth A. Hadly, Stanford University © All Rights Reserved [post_title] => 4_collection1 [post_excerpt] => Collecting the core. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 4_collection1 [to_ping] => [pinged] => [post_modified] => 2022-05-05 15:54:09 [post_modified_gmt] => 2022-05-05 13:54:09 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/4_collection1.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [349] => Array ( [ID] => 48051 [post_author] => 129 [post_date] => 2022-05-05 15:29:49 [post_date_gmt] => 2022-05-05 13:29:49 [post_content] => Image by R. Scott Anderson, Northern Arizona University © All Rights Reserved [post_title] => 3_pollen [post_excerpt] => Preliminary pollen record from Searsville Reservoir (data produced by R. Scott Anderson, Northern Arizona University). [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 3_pollen [to_ping] => [pinged] => [post_modified] => 2022-05-05 16:43:11 [post_modified_gmt] => 2022-05-05 14:43:11 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/3_pollen.pdf [menu_order] => 0 [post_type] => attachment [post_mime_type] => application/pdf [comment_count] => 0 [filter] => raw ) [350] => Array ( [ID] => 48050 [post_author] => 129 [post_date] => 2022-05-05 15:29:39 [post_date_gmt] => 2022-05-05 13:29:39 [post_content] =>
Photograph by Jeremy Bolen © All Rights Reserved [post_title] => 3_core3 [post_excerpt] => A section of core. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 3_core3-3 [to_ping] => [pinged] => [post_modified] => 2022-05-06 09:47:51 [post_modified_gmt] => 2022-05-06 07:47:51 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/3_core3.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [351] => Array ( [ID] => 48049 [post_author] => 129 [post_date] => 2022-05-05 15:29:26 [post_date_gmt] => 2022-05-05 13:29:26 [post_content] =>
Image by SeanPaul La Selle,
United States Geological Survey
© All Rights Reserved [post_title] => 3_core [post_excerpt] => Preliminary CT scan and
high resolution image of
a section of the core. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 3_core-10 [to_ping] => [pinged] => [post_modified] => 2022-05-06 09:40:45 [post_modified_gmt] => 2022-05-06 07:40:45 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/3_core-2.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [352] => Array ( [ID] => 48048 [post_author] => 129 [post_date] => 2022-05-05 15:28:14 [post_date_gmt] => 2022-05-05 13:28:14 [post_content] => [post_title] => searsville swatch [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => screenshot-2022-05-05-at-15-27-57 [to_ping] => [pinged] => [post_modified] => 2022-05-17 10:56:13 [post_modified_gmt] => 2022-05-17 08:56:13 [post_content_filtered] => [post_parent] => 48046 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/Screenshot-2022-05-05-at-15.27.57.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [353] => Array ( [ID] => 48047 [post_author] => 129 [post_date] => 2022-05-05 15:27:44 [post_date_gmt] => 2022-05-05 13:27:44 [post_content] => [post_title] => 3_core searsville scans [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 3_core-searsville-scans [to_ping] => [pinged] => [post_modified] => 2022-05-05 15:27:44 [post_modified_gmt] => 2022-05-05 13:27:44 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/3_core-searsville-scans.pdf [menu_order] => 0 [post_type] => attachment [post_mime_type] => application/pdf [comment_count] => 0 [filter] => raw ) [354] => Array ( [ID] => 48043 [post_author] => 129 [post_date] => 2022-05-05 15:24:30 [post_date_gmt] => 2022-05-05 13:24:30 [post_content] => Photograph by Anthony D. Barnosky, Stanford University © All Rights Reserved [post_title] => 2_wetseason [post_excerpt] => Sediment-laden water flows over Searsville Dam following a winter storm during the wet season (October-May). [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 2_wetseason [to_ping] => [pinged] => [post_modified] => 2022-05-05 16:30:35 [post_modified_gmt] => 2022-05-05 14:30:35 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/2_wetseason.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [355] => Array ( [ID] => 48042 [post_author] => 129 [post_date] => 2022-05-05 15:24:03 [post_date_gmt] => 2022-05-05 13:24:03 [post_content] => Image by Trevor Hébert, Stanford University © All Rights Reserved [post_title] => 2_map [post_excerpt] => Map showing Searsville Reservoir, Upper Lake, and Middle Lake, with core collection locations
marked. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 2_map-3 [to_ping] => [pinged] => [post_modified] => 2022-05-06 09:37:08 [post_modified_gmt] => 2022-05-06 07:37:08 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/2_map-2.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [356] => Array ( [ID] => 48041 [post_author] => 129 [post_date] => 2022-05-05 15:23:52 [post_date_gmt] => 2022-05-05 13:23:52 [post_content] => Photograph by Anthony D. Barnosky, Stanford University © All Rights Reserved [post_title] => 2_dryseason [post_excerpt] => Searsville Reservoir in October, during the dry season (May-October). [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 2_dryseason [to_ping] => [pinged] => [post_modified] => 2022-05-05 15:53:00 [post_modified_gmt] => 2022-05-05 13:53:00 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/2_dryseason.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [357] => Array ( [ID] => 48040 [post_author] => 129 [post_date] => 2022-05-05 15:23:42 [post_date_gmt] => 2022-05-05 13:23:42 [post_content] => Photograph by Schmiebel, Wikimedia Commons, CC BY-SA 3.0 [post_title] => 1_reservoir [post_excerpt] => Looking south across Searsville Reservoir from the dam. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 1_reservoir [to_ping] => [pinged] => [post_modified] => 2022-05-05 16:01:24 [post_modified_gmt] => 2022-05-05 14:01:24 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/1_reservoir.jpeg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [358] => Array ( [ID] => 48039 [post_author] => 129 [post_date] => 2022-05-05 15:23:36 [post_date_gmt] => 2022-05-05 13:23:36 [post_content] => Photograph by Schmiebel, Wikimedia Commons, CC BY-SA 3.0 [post_title] => 1_ohlone [post_excerpt] => Ohlone pestles and mortars near Jasper Ridge Biological Preserve Field Station. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 1_ohlone [to_ping] => [pinged] => [post_modified] => 2022-05-05 15:51:58 [post_modified_gmt] => 2022-05-05 13:51:58 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/1_ohlone.jpeg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [359] => Array ( [ID] => 48038 [post_author] => 129 [post_date] => 2022-05-05 15:23:32 [post_date_gmt] => 2022-05-05 13:23:32 [post_content] => Photograph by Schmiebel, Wikimedia Commons, CC BY-SA 3.0 [post_title] => 1_jasper2 [post_excerpt] => The San Francisquito Creek in Jasper Ridge Biological Preserve just below
Searsville Dam. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 1_jasper2 [to_ping] => [pinged] => [post_modified] => 2022-05-06 09:38:51 [post_modified_gmt] => 2022-05-06 07:38:51 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/1_jasper2.jpeg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [360] => Array ( [ID] => 48037 [post_author] => 129 [post_date] => 2022-05-05 15:23:30 [post_date_gmt] => 2022-05-05 13:23:30 [post_content] => Photograph by Schmiebel, Wikimedia Commons, CC BY-SA 3.0 [post_title] => 1_jasper1 [post_excerpt] => California redwoods in the Jasper Ridge Biological Preserve. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 1_jasper1 [to_ping] => [pinged] => [post_modified] => 2022-05-05 15:50:31 [post_modified_gmt] => 2022-05-05 13:50:31 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/1_jasper1.jpeg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [361] => Array ( [ID] => 48036 [post_author] => 129 [post_date] => 2022-05-05 15:23:26 [post_date_gmt] => 2022-05-05 13:23:26 [post_content] => Photograph by Schmiebel, Wikimedia Commons, CC BY-SA 3.0 [post_title] => 1_jaspar3 [post_excerpt] => Douglas fir towering above coast live oak and madrone woods on northeast peak of Jasper Ridge. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 1_jaspar3 [to_ping] => [pinged] => [post_modified] => 2022-05-05 15:49:16 [post_modified_gmt] => 2022-05-05 13:49:16 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/1_jaspar3.jpeg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [362] => Array ( [ID] => 48035 [post_author] => 129 [post_date] => 2022-05-05 15:23:24 [post_date_gmt] => 2022-05-05 13:23:24 [post_content] => Photograph by Yifei He, Wikimedia Commons [post_title] => 1_dam [post_excerpt] => Searsville Dam. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 1_dam [to_ping] => [pinged] => [post_modified] => 2022-05-05 15:45:04 [post_modified_gmt] => 2022-05-05 13:45:04 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/1_dam.jpeg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [363] => Array ( [ID] => 48034 [post_author] => 129 [post_date] => 2022-05-05 15:23:23 [post_date_gmt] => 2022-05-05 13:23:23 [post_content] => [post_title] => 1_dam construction [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 1_dam-construction [to_ping] => [pinged] => [post_modified] => 2022-05-05 15:23:23 [post_modified_gmt] => 2022-05-05 13:23:23 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/1_dam-construction.jpeg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [364] => Array ( [ID] => 48033 [post_author] => 129 [post_date] => 2022-05-05 15:23:22 [post_date_gmt] => 2022-05-05 13:23:22 [post_content] => Wikimedia Commons, public domain [post_title] => 1_creek watershed2 [post_excerpt] => Map of San Francisquito Creek watershed. Searsville Reservoir and the Jasper Ridge Biological Preserve are visible in the center. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 1_creek-watershed2 [to_ping] => [pinged] => [post_modified] => 2022-05-05 15:43:37 [post_modified_gmt] => 2022-05-05 13:43:37 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/1_creek-watershed2.jpeg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [365] => Array ( [ID] => 48032 [post_author] => 129 [post_date] => 2022-05-05 15:23:20 [post_date_gmt] => 2022-05-05 13:23:20 [post_content] =>
Photograph by Brian Cohen, Wikimedia Commons, CC BY-SA 3.0 [post_title] => 1_creek watershed [post_excerpt] => Map of San Francisquito Creek watershed. Searsville Reservoir and the Jasper Ridge
Biological Preserve are visible in the center. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 1_creek-watershed [to_ping] => [pinged] => [post_modified] => 2022-05-06 09:35:06 [post_modified_gmt] => 2022-05-06 07:35:06 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/1_creek-watershed.jpeg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [366] => Array ( [ID] => 48028 [post_author] => 129 [post_date] => 2022-05-05 15:19:11 [post_date_gmt] => 2022-05-05 13:19:11 [post_content] => [post_title] => 4_video SCPs [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 4_video-scps [to_ping] => [pinged] => [post_modified] => 2022-05-05 15:19:11 [post_modified_gmt] => 2022-05-05 13:19:11 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/4_video-SCPs.mov [menu_order] => 0 [post_type] => attachment [post_mime_type] => video/quicktime [comment_count] => 0 [filter] => raw ) [367] => Array ( [ID] => 48029 [post_author] => 129 [post_date] => 2022-05-05 15:19:11 [post_date_gmt] => 2022-05-05 13:19:11 [post_content] => [post_title] => [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 48029 [to_ping] => [pinged] => [post_modified] => 2022-05-05 15:19:11 [post_modified_gmt] => 2022-05-05 13:19:11 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/48029/ [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [368] => Array ( [ID] => 48008 [post_author] => 129 [post_date] => 2022-05-05 13:35:17 [post_date_gmt] => 2022-05-05 11:35:17 [post_content] => Photograph by Mark Williams © All Rights Reserved [post_title] => 5_team [post_excerpt] => Stephen Himson and Ian Wilkinson with a section of the core. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 5_team-7 [to_ping] => [pinged] => [post_modified] => 2022-05-05 13:44:22 [post_modified_gmt] => 2022-05-05 11:44:22 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/5_team-4.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [369] => Array ( [ID] => 48007 [post_author] => 129 [post_date] => 2022-05-05 13:35:03 [post_date_gmt] => 2022-05-05 11:35:03 [post_content] => Photograph by Stephen Himson, Mary McGann, Daniel Powers, Peter dal Ferro and Jennifer McKee © All Rights Reserved [post_title] => 4_lab [post_excerpt] => Sieving the extracted core sediment to retrieve microfossils. The sediment is washed through a series of sieves with decreasing diameter meshes. The resulting material includes microfossils, shell material, and larger grains of sediment. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 4_lab-5 [to_ping] => [pinged] => [post_modified] => 2022-05-05 13:41:07 [post_modified_gmt] => 2022-05-05 11:41:07 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/4_lab-4.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [370] => Array ( [ID] => 48006 [post_author] => 129 [post_date] => 2022-05-05 13:34:58 [post_date_gmt] => 2022-05-05 11:34:58 [post_content] => Photograph by Stephen Himson © All Rights Reserved [post_title] => 4_coring4 [post_excerpt] => Daniel Powers and Peter dal Ferro collecting the core from the estuary. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 4_coring4-2 [to_ping] => [pinged] => [post_modified] => 2022-05-05 13:38:31 [post_modified_gmt] => 2022-05-05 11:38:31 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/4_coring4-1.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [371] => Array ( [ID] => 48005 [post_author] => 129 [post_date] => 2022-05-05 13:34:55 [post_date_gmt] => 2022-05-05 11:34:55 [post_content] => Photograph by Stephen Himson, Mary McGann, Daniel Powers, Peter dal Ferro and Jennifer McKee © All Rights Reserved [post_title] => 4_coring3 [post_excerpt] => Mary McGann, Daniel Powers, and Peter dal Ferro collecting the core from the estuary. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 4_coring3-2 [to_ping] => [pinged] => [post_modified] => 2022-05-05 13:38:20 [post_modified_gmt] => 2022-05-05 11:38:20 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/4_coring3-1.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [372] => Array ( [ID] => 48004 [post_author] => 129 [post_date] => 2022-05-05 13:34:52 [post_date_gmt] => 2022-05-05 11:34:52 [post_content] => Photograph by Stephen Himson, Mary McGann, Daniel Powers, Peter dal Ferro and Jennifer McKee © All Rights Reserved [post_title] => 4_coring2 [post_excerpt] => Daniel Powers and Peter dal Ferro collecting the core from the estuary. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 4_coring2-2 [to_ping] => [pinged] => [post_modified] => 2022-05-05 13:38:05 [post_modified_gmt] => 2022-05-05 11:38:05 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/4_coring2-2.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [373] => Array ( [ID] => 48003 [post_author] => 129 [post_date] => 2022-05-05 13:34:49 [post_date_gmt] => 2022-05-05 11:34:49 [post_content] => Photograph by Stephen Himson, Mary McGann, Daniel Powers, Peter dal Ferro and Jennifer McKee © All Rights Reserved [post_title] => 4_coring1 [post_excerpt] => Daniel Powers collecting the core from the estuary. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 4_coring1-2 [to_ping] => [pinged] => [post_modified] => 2022-05-05 13:37:49 [post_modified_gmt] => 2022-05-05 11:37:49 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/4_coring1.jpeg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [374] => Array ( [ID] => 48002 [post_author] => 129 [post_date] => 2022-05-05 13:34:36 [post_date_gmt] => 2022-05-05 11:34:36 [post_content] => Image by Stephen Himson, Mark Williams, and Ian Wilkinson © All Rights Reserved [post_title] => 3_ostracod plate [post_excerpt] => Examples of the four invasive microorganisms found in the core (Bicornucythere bisanensis, Spinileberis quadriaculeata, Eusarsiella zostericola, and Trochammina hadai), imaged using an SEM. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 3_ostracod-plate [to_ping] => [pinged] => [post_modified] => 2022-05-05 13:37:36 [post_modified_gmt] => 2022-05-05 11:37:36 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/3_ostracod-plate.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [375] => Array ( [ID] => 48001 [post_author] => 129 [post_date] => 2022-05-05 13:34:26 [post_date_gmt] => 2022-05-05 11:34:26 [post_content] => Image by Stephen Himson, Mark Williams, Mary McGann, Ian Wilkinson, Cerin Pye, and Juan Carlos Berrio © All Rights Reserved [post_title] => 3_microfossil and stats plot [post_excerpt] => Plot of the microfossils found in the SFB-20A core. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 3_microfossil-and-stats-plot [to_ping] => [pinged] => [post_modified] => 2022-05-05 13:37:24 [post_modified_gmt] => 2022-05-05 11:37:24 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/3_microfossil-and-stats-plot.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [376] => Array ( [ID] => 48000 [post_author] => 129 [post_date] => 2022-05-05 13:34:23 [post_date_gmt] => 2022-05-05 11:34:23 [post_content] => Artwork by John Russell Bartlett, Wikimedia Commons , public domain [post_title] => 3_mercury mine [post_excerpt] => 1852 drawing of the New Almaden mercury mine that was in operation from 1870 to 1976, around 60 km away from San Francisco estuary. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 3_mercury-mine [to_ping] => [pinged] => [post_modified] => 2022-05-05 15:15:47 [post_modified_gmt] => 2022-05-05 13:15:47 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/3_mercury-mine.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [377] => Array ( [ID] => 47999 [post_author] => 129 [post_date] => 2022-05-05 13:34:18 [post_date_gmt] => 2022-05-05 11:34:18 [post_content] =>
Image by Stephen Himson
© All Rights Reserved [post_title] => 3_core [post_excerpt] => The SFB-20A core. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 3_core-9 [to_ping] => [pinged] => [post_modified] => 2022-05-06 09:54:36 [post_modified_gmt] => 2022-05-06 07:54:36 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/3_core-1.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [378] => Array ( [ID] => 47998 [post_author] => 129 [post_date] => 2022-05-05 13:34:16 [post_date_gmt] => 2022-05-05 11:34:16 [post_content] =>
Photograph by United States Geological Survey,
Wikimedia Commons [post_title] => 2_teredo [post_excerpt] => Teredo navalis (or naval shipworm) is a mollusk that bores into wood,
and has caused damage to wooden harbours in the bay
after it was introduced in the early twentieth century. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 2_teredo [to_ping] => [pinged] => [post_modified] => 2022-05-17 11:18:32 [post_modified_gmt] => 2022-05-17 09:18:32 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/2_teredo.jpeg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [379] => Array ( [ID] => 47997 [post_author] => 129 [post_date] => 2022-05-05 13:34:13 [post_date_gmt] => 2022-05-05 11:34:13 [post_content] => Photograph by USDA-NRCS PLANTS Database, Wikimedia Commons [post_title] => 2_spartina [post_excerpt] => Spartina alterniflora was first introduced into south San Francisco Bay in the 1970s in an attempt to reclaim marshland and now threatens native species. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 2_spartina [to_ping] => [pinged] => [post_modified] => 2022-05-05 15:12:35 [post_modified_gmt] => 2022-05-05 13:12:35 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/2_spartina.jpeg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [380] => Array ( [ID] => 47996 [post_author] => 129 [post_date] => 2022-05-05 13:34:09 [post_date_gmt] => 2022-05-05 11:34:09 [post_content] => Photograph by Stephen Himson © All Rights Reserved [post_title] => 2_core site [post_excerpt] => The core collection site. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 2_core-site [to_ping] => [pinged] => [post_modified] => 2022-05-05 13:43:19 [post_modified_gmt] => 2022-05-05 11:43:19 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/2_core-site.jpeg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [381] => Array ( [ID] => 47995 [post_author] => 129 [post_date] => 2022-05-05 13:33:42 [post_date_gmt] => 2022-05-05 11:33:42 [post_content] => Image by European Space Agency, Wikimedia Commons, CC BY-SA 3.0 IGO, additional labelling by Stephen Himson [post_title] => 2_core map [post_excerpt] => A satellite image of San Francisco Estuary, with the location of the GSSP-candidate core marked. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 2_core-map [to_ping] => [pinged] => [post_modified] => 2022-05-05 13:35:46 [post_modified_gmt] => 2022-05-05 11:35:46 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/2_core-map.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [382] => Array ( [ID] => 47994 [post_author] => 129 [post_date] => 2022-05-05 13:33:25 [post_date_gmt] => 2022-05-05 11:33:25 [post_content] => Photograph by Blake Everett, Wikimedia Commons, CC BY-SA 1.0 AT [post_title] => 1_Bridge [post_excerpt] => The iconic Golden Gate Bridge over San Francisco Bay, completed in 1937. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 1_bridge [to_ping] => [pinged] => [post_modified] => 2022-05-05 13:34:18 [post_modified_gmt] => 2022-05-05 11:34:18 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/1_Bridge.jpeg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [383] => Array ( [ID] => 47993 [post_author] => 129 [post_date] => 2022-05-05 13:31:11 [post_date_gmt] => 2022-05-05 11:31:11 [post_content] => [post_title] => SFE SWATCH [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => screenshot-2022-05-05-at-13-30-56 [to_ping] => [pinged] => [post_modified] => 2022-05-17 10:56:59 [post_modified_gmt] => 2022-05-17 08:56:59 [post_content_filtered] => [post_parent] => 47991 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/Screenshot-2022-05-05-at-13.30.56.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [384] => Array ( [ID] => 47987 [post_author] => 129 [post_date] => 2022-05-05 11:53:35 [post_date_gmt] => 2022-05-05 09:53:35 [post_content] => Photograph by Katrin Hornek © All Rights Reserved [post_title] => 5_team2 [post_excerpt] => Maria Meszar doing element measurements at the excavation site. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 5_team2-3 [to_ping] => [pinged] => [post_modified] => 2022-05-06 10:05:26 [post_modified_gmt] => 2022-05-06 08:05:26 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/5_team2-1.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [385] => Array ( [ID] => 47986 [post_author] => 129 [post_date] => 2022-05-05 11:43:30 [post_date_gmt] => 2022-05-05 09:43:30 [post_content] => Photograph by Susanne Gier © All Rights Reserved [post_title] => 5_team [post_excerpt] => Michael Wagreich explaining the geology of the Vienna Basin in a Viennese sand pit. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 5_team-6 [to_ping] => [pinged] => [post_modified] => 2022-05-05 11:59:26 [post_modified_gmt] => 2022-05-05 09:59:26 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/5_team-3.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [386] => Array ( [ID] => 47985 [post_author] => 129 [post_date] => 2022-05-05 11:43:19 [post_date_gmt] => 2022-05-05 09:43:19 [post_content] =>
Image by Maria Meszar and Michael Wagreich © All Rights Reserved [post_title] => 3_sed1 [post_excerpt] => The Karlsplatz section with fallout layers labeled. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 3_sed1 [to_ping] => [pinged] => [post_modified] => 2022-05-09 10:02:09 [post_modified_gmt] => 2022-05-09 08:02:09 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/3_sed1.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [387] => Array ( [ID] => 47984 [post_author] => 129 [post_date] => 2022-05-05 11:43:14 [post_date_gmt] => 2022-05-05 09:43:14 [post_content] =>
Image by Maria Meszar © All Rights Reserved [post_title] => 3_sed3 [post_excerpt] => The layers of sediment and logged section at the Karlsplatz site. Sample AZ5 corresponds to the fallout nuclide layer as base of the chronostratigraphic Anthropocene. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 3_sed3 [to_ping] => [pinged] => [post_modified] => 2022-05-09 10:02:16 [post_modified_gmt] => 2022-05-09 08:02:16 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/3_sed3.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [388] => Array ( [ID] => 47983 [post_author] => 129 [post_date] => 2022-05-05 11:42:48 [post_date_gmt] => 2022-05-05 09:42:48 [post_content] => Photograph by Katrin Hornek © All Rights Reserved [post_title] => 4_site1 [post_excerpt] => Preparing for sample collection from the 1959 layer. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 4_site1 [to_ping] => [pinged] => [post_modified] => 2022-05-05 11:58:50 [post_modified_gmt] => 2022-05-05 09:58:50 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/4_site1.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [389] => Array ( [ID] => 47982 [post_author] => 129 [post_date] => 2022-05-05 11:42:12 [post_date_gmt] => 2022-05-05 09:42:12 [post_content] => [post_title] => 5_team2 [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 5_team2-2 [to_ping] => [pinged] => [post_modified] => 2022-05-05 11:42:12 [post_modified_gmt] => 2022-05-05 09:42:12 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/5_team2.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [390] => Array ( [ID] => 47981 [post_author] => 129 [post_date] => 2022-05-05 11:41:47 [post_date_gmt] => 2022-05-05 09:41:47 [post_content] => Photograph by Katrin Hornek © All Rights Reserved [post_title] => 2_site [post_excerpt] => The Karlsplatz excavation site, with Wien Museum to the left. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 2_site-2 [to_ping] => [pinged] => [post_modified] => 2022-05-05 11:58:35 [post_modified_gmt] => 2022-05-05 09:58:35 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/2_site.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [391] => Array ( [ID] => 47980 [post_author] => 129 [post_date] => 2022-05-05 11:41:32 [post_date_gmt] => 2022-05-05 09:41:32 [post_content] => Photograph by Michael Wagreich © All Rights Reserved [post_title] => 5_team1 [post_excerpt] => Katrin Hornek recording the Karlsplatz excavation. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 5_team1 [to_ping] => [pinged] => [post_modified] => 2022-05-05 13:11:48 [post_modified_gmt] => 2022-05-05 11:11:48 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/5_team1.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [392] => Array ( [ID] => 47979 [post_author] => 129 [post_date] => 2022-05-05 11:40:54 [post_date_gmt] => 2022-05-05 09:40:54 [post_content] => Image by Maria Meszar © All Rights Reserved [post_title] => 3_site [post_excerpt] => World War Two technofossil found at the site. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 3_site [to_ping] => [pinged] => [post_modified] => 2022-05-05 11:58:06 [post_modified_gmt] => 2022-05-05 09:58:06 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/3_site.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [393] => Array ( [ID] => 47978 [post_author] => 129 [post_date] => 2022-05-05 11:40:37 [post_date_gmt] => 2022-05-05 09:40:37 [post_content] => Photograph by Karin Hain © All Rights Reserved [post_title] => 4_lab2 [post_excerpt] => VERA (Vienna Environmental Research Accelerator) where fallout radionuclides including Pu-239 have been measured. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 4_lab2-6 [to_ping] => [pinged] => [post_modified] => 2022-05-05 13:10:38 [post_modified_gmt] => 2022-05-05 11:10:38 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/4_lab2-4.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [394] => Array ( [ID] => 47977 [post_author] => 129 [post_date] => 2022-05-05 11:40:24 [post_date_gmt] => 2022-05-05 09:40:24 [post_content] => Photograph by Judith Silberling, Wikimedia Commons, CC BY-SA 3.0 AT [post_title] => 1_Karlskirche [post_excerpt] => The Karlskirche (a baroque church completed in 1737), in Vienna's Karlsplatz. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 1_karlskirche [to_ping] => [pinged] => [post_modified] => 2022-05-05 12:01:06 [post_modified_gmt] => 2022-05-05 10:01:06 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/1_Karlskirche.jpeg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [395] => Array ( [ID] => 47976 [post_author] => 129 [post_date] => 2022-05-05 11:40:21 [post_date_gmt] => 2022-05-05 09:40:21 [post_content] => Image source: Exhibition Historisches Museum, Wien, 1991, author unknown, Wikimedia Commons, public domain [post_title] => 1_river2 [post_excerpt] => Works between 1984 and 1900 to cover over the River Wien at Karlsplatz (photograph taken circa 1898). [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 1_river2 [to_ping] => [pinged] => [post_modified] => 2022-05-05 13:22:00 [post_modified_gmt] => 2022-05-05 11:22:00 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/1_river2.jpeg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [396] => Array ( [ID] => 47975 [post_author] => 129 [post_date] => 2022-05-05 11:40:18 [post_date_gmt] => 2022-05-05 09:40:18 [post_content] => Image source: Exhibition Historisches Museum, Wien, 1991, author unknown, Wikimedia Commons, public domain [post_title] => 1_river3 [post_excerpt] => Works between 1984 and 1900 to cover over the River Wien at Karlsplatz (photograph taken circa 1898). [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 1_river3 [to_ping] => [pinged] => [post_modified] => 2022-05-05 13:24:20 [post_modified_gmt] => 2022-05-05 11:24:20 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/1_river3.jpeg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [397] => Array ( [ID] => 47974 [post_author] => 129 [post_date] => 2022-05-05 11:40:15 [post_date_gmt] => 2022-05-05 09:40:15 [post_content] => Image source: Exhibition Historisches Museum, Wien, 1991, author unknown Wikimedia Commons, public domain [post_title] => 1_river1 [post_excerpt] => Works between 1984 and 1900 to cover over the River Wien at Karlsplatz (photograph taken circa 1898). The Karlskirche is visible in the background. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 1_river1 [to_ping] => [pinged] => [post_modified] => 2022-05-05 13:21:19 [post_modified_gmt] => 2022-05-05 11:21:19 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/1_river1.jpeg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [398] => Array ( [ID] => 47973 [post_author] => 129 [post_date] => 2022-05-05 11:40:12 [post_date_gmt] => 2022-05-05 09:40:12 [post_content] =>
Photography by Clemens Pfeiffer, Wikimedia Commons, public domain [post_title] => 1_wienmuseum [post_excerpt] => The Wien Museum in Vienna's Karlsplatz, adjacent to which is the research site. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 1_wienmuseum [to_ping] => [pinged] => [post_modified] => 2022-05-09 10:01:09 [post_modified_gmt] => 2022-05-09 08:01:09 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/1_wienmuseum.jpeg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [399] => Array ( [ID] => 47972 [post_author] => 129 [post_date] => 2022-05-05 11:40:07 [post_date_gmt] => 2022-05-05 09:40:07 [post_content] => Photograph by Michael Wagreich © All Rights Reserved [post_title] => 4_lab1 [post_excerpt] => Samples from the upper part of the Karlsplatz excavation site, arranged from oldest to the lower right (older than 1922) to the youngest in the upper left (younger than 1959). Sample AZ5 (from ca. 1959) in the middle contains fallout radionuclides from the 1950s. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 4_lab1-3 [to_ping] => [pinged] => [post_modified] => 2022-05-05 11:56:25 [post_modified_gmt] => 2022-05-05 09:56:25 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/4_lab1.jpeg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [400] => Array ( [ID] => 47971 [post_author] => 129 [post_date] => 2022-05-05 11:39:57 [post_date_gmt] => 2022-05-05 09:39:57 [post_content] => Photograph by Katrin Hornek © All Rights Reserved [post_title] => 2_digger [post_excerpt] => The Karlsplatz excavation site in front of the Wien Museum and the Karlskirche during sampling in October 2019. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 2_digger [to_ping] => [pinged] => [post_modified] => 2022-05-05 11:56:10 [post_modified_gmt] => 2022-05-05 09:56:10 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/2_digger.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [401] => Array ( [ID] => 47970 [post_author] => 129 [post_date] => 2022-05-05 11:39:46 [post_date_gmt] => 2022-05-05 09:39:46 [post_content] => Photograph by Katrin Hornek © All Rights Reserved [post_title] => 4_site2 [post_excerpt] => Samples taken from the youngest part of the Karlsplatz section including the fallout material. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 4_site2 [to_ping] => [pinged] => [post_modified] => 2022-05-05 11:55:57 [post_modified_gmt] => 2022-05-05 09:55:57 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/4_site2.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [402] => Array ( [ID] => 47969 [post_author] => 129 [post_date] => 2022-05-05 11:39:44 [post_date_gmt] => 2022-05-05 09:39:44 [post_content] => Image by Karin Hain and Janis Wolf © All Rights Reserved [post_title] => 3_graph2 [post_excerpt] => Concentration of Pu-239 and Pu-240 (atoms/g) in the Karsplatz section, from zero
(WMP3 layer older than 1922) to minimum (WM5 WW2 rubble with some downsection
contamination) to Wag09 (AZ5 base of 1959 layer) to A23 (sample from within the 1959
soil layer). [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 3_graph2-2 [to_ping] => [pinged] => [post_modified] => 2022-05-09 10:04:26 [post_modified_gmt] => 2022-05-09 08:04:26 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/3_graph2.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [403] => Array ( [ID] => 47967 [post_author] => 129 [post_date] => 2022-05-05 11:39:34 [post_date_gmt] => 2022-05-05 09:39:34 [post_content] => Image by Kira Lappé © All Rights Reserved [post_title] => 2_graph1 [post_excerpt] => Distribution of materials found by the larger project that looks at more than 60,000 borehole sites (from old wells) and archaeological data across the city. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 2_graph1 [to_ping] => [pinged] => [post_modified] => 2022-05-05 11:55:18 [post_modified_gmt] => 2022-05-05 09:55:18 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/2_graph1.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [404] => Array ( [ID] => 47966 [post_author] => 129 [post_date] => 2022-05-05 11:39:32 [post_date_gmt] => 2022-05-05 09:39:32 [post_content] => Image by Kira Lappé © All Rights Reserved [post_title] => 2_graph2 [post_excerpt] => Distribution of post-1950 anthropogenic materials found by the larger project that looks at more than 60,000 borehole sites (from old wells) and archaeological data across the city. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 2_graph2 [to_ping] => [pinged] => [post_modified] => 2022-05-06 09:57:39 [post_modified_gmt] => 2022-05-06 07:57:39 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/2_graph2.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [405] => Array ( [ID] => 47965 [post_author] => 129 [post_date] => 2022-05-05 11:39:12 [post_date_gmt] => 2022-05-05 09:39:12 [post_content] => [post_title] => Screenshot 2022-05-05 at 11.38.57 [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => screenshot-2022-05-05-at-11-38-57 [to_ping] => [pinged] => [post_modified] => 2022-05-17 10:57:41 [post_modified_gmt] => 2022-05-17 08:57:41 [post_content_filtered] => [post_parent] => 47964 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/Screenshot-2022-05-05-at-11.38.57.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [406] => Array ( [ID] => 47946 [post_author] => 129 [post_date] => 2022-05-05 11:08:53 [post_date_gmt] => 2022-05-05 09:08:53 [post_content] => Photograph by Kerry Allen © All Rights Reserved [post_title] => 5_team [post_excerpt] => From left to right: Arnoud Boom, Sue Sampson, Genna Tyrell, Adam Cox, and Jens Zinke. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 5_team-5 [to_ping] => [pinged] => [post_modified] => 2022-05-05 11:27:19 [post_modified_gmt] => 2022-05-05 09:27:19 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/5_team-2.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [407] => Array ( [ID] => 47944 [post_author] => 129 [post_date] => 2022-05-05 11:08:35 [post_date_gmt] => 2022-05-05 09:08:35 [post_content] => Photograph by Neal Cantin © All Rights Reserved [post_title] => 4_lab2 [post_excerpt] => Grace Frank (technician) and Neal Cantin (Principle Research scientist) doing the age assignment of the coral cores in the X-ray laboratory at AIMS in Townsville, Queensland, Australia. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 4_lab2-5 [to_ping] => [pinged] => [post_modified] => 2022-05-05 11:15:27 [post_modified_gmt] => 2022-05-05 09:15:27 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/4_lab2-3.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [408] => Array ( [ID] => 47943 [post_author] => 129 [post_date] => 2022-05-05 11:08:22 [post_date_gmt] => 2022-05-05 09:08:22 [post_content] => Photograph by Jens Zinke © All Rights Reserved [post_title] => 4_lab [post_excerpt] => 1.5 ml PVC autosampler vials where coral powder samples were stored. Front left: small Labco glass vials used to weigh out 2 mg of coral powder for later analysis in mass spectrometer. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 4_lab-4 [to_ping] => [pinged] => [post_modified] => 2022-05-05 11:15:52 [post_modified_gmt] => 2022-05-05 09:15:52 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/4_lab-3.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [409] => Array ( [ID] => 47942 [post_author] => 129 [post_date] => 2022-05-05 11:08:21 [post_date_gmt] => 2022-05-05 09:08:21 [post_content] => Video by Thomas DeCarlo © All Rights Reserved [post_title] => 4_coringvid2 [post_excerpt] => Thomas M. DeCarlo and Hugo Harrison removing the coral core after drilling. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 4_coringvid2-2 [to_ping] => [pinged] => [post_modified] => 2022-05-05 11:15:57 [post_modified_gmt] => 2022-05-05 09:15:57 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/4_coringvid2-1.mp4 [menu_order] => 0 [post_type] => attachment [post_mime_type] => video/mp4 [comment_count] => 0 [filter] => raw ) [410] => Array ( [ID] => 47941 [post_author] => 129 [post_date] => 2022-05-05 11:08:19 [post_date_gmt] => 2022-05-05 09:08:19 [post_content] => Video by Thomas DeCarlo © All Rights Reserved [post_title] => 4_coringvid1 [post_excerpt] => Thomas M. DeCarlo and Hugo Harrison drilling at Flinders Reef in Dec 2017. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 4_coringvid1-2 [to_ping] => [pinged] => [post_modified] => 2022-05-05 11:16:02 [post_modified_gmt] => 2022-05-05 09:16:02 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/4_coringvid1-1.mp4 [menu_order] => 0 [post_type] => attachment [post_mime_type] => video/mp4 [comment_count] => 0 [filter] => raw ) [411] => Array ( [ID] => 47940 [post_author] => 129 [post_date] => 2022-05-05 11:08:13 [post_date_gmt] => 2022-05-05 09:08:13 [post_content] => Photograph by Tane Taylor-Sinclair © All Rights Reserved [post_title] => 4_coring4 [post_excerpt] => Drilling a Porites coral in December 2017. A white core section that has already been retrieved is laying on another coral. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 4_coring4 [to_ping] => [pinged] => [post_modified] => 2022-05-05 11:22:34 [post_modified_gmt] => 2022-05-05 09:22:34 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/4_coring4.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [412] => Array ( [ID] => 47939 [post_author] => 129 [post_date] => 2022-05-05 11:08:08 [post_date_gmt] => 2022-05-05 09:08:08 [post_content] => Photograph by Tane Taylor-Sinclair © All Rights Reserved [post_title] => 4_coring3 [post_excerpt] => Drilling a Porites coral in December 2017. A white core section (lower right) that has already been retrieved is laying on another coral. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 4_coring3 [to_ping] => [pinged] => [post_modified] => 2022-05-05 11:16:12 [post_modified_gmt] => 2022-05-05 09:16:12 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/4_coring3.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [413] => Array ( [ID] => 47938 [post_author] => 129 [post_date] => 2022-05-05 11:07:59 [post_date_gmt] => 2022-05-05 09:07:59 [post_content] => Photograph by Jens Zinke © All Rights Reserved [post_title] => 4_coring2 [post_excerpt] => Jens Zinke and his ex-PhD student Craig Grove on fieldwork drilling a coral core in Madagascar. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => olympus-digital-camera-40 [to_ping] => [pinged] => [post_modified] => 2022-05-05 11:16:19 [post_modified_gmt] => 2022-05-05 09:16:19 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/4_coring2-1.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [414] => Array ( [ID] => 47937 [post_author] => 129 [post_date] => 2022-05-05 11:07:51 [post_date_gmt] => 2022-05-05 09:07:51 [post_content] => [post_title] => 4_coring [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 4_coring-2 [to_ping] => [pinged] => [post_modified] => 2022-05-05 11:07:51 [post_modified_gmt] => 2022-05-05 09:07:51 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/4_coring-1.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [415] => Array ( [ID] => 47936 [post_author] => 129 [post_date] => 2022-05-05 11:07:46 [post_date_gmt] => 2022-05-05 09:07:46 [post_content] =>
Image by Neal Cantin
© All Rights Reserved [post_title] => 3_core [post_excerpt] => X-ray positive prints of cores
FLI01A and FLI05A with sampling
transects indicated (black lines). [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 3_core-8 [to_ping] => [pinged] => [post_modified] => 2022-05-06 10:16:39 [post_modified_gmt] => 2022-05-06 08:16:39 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/3_core.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [416] => Array ( [ID] => 47935 [post_author] => 129 [post_date] => 2022-05-05 11:07:45 [post_date_gmt] => 2022-05-05 09:07:45 [post_content] => Image by Jens Zinke © All Rights Reserved [post_title] => 3_c14 [post_excerpt] => Carbon-14 of Flinders coral core (orange) compared to published records from across the Great Barrier Reef between 1900 and 2017. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 3_c14 [to_ping] => [pinged] => [post_modified] => 2022-05-05 11:16:57 [post_modified_gmt] => 2022-05-05 09:16:57 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/3_c14.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [417] => Array ( [ID] => 47934 [post_author] => 129 [post_date] => 2022-05-05 11:07:44 [post_date_gmt] => 2022-05-05 09:07:44 [post_content] => Photograph by Jens Zinke © All Rights Reserved [post_title] => 2_Porites [post_excerpt] => Example of a Porites sp. coral. This specimen is growing off St. Marie Island, Madagascar. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 2_porites [to_ping] => [pinged] => [post_modified] => 2022-05-05 11:19:56 [post_modified_gmt] => 2022-05-05 09:19:56 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/2_Porites.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [418] => Array ( [ID] => 47933 [post_author] => 129 [post_date] => 2022-05-05 11:07:42 [post_date_gmt] => 2022-05-05 09:07:42 [post_content] => Photograph by Ayanadak123, Wikimedia Commons [post_title] => 1_gbr2 [post_excerpt] => Part of the Great Barrier Reef, near Airlie beach, Queensland. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 1_gbr2 [to_ping] => [pinged] => [post_modified] => 2022-05-05 15:06:48 [post_modified_gmt] => 2022-05-05 13:06:48 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/1_gbr2.jpeg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [419] => Array ( [ID] => 47932 [post_author] => 129 [post_date] => 2022-05-05 11:07:41 [post_date_gmt] => 2022-05-05 09:07:41 [post_content] => Photograph by European Space Agency, Wikimedia Commons, CC BY-SA 3.0 IGO [post_title] => 1_gbr [post_excerpt] => A satellite image of north Queensland, Australia. The Great Barrier Reef is visible off the northeast coast, with Flinders being further out towards the bottom of the image. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 1_gbr [to_ping] => [pinged] => [post_modified] => 2022-05-05 11:17:37 [post_modified_gmt] => 2022-05-05 09:17:37 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/1_gbr.jpeg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [420] => Array ( [ID] => 47931 [post_author] => 129 [post_date] => 2022-05-05 11:07:38 [post_date_gmt] => 2022-05-05 09:07:38 [post_content] => Photograph by Matt Kieffer, Wikimedia Commons , CC BY-SA 2.0 AT [post_title] => 1_bleach [post_excerpt] => Bleached staghorn coral in the Great Barrier Reef. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 1_bleach [to_ping] => [pinged] => [post_modified] => 2022-05-05 15:10:04 [post_modified_gmt] => 2022-05-05 13:10:04 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/1_bleach.jpeg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [421] => Array ( [ID] => 47929 [post_author] => 12 [post_date] => 2022-05-05 11:07:15 [post_date_gmt] => 2022-05-05 09:07:15 [post_content] => [post_title] => sihailongwan [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => sihailongwan [to_ping] => [pinged] => [post_modified] => 2022-05-17 10:58:36 [post_modified_gmt] => 2022-05-17 08:58:36 [post_content_filtered] => [post_parent] => 47926 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/sihailongwan.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [422] => Array ( [ID] => 47927 [post_author] => 129 [post_date] => 2022-05-05 11:04:44 [post_date_gmt] => 2022-05-05 09:04:44 [post_content] => [post_title] => Screenshot 2022-05-05 at 11.04.25 [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => screenshot-2022-05-05-at-11-04-25 [to_ping] => [pinged] => [post_modified] => 2022-05-17 10:59:36 [post_modified_gmt] => 2022-05-17 08:59:36 [post_content_filtered] => [post_parent] => 47925 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/Screenshot-2022-05-05-at-11.04.25.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [423] => Array ( [ID] => 47922 [post_author] => 12 [post_date] => 2022-05-05 10:57:06 [post_date_gmt] => 2022-05-05 08:57:06 [post_content] => Photograph by Dewen Lei © All Rights Reserved [post_title] => image description [post_excerpt] => The XRF core scanner. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => image-description-2 [to_ping] => [pinged] => [post_modified] => 2022-05-05 10:57:42 [post_modified_gmt] => 2022-05-05 08:57:42 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/4_lab7.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [424] => Array ( [ID] => 47913 [post_author] => 129 [post_date] => 2022-05-05 10:37:37 [post_date_gmt] => 2022-05-05 08:37:37 [post_content] =>
Image by Ian Fairchild © All Rights Reserved [post_title] => 3_core4 [post_excerpt] => Thin section of ER77 in transmitted light. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => screenshot-2022-05-05-at-10-37-14 [to_ping] => [pinged] => [post_modified] => 2022-05-06 10:30:07 [post_modified_gmt] => 2022-05-06 08:30:07 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/Screenshot-2022-05-05-at-10.37.14.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [425] => Array ( [ID] => 47912 [post_author] => 129 [post_date] => 2022-05-05 10:31:43 [post_date_gmt] => 2022-05-05 08:31:43 [post_content] => Photograph by Andrea Borsato © All Rights Reserved [post_title] => 5_silvia [post_excerpt] => Silvia Frisia at the European Synchrotron Radiation Facility. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 5_silvia [to_ping] => [pinged] => [post_modified] => 2022-05-05 10:36:12 [post_modified_gmt] => 2022-05-05 08:36:12 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/5_silvia.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [426] => Array ( [ID] => 47911 [post_author] => 129 [post_date] => 2022-05-05 10:31:38 [post_date_gmt] => 2022-05-05 08:31:38 [post_content] =>
Photograph by Ian Fairchild © All Rights Reserved [post_title] => 5_Ian Fairchild and Edinburgh ion microprobe facility [post_excerpt] => Ian Fairchild at the Edinburgh Ion Microprobe facility. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 5_ian-fairchild-and-edinburgh-ion-microprobe-facility [to_ping] => [pinged] => [post_modified] => 2022-05-10 09:05:05 [post_modified_gmt] => 2022-05-10 07:05:05 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/5_Ian-Fairchild-and-Edinburgh-ion-microprobe-facility.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [427] => Array ( [ID] => 47909 [post_author] => 129 [post_date] => 2022-05-05 10:31:28 [post_date_gmt] => 2022-05-05 08:31:28 [post_content] => Photograph by Andrea Borsato © All Rights Reserved [post_title] => 4_lab3 [post_excerpt] => Silvia Frisia mounting a stalagmite slice at beamline ID22 at the European Synchrotron Radiation Facility (Grenoble, France). [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 4_lab3-3 [to_ping] => [pinged] => [post_modified] => 2022-05-05 10:47:17 [post_modified_gmt] => 2022-05-05 08:47:17 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/4_lab3-2.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [428] => Array ( [ID] => 47908 [post_author] => 129 [post_date] => 2022-05-05 10:31:24 [post_date_gmt] => 2022-05-05 08:31:24 [post_content] => Photograph by Andrea Borsato © All Rights Reserved [post_title] => 4_lab2 [post_excerpt] => View from above of the experimental hall at the European Synchrotron Radiation Facility (Grenoble, France). [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 4_lab2-4 [to_ping] => [pinged] => [post_modified] => 2022-05-05 10:35:45 [post_modified_gmt] => 2022-05-05 08:35:45 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/4_lab2-2.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [429] => Array ( [ID] => 47907 [post_author] => 129 [post_date] => 2022-05-05 10:31:15 [post_date_gmt] => 2022-05-05 08:31:15 [post_content] => Photograph by Andrea Borsato © All Rights Reserved [post_title] => 4_lab [post_excerpt] => Stalagmite slice mounting set-up at beamline ID22 at the European Synchrotron Radiation Facility (Grenoble, France). [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 4_lab-3 [to_ping] => [pinged] => [post_modified] => 2022-05-05 10:35:32 [post_modified_gmt] => 2022-05-05 08:35:32 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/4_lab-2.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [430] => Array ( [ID] => 47906 [post_author] => 129 [post_date] => 2022-05-05 10:31:06 [post_date_gmt] => 2022-05-05 08:31:06 [post_content] => Photograph by Andrea Borsato © All Rights Reserved [post_title] => 4_core samples [post_excerpt] => Thin sections of the topmost part of stalagmites ER76 and ER78. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 4_core-samples [to_ping] => [pinged] => [post_modified] => 2022-05-05 10:35:18 [post_modified_gmt] => 2022-05-05 08:35:18 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/4_core-samples.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [431] => Array ( [ID] => 47903 [post_author] => 129 [post_date] => 2022-05-05 10:30:46 [post_date_gmt] => 2022-05-05 08:30:46 [post_content] => Image by Andrea Borsato © All Rights Reserved [post_title] => 3_core3 [post_excerpt] => Calcium synchrotron radiation XRF map of the topmost part of stalagmite ER78. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 3_core3-2 [to_ping] => [pinged] => [post_modified] => 2022-05-05 10:34:38 [post_modified_gmt] => 2022-05-05 08:34:38 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/3_core3.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [432] => Array ( [ID] => 47902 [post_author] => 129 [post_date] => 2022-05-05 10:30:21 [post_date_gmt] => 2022-05-05 08:30:21 [post_content] => Image by Andrea Borsato © All Rights Reserved [post_title] => 3_core2 [post_excerpt] => Calcium synchrotron radiation XRF map of the topmost part of stalagmite ER78. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 3_core2-4 [to_ping] => [pinged] => [post_modified] => 2022-05-05 10:34:26 [post_modified_gmt] => 2022-05-05 08:34:26 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/3_core2.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [433] => Array ( [ID] => 47901 [post_author] => 129 [post_date] => 2022-05-05 10:30:14 [post_date_gmt] => 2022-05-05 08:30:14 [post_content] => Photograph by Andrea Borsato © All Rights Reserved [post_title] => 3_core [post_excerpt] => The ER77 stalagmite cut along its growth axis. Note the characteristic translucent calcite layer at the top. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 3_core-7 [to_ping] => [pinged] => [post_modified] => 2022-05-10 09:18:26 [post_modified_gmt] => 2022-05-10 07:18:26 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/3_core-4.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [434] => Array ( [ID] => 47896 [post_author] => 129 [post_date] => 2022-05-05 10:30:02 [post_date_gmt] => 2022-05-05 08:30:02 [post_content] => Photograph by Lohengrin Giraud, Wikimedia Commons , public domain [post_title] => 1_Asiago [post_excerpt] => Aftermath of an assault, during the Asiago Battle, which occurred in May 1915 on the Trentino Alps (Italian Front, WWI). [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 1_asiago [to_ping] => [pinged] => [post_modified] => 2022-05-05 15:03:33 [post_modified_gmt] => 2022-05-05 13:03:33 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/1_Asiago.jpeg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [435] => Array ( [ID] => 47897 [post_author] => 129 [post_date] => 2022-05-05 10:30:02 [post_date_gmt] => 2022-05-05 08:30:02 [post_content] => Photograph by Andrea Borsato © All Rights Reserved [post_title] => 1_cave [post_excerpt] => Stalagmites and stalactities in Ernesto Cave. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 1_cave [to_ping] => [pinged] => [post_modified] => 2022-05-05 10:38:53 [post_modified_gmt] => 2022-05-05 08:38:53 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/1_cave.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [436] => Array ( [ID] => 47895 [post_author] => 129 [post_date] => 2022-05-05 10:27:14 [post_date_gmt] => 2022-05-05 08:27:14 [post_content] => [post_title] => ernesto swatch [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => screenshot-2022-05-05-at-10-27-02 [to_ping] => [pinged] => [post_modified] => 2022-05-17 11:00:06 [post_modified_gmt] => 2022-05-17 09:00:06 [post_content_filtered] => [post_parent] => 47894 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/Screenshot-2022-05-05-at-10.27.02.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [437] => Array ( [ID] => 47893 [post_author] => 12 [post_date] => 2022-05-05 10:16:58 [post_date_gmt] => 2022-05-05 08:16:58 [post_content] => [post_title] => working on the Sihailongwan maar lake [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => working-on-the-sihailongwan-maar-lake [to_ping] => [pinged] => [post_modified] => 2022-08-30 11:33:36 [post_modified_gmt] => 2022-08-30 09:33:36 [post_content_filtered] => [post_parent] => 49837 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/working-on-the-Sihailongwan-maar-lake.mp4 [menu_order] => 0 [post_type] => attachment [post_mime_type] => video/mp4 [comment_count] => 0 [filter] => raw ) [438] => Array ( [ID] => 47891 [post_author] => 12 [post_date] => 2022-05-05 10:04:09 [post_date_gmt] => 2022-05-05 08:04:09 [post_content] => Image by Yongming Han © All Rights Reserved [post_title] => 4_SEM2 [post_excerpt] => Scanning electron microscope (SEM) image of char. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 4_sem2-2 [to_ping] => [pinged] => [post_modified] => 2022-05-05 10:55:41 [post_modified_gmt] => 2022-05-05 08:55:41 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/4_SEM2.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [439] => Array ( [ID] => 47892 [post_author] => 12 [post_date] => 2022-05-05 10:04:09 [post_date_gmt] => 2022-05-05 08:04:09 [post_content] => Image by Yongming Han © All Rights Reserved [post_title] => 4_SEM3 [post_excerpt] => Scanning electron microscope (SEM) image of soot. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 4_sem3-2 [to_ping] => [pinged] => [post_modified] => 2022-05-05 10:55:31 [post_modified_gmt] => 2022-05-05 08:55:31 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/4_SEM3.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [440] => Array ( [ID] => 47890 [post_author] => 12 [post_date] => 2022-05-05 10:04:08 [post_date_gmt] => 2022-05-05 08:04:08 [post_content] => Image by Yongming Han © All Rights Reserved [post_title] => 4_SEM1 [post_excerpt] => Scanning electron microscope (SEM) image of char. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 4_sem1-2 [to_ping] => [pinged] => [post_modified] => 2022-05-05 10:43:22 [post_modified_gmt] => 2022-05-05 08:43:22 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/4_SEM1.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [441] => Array ( [ID] => 47889 [post_author] => 12 [post_date] => 2022-05-05 10:04:01 [post_date_gmt] => 2022-05-05 08:04:01 [post_content] => Image by Xue Zhao © All Rights Reserved [post_title] => 3_Pu and 137Cs [post_excerpt] => Concentrations of plutonium and caesium-137. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 3_pu-and-137cs-2 [to_ping] => [pinged] => [post_modified] => 2022-05-05 10:13:01 [post_modified_gmt] => 2022-05-05 08:13:01 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/3_Pu-and-137Cs.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [442] => Array ( [ID] => 47888 [post_author] => 12 [post_date] => 2022-05-05 10:03:49 [post_date_gmt] => 2022-05-05 08:03:49 [post_content] => Photographs by Dewen Lei © All Rights Reserved [post_title] => image description [post_excerpt] => The twenty frozen cores collected from Sihailongwan
Maar. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => image-description-4 [to_ping] => [pinged] => [post_modified] => 2022-05-16 10:32:44 [post_modified_gmt] => 2022-05-16 08:32:44 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/3_24cores.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [443] => Array ( [ID] => 47867 [post_author] => 12 [post_date] => 2022-05-04 17:55:02 [post_date_gmt] => 2022-05-04 15:55:02 [post_content] => Photograph by Rolfmueller, Wikimedia Commons, CC BY-SA 3.0 [post_title] => image [post_excerpt] => Forest in the Jilin Longwan National Natural Reserve. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => image-9 [to_ping] => [pinged] => [post_modified] => 2022-05-14 10:56:26 [post_modified_gmt] => 2022-05-14 08:56:26 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/image.jpeg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [444] => Array ( [ID] => 47866 [post_author] => 12 [post_date] => 2022-05-04 17:54:50 [post_date_gmt] => 2022-05-04 15:54:50 [post_content] =>
Photograph by Dewen Lei © All Rights Reserved [post_title] => 5_Yongming [post_excerpt] => Yongming Han (chief scientist)
working on Sihailongwan Maar Lake on September 18, 2020. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 5_yongming [to_ping] => [pinged] => [post_modified] => 2022-05-06 14:32:59 [post_modified_gmt] => 2022-05-06 12:32:59 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/5_Yongming.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [445] => Array ( [ID] => 47865 [post_author] => 12 [post_date] => 2022-05-04 17:54:28 [post_date_gmt] => 2022-05-04 15:54:28 [post_content] =>
Photograph by Yalan Tang
© All Rights Reserved [post_title] => 5_yalan [post_excerpt] => Yalan Tang in the lab. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 5_yalan [to_ping] => [pinged] => [post_modified] => 2022-05-06 14:33:14 [post_modified_gmt] => 2022-05-06 12:33:14 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/5_yalan.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [446] => Array ( [ID] => 47864 [post_author] => 12 [post_date] => 2022-05-04 17:54:13 [post_date_gmt] => 2022-05-04 15:54:13 [post_content] =>
Photograph by Xue Zhao © All Rights Reserved [post_title] => 5_xue [post_excerpt] => Xue Zhao working on Sihailongwan Maar Lake January 2021. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 5_xue [to_ping] => [pinged] => [post_modified] => 2022-05-06 14:33:24 [post_modified_gmt] => 2022-05-06 12:33:24 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/5_xue.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [447] => Array ( [ID] => 47863 [post_author] => 12 [post_date] => 2022-05-04 17:54:07 [post_date_gmt] => 2022-05-04 15:54:07 [post_content] => Photograph by Xu Xing © All Rights Reserved [post_title] => 5_team2 [post_excerpt] => From left to right: Dewen Lei, Jianghu Lan, Ning Chen, Peng Cheng, Weijian Zhou, Zhisheng An, Yongming Han, Luyuan Zhang,Tianli Wang, Yalan Tang, Yalan, and Yunning Cao. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 5_team2 [to_ping] => [pinged] => [post_modified] => 2022-05-05 11:03:14 [post_modified_gmt] => 2022-05-05 09:03:14 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/5_team2.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [448] => Array ( [ID] => 47862 [post_author] => 12 [post_date] => 2022-05-04 17:53:49 [post_date_gmt] => 2022-05-04 15:53:49 [post_content] => Photograph by Dewen Lei © All Rights Reserved [post_title] => 5_team [post_excerpt] => Team members working on Sihailongwan Maar Lake in January 2021 (from left to right: Dewen Lei, Hong Wang, and Jianghu Lan). [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 5_team-4 [to_ping] => [pinged] => [post_modified] => 2022-05-05 11:03:22 [post_modified_gmt] => 2022-05-05 09:03:22 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/5_team-1.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [449] => Array ( [ID] => 47861 [post_author] => 12 [post_date] => 2022-05-04 17:53:08 [post_date_gmt] => 2022-05-04 15:53:08 [post_content] => Image by Yongming Han © All Rights Reserved [post_title] => 4_XRFresult [post_excerpt] => The XRF core scanning result. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 4_xrfresult [to_ping] => [pinged] => [post_modified] => 2022-05-06 11:06:52 [post_modified_gmt] => 2022-05-06 09:06:52 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/4_XRFresult.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [450] => Array ( [ID] => 47860 [post_author] => 12 [post_date] => 2022-05-04 17:53:01 [post_date_gmt] => 2022-05-04 15:53:01 [post_content] => Image by Yongming Han © All Rights Reserved [post_title] => 4_varve counting [post_excerpt] => Varve counting. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 4_varve-counting [to_ping] => [pinged] => [post_modified] => 2022-05-05 10:12:43 [post_modified_gmt] => 2022-05-05 08:12:43 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/4_varve-counting.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [451] => Array ( [ID] => 47859 [post_author] => 12 [post_date] => 2022-05-04 17:52:39 [post_date_gmt] => 2022-05-04 15:52:39 [post_content] => Photograph by Dewen Lei © All Rights Reserved [post_title] => 4_storage and transportion [post_excerpt] => Preparing the cores for transportation. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 4_storage-and-transportion [to_ping] => [pinged] => [post_modified] => 2022-05-05 10:19:41 [post_modified_gmt] => 2022-05-05 08:19:41 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/4_storage-and-transportion.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [452] => Array ( [ID] => 47855 [post_author] => 12 [post_date] => 2022-05-04 17:51:57 [post_date_gmt] => 2022-05-04 15:51:57 [post_content] =>
Photograph by Dewen Lei © All Rights Reserved [post_title] => 4_packedcores [post_excerpt] => The cores packaged for transportation. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 4_packedcores [to_ping] => [pinged] => [post_modified] => 2022-05-06 14:30:27 [post_modified_gmt] => 2022-05-06 12:30:27 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/4_packedcores.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [453] => Array ( [ID] => 47853 [post_author] => 12 [post_date] => 2022-05-04 17:50:15 [post_date_gmt] => 2022-05-04 15:50:15 [post_content] =>
Photograph by Yongming Han © All Rights Reserved [post_title] => 4_lab6 [post_excerpt] => The treated sediment is filtered on a filter membrane
for the measurement of black carbon, char, and soot. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 4_lab6 [to_ping] => [pinged] => [post_modified] => 2022-05-06 14:32:29 [post_modified_gmt] => 2022-05-06 12:32:29 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/4_lab6.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [454] => Array ( [ID] => 47852 [post_author] => 12 [post_date] => 2022-05-04 17:50:02 [post_date_gmt] => 2022-05-04 15:50:02 [post_content] => Photograph by Yongming Han © All Rights Reserved [post_title] => 4_lab5 [post_excerpt] => The core shown under a microscope. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 4_lab5 [to_ping] => [pinged] => [post_modified] => 2022-05-05 10:23:07 [post_modified_gmt] => 2022-05-05 08:23:07 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/4_lab5.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [455] => Array ( [ID] => 47851 [post_author] => 12 [post_date] => 2022-05-04 17:49:49 [post_date_gmt] => 2022-05-04 15:49:49 [post_content] => Photograph by Yongming Han © All Rights Reserved [post_title] => 4_lab4 [post_excerpt] => Photograph by Dewen Lei © All Rights Reserved [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 4_lab4-2 [to_ping] => [pinged] => [post_modified] => 2022-05-05 10:22:57 [post_modified_gmt] => 2022-05-05 08:22:57 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/4_lab4-1.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [456] => Array ( [ID] => 47850 [post_author] => 12 [post_date] => 2022-05-04 17:49:39 [post_date_gmt] => 2022-05-04 15:49:39 [post_content] => Photograph by Yongming Han © All Rights Reserved [post_title] => 4_lab3a [post_excerpt] => Cutting the core into a thin section. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 4_lab3a [to_ping] => [pinged] => [post_modified] => 2022-05-05 10:20:58 [post_modified_gmt] => 2022-05-05 08:20:58 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/4_lab3a.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [457] => Array ( [ID] => 47849 [post_author] => 12 [post_date] => 2022-05-04 17:49:31 [post_date_gmt] => 2022-05-04 15:49:31 [post_content] => Photograph by Dewen Lei © All Rights Reserved [post_title] => 4_lab3 [post_excerpt] => A thin section of core. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 4_lab3-2 [to_ping] => [pinged] => [post_modified] => 2022-05-05 10:21:09 [post_modified_gmt] => 2022-05-05 08:21:09 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/4_lab3-1.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [458] => Array ( [ID] => 47848 [post_author] => 12 [post_date] => 2022-05-04 17:49:21 [post_date_gmt] => 2022-05-04 15:49:21 [post_content] => Photograph by Yongming Han © All Rights Reserved [post_title] => 4_lab2 [post_excerpt] => Vacuum mounting. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 4_lab2-3 [to_ping] => [pinged] => [post_modified] => 2022-05-05 10:20:34 [post_modified_gmt] => 2022-05-05 08:20:34 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/4_lab2-1.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [459] => Array ( [ID] => 47847 [post_author] => 12 [post_date] => 2022-05-04 17:49:11 [post_date_gmt] => 2022-05-04 15:49:11 [post_content] => Photograph by Yongming Han © All Rights Reserved [post_title] => 4_lab1 [post_excerpt] => Freeze-dried core sections. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 4_lab1-2 [to_ping] => [pinged] => [post_modified] => 2022-05-05 10:20:22 [post_modified_gmt] => 2022-05-05 08:20:22 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/4_lab1-1.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [460] => Array ( [ID] => 47846 [post_author] => 12 [post_date] => 2022-05-04 17:48:50 [post_date_gmt] => 2022-05-04 15:48:50 [post_content] =>
Photograph by Yongming Han
© All Rights Reserved [post_title] => 4_cutting [post_excerpt] => Cutting the core in a cold storage. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 4_cutting [to_ping] => [pinged] => [post_modified] => 2022-05-06 14:30:49 [post_modified_gmt] => 2022-05-06 12:30:49 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/4_cutting.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [461] => Array ( [ID] => 47845 [post_author] => 12 [post_date] => 2022-05-04 17:48:39 [post_date_gmt] => 2022-05-04 15:48:39 [post_content] => [post_title] => 4_coringvid2 [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 4_coringvid2 [to_ping] => [pinged] => [post_modified] => 2022-05-04 17:48:39 [post_modified_gmt] => 2022-05-04 15:48:39 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/4_coringvid2.mp4 [menu_order] => 0 [post_type] => attachment [post_mime_type] => video/mp4 [comment_count] => 0 [filter] => raw ) [462] => Array ( [ID] => 47844 [post_author] => 12 [post_date] => 2022-05-04 17:48:27 [post_date_gmt] => 2022-05-04 15:48:27 [post_content] => [post_title] => 4_coringvid1 [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 4_coringvid1 [to_ping] => [pinged] => [post_modified] => 2022-05-04 17:48:27 [post_modified_gmt] => 2022-05-04 15:48:27 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/4_coringvid1.mp4 [menu_order] => 0 [post_type] => attachment [post_mime_type] => video/mp4 [comment_count] => 0 [filter] => raw ) [463] => Array ( [ID] => 47843 [post_author] => 12 [post_date] => 2022-05-04 17:48:01 [post_date_gmt] => 2022-05-04 15:48:01 [post_content] =>
Photograph by Dewen Lei © All Rights Reserved [post_title] => 4_coring [post_excerpt] => Scientists working on Sihailongwan Maar Lake in February 2021. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 4_coring [to_ping] => [pinged] => [post_modified] => 2022-05-14 10:43:13 [post_modified_gmt] => 2022-05-14 08:43:13 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/4_coring.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [464] => Array ( [ID] => 47842 [post_author] => 12 [post_date] => 2022-05-04 17:47:39 [post_date_gmt] => 2022-05-04 15:47:39 [post_content] => Photograph by Dewen Lei © All Rights Reserved [post_title] => 4_core [post_excerpt] => A core right after collection from the lake. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 4_core [to_ping] => [pinged] => [post_modified] => 2022-05-05 10:18:39 [post_modified_gmt] => 2022-05-05 08:18:39 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/4_core.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [465] => Array ( [ID] => 47841 [post_author] => 12 [post_date] => 2022-05-04 17:47:32 [post_date_gmt] => 2022-05-04 15:47:32 [post_content] => Image by Neil Rose © All Rights Reserved [post_title] => 3_scp [post_excerpt] => Image by Yongming Han © All Rights Reserved [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 3_scp-2 [to_ping] => [pinged] => [post_modified] => 2022-05-05 16:39:17 [post_modified_gmt] => 2022-05-05 14:39:17 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/3_scp-1.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [466] => Array ( [ID] => 47839 [post_author] => 12 [post_date] => 2022-05-04 17:46:58 [post_date_gmt] => 2022-05-04 15:46:58 [post_content] => Image by Yongming Han © All Rights Reserved [post_title] => 3_PAHs [post_excerpt] => Concentartions of Polycyclic Aromatic Hydrocarbons (PAHs). [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 3_pahs [to_ping] => [pinged] => [post_modified] => 2022-05-05 10:14:09 [post_modified_gmt] => 2022-05-05 08:14:09 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/3_PAHs.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [467] => Array ( [ID] => 47838 [post_author] => 12 [post_date] => 2022-05-04 17:46:32 [post_date_gmt] => 2022-05-04 15:46:32 [post_content] => Image by Yongming Han © All Rights Reserved [post_title] => 3_mercury [post_excerpt] => Concentrations of mercury and mercury isotopes. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 3_mercury [to_ping] => [pinged] => [post_modified] => 2022-05-05 10:14:01 [post_modified_gmt] => 2022-05-05 08:14:01 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/3_mercury.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [468] => Array ( [ID] => 47837 [post_author] => 12 [post_date] => 2022-05-04 17:46:28 [post_date_gmt] => 2022-05-04 15:46:28 [post_content] => Photograph by Yongming Han © All Rights Reserved [post_title] => 3_corestrip [post_excerpt] => A frozen core strip, 20 cm long, 2 cm wide. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 3_corestrip [to_ping] => [pinged] => [post_modified] => 2022-05-05 10:11:44 [post_modified_gmt] => 2022-05-05 08:11:44 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/3_corestrip.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [469] => Array ( [ID] => 47836 [post_author] => 12 [post_date] => 2022-05-04 17:45:50 [post_date_gmt] => 2022-05-04 15:45:50 [post_content] => Photographs by Dewen Lei © All Rights Reserved [post_title] => 3_core [post_excerpt] => The frozen core. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 3_core-6 [to_ping] => [pinged] => [post_modified] => 2022-05-05 16:03:22 [post_modified_gmt] => 2022-05-05 14:03:22 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/3_core-3.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [470] => Array ( [ID] => 47835 [post_author] => 12 [post_date] => 2022-05-04 17:45:16 [post_date_gmt] => 2022-05-04 15:45:16 [post_content] => Image by Yongming Han © All Rights Reserved [post_title] => 3_char and soot concentration [post_excerpt] => Concentrations of char and soot. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 3_char-and-soot-concentration [to_ping] => [pinged] => [post_modified] => 2022-05-05 10:13:38 [post_modified_gmt] => 2022-05-05 08:13:38 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/3_char-and-soot-concentration.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [471] => Array ( [ID] => 47833 [post_author] => 12 [post_date] => 2022-05-04 17:42:50 [post_date_gmt] => 2022-05-04 15:42:50 [post_content] => Image by Yongming Han © All Rights Reserved [post_title] => 2_samplesite [post_excerpt] => The coring location in Sihailongwan Maar, the diameter of which is about 750 meters. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 2_samplesite [to_ping] => [pinged] => [post_modified] => 2022-05-14 10:55:49 [post_modified_gmt] => 2022-05-14 08:55:49 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/2_samplesite.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [472] => Array ( [ID] => 47832 [post_author] => 12 [post_date] => 2022-05-04 17:42:22 [post_date_gmt] => 2022-05-04 15:42:22 [post_content] => [post_title] => 2_depth [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 2_depth [to_ping] => [pinged] => [post_modified] => 2022-05-04 17:42:22 [post_modified_gmt] => 2022-05-04 15:42:22 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/2_depth.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [473] => Array ( [ID] => 47831 [post_author] => 12 [post_date] => 2022-05-04 17:41:58 [post_date_gmt] => 2022-05-04 15:41:58 [post_content] => Photograph by Ji Pengfei, Jilin TV Station © All Rights Reserved [post_title] => 1_SHLW [post_excerpt] => Sihailongwan Maar Lake and the surrounding forest. The raised rim at the edge of the volcanic crater is visible. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 1_shlw [to_ping] => [pinged] => [post_modified] => 2022-08-11 14:39:59 [post_modified_gmt] => 2022-08-11 12:39:59 [post_content_filtered] => [post_parent] => 49465 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/1_SHLW.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [474] => Array ( [ID] => 47830 [post_author] => 12 [post_date] => 2022-05-04 17:41:10 [post_date_gmt] => 2022-05-04 15:41:10 [post_content] => Image by Yongming Han © All Rights Reserved [post_title] => 1_map [post_excerpt] => Location of the Sihailongwan Maar Lake. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 1_map-5 [to_ping] => [pinged] => [post_modified] => 2022-05-05 11:18:37 [post_modified_gmt] => 2022-05-05 09:18:37 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/1_map.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [475] => Array ( [ID] => 47812 [post_author] => 12 [post_date] => 2022-05-04 16:33:58 [post_date_gmt] => 2022-05-04 14:33:58 [post_content] => [post_title] => sniezka [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => sniezka [to_ping] => [pinged] => [post_modified] => 2022-05-17 11:04:10 [post_modified_gmt] => 2022-05-17 09:04:10 [post_content_filtered] => [post_parent] => 47764 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/sniezka.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [476] => Array ( [ID] => 47811 [post_author] => 129 [post_date] => 2022-05-04 16:26:13 [post_date_gmt] => 2022-05-04 14:26:13 [post_content] => Photograph by Nadine Hollmann © All Rights Reserved [post_title] => Screenshot 2022-05-04 at 16.26.00 [post_excerpt] => Desulfurization of the total lipid extracts of the sediments. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => screenshot-2022-05-04-at-16-26-00 [to_ping] => [pinged] => [post_modified] => 2022-05-04 16:32:26 [post_modified_gmt] => 2022-05-04 14:32:26 [post_content_filtered] => [post_parent] => 47807 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/Screenshot-2022-05-04-at-16.26.00.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [477] => Array ( [ID] => 47810 [post_author] => 129 [post_date] => 2022-05-04 16:25:02 [post_date_gmt] => 2022-05-04 14:25:02 [post_content] => Photograph by Nadine Hollmann © All Rights Reserved [post_title] => Screenshot 2022-05-04 at 16.24.48 [post_excerpt] => Desulfurization of the total lipid extracts of the sediments. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => screenshot-2022-05-04-at-16-24-48 [to_ping] => [pinged] => [post_modified] => 2022-05-04 16:26:27 [post_modified_gmt] => 2022-05-04 14:26:27 [post_content_filtered] => [post_parent] => 47807 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/Screenshot-2022-05-04-at-16.24.48.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [478] => Array ( [ID] => 47808 [post_author] => 129 [post_date] => 2022-05-04 16:19:10 [post_date_gmt] => 2022-05-04 14:19:10 [post_content] => [post_title] => egb swatch [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => screenshot-2022-05-04-at-16-18-59 [to_ping] => [pinged] => [post_modified] => 2022-05-17 11:00:41 [post_modified_gmt] => 2022-05-17 09:00:41 [post_content_filtered] => [post_parent] => 47807 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/Screenshot-2022-05-04-at-16.18.59.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [479] => Array ( [ID] => 47806 [post_author] => 12 [post_date] => 2022-05-04 16:15:41 [post_date_gmt] => 2022-05-04 14:15:41 [post_content] => Image by Sarah Roberts © All Rights Reserved [post_title] => 3_SCP [post_excerpt] => SCP analysis of the Śnieżka Peatland core. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 3_scp [to_ping] => [pinged] => [post_modified] => 2022-05-04 17:05:08 [post_modified_gmt] => 2022-05-04 15:05:08 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/3_SCP.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [480] => Array ( [ID] => 47805 [post_author] => 129 [post_date] => 2022-05-04 16:14:10 [post_date_gmt] => 2022-05-04 14:14:10 [post_content] =>
Image courtesy Leibniz Institute for Baltic Sea Research
Warnemünde (IOW) © All Rights Reserved [post_title] => 1_depthmap [post_excerpt] => Map showing depths of the Baltic Sea. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 1_depthmap [to_ping] => [pinged] => [post_modified] => 2022-05-06 10:39:19 [post_modified_gmt] => 2022-05-06 08:39:19 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/1_depthmap.jpeg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [481] => Array ( [ID] => 47804 [post_author] => 129 [post_date] => 2022-05-04 16:14:09 [post_date_gmt] => 2022-05-04 14:14:09 [post_content] => Photograph by Jerome Kaiser © All Rights Reserved [post_title] => 3_core [post_excerpt] => The East Gotland Basin Core. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 3_core-5 [to_ping] => [pinged] => [post_modified] => 2022-05-06 10:47:46 [post_modified_gmt] => 2022-05-06 08:47:46 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/3_core-2.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [482] => Array ( [ID] => 47803 [post_author] => 129 [post_date] => 2022-05-04 16:14:05 [post_date_gmt] => 2022-05-04 14:14:05 [post_content] =>
Image by Alf van Beem,
Wikimedia Commons
CC BY-SA 1.0 AT [post_title] => 3_DDT [post_excerpt] => Discontinued Dutch DDT
product. The text translates
as "DDT Pump Sprayer with
Pyrethrum". [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 3_ddt [to_ping] => [pinged] => [post_modified] => 2022-05-06 11:00:23 [post_modified_gmt] => 2022-05-06 09:00:23 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/3_DDT.jpeg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [483] => Array ( [ID] => 47802 [post_author] => 129 [post_date] => 2022-05-04 16:14:04 [post_date_gmt] => 2022-05-04 14:14:04 [post_content] => Video by Patricia Roeser © All Rights Reserved [post_title] => 4_coring1 [post_excerpt] => Lowering the corer into the water. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 4_coring1 [to_ping] => [pinged] => [post_modified] => 2022-05-04 16:16:13 [post_modified_gmt] => 2022-05-04 14:16:13 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/4_coring1.m4v [menu_order] => 0 [post_type] => attachment [post_mime_type] => video/mp4 [comment_count] => 0 [filter] => raw ) [484] => Array ( [ID] => 47801 [post_author] => 129 [post_date] => 2022-05-04 16:13:19 [post_date_gmt] => 2022-05-04 14:13:19 [post_content] => Video by Patricia Roeser © All Rights Reserved [post_title] => 4_coring2 [post_excerpt] => Retrieving the corer from the water. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 4_coring2 [to_ping] => [pinged] => [post_modified] => 2022-05-04 16:16:04 [post_modified_gmt] => 2022-05-04 14:16:04 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/4_coring2.m4v [menu_order] => 0 [post_type] => attachment [post_mime_type] => video/mp4 [comment_count] => 0 [filter] => raw ) [485] => Array ( [ID] => 47799 [post_author] => 129 [post_date] => 2022-05-04 16:13:03 [post_date_gmt] => 2022-05-04 14:13:03 [post_content] => [post_title] => crawford swatch2 [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => screenshot-2022-05-04-at-16-12-41 [to_ping] => [pinged] => [post_modified] => 2022-05-17 11:01:16 [post_modified_gmt] => 2022-05-17 09:01:16 [post_content_filtered] => [post_parent] => 47742 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/Screenshot-2022-05-04-at-16.12.41.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [486] => Array ( [ID] => 47798 [post_author] => 129 [post_date] => 2022-05-04 16:12:23 [post_date_gmt] => 2022-05-04 14:12:23 [post_content] => Photograph by Iris Liskow © All Rights Reserved [post_title] => 4_labIRMS_4 [post_excerpt] => Press to pack the samples in tin foil into pellets for the elemental analyzer. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 4_labirms_4 [to_ping] => [pinged] => [post_modified] => 2022-05-04 16:32:28 [post_modified_gmt] => 2022-05-04 14:32:28 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/4_labIRMS_4.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [487] => Array ( [ID] => 47797 [post_author] => 129 [post_date] => 2022-05-04 16:12:19 [post_date_gmt] => 2022-05-04 14:12:19 [post_content] =>
Photograph by NASA's Goddard Space Flight Center/USGS,
Wikimedia Commons, public domain [post_title] => 1_algal [post_excerpt] => Satellite image of algal blooms around Gotland Island in the Baltic Sea.
Such blooms are fed by runoff of agricultural fertilizers from land. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 1_algal [to_ping] => [pinged] => [post_modified] => 2022-05-06 10:51:45 [post_modified_gmt] => 2022-05-06 08:51:45 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/1_algal.jpeg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [488] => Array ( [ID] => 47796 [post_author] => 129 [post_date] => 2022-05-04 16:12:13 [post_date_gmt] => 2022-05-04 14:12:13 [post_content] => Image by European Space Agency, Wikimedia Commons, public domain [post_title] => 1_algal2 [post_excerpt] => Satellite image of algal blooms around Gotland Island in the Baltic Sea. Such blooms are fed by runoff of agricultural fertilizers from land. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 1_algal2 [to_ping] => [pinged] => [post_modified] => 2022-05-05 14:39:19 [post_modified_gmt] => 2022-05-05 12:39:19 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/1_algal2.jpeg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [489] => Array ( [ID] => 47795 [post_author] => 129 [post_date] => 2022-05-04 16:11:58 [post_date_gmt] => 2022-05-04 14:11:58 [post_content] =>
Image by NormanEinstein, Wikimedia Commons, CC BY-SA 3.0 AT [post_title] => 1_map [post_excerpt] => Map of the Baltic Sea showing the nations that surround it. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 1_map-4 [to_ping] => [pinged] => [post_modified] => 2022-05-06 10:54:27 [post_modified_gmt] => 2022-05-06 08:54:27 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/1_map-2.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [490] => Array ( [ID] => 47794 [post_author] => 129 [post_date] => 2022-05-04 16:11:57 [post_date_gmt] => 2022-05-04 14:11:57 [post_content] => Image by Jerome Kaiser © All Rights Reserved [post_title] => 2_MBIs [post_excerpt] => Figure showing the years and intensity of Major Baltic Inflows. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 2_mbis [to_ping] => [pinged] => [post_modified] => 2022-05-04 16:14:59 [post_modified_gmt] => 2022-05-04 14:14:59 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/2_MBIs.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [491] => Array ( [ID] => 47793 [post_author] => 129 [post_date] => 2022-05-04 16:11:55 [post_date_gmt] => 2022-05-04 14:11:55 [post_content] =>
Image by Jerome Kaiser © All Rights Reserved [post_title] => 3_core labelled [post_excerpt] => The East Gotland Basin Core with significant time markers labelled. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 3_core-labelled [to_ping] => [pinged] => [post_modified] => 2022-05-06 10:52:30 [post_modified_gmt] => 2022-05-06 08:52:30 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/3_core-labelled.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [492] => Array ( [ID] => 47792 [post_author] => 129 [post_date] => 2022-05-04 16:11:46 [post_date_gmt] => 2022-05-04 14:11:46 [post_content] => Photograph by Jerome Kaiser © All Rights Reserved [post_title] => 5_Juliana & Jerome 1 [post_excerpt] => Juliana Ivar do Sul and Jerome Kaiser (PIs of the East Gotland Basin team) with a model of the Elisabeth Mann Borgese, the research vessel used to collect the GSSP-candidate core. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 5_juliana-jerome-1 [to_ping] => [pinged] => [post_modified] => 2022-05-04 16:33:46 [post_modified_gmt] => 2022-05-04 14:33:46 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/5_Juliana-Jerome-1.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [493] => Array ( [ID] => 47791 [post_author] => 129 [post_date] => 2022-05-04 16:11:39 [post_date_gmt] => 2022-05-04 14:11:39 [post_content] =>
Image by Jerome Kaiser © All Rights Reserved [post_title] => 2_core location [post_excerpt] => Map of the East Gotland Basin with sediment sampling stations marked
and GSSP-candidate core EMB201/7-4 circled. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 2_core-location [to_ping] => [pinged] => [post_modified] => 2022-05-10 10:45:23 [post_modified_gmt] => 2022-05-10 08:45:23 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/2_core-location.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [494] => Array ( [ID] => 47790 [post_author] => 12 [post_date] => 2022-05-04 16:09:20 [post_date_gmt] => 2022-05-04 14:09:20 [post_content] => Photograph by Barbara Fiałkiewicz-Kozieł © All Rights Reserved [post_title] => 5_team2810 [post_excerpt] => From left to right: Edyta Łokas, Barbara Fiałkiewicz-Kozieł, and Beata Smieja-Król. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 5_team2810 [to_ping] => [pinged] => [post_modified] => 2022-05-11 09:51:01 [post_modified_gmt] => 2022-05-11 07:51:01 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/5_team2810.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [495] => Array ( [ID] => 47789 [post_author] => 12 [post_date] => 2022-05-04 16:08:45 [post_date_gmt] => 2022-05-04 14:08:45 [post_content] => Photograph by Barbara Fiałkiewicz-Kozieł © All Rights Reserved [post_title] => 5_team2608 [post_excerpt] => From left to right: Edyta Łokas, Beata Smieja-Król, Paweł Wąsowicz, Mariusz Gałka, Barbara Fiałkiewicz-Kozieł, and Krzysztof Kozieł (coring manager). [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 5_team2608 [to_ping] => [pinged] => [post_modified] => 2022-05-11 09:51:07 [post_modified_gmt] => 2022-05-11 07:51:07 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/5_team2608.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [496] => Array ( [ID] => 47788 [post_author] => 12 [post_date] => 2022-05-04 16:08:22 [post_date_gmt] => 2022-05-04 14:08:22 [post_content] => Photograph by Edyta Łokas © All Rights Reserved [post_title] => 4_lab4 [post_excerpt] => Separating plutonium from the samples. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 4_lab4 [to_ping] => [pinged] => [post_modified] => 2022-05-04 17:08:50 [post_modified_gmt] => 2022-05-04 15:08:50 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/4_lab4.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [497] => Array ( [ID] => 47787 [post_author] => 12 [post_date] => 2022-05-04 16:08:09 [post_date_gmt] => 2022-05-04 14:08:09 [post_content] => Photograph by Edyta Łokas © All Rights Reserved [post_title] => 4_lab3 [post_excerpt] => Plutonium spectra. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 4_lab3 [to_ping] => [pinged] => [post_modified] => 2022-05-04 16:14:20 [post_modified_gmt] => 2022-05-04 14:14:20 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/4_lab3.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [498] => Array ( [ID] => 47786 [post_author] => 12 [post_date] => 2022-05-04 16:07:57 [post_date_gmt] => 2022-05-04 14:07:57 [post_content] => Photograph by Adrian Sitarz © All Rights Reserved [post_title] => 4_lab2 [post_excerpt] => Samples of the core ready for analysis. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 4_lab2-2 [to_ping] => [pinged] => [post_modified] => 2022-05-04 16:14:33 [post_modified_gmt] => 2022-05-04 14:14:33 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/4_lab2.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [499] => Array ( [ID] => 47785 [post_author] => 12 [post_date] => 2022-05-04 16:07:42 [post_date_gmt] => 2022-05-04 14:07:42 [post_content] =>
Photograph by Adrian Sitarz © All Rights Reserved [post_title] => 4_lab [post_excerpt] => Precise sampling of the core for analyses. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 4_lab-2 [to_ping] => [pinged] => [post_modified] => 2022-05-06 10:37:19 [post_modified_gmt] => 2022-05-06 08:37:19 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/4_lab-1.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [500] => Array ( [ID] => 47784 [post_author] => 12 [post_date] => 2022-05-04 16:07:25 [post_date_gmt] => 2022-05-04 14:07:25 [post_content] => Photograph by Beata Smieja-Król © All Rights Reserved [post_title] => [post_excerpt] => PI Barbara Fiałkiewicz-Kozieł with the corer. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => sony-dsc-4 [to_ping] => [pinged] => [post_modified] => 2022-05-09 14:52:55 [post_modified_gmt] => 2022-05-09 12:52:55 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/4_coring2.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [501] => Array ( [ID] => 47783 [post_author] => 12 [post_date] => 2022-05-04 16:07:18 [post_date_gmt] => 2022-05-04 14:07:18 [post_content] => [post_title] => 4_coring1convertX [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 4_coring1convertx [to_ping] => [pinged] => [post_modified] => 2022-05-04 16:07:18 [post_modified_gmt] => 2022-05-04 14:07:18 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/4_coring1convertX.m4v [menu_order] => 0 [post_type] => attachment [post_mime_type] => video/mp4 [comment_count] => 0 [filter] => raw ) [502] => Array ( [ID] => 47781 [post_author] => 12 [post_date] => 2022-05-04 16:06:39 [post_date_gmt] => 2022-05-04 14:06:39 [post_content] => Image by Barbara Fiałkiewicz-Kozieł © All Rights Reserved [post_title] => 3_SAP [post_excerpt] => Patterns of distribution of Pb and selected indicators of dust (Ti, Sc, Al, and rare earth elements) in Sn1. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 3_sap [to_ping] => [pinged] => [post_modified] => 2022-05-04 16:16:25 [post_modified_gmt] => 2022-05-04 14:16:25 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/3_SAP.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [503] => Array ( [ID] => 47779 [post_author] => 12 [post_date] => 2022-05-04 16:06:31 [post_date_gmt] => 2022-05-04 14:06:31 [post_content] => Image by Barbara Fiałkiewicz-Kozieł, Edyta Łokas, and Tomasz Mróz © All Rights Reserved [post_title] => 3_CsPu2 [post_excerpt] => Comparison of 137Cs and 239+240Pu activity with 210Pb activity for core SN0. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 3_cspu2 [to_ping] => [pinged] => [post_modified] => 2022-05-04 16:16:37 [post_modified_gmt] => 2022-05-04 14:16:37 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/3_CsPu2.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [504] => Array ( [ID] => 47778 [post_author] => 12 [post_date] => 2022-05-04 16:06:24 [post_date_gmt] => 2022-05-04 14:06:24 [post_content] => Image by Barbara Fiałkiewicz-Kozieł and Edyta Łokas © All Rights Reserved [post_title] => 3_CsPu [post_excerpt] => Comparison of 137Cs and 239+240Pu activity with CRS model based on 210Pb for core SN1. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 3_cspu [to_ping] => [pinged] => [post_modified] => 2022-05-04 16:16:53 [post_modified_gmt] => 2022-05-04 14:16:53 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/3_CsPu.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [505] => Array ( [ID] => 47777 [post_author] => 12 [post_date] => 2022-05-04 16:06:14 [post_date_gmt] => 2022-05-04 14:06:14 [post_content] => Photograph by Barbara Fiałkiewicz-Kozieł © All Rights Reserved [post_title] => 3_core2 [post_excerpt] => The peat core in the lab. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 3_core2-3 [to_ping] => [pinged] => [post_modified] => 2022-05-04 16:48:07 [post_modified_gmt] => 2022-05-04 14:48:07 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/3_core2-1.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [506] => Array ( [ID] => 47776 [post_author] => 12 [post_date] => 2022-05-04 16:06:00 [post_date_gmt] => 2022-05-04 14:06:00 [post_content] => Photograph by Barbara Fiałkiewicz-Kozieł © All Rights Reserved [post_title] => 3_core1 [post_excerpt] => The peat core in the lab. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 3_core1 [to_ping] => [pinged] => [post_modified] => 2022-05-06 10:36:25 [post_modified_gmt] => 2022-05-06 08:36:25 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/3_core1.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [507] => Array ( [ID] => 47775 [post_author] => 12 [post_date] => 2022-05-04 16:05:46 [post_date_gmt] => 2022-05-04 14:05:46 [post_content] =>
Photograph by Marek Dobrowolski
© All Rights Reserved [post_title] => 3_core [post_excerpt] => The peat core in the corer on site. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 3_core-4 [to_ping] => [pinged] => [post_modified] => 2022-05-09 10:47:20 [post_modified_gmt] => 2022-05-09 08:47:20 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/3_core.jpeg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [508] => Array ( [ID] => 47774 [post_author] => 12 [post_date] => 2022-05-04 16:05:22 [post_date_gmt] => 2022-05-04 14:05:22 [post_content] =>
Photograph by Adrian Sitarz © All Rights Reserved [post_title] => 2_spagnum [post_excerpt] => Sphagnum moss from the core. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 2_spagnum [to_ping] => [pinged] => [post_modified] => 2022-05-06 10:33:49 [post_modified_gmt] => 2022-05-06 08:33:49 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/2_spagnum.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [509] => Array ( [ID] => 47773 [post_author] => 12 [post_date] => 2022-05-04 16:05:08 [post_date_gmt] => 2022-05-04 14:05:08 [post_content] => Photograph by Marek Król © All Rights Reserved [post_title] => [post_excerpt] => Równia pod Śnieżka, a rain-fed, sphagnum-moss peatland on a high plateau to the west of Śnieżka peak. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => sony-dsc-3 [to_ping] => [pinged] => [post_modified] => 2022-05-09 14:54:39 [post_modified_gmt] => 2022-05-09 12:54:39 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/2_site2.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [510] => Array ( [ID] => 47772 [post_author] => 12 [post_date] => 2022-05-04 16:04:43 [post_date_gmt] => 2022-05-04 14:04:43 [post_content] => Photograph by Marek Król © All Rights Reserved [post_title] => 2_site [post_excerpt] => Równia pod Śnieżka, a rain-fed, sphagnum-moss peatland on a high plateau to the west of Śnieżka peak. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 2_site [to_ping] => [pinged] => [post_modified] => 2022-05-09 14:54:29 [post_modified_gmt] => 2022-05-09 12:54:29 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/2_site.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [511] => Array ( [ID] => 47771 [post_author] => 12 [post_date] => 2022-05-04 16:04:25 [post_date_gmt] => 2022-05-04 14:04:25 [post_content] => Photograph by Marek Król © All Rights Reserved [post_title] => [post_excerpt] => View during walk to Śnieżka peak. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => sony-dsc-2 [to_ping] => [pinged] => [post_modified] => 2022-05-04 16:12:37 [post_modified_gmt] => 2022-05-04 14:12:37 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/1_site2.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [512] => Array ( [ID] => 47770 [post_author] => 12 [post_date] => 2022-05-04 16:04:06 [post_date_gmt] => 2022-05-04 14:04:06 [post_content] => Photograph by Pudulek, Wikimedia Commons [post_title] => 1_site [post_excerpt] => Śnieżka Mountain, the highest peak in the Sudetes range at 1,603 m. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 1_site [to_ping] => [pinged] => [post_modified] => 2022-05-09 14:42:05 [post_modified_gmt] => 2022-05-09 12:42:05 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/1_site.jpeg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [513] => Array ( [ID] => 47769 [post_author] => 12 [post_date] => 2022-05-04 16:03:54 [post_date_gmt] => 2022-05-04 14:03:54 [post_content] => Photograph by Petr Vodička, Wikimedia Commons [post_title] => DCIM100MEDIADJI_0012.JPG [post_excerpt] => Turów coal mine and power station, Poland. The "Black Triangle" area has had a long history of extraction and industry. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => dcim100mediadji_0012-jpg [to_ping] => [pinged] => [post_modified] => 2022-05-09 14:51:00 [post_modified_gmt] => 2022-05-09 12:51:00 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/1_mine.jpeg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [514] => Array ( [ID] => 47766 [post_author] => 12 [post_date] => 2022-05-04 16:03:29 [post_date_gmt] => 2022-05-04 14:03:29 [post_content] => Image by Tomasz Majtyka, Wikimedia Commons, CC BY-SA 3.0 [post_title] => 1_map [post_excerpt] => Map showing three peaks of the eastern Sudetes. The light gray lines are national borders and the hatched patches are cities, with Dresden (Germany) top left, Wrocław (Poland) top right, and Prague (Czech Republic) bottom left. This region between the three nations was dubbed the "Black Triangle" in the 1980s due to high levels of industrial pollution. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 1_map-3 [to_ping] => [pinged] => [post_modified] => 2022-05-04 16:43:18 [post_modified_gmt] => 2022-05-04 14:43:18 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/1_map-1.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [515] => Array ( [ID] => 47763 [post_author] => 129 [post_date] => 2022-05-04 15:53:24 [post_date_gmt] => 2022-05-04 13:53:24 [post_content] => Image by Sarah Roberts © All Rights Reserved [post_title] => Screenshot 2022-05-04 at 15.53.07 [post_excerpt] => SCP analysis of the Crawford Lake core. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => screenshot-2022-05-04-at-15-53-07 [to_ping] => [pinged] => [post_modified] => 2022-05-04 16:01:54 [post_modified_gmt] => 2022-05-04 14:01:54 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/Screenshot-2022-05-04-at-15.53.07.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [516] => Array ( [ID] => 47761 [post_author] => 129 [post_date] => 2022-05-04 15:45:45 [post_date_gmt] => 2022-05-04 13:45:45 [post_content] => Image by Alex Laney, Wikimedia Commons CC BY-SA 3.0 AT [post_title] => 1_Lake5 [post_excerpt] => Crawford Lake with partial ice cover. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 1_lake5 [to_ping] => [pinged] => [post_modified] => 2022-05-04 15:55:57 [post_modified_gmt] => 2022-05-04 13:55:57 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/1_Lake5.jpeg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [518] => Array ( [ID] => 47760 [post_author] => 129 [post_date] => 2022-05-04 15:45:42 [post_date_gmt] => 2022-05-04 13:45:42 [post_content] =>
Image by Tim Patterson © All Rights Reserved [post_title] => 3_core section [post_excerpt] => Section of a core from Crawford Lake. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 3_core-section [to_ping] => [pinged] => [post_modified] => 2022-05-09 16:23:22 [post_modified_gmt] => 2022-05-09 14:23:22 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/3_core-section.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [519] => Array ( [ID] => 47757 [post_author] => 129 [post_date] => 2022-05-04 15:45:16 [post_date_gmt] => 2022-05-04 13:45:16 [post_content] => Photograph courtesy Conservation Halton © All Rights Reserved [post_title] => 1_Lake3 [post_excerpt] => Crawford Lake in summer. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 1_lake3 [to_ping] => [pinged] => [post_modified] => 2022-05-04 15:53:55 [post_modified_gmt] => 2022-05-04 13:53:55 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/1_Lake3.jpeg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [520] => Array ( [ID] => 47756 [post_author] => 129 [post_date] => 2022-05-04 15:45:06 [post_date_gmt] => 2022-05-04 13:45:06 [post_content] => Photograph courtesy Conservation Halton © All Rights Reserved [post_title] => 1_Lake2 [post_excerpt] => Trees by Crawford Lake in summer. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 1_lake2 [to_ping] => [pinged] => [post_modified] => 2022-05-04 15:54:11 [post_modified_gmt] => 2022-05-04 13:54:11 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/1_Lake2.jpeg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [521] => Array ( [ID] => 47755 [post_author] => 129 [post_date] => 2022-05-04 15:44:52 [post_date_gmt] => 2022-05-04 13:44:52 [post_content] => Photograph courtesy Conservation Halton © All Rights Reserved [post_title] => 1_Lake [post_excerpt] => Crawford Lake. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 1_lake [to_ping] => [pinged] => [post_modified] => 2022-08-12 12:03:59 [post_modified_gmt] => 2022-08-12 10:03:59 [post_content_filtered] => [post_parent] => 49459 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/1_Lake.jpeg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [522] => Array ( [ID] => 47754 [post_author] => 129 [post_date] => 2022-05-04 15:44:40 [post_date_gmt] => 2022-05-04 13:44:40 [post_content] => Image by Francine McCarthy © All Rights Reserved [post_title] => 2_Layers [post_excerpt] => Meromictic layers of Crawford Lake. Higher density below the chemocline prevents mixing of the monimolimnion with the overlying mixolimnion. Oxygenated groundwater feeds the monimolimnion. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 2_layers [to_ping] => [pinged] => [post_modified] => 2022-05-04 16:00:23 [post_modified_gmt] => 2022-05-04 14:00:23 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/2_Layers.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [523] => Array ( [ID] => 47753 [post_author] => 129 [post_date] => 2022-05-04 15:44:37 [post_date_gmt] => 2022-05-04 13:44:37 [post_content] => Image by Laslovarga, Wikimedia Commons CC BY-SA 3.0 AT [post_title] => 1_Lake4 [post_excerpt] => Crawford Lake in Winter [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 1_lake4 [to_ping] => [pinged] => [post_modified] => 2022-05-04 15:55:33 [post_modified_gmt] => 2022-05-04 13:55:33 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/1_Lake4.jpeg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [524] => Array ( [ID] => 47751 [post_author] => 129 [post_date] => 2022-05-04 15:44:36 [post_date_gmt] => 2022-05-04 13:44:36 [post_content] => Photograph courtesy Conservation Halton © All Rights Reserved [post_title] => 3_Mill [post_excerpt] => Crawford Lake sawmill in 1885. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 3_mill [to_ping] => [pinged] => [post_modified] => 2022-05-04 16:01:17 [post_modified_gmt] => 2022-05-04 14:01:17 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/3_Mill.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [525] => Array ( [ID] => 47752 [post_author] => 129 [post_date] => 2022-05-04 15:44:36 [post_date_gmt] => 2022-05-04 13:44:36 [post_content] =>
Image by Tim Patterson
© All Rights Reserved [post_title] => 3_DatedCore [post_excerpt] => Section of the Crawford Lake core
with annual layers and significant
events labelled. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 3_datedcore [to_ping] => [pinged] => [post_modified] => 2022-05-09 16:23:12 [post_modified_gmt] => 2022-05-09 14:23:12 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/3_DatedCore.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [526] => Array ( [ID] => 47749 [post_author] => 129 [post_date] => 2022-05-04 15:44:31 [post_date_gmt] => 2022-05-04 13:44:31 [post_content] => Photograph by Brenna Bartley, courtesy Conservation Halton © All Rights Reserved [post_title] => 5_team [post_excerpt] => Members of the Crawford Lake team working on the lake, with PI Francine McCarthy and Martin Head (previous Chair of the Subcommission on the Quaternary) looking on. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 5_team-3 [to_ping] => [pinged] => [post_modified] => 2022-05-04 16:02:32 [post_modified_gmt] => 2022-05-04 14:02:32 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/5_team.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [527] => Array ( [ID] => 47748 [post_author] => 129 [post_date] => 2022-05-04 15:42:24 [post_date_gmt] => 2022-05-04 13:42:24 [post_content] => [post_title] => crawford swatch [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => screenshot-2022-05-04-at-15-41-50 [to_ping] => [pinged] => [post_modified] => 2022-05-04 15:42:41 [post_modified_gmt] => 2022-05-04 13:42:41 [post_content_filtered] => [post_parent] => 47742 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/Screenshot-2022-05-04-at-15.41.50.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [528] => Array ( [ID] => 47747 [post_author] => 129 [post_date] => 2022-05-04 15:42:04 [post_date_gmt] => 2022-05-04 13:42:04 [post_content] => [post_title] => crawford swatch [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => screenshot-2022-05-04-at-15-41-40 [to_ping] => [pinged] => [post_modified] => 2022-05-04 15:43:10 [post_modified_gmt] => 2022-05-04 13:43:10 [post_content_filtered] => [post_parent] => 47742 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/Screenshot-2022-05-04-at-15.41.40.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [529] => Array ( [ID] => 47724 [post_author] => 12 [post_date] => 2022-05-04 14:39:13 [post_date_gmt] => 2022-05-04 12:39:13 [post_content] => [post_title] => 4_Running ICP-OES_2020convertedX [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 4_running-icp-oes_2020convertedx [to_ping] => [pinged] => [post_modified] => 2022-05-04 14:39:13 [post_modified_gmt] => 2022-05-04 12:39:13 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/4_Running-ICP-OES_2020convertedX.m4v [menu_order] => 0 [post_type] => attachment [post_mime_type] => video/mp4 [comment_count] => 0 [filter] => raw ) [530] => Array ( [ID] => 47722 [post_author] => 12 [post_date] => 2022-05-04 14:34:17 [post_date_gmt] => 2022-05-04 12:34:17 [post_content] => [post_title] => 4_Micro-millingconvertedX [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 4_micro-millingconvertedx [to_ping] => [pinged] => [post_modified] => 2022-05-04 14:34:17 [post_modified_gmt] => 2022-05-04 12:34:17 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/4_Micro-millingconvertedX.m4v [menu_order] => 0 [post_type] => attachment [post_mime_type] => video/mp4 [comment_count] => 0 [filter] => raw ) [531] => Array ( [ID] => 47715 [post_author] => 129 [post_date] => 2022-05-04 14:25:33 [post_date_gmt] => 2022-05-04 12:25:33 [post_content] => Photograph by Eri Furuichi and Akane Yamamoto © All Rights Reserved [post_title] => 4_Fish scale sample [post_excerpt] => Fish scale samples in the lab. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 4_fish-scale-sample [to_ping] => [pinged] => [post_modified] => 2022-05-04 14:25:48 [post_modified_gmt] => 2022-05-04 12:25:48 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/4_Fish-scale-sample.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [532] => Array ( [ID] => 47714 [post_author] => 129 [post_date] => 2022-05-04 14:25:32 [post_date_gmt] => 2022-05-04 12:25:32 [post_content] => Photograph by Eri Furuichi © All Rights Reserved [post_title] => 4_Taking photo of fish scale using microscope [post_excerpt] => Photographing a fish scale with a microscope. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 4_taking-photo-of-fish-scale-using-microscope [to_ping] => [pinged] => [post_modified] => 2022-05-04 14:26:53 [post_modified_gmt] => 2022-05-04 12:26:53 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/4_Taking-photo-of-fish-scale-using-microscope.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [533] => Array ( [ID] => 47713 [post_author] => 129 [post_date] => 2022-05-04 14:25:31 [post_date_gmt] => 2022-05-04 12:25:31 [post_content] => Photograph by Michinobu Kuwae © All Rights Reserved [post_title] => 4_Cleaning fish scales by dichloromethane [post_excerpt] => Cleaning fish scales in the lab using dichloromethane. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 4_cleaning-fish-scales-by-dichloromethane [to_ping] => [pinged] => [post_modified] => 2022-05-04 14:26:24 [post_modified_gmt] => 2022-05-04 12:26:24 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/4_Cleaning-fish-scales-by-dichloromethane.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [534] => Array ( [ID] => 47705 [post_author] => 129 [post_date] => 2022-05-04 14:13:08 [post_date_gmt] => 2022-05-04 12:13:08 [post_content] => Photograph by Kingfisher, Wikimedia Commons CC BY-SA 4.0 AT [post_title] => 1599px-Engraulis_japonicus_01 [post_excerpt] => Japanese anchovy (Engraulis japonicas), found in Beppu Bay. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 1599px-engraulis_japonicus_01 [to_ping] => [pinged] => [post_modified] => 2022-05-04 14:21:33 [post_modified_gmt] => 2022-05-04 12:21:33 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/1599px-Engraulis_japonicus_01.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [535] => Array ( [ID] => 47703 [post_author] => 129 [post_date] => 2022-05-04 14:12:17 [post_date_gmt] => 2022-05-04 12:12:17 [post_content] => Photograph by Dime Gontar, Wikimedia Commons, CC BY-SA 2.0 AT [post_title] => 1_Bay [post_excerpt] => Beppu Bay taken from Mount Tsurumi, Oita Prefecture, Japan. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 1_bay [to_ping] => [pinged] => [post_modified] => 2022-05-04 14:17:51 [post_modified_gmt] => 2022-05-04 12:17:51 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/1_Bay.jpeg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [536] => Array ( [ID] => 47702 [post_author] => 129 [post_date] => 2022-05-04 14:12:16 [post_date_gmt] => 2022-05-04 12:12:16 [post_content] => Photograph by Kingfisher, Wikimedia Commons CC BY-SA 4.0 AT [post_title] => 2_anchovy [post_excerpt] => Japanese anchovy (Engraulis japonicas), found in Beppu Bay. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 2_anchovy [to_ping] => [pinged] => [post_modified] => 2022-05-04 14:14:36 [post_modified_gmt] => 2022-05-04 12:14:36 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/2_anchovy.jpeg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [537] => Array ( [ID] => 47701 [post_author] => 129 [post_date] => 2022-05-04 14:12:12 [post_date_gmt] => 2022-05-04 12:12:12 [post_content] => Photograph by 大分帰省中, Wikimedia Commons, CC BY-SA 3.0 AT [post_title] => 3_Oitaindustry [post_excerpt] => Oita Industrial Area, Oita Pref., Japan [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 3_oitaindustry [to_ping] => [pinged] => [post_modified] => 2022-05-04 14:14:55 [post_modified_gmt] => 2022-05-04 12:14:55 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/3_Oitaindustry.jpeg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [538] => Array ( [ID] => 47700 [post_author] => 129 [post_date] => 2022-05-04 14:12:11 [post_date_gmt] => 2022-05-04 12:12:11 [post_content] => [post_title] => Beppu Bay GSSP research team member [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => beppu-bay-gssp-research-team-member [to_ping] => [pinged] => [post_modified] => 2022-05-04 14:12:11 [post_modified_gmt] => 2022-05-04 12:12:11 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/Beppu-Bay-GSSP-research-team-member.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [539] => Array ( [ID] => 47699 [post_author] => 129 [post_date] => 2022-05-04 14:12:08 [post_date_gmt] => 2022-05-04 12:12:08 [post_content] => Photograph by Masanobu Yamamoto © All Rights Reserved [post_title] => 5_team [post_excerpt] => The Beppu Bay research team, from left of the lower row: Dr. Tsuyoshi Haraguchi, Osaka City University, Dr. Michinobu Kuwae, Ehime University, Dr. Keiji Takemura, Kyoto University, Dr. Masanobu Yamamoto, Hokkaido University; from left of the middle row: Dr. Tomohisa Irino, Hokkaido University; Dr. Ken Ikehara, National Institute of Advanced Industrial Science and Technology, Dr. Hikaru Takahara, Kyoto Prefectural University; from left of the upper row: Dr. Akira Hayashida, Doshisha University, Dr. Keitaro Yamada Ritsumeikan University, Dr. Takayuki Ohmori, The university of Tokyo, Dr. Toshimichi Nakanishi, Museum of Natural and Environmental History, Shizuoka, Dr. Yoshiaki Suzuki, National Institute of Advanced Industrial Science and Technology. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 5_team-2 [to_ping] => [pinged] => [post_modified] => 2022-05-04 14:27:44 [post_modified_gmt] => 2022-05-04 12:27:44 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/5_team.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [540] => Array ( [ID] => 47698 [post_author] => 129 [post_date] => 2022-05-04 14:12:05 [post_date_gmt] => 2022-05-04 12:12:05 [post_content] => Image by Jun Inoue © All Rights Reserved [post_title] => 3_SCPs [post_excerpt] => Concentration of SCPs (a marker of air pollution from fossil fuel combustion) in the BG19 S1-5 core. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 3_scps [to_ping] => [pinged] => [post_modified] => 2022-05-04 14:22:58 [post_modified_gmt] => 2022-05-04 12:22:58 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/3_SCPs.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [541] => Array ( [ID] => 47697 [post_author] => 129 [post_date] => 2022-05-04 14:11:58 [post_date_gmt] => 2022-05-04 12:11:58 [post_content] =>
Image by Michinobu
Kuwae © All
Rights Reserved [post_title] => 3_core [post_excerpt] => The core. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 3_core-3 [to_ping] => [pinged] => [post_modified] => 2022-05-06 11:09:39 [post_modified_gmt] => 2022-05-06 09:09:39 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/3_core-1.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [542] => Array ( [ID] => 47696 [post_author] => 129 [post_date] => 2022-05-04 14:11:54 [post_date_gmt] => 2022-05-04 12:11:54 [post_content] => Image by Michinobu Kuwae © All Rights Reserved [post_title] => 3_cesium [post_excerpt] => Radioactivity spikes of cesium-137 in Beppu Bay sediments. The records track the fallout maximum of nuclear bomb tests in 1964 CE and the Fukushima nuclear power plant accident in 2011 CE. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 3_cesium [to_ping] => [pinged] => [post_modified] => 2022-05-04 14:16:07 [post_modified_gmt] => 2022-05-04 12:16:07 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/3_cesium.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [543] => Array ( [ID] => 47695 [post_author] => 129 [post_date] => 2022-05-04 14:11:52 [post_date_gmt] => 2022-05-04 12:11:52 [post_content] => Image by Tsuyoshi Haraguchi © All Rights Reserved [post_title] => 2_map2 [post_excerpt] => Topographic map of Beppu Bay basin and the surrounding land. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 2_map2 [to_ping] => [pinged] => [post_modified] => 2022-05-04 14:16:23 [post_modified_gmt] => 2022-05-04 12:16:23 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/2_map2.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [544] => Array ( [ID] => 47694 [post_author] => 129 [post_date] => 2022-05-04 14:11:49 [post_date_gmt] => 2022-05-04 12:11:49 [post_content] => Image by Tsuyoshi Haraguchi © All Rights Reserved [post_title] => 2_map1 [post_excerpt] => Topographic map of part of Beppu Bay basin, with the location of the GSSP-candidate core marked. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 2_map1 [to_ping] => [pinged] => [post_modified] => 2022-05-04 14:16:36 [post_modified_gmt] => 2022-05-04 12:16:36 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/2_map1.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [545] => Array ( [ID] => 47692 [post_author] => 129 [post_date] => 2022-05-04 14:09:33 [post_date_gmt] => 2022-05-04 12:09:33 [post_content] => [post_title] => beppu core swatch [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => screenshot-2022-05-04-at-14-09-14 [to_ping] => [pinged] => [post_modified] => 2022-05-17 11:05:34 [post_modified_gmt] => 2022-05-17 09:05:34 [post_content_filtered] => [post_parent] => 47691 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/Screenshot-2022-05-04-at-14.09.14.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [546] => Array ( [ID] => 47679 [post_author] => 12 [post_date] => 2022-05-04 12:02:17 [post_date_gmt] => 2022-05-04 10:02:17 [post_content] => Photograph by Irka Hajdas © All Rights Reserved [post_title] => 4_lab2 [post_excerpt] => Close up of the Mini Carbon Dating System (MICADAS) ion source at the ETH AMS facility, Zürich. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 4_lab2 [to_ping] => [pinged] => [post_modified] => 2022-05-04 12:15:48 [post_modified_gmt] => 2022-05-04 10:15:48 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/4_lab2.jpeg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [547] => Array ( [ID] => 47678 [post_author] => 12 [post_date] => 2022-05-04 12:01:59 [post_date_gmt] => 2022-05-04 10:01:59 [post_content] => Photograph by Kylie Palmer © All Rights Reserved [post_title] => 5_mudith [post_excerpt] => Mudith Weerabaddana microsampling the coral. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 5_mudith [to_ping] => [pinged] => [post_modified] => 2022-05-04 14:13:01 [post_modified_gmt] => 2022-05-04 12:13:01 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/5_mudith.jpeg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [548] => Array ( [ID] => 47674 [post_author] => 12 [post_date] => 2022-05-04 11:55:16 [post_date_gmt] => 2022-05-04 09:55:16 [post_content] => Photograph by Irka Hajdas © All Rights Reserved [post_title] => 4_lab1 [post_excerpt] => Overview of the AMS equipment at the ETH, Zürich. The Mini Carbon Dating System (MICADAS) is equipped with an Elemental Analyser (bottom, left) and a tube cracker (bottom, center) for a transfer of CO2 directly to the ion source (bottom, right) for 14C analysis. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 4_lab1 [to_ping] => [pinged] => [post_modified] => 2022-05-04 14:05:21 [post_modified_gmt] => 2022-05-04 12:05:21 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/4_lab1.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [549] => Array ( [ID] => 47673 [post_author] => 12 [post_date] => 2022-05-04 11:55:12 [post_date_gmt] => 2022-05-04 09:55:12 [post_content] => Photograph by Kristine DeLong © All Rights Reserved [post_title] => 4_lab microscope [post_excerpt] => Microscope image of the core slab after micromilling for samples. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 4_lab-microscope [to_ping] => [pinged] => [post_modified] => 2022-05-04 12:43:52 [post_modified_gmt] => 2022-05-04 10:43:52 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/4_lab-microscope.bmp [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/bmp [comment_count] => 0 [filter] => raw ) [550] => Array ( [ID] => 47671 [post_author] => 12 [post_date] => 2022-05-04 11:39:45 [post_date_gmt] => 2022-05-04 09:39:45 [post_content] => Photograph by Kylie Palmer © All Rights Reserved [post_title] => 3_core3 [post_excerpt] => Coral core quarter sections of 05WFGB3-1-A awaiting analysis. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 3_core3 [to_ping] => [pinged] => [post_modified] => 2022-05-11 11:31:37 [post_modified_gmt] => 2022-05-11 09:31:37 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/3_core3.jpeg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [551] => Array ( [ID] => 47670 [post_author] => 12 [post_date] => 2022-05-04 11:39:39 [post_date_gmt] => 2022-05-04 09:39:39 [post_content] => Image by Mudith M. Weerabaddana,
Kristine L. DeLong, Amy J. Wagner, Deborah W.Y. Loke,
K. Halimeda Kilbourne, Niall Slowey, Hsun-Ming Hu,
and Chuan-Chou Shen,
https://doi.org/10.1016/j.marpolbul.2021.112930 [post_title] => 3_core2 [post_excerpt] => X-radiographs and scans of the S. siderea coral slabs.
Years are noted starting from the core top (2005) with
sampling paths locations. Scale bar is 50 mm with 10
mm intervals. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 3_core2-2 [to_ping] => [pinged] => [post_modified] => 2022-05-11 11:40:49 [post_modified_gmt] => 2022-05-11 09:40:49 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/3_core2.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [552] => Array ( [ID] => 47668 [post_author] => 12 [post_date] => 2022-05-04 11:39:26 [post_date_gmt] => 2022-05-04 09:39:26 [post_content] =>
Image by Mudith M. Weerabaddana, Kristine L. DeLong, Amy J. Wagner,
Deborah W.Y. Loke, K. Halimeda Kilbourne, Niall Slowey, Hsun-Ming Hu,
and Chuan-Chou Shen, https://doi.org/10.1016/j.marpolbul.2021.112930 [post_title] => 3_barite [post_excerpt] => Oil drilling using barite as a drilling mud that is left on the seafloor.
This barite may dissolve in seawater thus increasing the barium
concentration in seawater, which is recorded in corals. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 3_barite [to_ping] => [pinged] => [post_modified] => 2022-05-06 14:46:03 [post_modified_gmt] => 2022-05-06 12:46:03 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/3_barite.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [553] => Array ( [ID] => 47667 [post_author] => 12 [post_date] => 2022-05-04 11:39:12 [post_date_gmt] => 2022-05-04 09:39:12 [post_content] => Image by Mudith M. Weerabaddana, Kristine L. DeLong, Amy J. Wagner, Deborah W.Y. Loke, K. Halimeda Kilbourne, Niall Slowey, Hsun-Ming Hu, and Chuan-Chou Shen, https://doi.org/10.1016/j.marpolbul.2021.112930 [post_title] => 3_barite graph [post_excerpt] => Annual US barite production (black line) from 1900 to 2015 (Kelly and Matos, 2014) and annual minimum coral Ba/Ca (orange dashed line) plotted with adjustment for two-year lag (solid orange line). Coral Ba/Ca is converted to seawater barium concentration using the Porites equation (LaVigne et al., 2016). The coral Ba/Ca in the blue area follows the annual US barite production with a two- to three-year lag whereas in the grey area it does not. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 3_barite-graph [to_ping] => [pinged] => [post_modified] => 2022-05-04 14:21:38 [post_modified_gmt] => 2022-05-04 12:21:38 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/3_barite-graph.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [554] => Array ( [ID] => 47666 [post_author] => 12 [post_date] => 2022-05-04 11:39:03 [post_date_gmt] => 2022-05-04 09:39:03 [post_content] =>
Image courtesy NOAA, National Marine Sanctuaries, public domain [post_title] => 2_westbankmap [post_excerpt] => Bathymetric map showing depths of the West Flower Garden Bank. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 2_westbankmap [to_ping] => [pinged] => [post_modified] => 2022-05-11 11:41:38 [post_modified_gmt] => 2022-05-11 09:41:38 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/2_westbankmap.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [555] => Array ( [ID] => 47665 [post_author] => 12 [post_date] => 2022-05-04 11:38:43 [post_date_gmt] => 2022-05-04 09:38:43 [post_content] => Image by US Energy Information Administration, Wikimedia Commons, public domain [post_title] => 2_petroleum [post_excerpt] => Natural gas production in the Gulf of Mexico. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 2_petroleum [to_ping] => [pinged] => [post_modified] => 2022-05-06 14:38:21 [post_modified_gmt] => 2022-05-06 12:38:21 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/2_petroleum.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [556] => Array ( [ID] => 47664 [post_author] => 12 [post_date] => 2022-05-04 11:38:38 [post_date_gmt] => 2022-05-04 09:38:38 [post_content] => Photograph courtesy NOAA, Wikimedia Commons, public domain [post_title] => 2_coral [post_excerpt] => A siderastrea siderea (also known as the massive starlet coral or round starlet coral) in the Flower Garden Banks. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 2_coral [to_ping] => [pinged] => [post_modified] => 2022-05-11 11:33:14 [post_modified_gmt] => 2022-05-11 09:33:14 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/2_coral.jpeg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [557] => Array ( [ID] => 47663 [post_author] => 12 [post_date] => 2022-05-04 11:38:16 [post_date_gmt] => 2022-05-04 09:38:16 [post_content] =>
Image by Mudith M. Weerabaddana, Kristine L. DeLong, Amy J. Wagner, Deborah W.Y. Loke,
K. Halimeda Kilbourne, Niall Slowey, Hsun-Ming Hu, and Chuan-Chou Shen,
https://doi.org/10.1016/j.marpolbul.2021.112930
[post_title] => 2_colonymap [post_excerpt] => The S. siderea colony sampled is located on the north
side of WFGB at a water depth of 23.8 m (black dot). [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 2_colonymap [to_ping] => [pinged] => [post_modified] => 2022-05-06 14:37:28 [post_modified_gmt] => 2022-05-06 12:37:28 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/2_colonymap.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [558] => Array ( [ID] => 47662 [post_author] => 12 [post_date] => 2022-05-04 11:38:06 [post_date_gmt] => 2022-05-04 09:38:06 [post_content] => Photograph courtesy National Marine Sanctuaries, Wikimedia Commons, public domain [post_title] => 1_Stetson Bank [post_excerpt] => Fish and coral on Steson Bank, on of the seventeen reefs and banks protected as part of the Flower Garden Banks National Marine Sanctuary. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 1_stetson-bank [to_ping] => [pinged] => [post_modified] => 2022-05-05 14:45:25 [post_modified_gmt] => 2022-05-05 12:45:25 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/1_Stetson-Bank.jpeg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [559] => Array ( [ID] => 47661 [post_author] => 12 [post_date] => 2022-05-04 11:37:55 [post_date_gmt] => 2022-05-04 09:37:55 [post_content] => Image by National Marine Sanctuaries, public domain [post_title] => 1_sanctuarymap [post_excerpt] => The seventeen banks of the Flower Garden Banks National Marine Sanctuary. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 1_sanctuarymap [to_ping] => [pinged] => [post_modified] => 2022-05-11 11:43:44 [post_modified_gmt] => 2022-05-11 09:43:44 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/1_sanctuarymap.jpeg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [560] => Array ( [ID] => 47660 [post_author] => 12 [post_date] => 2022-05-04 11:37:50 [post_date_gmt] => 2022-05-04 09:37:50 [post_content] => Image by Shannon, Wikimedia Commons, public domain [post_title] => 1_map [post_excerpt] => Topographic map showing the West and East Flower Garden Banks and their position in the Gulf of Mexico. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 1_map-2 [to_ping] => [pinged] => [post_modified] => 2022-05-11 11:37:15 [post_modified_gmt] => 2022-05-11 09:37:15 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/1_map.jpeg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [562] => Array ( [ID] => 47658 [post_author] => 12 [post_date] => 2022-05-04 11:37:29 [post_date_gmt] => 2022-05-04 09:37:29 [post_content] => Photograph by Kristine DeLong © All Rights Reserved [post_title] => 1_coral [post_excerpt] => Coral photo taken during diving trip to Flower Garden Banks. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 1_coral [to_ping] => [pinged] => [post_modified] => 2022-08-12 11:27:53 [post_modified_gmt] => 2022-08-12 09:27:53 [post_content_filtered] => [post_parent] => 49468 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/1_coral.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [563] => Array ( [ID] => 47656 [post_author] => 12 [post_date] => 2022-05-04 11:35:44 [post_date_gmt] => 2022-05-04 09:35:44 [post_content] => [post_title] => west-flower [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => west-flower [to_ping] => [pinged] => [post_modified] => 2022-05-17 11:02:29 [post_modified_gmt] => 2022-05-17 09:02:29 [post_content_filtered] => [post_parent] => 47654 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/west-flower.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [564] => Array ( [ID] => 47652 [post_author] => 129 [post_date] => 2022-05-04 10:34:01 [post_date_gmt] => 2022-05-04 08:34:01 [post_content] => Image by Daniel Emanuelsson © All Rights Reserved [post_title] => 3_Palmernssso4age-scale [post_excerpt] => Age scale for the Palmer Core. Annual layer counting validated using known volcanic eruptions. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => screenshot-2022-05-04-at-10-33-33 [to_ping] => [pinged] => [post_modified] => 2022-05-04 10:34:47 [post_modified_gmt] => 2022-05-04 08:34:47 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/Screenshot-2022-05-04-at-10.33.33.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [565] => Array ( [ID] => 47651 [post_author] => 129 [post_date] => 2022-05-04 10:33:10 [post_date_gmt] => 2022-05-04 08:33:10 [post_content] => [post_title] => IMG_5205 [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => img_5205 [to_ping] => [pinged] => [post_modified] => 2022-05-04 10:33:10 [post_modified_gmt] => 2022-05-04 08:33:10 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/IMG_5205.mov [menu_order] => 0 [post_type] => attachment [post_mime_type] => video/quicktime [comment_count] => 0 [filter] => raw ) [566] => Array ( [ID] => 47650 [post_author] => 129 [post_date] => 2022-05-04 10:32:39 [post_date_gmt] => 2022-05-04 08:32:39 [post_content] => [post_title] => Antarctic Peninsula ice core drilling [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => antarctic-peninsula-ice-core-drilling [to_ping] => [pinged] => [post_modified] => 2022-05-04 10:32:39 [post_modified_gmt] => 2022-05-04 08:32:39 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/Antarctic-Peninsula-ice-core-drilling.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [567] => Array ( [ID] => 47649 [post_author] => 129 [post_date] => 2022-05-04 10:32:28 [post_date_gmt] => 2022-05-04 08:32:28 [post_content] => Photograph by Liz Thomas © All Rights Reserved [post_title] => 5_Team [post_excerpt] => The Palmer core research team. From left to right: Dr Dieter Tetzner, Dr Daniel Emanuelsson, Dr Jack Humby, Dr Liz Thomas, and Dr Diana Vladimirova. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 5_team [to_ping] => [pinged] => [post_modified] => 2022-05-04 10:42:30 [post_modified_gmt] => 2022-05-04 08:42:30 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/5_Team.jpeg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [568] => Array ( [ID] => 47648 [post_author] => 129 [post_date] => 2022-05-04 10:32:17 [post_date_gmt] => 2022-05-04 08:32:17 [post_content] => Photograph by Sarah Roberts © All Rights Reserved [post_title] => 4_Samples [post_excerpt] => Samples of the Palmer core bottled for SCP analysis. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 4_samples [to_ping] => [pinged] => [post_modified] => 2022-05-04 10:40:04 [post_modified_gmt] => 2022-05-04 08:40:04 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/4_Samples.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [569] => Array ( [ID] => 47647 [post_author] => 129 [post_date] => 2022-05-04 10:32:06 [post_date_gmt] => 2022-05-04 08:32:06 [post_content] => Photograph by Daniel Emanuelsson © All Rights Reserved [post_title] => 4_Lab [post_excerpt] => Samples being analyzed in the lab. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 4_lab [to_ping] => [pinged] => [post_modified] => 2022-05-04 10:39:51 [post_modified_gmt] => 2022-05-04 08:39:51 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/4_Lab.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [570] => Array ( [ID] => 47646 [post_author] => 129 [post_date] => 2022-05-04 10:32:02 [post_date_gmt] => 2022-05-04 08:32:02 [post_content] => Photograph by Liz Thomas © All Rights Reserved [post_title] => 4_Flying the ice cores from Antarctica [post_excerpt] => Ice core sections packaged and ready to be flown to the lab. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 4_flying-the-ice-cores-from-antarctica-2 [to_ping] => [pinged] => [post_modified] => 2022-05-04 10:39:18 [post_modified_gmt] => 2022-05-04 08:39:18 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/4_Flying-the-ice-cores-from-Antarctica.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [571] => Array ( [ID] => 47645 [post_author] => 129 [post_date] => 2022-05-04 10:31:54 [post_date_gmt] => 2022-05-04 08:31:54 [post_content] =>
Photograph by Liz Thomas © All Rights Reserved [post_title] => 4_drilling9a [post_excerpt] => Drilling the core and cutting it into 80-cm-long-sections on site. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 4_drilling9a [to_ping] => [pinged] => [post_modified] => 2022-05-09 11:26:08 [post_modified_gmt] => 2022-05-09 09:26:08 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/4_drilling9a.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [572] => Array ( [ID] => 47644 [post_author] => 129 [post_date] => 2022-05-04 10:31:43 [post_date_gmt] => 2022-05-04 08:31:43 [post_content] => Photograph by Liz Thomas © All Rights Reserved [post_title] => 4_drilling8 [post_excerpt] => Drilling the core and cutting it into 80-cm-long-sections on site. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 4_drilling8 [to_ping] => [pinged] => [post_modified] => 2022-05-04 10:38:36 [post_modified_gmt] => 2022-05-04 08:38:36 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/4_drilling8.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [573] => Array ( [ID] => 47643 [post_author] => 129 [post_date] => 2022-05-04 10:31:29 [post_date_gmt] => 2022-05-04 08:31:29 [post_content] => Photograph by Liz Thomas © All Rights Reserved [post_title] => 4_drilling7 [post_excerpt] => Drilling the core and cutting it into 80-cm-long-sections on site. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 4_drilling7 [to_ping] => [pinged] => [post_modified] => 2022-05-04 10:38:39 [post_modified_gmt] => 2022-05-04 08:38:39 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/4_drilling7.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [574] => Array ( [ID] => 47642 [post_author] => 129 [post_date] => 2022-05-04 10:31:18 [post_date_gmt] => 2022-05-04 08:31:18 [post_content] => Photograph by Liz Thomas © All Rights Reserved [post_title] => 4_drilling6 [post_excerpt] => Drilling the core and cutting it into 80-cm-long-sections on site. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 4_drilling6 [to_ping] => [pinged] => [post_modified] => 2022-05-04 10:38:41 [post_modified_gmt] => 2022-05-04 08:38:41 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/4_drilling6.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [575] => Array ( [ID] => 47641 [post_author] => 129 [post_date] => 2022-05-04 10:31:07 [post_date_gmt] => 2022-05-04 08:31:07 [post_content] => Photograph by Liz Thomas © All Rights Reserved [post_title] => 4_drilling5 [post_excerpt] => Drilling the core and cutting it into 80-cm-long-sections on site. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 4_drilling5 [to_ping] => [pinged] => [post_modified] => 2022-05-04 10:38:44 [post_modified_gmt] => 2022-05-04 08:38:44 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/4_drilling5.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [576] => Array ( [ID] => 47640 [post_author] => 129 [post_date] => 2022-05-04 10:30:57 [post_date_gmt] => 2022-05-04 08:30:57 [post_content] =>
Photograph by Liz Thomas © All Rights Reserved [post_title] => 4_drilling4 [post_excerpt] => Drilling the core and cutting it into 80-cm-long-sections on site. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 4_drilling4 [to_ping] => [pinged] => [post_modified] => 2022-05-09 11:32:35 [post_modified_gmt] => 2022-05-09 09:32:35 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/4_drilling4.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [577] => Array ( [ID] => 47639 [post_author] => 129 [post_date] => 2022-05-04 10:30:54 [post_date_gmt] => 2022-05-04 08:30:54 [post_content] =>
Photograph by Liz Thomas © All Rights Reserved [post_title] => 4_drilling3 [post_excerpt] => Drilling the core and cutting it into 80-cm-long-sections on site. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 4_drilling3 [to_ping] => [pinged] => [post_modified] => 2022-05-09 12:22:29 [post_modified_gmt] => 2022-05-09 10:22:29 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/4_drilling3.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [578] => Array ( [ID] => 47638 [post_author] => 129 [post_date] => 2022-05-04 10:30:44 [post_date_gmt] => 2022-05-04 08:30:44 [post_content] =>
Photograph by Liz Thomas © All Rights Reserved [post_title] => 4_drilling2 [post_excerpt] => Drilling the core and cutting it into 80-cm-long-sections on site. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 4_drilling2 [to_ping] => [pinged] => [post_modified] => 2022-05-09 12:23:17 [post_modified_gmt] => 2022-05-09 10:23:17 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/4_drilling2.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [579] => Array ( [ID] => 47637 [post_author] => 129 [post_date] => 2022-05-04 10:30:32 [post_date_gmt] => 2022-05-04 08:30:32 [post_content] =>
Photograph by Liz Thomas © All Rights Reserved [post_title] => 4_drilling1 [post_excerpt] => Drilling the core and cutting it into 80-cm-long-sections on site. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 4_drilling1 [to_ping] => [pinged] => [post_modified] => 2022-05-09 12:24:12 [post_modified_gmt] => 2022-05-09 10:24:12 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/4_drilling1.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [580] => Array ( [ID] => 47636 [post_author] => 129 [post_date] => 2022-05-04 10:30:28 [post_date_gmt] => 2022-05-04 08:30:28 [post_content] => Video by Liz Thomas © All Rights Reserved [post_title] => 4_CFA [post_excerpt] => The ice core being melted for continuous flow analysis. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 4_cfa [to_ping] => [pinged] => [post_modified] => 2022-05-04 10:37:35 [post_modified_gmt] => 2022-05-04 08:37:35 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/4_CFA.mov [menu_order] => 0 [post_type] => attachment [post_mime_type] => video/quicktime [comment_count] => 0 [filter] => raw ) [581] => Array ( [ID] => 47635 [post_author] => 129 [post_date] => 2022-05-04 10:27:36 [post_date_gmt] => 2022-05-04 08:27:36 [post_content] => Image by Daniel Emanuelsson © All Rights Reserved [post_title] => 4_CFA set-up [post_excerpt] => The continuous flow analysis set-up. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 4_cfa-set-up [to_ping] => [pinged] => [post_modified] => 2022-05-06 14:51:17 [post_modified_gmt] => 2022-05-06 12:51:17 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/4_CFA-set-up.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [582] => Array ( [ID] => 47634 [post_author] => 129 [post_date] => 2022-05-04 10:27:35 [post_date_gmt] => 2022-05-04 08:27:35 [post_content] => [post_title] => image description [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => image-description [to_ping] => [pinged] => [post_modified] => 2022-05-14 10:51:45 [post_modified_gmt] => 2022-05-14 08:51:45 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/3_Palmer-nssso4-age-scale.tif [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/tiff [comment_count] => 0 [filter] => raw ) [583] => Array ( [ID] => 47633 [post_author] => 129 [post_date] => 2022-05-04 10:27:11 [post_date_gmt] => 2022-05-04 08:27:11 [post_content] => Image by Daniel Emanuelsson © All Rights Reserved [post_title] => 3_Core2 [post_excerpt] => A scan of the Palmer ice core. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 3_core2 [to_ping] => [pinged] => [post_modified] => 2022-05-04 10:35:47 [post_modified_gmt] => 2022-05-04 08:35:47 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/3_Core2.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [584] => Array ( [ID] => 47632 [post_author] => 129 [post_date] => 2022-05-04 10:26:40 [post_date_gmt] => 2022-05-04 08:26:40 [post_content] => Photograph by Liz Thomas © All Rights Reserved [post_title] => 3_Core [post_excerpt] => A section of the Palmer ice core. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 3_core [to_ping] => [pinged] => [post_modified] => 2022-05-04 10:28:39 [post_modified_gmt] => 2022-05-04 08:28:39 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/3_Core.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [585] => Array ( [ID] => 47631 [post_author] => 129 [post_date] => 2022-05-04 10:26:38 [post_date_gmt] => 2022-05-04 08:26:38 [post_content] => Photograph by Liz Thomas © All Rights Reserved [post_title] => 2_Peninsula field camp [post_excerpt] => Field camp at the Palmer core collection site on the Antarctic Peninsula ice sheet. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 2_peninsula-field-camp [to_ping] => [pinged] => [post_modified] => 2022-05-04 10:28:22 [post_modified_gmt] => 2022-05-04 08:28:22 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/2_Peninsula-field-camp.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [586] => Array ( [ID] => 47630 [post_author] => 129 [post_date] => 2022-05-04 10:26:30 [post_date_gmt] => 2022-05-04 08:26:30 [post_content] => Photograph by Liz Thomas © All Rights Reserved [post_title] => 2_Antarctic field camp2 [post_excerpt] => Field camp at the Palmer core collection site on the Antarctic Peninsula ice sheet. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 2_antarctic-field-camp2-2 [to_ping] => [pinged] => [post_modified] => 2022-08-11 15:10:41 [post_modified_gmt] => 2022-08-11 13:10:41 [post_content_filtered] => [post_parent] => 49462 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/2_Antarctic-field-camp2-1.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [587] => Array ( [ID] => 47629 [post_author] => 129 [post_date] => 2022-05-04 10:26:19 [post_date_gmt] => 2022-05-04 08:26:19 [post_content] => Photograph by Liz Thomas © All Rights Reserved [post_title] => 2_Antarctic field camp [post_excerpt] => Field camp at the Palmer core collection site on the Antarctic Peninsula ice sheet. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 2_antarctic-field-camp [to_ping] => [pinged] => [post_modified] => 2022-05-04 10:27:45 [post_modified_gmt] => 2022-05-04 08:27:45 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/05/2_Antarctic-field-camp.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [588] => Array ( [ID] => 47628 [post_author] => 129 [post_date] => 2022-05-04 10:26:02 [post_date_gmt] => 2022-05-04 08:26:02 [post_content] => Image by Dave Pape, Wikimedia Commons, public domain [post_title] => 1_Satellite [post_excerpt] => Antarctica. An orthographic projection of NASA's Blue Marble data set (1 km resolution global satellite composite). 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https://www.anthropocene-curriculum.org/?post_type=event&p=47516 [menu_order] => 0 [post_type] => event [post_mime_type] => [comment_count] => 0 [filter] => raw ) [599] => Array ( [ID] => 47514 [post_author] => 103 [post_date] => 2022-04-26 15:29:47 [post_date_gmt] => 2022-04-26 13:29:47 [post_content] => [post_title] => siteguide_dummy [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => siteguide_dummy [to_ping] => [pinged] => [post_modified] => 2022-05-02 17:32:14 [post_modified_gmt] => 2022-05-02 15:32:14 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/siteguide_dummy.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [600] => Array ( [ID] => 47511 [post_author] => 105 [post_date] => 2022-04-26 13:09:29 [post_date_gmt] => 2022-04-26 11:09:29 [post_content] => 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2022-04-26 13:08:05 [post_date_gmt] => 2022-04-26 11:08:05 [post_content] => [post_title] => Screenshot 2022-04-26 at 13-06-34 Vimeo [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => screenshot-2022-04-26-at-13-06-34-vimeo [to_ping] => [pinged] => [post_modified] => 2022-04-26 13:08:05 [post_modified_gmt] => 2022-04-26 11:08:05 [post_content_filtered] => [post_parent] => 47489 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/Screenshot-2022-04-26-at-13-06-34-Vimeo.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [602] => Array ( [ID] => 47507 [post_author] => 105 [post_date] => 2022-04-26 13:07:42 [post_date_gmt] => 2022-04-26 11:07:42 [post_content] => [post_title] => Screenshot 2022-04-26 at 13-06-59 Vimeo [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed 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frame-7thick_re [to_ping] => [pinged] => [post_modified] => 2022-04-25 18:30:04 [post_modified_gmt] => 2022-04-25 16:30:04 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/Frame-7thick_re.svg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/svg+xml [comment_count] => 0 [filter] => raw ) [610] => Array ( [ID] => 47469 [post_author] => 103 [post_date] => 2022-04-25 18:24:03 [post_date_gmt] => 2022-04-25 16:24:03 [post_content] => [post_title] => Frame 1thick_re [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => frame-1thick_re [to_ping] => [pinged] => [post_modified] => 2022-04-25 18:24:03 [post_modified_gmt] => 2022-04-25 16:24:03 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/Frame-1thick_re.svg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/svg+xml [comment_count] => 0 [filter] => raw ) [611] => Array ( [ID] => 47443 [post_author] => 105 [post_date] => 2022-04-23 16:01:49 [post_date_gmt] => 2022-04-23 14:01:49 [post_content] => Photo by Alexandra van der Eijk © All rights reserved [post_title] => IMG_20200826_161318EDIT [post_excerpt] => Set of baseline tests, resulting in minimal verdigris effects. 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[post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => xandra-2-01 [to_ping] => [pinged] => [post_modified] => 2022-05-31 15:08:44 [post_modified_gmt] => 2022-05-31 13:08:44 [post_content_filtered] => [post_parent] => 47345 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2000/04/Xandra-2-01.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [614] => Array ( [ID] => 47440 [post_author] => 105 [post_date] => 2022-04-23 15:53:50 [post_date_gmt] => 2022-04-23 13:53:50 [post_content] => Alexandra van der Eijk © All rights reserved [post_title] => Rozelle-Blackwattle [post_excerpt] => Blackwattle Bay, 2022. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => rozelle-blackwattle [to_ping] => [pinged] => [post_modified] => 2022-05-31 15:08:31 [post_modified_gmt] => 2022-05-31 13:08:31 [post_content_filtered] => [post_parent] => 47345 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2000/04/Rozelle-Blackwattle.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [615] => Array ( [ID] => 47439 [post_author] => 105 [post_date] => 2022-04-23 15:48:21 [post_date_gmt] => 2022-04-23 13:48:21 [post_content] => Photo by Alexandra van der Eijk © All rights reserved [post_title] => BlackwattleBay2 [post_excerpt] => Blackwattle Bay, 2022. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => blackwattlebay2 [to_ping] => [pinged] => [post_modified] => 2022-05-31 15:07:57 [post_modified_gmt] => 2022-05-31 13:07:57 [post_content_filtered] => [post_parent] => 47345 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2000/04/BlackwattleBay2.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [616] => Array ( [ID] => 47438 [post_author] => 105 [post_date] => 2022-04-23 15:46:05 [post_date_gmt] => 2022-04-23 13:46:05 [post_content] => Photo by Alexandra van der Eijk © All rights reserved [post_title] => RozelleBay_EDIT [post_excerpt] => Rozelle Bay, adjoining Blackwattle Bay, 2022. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => rozellebay_edit [to_ping] => [pinged] => [post_modified] => 2022-05-31 15:07:44 [post_modified_gmt] => 2022-05-31 13:07:44 [post_content_filtered] => [post_parent] => 47345 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2000/04/RozelleBay_EDIT.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [617] => Array ( [ID] => 47435 [post_author] => 105 [post_date] => 2022-04-23 13:34:38 [post_date_gmt] => 2022-04-23 11:34:38 [post_content] => Photo by Alexandra van der Eijk, © All rights reserved Alexandra van der Eijk [post_title] => Xandra-11and12 [post_excerpt] => Mixing samples with solvents before application. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => xandra-11and12 [to_ping] => [pinged] => [post_modified] => 2022-04-23 13:35:55 [post_modified_gmt] => 2022-04-23 11:35:55 [post_content_filtered] => [post_parent] => 47345 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2000/04/Xandra-11and12.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [618] => Array ( [ID] => 47434 [post_author] => 105 [post_date] => 2022-04-23 13:30:05 [post_date_gmt] => 2022-04-23 11:30:05 [post_content] => Alexandra van der Eijk © All rights reserved [post_title] => Sample_C-02 [post_excerpt] => Sample C | Variants 3 and 4. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => sample_c-02 [to_ping] => [pinged] => [post_modified] => 2022-05-31 15:09:58 [post_modified_gmt] => 2022-05-31 13:09:58 [post_content_filtered] => [post_parent] => 47345 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2000/04/Sample_C-02.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [619] => Array ( [ID] => 47433 [post_author] => 105 [post_date] => 2022-04-23 13:29:56 [post_date_gmt] => 2022-04-23 11:29:56 [post_content] => Alexandra van der Eijk © All rights reserved [post_title] => Sample_C-01 [post_excerpt] => Sample C | Variant 1, two phases (left), Variant 2, two phases (right). [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => sample_c-01 [to_ping] => [pinged] => [post_modified] => 2022-05-31 15:09:54 [post_modified_gmt] => 2022-05-31 13:09:54 [post_content_filtered] => [post_parent] => 47345 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2000/04/Sample_C-01.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [620] => Array ( [ID] => 47432 [post_author] => 105 [post_date] => 2022-04-23 13:29:48 [post_date_gmt] => 2022-04-23 11:29:48 [post_content] => Alexandra van der Eijk © All rights reserved [post_title] => Sample_B-02 [post_excerpt] => Sample B | Variants 3 and 4. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => sample_b-02 [to_ping] => [pinged] => [post_modified] => 2022-05-31 15:10:10 [post_modified_gmt] => 2022-05-31 13:10:10 [post_content_filtered] => [post_parent] => 47345 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2000/04/Sample_B-02.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [621] => Array ( [ID] => 47431 [post_author] => 105 [post_date] => 2022-04-23 13:29:40 [post_date_gmt] => 2022-04-23 11:29:40 [post_content] => Alexandra van der Eijk © All rights reserved [post_title] => Sample_B-01 [post_excerpt] => Sample B | Variant 1 (left), Variant 2, two phases (right). [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => sample_b-01 [to_ping] => [pinged] => [post_modified] => 2022-05-31 15:10:05 [post_modified_gmt] => 2022-05-31 13:10:05 [post_content_filtered] => [post_parent] => 47345 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2000/04/Sample_B-01.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [622] => Array ( [ID] => 47430 [post_author] => 105 [post_date] => 2022-04-23 13:29:31 [post_date_gmt] => 2022-04-23 11:29:31 [post_content] => Alexandra van der Eijk © All rights reserved [post_title] => Sample_A-02 [post_excerpt] => Sample A | Variant 3, two phases (left), and Solvent 4, two phases (right). [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => sample_a-02 [to_ping] => [pinged] => [post_modified] => 2022-05-31 15:10:21 [post_modified_gmt] => 2022-05-31 13:10:21 [post_content_filtered] => [post_parent] => 47345 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2000/04/Sample_A-02.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [623] => Array ( [ID] => 47429 [post_author] => 105 [post_date] => 2022-04-23 13:29:20 [post_date_gmt] => 2022-04-23 11:29:20 [post_content] => Alexandra van der Eijk © All rights reserved [post_title] => Sample_A-01 [post_excerpt] => Sample A | Variant 1, three phases, and Variant 2 (far right). [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => sample_a-01 [to_ping] => [pinged] => [post_modified] => 2022-05-31 15:10:16 [post_modified_gmt] => 2022-05-31 13:10:16 [post_content_filtered] => [post_parent] => 47345 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2000/04/Sample_A-01.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [624] => Array ( [ID] => 47426 [post_author] => 105 [post_date] => 2022-04-23 13:26:23 [post_date_gmt] => 2022-04-23 11:26:23 [post_content] => Alexandra van der Eijk © All rights reserved [post_title] => Sample_D-02 [post_excerpt] => Sample D | Variants 3 and 4. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => sample_d-02 [to_ping] => [pinged] => [post_modified] => 2022-05-31 15:09:36 [post_modified_gmt] => 2022-05-31 13:09:36 [post_content_filtered] => [post_parent] => 47345 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2000/04/Sample_D-02.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [625] => Array ( [ID] => 47425 [post_author] => 105 [post_date] => 2022-04-23 13:26:15 [post_date_gmt] => 2022-04-23 11:26:15 [post_content] => Alexandra van der Eijk © All rights reserved [post_title] => Sample_D-01 [post_excerpt] => Sample D | Variant 1, two phases (left), Variant 2, two phases (right). [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => sample_d-01-2 [to_ping] => [pinged] => [post_modified] => 2022-05-31 15:09:41 [post_modified_gmt] => 2022-05-31 13:09:41 [post_content_filtered] => [post_parent] => 47345 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2000/04/Sample_D-01-1.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [626] => Array ( [ID] => 47420 [post_author] => 105 [post_date] => 2022-04-23 13:03:27 [post_date_gmt] => 2022-04-23 11:03:27 [post_content] => © All rights reserved Alexandra van der Eijk [post_title] => Sample_D-01 [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => sample_d-01 [to_ping] => [pinged] => [post_modified] => 2022-04-23 13:04:41 [post_modified_gmt] => 2022-04-23 11:04:41 [post_content_filtered] => [post_parent] => 47345 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2000/04/Sample_D-01.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [627] => Array ( [ID] => 47393 [post_author] => 12 [post_date] => 2022-04-22 17:08:18 [post_date_gmt] => 2022-04-22 15:08:18 [post_content] => [post_title] => Earth Indices [post_excerpt] => [post_status] => publish [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => earth-indices [to_ping] => [pinged] => [post_modified] => 2022-05-17 17:56:57 [post_modified_gmt] => 2022-05-17 15:56:57 [post_content_filtered] => [post_parent] => 0 [guid] => https://www.anthropocene-curriculum.org/?post_type=event&p=47393 [menu_order] => 0 [post_type] => event [post_mime_type] => [comment_count] => 0 [filter] => raw ) [628] => Array ( [ID] => 47392 [post_author] => 105 [post_date] => 2022-04-22 17:06:15 [post_date_gmt] => 2022-04-22 15:06:15 [post_content] => © All rights reserved Alexandra van der Eijk [post_title] => SampleA-T9-M [post_excerpt] => Sample A | Solvent 4, earlier stage. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => samplea-t9-m [to_ping] => [pinged] => [post_modified] => 2022-04-22 17:07:39 [post_modified_gmt] => 2022-04-22 15:07:39 [post_content_filtered] => [post_parent] => 47345 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2000/04/SampleA-T9-M.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [629] => Array ( [ID] => 47391 [post_author] => 105 [post_date] => 2022-04-22 17:01:13 [post_date_gmt] => 2022-04-22 15:01:13 [post_content] => © All rights reserved Alexandra van der Eijk [post_title] => SampleA-T9-M-laterstage [post_excerpt] => Sample A | Solvent 4, later stage. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => samplea-t9-m-laterstage [to_ping] => [pinged] => [post_modified] => 2022-04-22 17:07:40 [post_modified_gmt] => 2022-04-22 15:07:40 [post_content_filtered] => [post_parent] => 47345 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2000/04/SampleA-T9-M-laterstage.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [630] => Array ( [ID] => 47390 [post_author] => 105 [post_date] => 2022-04-22 17:01:06 [post_date_gmt] => 2022-04-22 15:01:06 [post_content] => © All rights reserved Alexandra van der Eijk [post_title] => SampleA-T9-3 [post_excerpt] => Sample A | Variant 1, stage 1. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => samplea-t9-3 [to_ping] => [pinged] => [post_modified] => 2022-04-22 17:07:28 [post_modified_gmt] => 2022-04-22 15:07:28 [post_content_filtered] => [post_parent] => 47345 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2000/04/SampleA-T9-3.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [631] => Array ( [ID] => 47389 [post_author] => 105 [post_date] => 2022-04-22 17:00:57 [post_date_gmt] => 2022-04-22 15:00:57 [post_content] => © All rights reserved Alexandra van der Eijk [post_title] => SampleA-T9-3-laterstage2 [post_excerpt] => Sample A | Variant 1, stage 2. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => samplea-t9-3-laterstage2 [to_ping] => [pinged] => [post_modified] => 2022-04-22 17:07:30 [post_modified_gmt] => 2022-04-22 15:07:30 [post_content_filtered] => [post_parent] => 47345 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2000/04/SampleA-T9-3-laterstage2.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [632] => Array ( [ID] => 47388 [post_author] => 105 [post_date] => 2022-04-22 17:00:50 [post_date_gmt] => 2022-04-22 15:00:50 [post_content] => © All rights reserved Alexandra van der Eijk [post_title] => SampleA-T9-3-laterstage1 [post_excerpt] => Sample A | Variant 1, stage 3. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => samplea-t9-3-laterstage1 [to_ping] => [pinged] => [post_modified] => 2022-04-22 17:07:32 [post_modified_gmt] => 2022-04-22 15:07:32 [post_content_filtered] => [post_parent] => 47345 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2000/04/SampleA-T9-3-laterstage1.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [633] => Array ( [ID] => 47387 [post_author] => 105 [post_date] => 2022-04-22 17:00:42 [post_date_gmt] => 2022-04-22 15:00:42 [post_content] => © All rights reserved Alexandra van der Eijk [post_title] => SampleA-T9-1 [post_excerpt] => Sample A | Variant 3, earlier stage. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => samplea-t9-1 [to_ping] => [pinged] => [post_modified] => 2022-04-22 17:07:35 [post_modified_gmt] => 2022-04-22 15:07:35 [post_content_filtered] => [post_parent] => 47345 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2000/04/SampleA-T9-1.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [634] => Array ( [ID] => 47386 [post_author] => 105 [post_date] => 2022-04-22 17:00:35 [post_date_gmt] => 2022-04-22 15:00:35 [post_content] => © All rights reserved Alexandra van der Eijk [post_title] => SampleA-T9-1-laterstage [post_excerpt] => Sample A | Variant 3, later stage. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => samplea-t9-1-laterstage [to_ping] => [pinged] => [post_modified] => 2022-04-22 17:07:37 [post_modified_gmt] => 2022-04-22 15:07:37 [post_content_filtered] => [post_parent] => 47345 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2000/04/SampleA-T9-1-laterstage.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [635] => Array ( [ID] => 47385 [post_author] => 105 [post_date] => 2022-04-22 17:00:27 [post_date_gmt] => 2022-04-22 15:00:27 [post_content] => © All rights reserved Alexandra van der Eijk [post_title] => SampleA-T4-3 [post_excerpt] => Sample A | Variant 2 [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => samplea-t4-3 [to_ping] => [pinged] => [post_modified] => 2022-04-22 17:07:34 [post_modified_gmt] => 2022-04-22 15:07:34 [post_content_filtered] => [post_parent] => 47345 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2000/04/SampleA-T4-3.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [636] => Array ( [ID] => 47345 [post_author] => 105 [post_date] => 2022-04-22 16:54:02 [post_date_gmt] => 2022-04-22 14:54:02 [post_content] =>

What insights can artistic research data produce in the scientific analysis of the natural archive? Xandra van der Eijk addresses the value of artmaking with, through, and between the materiality of place in the sediment samples of Sydney Harbour.

Artistic experiments on polluted sediment and the anthropogenic evolution of minerals

What insights can artistic research data produce in the scientific analysis of the natural archive? In practicing aesthetic attunement to material intra-actions between nonhuman entities, artist and researcher Xandra van der Eijk addresses the value of artmaking with, through, and between the materiality of place. Visualizing anthropogenic markers present in the sediment samples of Sydney Harbour, one of the most polluted estuaries in the world, she undertakes a hybridization of artistic and scientific method.

[post_title] => Visualizing the Vibrant Materiality of Place [post_excerpt] => [post_status] => publish [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => visualizing-the-vibrant-materiality-of-place [to_ping] => [pinged] => [post_modified] => 2022-05-31 15:10:36 [post_modified_gmt] => 2022-05-31 13:10:36 [post_content_filtered] => [post_parent] => 0 [guid] => https://www.anthropocene-curriculum.org/?post_type=contribution&p=47345 [menu_order] => 0 [post_type] => contribution [post_mime_type] => [comment_count] => 0 [filter] => raw ) [637] => Array ( [ID] => 47380 [post_author] => 105 [post_date] => 2022-04-22 16:50:59 [post_date_gmt] => 2022-04-22 14:50:59 [post_content] => © All rights reserved Alexandra van der Eijk [post_title] => SampleB-T15-3 [post_excerpt] => Sample B | Variant 3 [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => sampleb-t15-3 [to_ping] => [pinged] => [post_modified] => 2022-04-22 16:58:05 [post_modified_gmt] => 2022-04-22 14:58:05 [post_content_filtered] => [post_parent] => 47345 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/SampleB-T15-3.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [638] => Array ( [ID] => 47379 [post_author] => 105 [post_date] => 2022-04-22 16:50:51 [post_date_gmt] => 2022-04-22 14:50:51 [post_content] => © All rights reserved Alexandra van der Eijk [post_title] => SampleB-T10-M [post_excerpt] => Sample B | Variant 4. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => sampleb-t10-m [to_ping] => [pinged] => [post_modified] => 2022-04-22 16:57:56 [post_modified_gmt] => 2022-04-22 14:57:56 [post_content_filtered] => [post_parent] => 47345 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/SampleB-T10-M.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [639] => Array ( [ID] => 47378 [post_author] => 105 [post_date] => 2022-04-22 16:50:44 [post_date_gmt] => 2022-04-22 14:50:44 [post_content] => © All rights reserved Alexandra van der Eijk [post_title] => SampleB-T10-1v2 [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => sampleb-t10-1v2 [to_ping] => [pinged] => [post_modified] => 2022-04-22 16:56:35 [post_modified_gmt] => 2022-04-22 14:56:35 [post_content_filtered] => [post_parent] => 47345 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/SampleB-T10-1v2.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [640] => Array ( [ID] => 47377 [post_author] => 105 [post_date] => 2022-04-22 16:50:36 [post_date_gmt] => 2022-04-22 14:50:36 [post_content] => © All rights reserved Alexandra van der Eijk [post_title] => SampleB-T10-1b [post_excerpt] => Sample B | Variant 2, earlier stage. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => sampleb-t10-1b [to_ping] => [pinged] => [post_modified] => 2022-04-22 16:57:29 [post_modified_gmt] => 2022-04-22 14:57:29 [post_content_filtered] => [post_parent] => 47345 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/SampleB-T10-1b.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [641] => Array ( [ID] => 47376 [post_author] => 105 [post_date] => 2022-04-22 16:50:28 [post_date_gmt] => 2022-04-22 14:50:28 [post_content] => © All rights reserved Alexandra van der Eijk [post_title] => SampleB-T10-1b-laterstage [post_excerpt] => Sample B | Variant 2, later stage. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => sampleb-t10-1b-laterstage [to_ping] => [pinged] => [post_modified] => 2022-04-22 16:57:22 [post_modified_gmt] => 2022-04-22 14:57:22 [post_content_filtered] => [post_parent] => 47345 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/SampleB-T10-1b-laterstage.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [642] => Array ( [ID] => 47375 [post_author] => 105 [post_date] => 2022-04-22 16:50:20 [post_date_gmt] => 2022-04-22 14:50:20 [post_content] => © All rights reserved Alexandra van der Eijk [post_title] => SampleB-T10-1 [post_excerpt] => Sample B | Variant 1. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => sampleb-t10-1 [to_ping] => [pinged] => [post_modified] => 2022-04-22 16:57:01 [post_modified_gmt] => 2022-04-22 14:57:01 [post_content_filtered] => [post_parent] => 47345 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/SampleB-T10-1.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [643] => Array ( [ID] => 47374 [post_author] => 105 [post_date] => 2022-04-22 16:50:12 [post_date_gmt] => 2022-04-22 14:50:12 [post_content] => © All rights reserved Alexandra van der Eijk [post_title] => SampleB-T5-3 [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => sampleb-t5-3 [to_ping] => [pinged] => [post_modified] => 2022-04-22 16:56:26 [post_modified_gmt] => 2022-04-22 14:56:26 [post_content_filtered] => [post_parent] => 47345 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/SampleB-T5-3.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [644] => Array ( [ID] => 47373 [post_author] => 105 [post_date] => 2022-04-22 16:50:04 [post_date_gmt] => 2022-04-22 14:50:04 [post_content] => © All rights reserved Alexandra van der Eijk [post_title] => SampleB-T5-2 [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => sampleb-t5-2 [to_ping] => [pinged] => [post_modified] => 2022-04-22 16:58:27 [post_modified_gmt] => 2022-04-22 14:58:27 [post_content_filtered] => [post_parent] => 47345 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/SampleB-T5-2.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [645] => Array ( [ID] => 47372 [post_author] => 105 [post_date] => 2022-04-22 16:49:57 [post_date_gmt] => 2022-04-22 14:49:57 [post_content] => © All rights reserved Alexandra van der Eijk [post_title] => SampleC-T11-2 [post_excerpt] => Sample C | Variant 2, earlier stage. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => samplec-t11-2 [to_ping] => [pinged] => [post_modified] => 2022-04-22 16:56:15 [post_modified_gmt] => 2022-04-22 14:56:15 [post_content_filtered] => [post_parent] => 47345 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/SampleC-T11-2.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [646] => Array ( [ID] => 47371 [post_author] => 105 [post_date] => 2022-04-22 16:49:48 [post_date_gmt] => 2022-04-22 14:49:48 [post_content] => © All rights reserved Alexandra van der Eijk [post_title] => SampleC-T11-2-laterstage [post_excerpt] => Sample C | Variant 2, later stage. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => samplec-t11-2-laterstage [to_ping] => [pinged] => [post_modified] => 2022-04-22 16:56:17 [post_modified_gmt] => 2022-04-22 14:56:17 [post_content_filtered] => [post_parent] => 47345 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/SampleC-T11-2-laterstage.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [647] => Array ( [ID] => 47370 [post_author] => 105 [post_date] => 2022-04-22 16:49:39 [post_date_gmt] => 2022-04-22 14:49:39 [post_content] => © All rights reserved Alexandra van der Eijk [post_title] => SampleC-T11-1a [post_excerpt] => Sample C | Variant 1, earlier stage. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => samplec-t11-1a [to_ping] => [pinged] => [post_modified] => 2022-04-22 16:56:12 [post_modified_gmt] => 2022-04-22 14:56:12 [post_content_filtered] => [post_parent] => 47345 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/SampleC-T11-1a.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [648] => Array ( [ID] => 47369 [post_author] => 105 [post_date] => 2022-04-22 16:49:32 [post_date_gmt] => 2022-04-22 14:49:32 [post_content] => © All rights reserved Alexandra van der Eijk [post_title] => SampleC-T11-1a-laterstage [post_excerpt] => Sample C | Variant 1 later stage. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => samplec-t11-1a-laterstage [to_ping] => [pinged] => [post_modified] => 2022-04-22 16:56:14 [post_modified_gmt] => 2022-04-22 14:56:14 [post_content_filtered] => [post_parent] => 47345 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/SampleC-T11-1a-laterstage.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [649] => Array ( [ID] => 47368 [post_author] => 105 [post_date] => 2022-04-22 16:49:25 [post_date_gmt] => 2022-04-22 14:49:25 [post_content] => © All rights reserved Alexandra van der Eijk [post_title] => SampleC-T11-1 [post_excerpt] => Sample C | Variant 3 [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => samplec-t11-1 [to_ping] => [pinged] => [post_modified] => 2022-04-22 16:56:19 [post_modified_gmt] => 2022-04-22 14:56:19 [post_content_filtered] => [post_parent] => 47345 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/SampleC-T11-1.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [650] => Array ( [ID] => 47367 [post_author] => 105 [post_date] => 2022-04-22 16:49:17 [post_date_gmt] => 2022-04-22 14:49:17 [post_content] => © All rights reserved Alexandra van der Eijk [post_title] => SampleC-T6-3 [post_excerpt] => Sample C | Variant 4 [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => samplec-t6-3 [to_ping] => [pinged] => [post_modified] => 2022-04-22 16:56:20 [post_modified_gmt] => 2022-04-22 14:56:20 [post_content_filtered] => [post_parent] => 47345 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/SampleC-T6-3.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [651] => Array ( [ID] => 47366 [post_author] => 105 [post_date] => 2022-04-22 16:45:20 [post_date_gmt] => 2022-04-22 14:45:20 [post_content] => [post_title] => SampleD-T12-M [post_excerpt] => Sample D | Variant 2, earlier stage. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => sampled-t12-m [to_ping] => [pinged] => [post_modified] => 2022-04-23 00:01:58 [post_modified_gmt] => 2022-04-22 22:01:58 [post_content_filtered] => [post_parent] => 47345 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/SampleD-T12-M.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [652] => Array ( [ID] => 47365 [post_author] => 105 [post_date] => 2022-04-22 16:45:12 [post_date_gmt] => 2022-04-22 14:45:12 [post_content] => [post_title] => SampleD-T12-M-laterstage [post_excerpt] => Sample D | Variant 2, later stage. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => sampled-t12-m-laterstage [to_ping] => [pinged] => [post_modified] => 2022-04-23 00:02:00 [post_modified_gmt] => 2022-04-22 22:02:00 [post_content_filtered] => [post_parent] => 47345 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/SampleD-T12-M-laterstage.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [653] => Array ( [ID] => 47364 [post_author] => 105 [post_date] => 2022-04-22 16:45:05 [post_date_gmt] => 2022-04-22 14:45:05 [post_content] => [post_title] => SampleD-T12-2b [post_excerpt] => Sample D | Variant 4 [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => sampled-t12-2b [to_ping] => [pinged] => [post_modified] => 2022-04-23 00:16:13 [post_modified_gmt] => 2022-04-22 22:16:13 [post_content_filtered] => [post_parent] => 47345 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/SampleD-T12-2b.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [654] => Array ( [ID] => 47363 [post_author] => 105 [post_date] => 2022-04-22 16:44:58 [post_date_gmt] => 2022-04-22 14:44:58 [post_content] => [post_title] => SampleD-T12-2 [post_excerpt] => Sample D | Variant 1, earlier stage. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => sampled-t12-2 [to_ping] => [pinged] => [post_modified] => 2022-04-23 00:01:53 [post_modified_gmt] => 2022-04-22 22:01:53 [post_content_filtered] => [post_parent] => 47345 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/SampleD-T12-2.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [655] => Array ( [ID] => 47362 [post_author] => 105 [post_date] => 2022-04-22 16:44:52 [post_date_gmt] => 2022-04-22 14:44:52 [post_content] => [post_title] => SampleD-T12-2-laterstage [post_excerpt] => Sample D | Variant 1, later stage. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => sampled-t12-2-laterstage [to_ping] => [pinged] => [post_modified] => 2022-04-23 00:01:56 [post_modified_gmt] => 2022-04-22 22:01:56 [post_content_filtered] => [post_parent] => 47345 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/SampleD-T12-2-laterstage.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [656] => Array ( [ID] => 47361 [post_author] => 105 [post_date] => 2022-04-22 16:44:44 [post_date_gmt] => 2022-04-22 14:44:44 [post_content] => [post_title] => SampleD-T7 [post_excerpt] => Sample D | Variant 3 [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => sampled-t7 [to_ping] => [pinged] => [post_modified] => 2022-04-23 00:20:06 [post_modified_gmt] => 2022-04-22 22:20:06 [post_content_filtered] => [post_parent] => 47345 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/SampleD-T7.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [657] => Array ( [ID] => 47360 [post_author] => 105 [post_date] => 2022-04-22 16:21:52 [post_date_gmt] => 2022-04-22 14:21:52 [post_content] => Photo by Alexandra van der Eijk, © All rights reserved Alexandra van der Eijk [post_title] => Xandra_fig13 [post_excerpt] => Set of baseline tests, resulting in minimal verdigris effects. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => xandra_fig13 [to_ping] => [pinged] => [post_modified] => 2022-04-22 16:32:46 [post_modified_gmt] => 2022-04-22 14:32:46 [post_content_filtered] => [post_parent] => 47345 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/Xandra_fig13.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [658] => Array ( [ID] => 47359 [post_author] => 105 [post_date] => 2022-04-22 16:21:41 [post_date_gmt] => 2022-04-22 14:21:41 [post_content] => Photo by Alexandra van der Eijk, © All rights reserved Alexandra van der Eijk [post_title] => Xandra_fig12 [post_excerpt] => Mixing samples with solvents before application. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => xandra_fig12 [to_ping] => [pinged] => [post_modified] => 2022-04-22 16:31:37 [post_modified_gmt] => 2022-04-22 14:31:37 [post_content_filtered] => [post_parent] => 47345 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/Xandra_fig12.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [659] => Array ( [ID] => 47358 [post_author] => 105 [post_date] => 2022-04-22 16:21:30 [post_date_gmt] => 2022-04-22 14:21:30 [post_content] => Photo by Alexandra van der Eijk, © All rights reserved Alexandra van der Eijk [post_title] => Xandra_fig11 [post_excerpt] => Mixing samples with solvents before application. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => xandra_fig11 [to_ping] => [pinged] => [post_modified] => 2022-04-22 16:31:32 [post_modified_gmt] => 2022-04-22 14:31:32 [post_content_filtered] => [post_parent] => 47345 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/Xandra_fig11.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [660] => Array ( [ID] => 47357 [post_author] => 105 [post_date] => 2022-04-22 16:21:15 [post_date_gmt] => 2022-04-22 14:21:15 [post_content] => Photo by Alexandra van der Eijk, © All rights reserved Alexandra van der Eijk [post_title] => Xandra_fig10 [post_excerpt] => Sampling polluted sediment after a heavy storm. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => xandra_fig10 [to_ping] => [pinged] => [post_modified] => 2022-04-22 16:28:24 [post_modified_gmt] => 2022-04-22 14:28:24 [post_content_filtered] => [post_parent] => 47345 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/Xandra_fig10.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [661] => Array ( [ID] => 47356 [post_author] => 105 [post_date] => 2022-04-22 16:20:59 [post_date_gmt] => 2022-04-22 14:20:59 [post_content] => Photo by Alexandra van der Eijk © All rights reserved [post_title] => Xandra_fig9 [post_excerpt] => Core 8, Birch & Lean, Blackwattle Bay. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => xandra_fig9 [to_ping] => [pinged] => [post_modified] => 2022-05-31 15:08:17 [post_modified_gmt] => 2022-05-31 13:08:17 [post_content_filtered] => [post_parent] => 47345 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/Xandra_fig9.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [662] => Array ( [ID] => 47355 [post_author] => 105 [post_date] => 2022-04-22 16:20:37 [post_date_gmt] => 2022-04-22 14:20:37 [post_content] => Photo by Alexandra van der Eijk © All rights reserved [post_title] => Xandra_fig8 [post_excerpt] => Core storage at the University of Sydney. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => xandra_fig8 [to_ping] => [pinged] => [post_modified] => 2022-05-31 15:08:09 [post_modified_gmt] => 2022-05-31 13:08:09 [post_content_filtered] => [post_parent] => 47345 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/Xandra_fig8.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [663] => Array ( [ID] => 47354 [post_author] => 105 [post_date] => 2022-04-22 16:20:19 [post_date_gmt] => 2022-04-22 14:20:19 [post_content] => Photo by Alexandra van der Eijk, © All rights reserved Alexandra van der Eijk [post_title] => Xandra_fig7 [post_excerpt] => Sydney Estuary at low tide, near a storm drain. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => xandra_fig7 [to_ping] => [pinged] => [post_modified] => 2022-04-22 16:23:36 [post_modified_gmt] => 2022-04-22 14:23:36 [post_content_filtered] => [post_parent] => 47345 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/Xandra_fig7.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [664] => Array ( [ID] => 47353 [post_author] => 105 [post_date] => 2022-04-22 16:07:30 [post_date_gmt] => 2022-04-22 14:07:30 [post_content] => Map courtesy Sacha van den Haak [post_title] => Xandra_fig6 [post_excerpt] => Sydney estuary and the location of cores discussed in this contribution. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => xandra_fig6 [to_ping] => [pinged] => [post_modified] => 2022-04-22 16:16:06 [post_modified_gmt] => 2022-04-22 14:16:06 [post_content_filtered] => [post_parent] => 47345 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/Xandra_fig6.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [665] => Array ( [ID] => 47352 [post_author] => 105 [post_date] => 2022-04-22 16:07:21 [post_date_gmt] => 2022-04-22 14:07:21 [post_content] => Photo by Alexandra van der Eijk, © All rights reserved Alexandra van der Eijk [post_title] => Xandra_fig5 [post_excerpt] => Port Jackson, 2020. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => xandra_fig5 [to_ping] => [pinged] => [post_modified] => 2022-04-22 16:14:38 [post_modified_gmt] => 2022-04-22 14:14:38 [post_content_filtered] => [post_parent] => 47345 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/Xandra_fig5.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [666] => Array ( [ID] => 47351 [post_author] => 105 [post_date] => 2022-04-22 16:07:08 [post_date_gmt] => 2022-04-22 14:07:08 [post_content] => Photo courtesy Dutch Invertuals/Ronald Smits, Alexandra van der Eijk © All rights reserved [post_title] => Dutch Invertuals - Mutant Matter [post_excerpt] => Future Remnants presented with Dutch Invertuals at Milan Design Week. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => dutch-invertuals-mutant-matter-4 [to_ping] => [pinged] => [post_modified] => 2022-05-31 15:07:19 [post_modified_gmt] => 2022-05-31 13:07:19 [post_content_filtered] => [post_parent] => 47345 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/Xandra_fig4.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [667] => Array ( [ID] => 47350 [post_author] => 105 [post_date] => 2022-04-22 16:06:59 [post_date_gmt] => 2022-04-22 14:06:59 [post_content] => Photo courtesy Dutch Invertuals/Ronald Smits, Alexandra van der Eijk © All rights reserved [post_title] => Dutch Invertuals - Mutant Matter [post_excerpt] => Future Remnants presented with Dutch Invertuals at Milan Design Week. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => dutch-invertuals-mutant-matter-3 [to_ping] => [pinged] => [post_modified] => 2022-05-31 15:07:07 [post_modified_gmt] => 2022-05-31 13:07:07 [post_content_filtered] => [post_parent] => 47345 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/Xandra_fig3.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [668] => Array ( [ID] => 47349 [post_author] => 105 [post_date] => 2022-04-22 16:06:49 [post_date_gmt] => 2022-04-22 14:06:49 [post_content] => Photo courtesy Dutch Invertuals/Ronald Smits, Alexandra van der Eijk © All rights reserved [post_title] => Dutch Invertuals - Mutant Matter [post_excerpt] => Future Remnants presented with Dutch Invertuals at Milan Design Week. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => dutch-invertuals-mutant-matter-2 [to_ping] => [pinged] => [post_modified] => 2022-05-31 15:06:55 [post_modified_gmt] => 2022-05-31 13:06:55 [post_content_filtered] => [post_parent] => 47345 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/Xandra_fig2.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [669] => Array ( [ID] => 47348 [post_author] => 105 [post_date] => 2022-04-22 16:06:37 [post_date_gmt] => 2022-04-22 14:06:37 [post_content] => Photo courtesy Dutch Invertuals/Ronald Smits. Alexandra van der Eijk © All rights reserved [post_title] => Dutch Invertuals - Mutant Matter [post_excerpt] => Future Remnants presented with Dutch Invertuals at Milan Design Week. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => dutch-invertuals-mutant-matter [to_ping] => [pinged] => [post_modified] => 2022-05-31 15:05:44 [post_modified_gmt] => 2022-05-31 13:05:44 [post_content_filtered] => [post_parent] => 47345 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/Xandra_fig1.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [670] => Array ( [ID] => 44663 [post_author] => 105 [post_date] => 2022-04-22 10:34:21 [post_date_gmt] => 2022-04-22 08:34:21 [post_content] =>

It’s possible that the most suitable golden spike for marking the beginning of the Anthropocene does not yet exist.

A Future Marker for the Anthropocene

Considering the hitherto short duration of the Anthropocene, it’s possible that the most suitable golden spike for geologically marking the epoch’s beginning does not yet exist. Physicist and historian Benjamin Johnson argues that if Earth-human interaction is to endure and eventually merit recognition as a geological age, one necessary development is for humans to close the biogeochemical cycles they have fundamentally perturbed. Such an intentional closing would be linked to human action and could be precisely marked in time, presenting a clear sign of a stabilizing Anthropocene. Born and raised in Alaska, Johnson accompanies his contribution with images from the state’s northernmost point, Point Barrow, or Nuvuk, where the changing carbon concentration in the atmosphere has been tracked since the 1970s. Nuvuk acts as a reminder that even the most remote regions of the globe are impacted by anthropogenic action.

[post_title] => Closed Chemical Cycles [post_excerpt] => [post_status] => publish [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => closed-chemical-cycles [to_ping] => [pinged] => [post_modified] => 2022-05-31 11:47:14 [post_modified_gmt] => 2022-05-31 09:47:14 [post_content_filtered] => [post_parent] => 0 [guid] => https://www.anthropocene-curriculum.org/?post_type=contribution&p=44663 [menu_order] => 0 [post_type] => contribution [post_mime_type] => [comment_count] => 0 [filter] => raw ) [671] => Array ( [ID] => 45642 [post_author] => 103 [post_date] => 2022-04-22 10:13:15 [post_date_gmt] => 2022-04-22 08:13:15 [post_content] =>

Lakes, seas, estuaries, and wetlands provide important archives of humanity’s reconfiguration of life in the Anthropocene.

[post_title] => Biological and Paleontological Signatures of the Anthropocene [post_excerpt] => [post_status] => publish [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => biological-and-paleontological-signatures-of-the-anthropocene [to_ping] => [pinged] => [post_modified] => 2022-08-19 15:34:59 [post_modified_gmt] => 2022-08-19 13:34:59 [post_content_filtered] => [post_parent] => 0 [guid] => https://www.anthropocene-curriculum.org/?post_type=contribution&p=45642 [menu_order] => 0 [post_type] => contribution [post_mime_type] => [comment_count] => 0 [filter] => raw ) [672] => Array ( [ID] => 44795 [post_author] => 105 [post_date] => 2022-04-22 10:09:32 [post_date_gmt] => 2022-04-22 08:09:32 [post_content] =>

The artist Julian Charrière artificially remodels a biogeochemical cycle and casts it into a performance of reverse extraction: carbon molecules are captured from the air and turned into diamonds which are then “wastefully” cast into a glacier.

This contribution by artist Julian Charrière is based on research and materials gathered during a scientific expedition in Northern Greenland in the summer of 2021. Charrière artificially remodels a biogeochemical cycle and casts it into a performance of reverse extraction: in the installation Weight of Shadows and the accompanying video work Pure Waste, carbon molecules are captured from the air before they sink into polar glaciers, and turned into diamonds which are then “wastefully” cast into that same glacier’s crevasses.

[post_title] => Weight of Shadows [post_excerpt] => [post_status] => publish [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => weight-of-shadows [to_ping] => [pinged] => [post_modified] => 2022-05-31 11:39:54 [post_modified_gmt] => 2022-05-31 09:39:54 [post_content_filtered] => [post_parent] => 0 [guid] => https://www.anthropocene-curriculum.org/?post_type=contribution&p=44795 [menu_order] => 0 [post_type] => contribution [post_mime_type] => [comment_count] => 0 [filter] => raw ) [673] => Array ( [ID] => 45645 [post_author] => 103 [post_date] => 2022-04-22 10:05:07 [post_date_gmt] => 2022-04-22 08:05:07 [post_content] => [post_title] => The Anthropocene Signal Amidst the Noise [post_excerpt] => [post_status] => publish [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => the-anthropocene-signal-amidst-the-noise [to_ping] => [pinged] => [post_modified] => 2022-07-11 17:21:10 [post_modified_gmt] => 2022-07-11 15:21:10 [post_content_filtered] => [post_parent] => 0 [guid] => https://www.anthropocene-curriculum.org/?post_type=contribution&p=45645 [menu_order] => 0 [post_type] => contribution [post_mime_type] => [comment_count] => 0 [filter] => raw ) [674] => Array ( [ID] => 47078 [post_author] => 105 [post_date] => 2022-04-22 10:04:23 [post_date_gmt] => 2022-04-22 08:04:23 [post_content] =>

What kind of sign is a marker? Jürgen Renn and Nathaniel LaCelle-Peterson sketch the dual role of markers as traces in the strata and symptoms of a destabilized Earth System—an interface between natural archives and human societies.

The semiotics of anthropogenic markers

What kind of sign is a marker? This question is at the heart of the multi-disciplinary discussions that animate the conversations of these dossiers, and is fundamentally a question of semiotics: the study of signs. In this reflection, science historian Jürgen Renn and literary scholar Nathaniel LaCelle-Peterson sketch out how the dual role of markers as traces in the strata and symptoms of the dangerous destabilization of the Earth System turns them into a crucial interface between natural archives and human societies.

[post_title] => Traces and Symptoms [post_excerpt] => [post_status] => publish [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => traces-and-symptoms [to_ping] => [pinged] => [post_modified] => 2022-05-16 12:05:06 [post_modified_gmt] => 2022-05-16 10:05:06 [post_content_filtered] => [post_parent] => 0 [guid] => https://www.anthropocene-curriculum.org/?post_type=contribution&p=47078 [menu_order] => 0 [post_type] => contribution [post_mime_type] => [comment_count] => 0 [filter] => raw ) [675] => Array ( [ID] => 47301 [post_author] => 12 [post_date] => 2022-04-22 10:00:05 [post_date_gmt] => 2022-04-22 08:00:05 [post_content] => © All rights reserved Protey Temen [post_title] => AnthropogenicMarkers-Covers-Vertical-3 [post_excerpt] => Art by Protey Temen. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => anthropogenicmarkers-covers-vertical-3 [to_ping] => [pinged] => [post_modified] => 2022-04-22 10:11:27 [post_modified_gmt] => 2022-04-22 08:11:27 [post_content_filtered] => [post_parent] => 47008 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/AnthropogenicMarkers-Covers-Vertical-3.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [676] => Array ( [ID] => 44598 [post_author] => 105 [post_date] => 2022-04-22 10:00:02 [post_date_gmt] => 2022-04-22 08:00:02 [post_content] =>

Through the case of the nuclear accident at Palomares, Spain, historian of science Xavier Roqué shows the importance of local actants and scarce resources in registering and understanding Anthropocene-scale phenomena.

Local Words for the Palomares Accident

The science of global changes emerges from a period when large-scale international research defined by the military-industrial-academic complex was the norm. Historian of science Xavier Roqué subverts this historical supremacy of big science in the nuclear age by highlighting the role of small-scale science and local research. Through the case of the nuclear accident at Palomares, Spain, he shows the importance of local actants and scarce resources in registering and understanding Anthropocene-scale phenomena.

[post_title] => Small Agency in the Nuclear Anthropocene [post_excerpt] => [post_status] => publish [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => small-agency-in-the-nuclear-anthropocene [to_ping] => [pinged] => [post_modified] => 2022-05-16 12:05:28 [post_modified_gmt] => 2022-05-16 10:05:28 [post_content_filtered] => [post_parent] => 0 [guid] => https://www.anthropocene-curriculum.org/?post_type=contribution&p=44598 [menu_order] => 0 [post_type] => contribution [post_mime_type] => [comment_count] => 0 [filter] => raw ) [677] => Array ( [ID] => 44134 [post_author] => 130 [post_date] => 2022-04-22 09:59:46 [post_date_gmt] => 2022-04-22 07:59:46 [post_content] =>

Knowledge of the onset of the Anthropocene is intimately connected to nuclear technoscience on the one hand and to the governance of environmental problems, such as atmospheric pollution, on the other.

Knowledge of the onset of the Anthropocene is intimately connected to nuclear technoscience on the one hand and to the governance of environmental problems, such as atmospheric pollution, on the other. Historian of science Néstor Herran describes the historical roots of global environmental monitoring that helped frame the twin concepts of the Anthropocene and the “Great Acceleration.” He shows how the roots of global atmospheric monitoring go back to the demands and institutions of nuclear military surveillance, and the varied ways in which these new research practices and data infrastructures were deployed to assess the impact of radioactive fallout.

[post_title] => Monitoring the Nuclear Anthropocene [post_excerpt] => [post_status] => publish [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => monitoring-the-nuclear-anthropocene [to_ping] => [pinged] => [post_modified] => 2022-05-16 12:05:47 [post_modified_gmt] => 2022-05-16 10:05:47 [post_content_filtered] => [post_parent] => 0 [guid] => https://www.anthropocene-curriculum.org/?post_type=contribution&p=44134 [menu_order] => 0 [post_type] => contribution [post_mime_type] => [comment_count] => 0 [filter] => raw ) [678] => Array ( [ID] => 43824 [post_author] => 105 [post_date] => 2022-04-22 09:59:42 [post_date_gmt] => 2022-04-22 07:59:42 [post_content] =>

Comparing the approaches to radioactive fallout in the US and USSR, Kate Brown retraces the ways in which radio biologists and ecologists assessed and contorted radioactive contamination to study the resilience of ecosystems and human bodies.

An alarming impact or a mere perturbation? Comparing the approaches to radioactive fallout in US and USSR public health, radiation historian and archival vagabond Kate Brown retraces the ways in which radio biologists and ecologists assessed, rated, and contorted radioactive contamination in studying the resilience of ecosystems and human bodies. Brown contends that even buried human bones contain persistent markers from the mid-twentieth century.

[post_title] => The Skeletal Remains of the Nuclear Anthropocene [post_excerpt] => [post_status] => publish [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => the-skeletal-remains-of-the-nuclear-anthropocene [to_ping] => [pinged] => [post_modified] => 2022-05-16 12:06:04 [post_modified_gmt] => 2022-05-16 10:06:04 [post_content_filtered] => [post_parent] => 0 [guid] => https://www.anthropocene-curriculum.org/?post_type=contribution&p=43824 [menu_order] => 0 [post_type] => contribution [post_mime_type] => [comment_count] => 0 [filter] => raw ) [679] => Array ( [ID] => 44925 [post_author] => 130 [post_date] => 2022-04-22 09:59:28 [post_date_gmt] => 2022-04-22 07:59:28 [post_content] =>

Artists Nina Canell and Robin Watkins recover the deep-time aquatic past of the limestone environment that formed the island of Gotland and delineate the temporal entanglements between ancient life creation and modern-day living.

Post-Industrial Tropical Reefs on Northern Gotland

One of the most promising candidates for an Anthropocene Global Boundary Stratotype Section and Point is a short marine core from the Baltic Sea, taken from the Gotland Deep anoxic basin near the island of that same name. In this contribution, artists Nina Canell and Robin Watkins recover the deep-time aquatic past of the limestone environment that formed the island. Looking at what once were tropical reefs and now have become the building blocks of our modern industrial construction economy, they delineate the temporal entanglements between ancient life creation and modern-day living.

[post_title] => Silurian Harvest [post_excerpt] => [post_status] => publish [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => silurian-harvest [to_ping] => [pinged] => [post_modified] => 2022-05-31 12:00:26 [post_modified_gmt] => 2022-05-31 10:00:26 [post_content_filtered] => [post_parent] => 0 [guid] => https://www.anthropocene-curriculum.org/?post_type=contribution&p=44925 [menu_order] => 0 [post_type] => contribution [post_mime_type] => [comment_count] => 0 [filter] => raw ) [680] => Array ( [ID] => 44798 [post_author] => 130 [post_date] => 2022-04-22 09:59:15 [post_date_gmt] => 2022-04-22 07:59:15 [post_content] =>

In search for the normative elements of technofossil classification, Anna Echterhölter reflects on this history of mineral classification in the European tradition and the thick classification of Pacific totemism.

Taxonomy, Totemism, and the Technofossils of the Anthropocene

There has never been “pure matter.” The Western definition of minerals as simple substances emerged from an intricate interconnection of practical issues dealing with value, weight, and measurement. From this vantage point, the concept of a technofossil represents an innovation in how it explicitly mingles human agency with geological classification. In search for the normative elements of this new material domain, historian of science and cultural scholar Anna Echterhölter reflects on this history of mineral classification in the European tradition and the thick classification of Pacific totemism.

[post_title] => Human-Mineral Classification [post_excerpt] => [post_status] => publish [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => human-mineral-classification [to_ping] => [pinged] => [post_modified] => 2022-05-16 12:06:42 [post_modified_gmt] => 2022-05-16 10:06:42 [post_content_filtered] => [post_parent] => 0 [guid] => https://www.anthropocene-curriculum.org/?post_type=contribution&p=44798 [menu_order] => 0 [post_type] => contribution [post_mime_type] => [comment_count] => 0 [filter] => raw ) [681] => Array ( [ID] => 44742 [post_author] => 130 [post_date] => 2022-04-22 09:59:09 [post_date_gmt] => 2022-04-22 07:59:09 [post_content] =>

Plastic represents a particularly alluring material legacy in the rock record—but as Andrea Westermann shows, for its health and environmental hazards, consumerism and the exploitation of migrant labor, plastic is a deeply troubling material.

Considering Migrant Labor and Petrochemical Feedstocks in the Future History of Plastic

Plastic and its waste are eye-catching and culturally laden materials. Given that their histories have become entangled with the notion of the technofossil, how can we resist the temptation to aestheticize this material legacy which is accumulating in the rock record? Guiding us through the historical roots, current excesses, and future imaginations of plasticulture in Germany, Spain, and Brazil, historian of technology Andrea Westermann highlights the interconnection of health and environmental hazards as well as consumerism and the exploitation of migrant labor. She calls for including mining and mineral resource issues into future histories of plastic.

[post_title] => Against the Aestheticization of Technofossils [post_excerpt] => [post_status] => publish [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => against-the-aestheticization-of-technofossils [to_ping] => [pinged] => [post_modified] => 2022-06-24 11:03:42 [post_modified_gmt] => 2022-06-24 09:03:42 [post_content_filtered] => [post_parent] => 0 [guid] => https://www.anthropocene-curriculum.org/?post_type=contribution&p=44742 [menu_order] => 0 [post_type] => contribution [post_mime_type] => [comment_count] => 0 [filter] => raw ) [682] => Array ( [ID] => 45201 [post_author] => 105 [post_date] => 2022-04-22 09:58:48 [post_date_gmt] => 2022-04-22 07:58:48 [post_content] =>

Media scholar Adam Wickberg outlines ​​how knowledge about the environment and media technologies ​have always ​evolve​d​ in tandem​; the history of anthropogenic markers can therefore be understood as a process of environing media.

Media technologies have always been decisive for the epistemic registers and imaginations humans create and associate with nature. In his essay, media scholar Adam Wickberg outlines ​​how knowledge about the environment and media technologies ​have always ​evolve​d​ in tandem​; the history of anthropogenic markers can therefore be understood as a process of environing media. Getting us from the chemical composition of the atmosphere to pre-Columbian Amazonia to the rise of computational media in the late twentieth century, Wickberg chronicles and illustrates how anthropogenic markers are now a subset of a generically mediated planet.

[post_title] => Anthropogenic Markers as Environing Media [post_excerpt] => [post_status] => publish [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => anthropogenic-markers-as-environing-media [to_ping] => [pinged] => [post_modified] => 2022-05-16 12:07:26 [post_modified_gmt] => 2022-05-16 10:07:26 [post_content_filtered] => [post_parent] => 0 [guid] => https://www.anthropocene-curriculum.org/?post_type=contribution&p=45201 [menu_order] => 0 [post_type] => contribution [post_mime_type] => [comment_count] => 0 [filter] => raw ) [683] => Array ( [ID] => 45260 [post_author] => 105 [post_date] => 2022-04-22 09:58:01 [post_date_gmt] => 2022-04-22 07:58:01 [post_content] =>

Julian Charrière and Nadim Samman take us on a dive into Bikini Atoll to tell the story of the post-atomic ghostlands and the never-to-end heritage of contamination in the blasted reefs.

Within Bikini Atoll (extract)

Artist Julian Charrière and curator and writer Nadim Samman take us on a dive into an underwater atrocity museum. It was formed by one of the most gruesome of all field experiments: the nuclear weapon tests on Bikini Atoll in 1946 that started off a decade of nuclear devastation on the Marshall Islands and the rise of the global fallout signal. Reflecting on their own role in the alienating iconographic history of the site, Charrière and Samman’s travelog warily tells the story of the post-atomic ghostlands and the never-to-end heritage of contamination in the blasted reefs. They capture lush afterlife in maritime ruins, corals that were first pulverized and then petrified, and the story of Pacific islanders who have been deceived to give away their archipelagic home for an alleged “end to all wars.”

[post_title] => As We Used to Float [post_excerpt] => [post_status] => publish [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => as-we-used-to-float [to_ping] => [pinged] => [post_modified] => 2022-05-16 12:07:48 [post_modified_gmt] => 2022-05-16 10:07:48 [post_content_filtered] => [post_parent] => 0 [guid] => https://www.anthropocene-curriculum.org/?post_type=contribution&p=45260 [menu_order] => 0 [post_type] => contribution [post_mime_type] => [comment_count] => 0 [filter] => raw ) [684] => Array ( [ID] => 44142 [post_author] => 130 [post_date] => 2022-04-22 09:57:48 [post_date_gmt] => 2022-04-22 07:57:48 [post_content] =>

Assessing the effects of artificial radioactivity on human bodies and natural environments has a special place in the history of risk regulation, and has provided a key basis for understanding and defining the anthropogenic danger to life on Earth.

Assessing the effects of artificial radioactivity on human bodies and natural environments has a special place in the history of risk regulation. Angela Creager shows how studies of the effects of (low-dose) radiation exposure on ecosystems and the food web moved ecologists, geneticists, and biomedical researchers to create tools for researching, assessing, and regulating the health and environmental impacts of toxic chemicals and other contaminants. This, in turn, has provided a key basis, and an epistemological reckoning, for understanding and defining the anthropogenic danger to life on Earth.

[post_title] => The Radioactive Footprint of the Anthropocene [post_excerpt] => [post_status] => publish [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => the-radioactive-footprint-of-the-anthropocene [to_ping] => [pinged] => [post_modified] => 2022-05-16 12:08:08 [post_modified_gmt] => 2022-05-16 10:08:08 [post_content_filtered] => [post_parent] => 0 [guid] => https://www.anthropocene-curriculum.org/?post_type=contribution&p=44142 [menu_order] => 0 [post_type] => contribution [post_mime_type] => [comment_count] => 0 [filter] => raw ) [685] => Array ( [ID] => 47295 [post_author] => 105 [post_date] => 2022-04-22 09:57:43 [post_date_gmt] => 2022-04-22 07:57:43 [post_content] => [post_title] => Bolen : Holmes – Hourglass River Part 3 [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => bolen-holmes-hourglass-river-part-3 [to_ping] => [pinged] => [post_modified] => 2022-04-22 09:57:43 [post_modified_gmt] => 2022-04-22 07:57:43 [post_content_filtered] => [post_parent] => 46376 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/Bolen-Holmes-–-Hourglass-River-Part-3.pdf [menu_order] => 0 [post_type] => attachment [post_mime_type] => application/pdf [comment_count] => 0 [filter] => raw ) [686] => Array ( [ID] => 44674 [post_author] => 130 [post_date] => 2022-04-22 09:57:10 [post_date_gmt] => 2022-04-22 07:57:10 [post_content] =>

How do tropes and images of a changing ocean operate in a larger system of cultural sensemaking? Killian Quigley collects a range of threads to map the disfiguration and deformation of an anthropocenic biosphere that swells below the sea’s surface.

How do tropes and images of a changing ocean—its creatures and depths, abundances and dangers—operate in a larger system of cultural sensemaking? Literary scholar Killian Quigley engages the “weave of image, mode, and genre” through which (sub)marine spaces and their futurities are written and read, tracing the disfiguration and deformation of an anthropocenic biosphere that swells beneath the sea’s surface.

[post_title] => Reading the Anthropocene Ocean [post_excerpt] => [post_status] => publish [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => reading-the-anthropocene-ocean [to_ping] => [pinged] => [post_modified] => 2022-05-31 11:54:11 [post_modified_gmt] => 2022-05-31 09:54:11 [post_content_filtered] => [post_parent] => 0 [guid] => https://www.anthropocene-curriculum.org/?post_type=contribution&p=44674 [menu_order] => 0 [post_type] => contribution [post_mime_type] => [comment_count] => 0 [filter] => raw ) [687] => Array ( [ID] => 47293 [post_author] => 105 [post_date] => 2022-04-22 09:56:50 [post_date_gmt] => 2022-04-22 07:56:50 [post_content] => [post_title] => Bolen : Holmes – Hourglass River Part 2 [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => bolen-holmes-hourglass-river-part-2 [to_ping] => [pinged] => [post_modified] => 2022-04-22 09:56:50 [post_modified_gmt] => 2022-04-22 07:56:50 [post_content_filtered] => [post_parent] => 46373 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/Bolen-Holmes-–-Hourglass-River-Part-2.pdf [menu_order] => 0 [post_type] => attachment [post_mime_type] => application/pdf [comment_count] => 0 [filter] => raw ) [688] => Array ( [ID] => 46812 [post_author] => 105 [post_date] => 2022-04-22 09:56:25 [post_date_gmt] => 2022-04-22 07:56:25 [post_content] =>

Air pollution is currently the top environmental killer, but the fleeting nature of atmospheric pollution often keeps it from being observed through a global perspective and being included in the planetary cycles of the Anthropocene.

The global expanse of air pollution in the Anthropocene

Air pollution is currently the top environmental killer. The fleeting nature of atmospheric pollution often keeps it from being observed through a global perspective and being included in the planetary cycles of the Anthropocene. Atmosphere enthusiast Riddhima Puri sets out to explore its temporal and spatial scale as part of the intersection between human history and deep geological time. She uncovers the effects of the anthropogenic pollutant black carbon on a journey from the smog-filled streets of St. Louis, Missouri during “Black Tuesday,” 1939, to the burning tropical forests in Indonesian provinces of 2019.

[post_title] => The Breathable Materiality of Combustion [post_excerpt] => [post_status] => publish [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => the-breathable-materiality-of-combustion [to_ping] => [pinged] => [post_modified] => 2022-05-31 14:07:33 [post_modified_gmt] => 2022-05-31 12:07:33 [post_content_filtered] => [post_parent] => 0 [guid] => https://www.anthropocene-curriculum.org/?post_type=contribution&p=46812 [menu_order] => 0 [post_type] => contribution [post_mime_type] => [comment_count] => 0 [filter] => raw ) [689] => Array ( [ID] => 47291 [post_author] => 105 [post_date] => 2022-04-22 09:55:47 [post_date_gmt] => 2022-04-22 07:55:47 [post_content] => [post_title] => Bolen : Holmes – Hourglass River Part 1 [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => bolen-holmes-hourglass-river-part-1 [to_ping] => [pinged] => [post_modified] => 2022-04-22 09:55:47 [post_modified_gmt] => 2022-04-22 07:55:47 [post_content_filtered] => [post_parent] => 46370 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/Bolen-Holmes-–-Hourglass-River-Part-1.pdf [menu_order] => 0 [post_type] => attachment [post_mime_type] => application/pdf [comment_count] => 0 [filter] => raw ) [690] => Array ( [ID] => 45001 [post_author] => 105 [post_date] => 2022-04-22 09:53:08 [post_date_gmt] => 2022-04-22 07:53:08 [post_content] =>

Starting from a review of the Orbis Spike hypothesis, this essay by the Anthropocene historian Franz Mauelshagen compares the early modern “Agrarian Acceleration” during the Little Ice Age with the material world of the twentieth century.

When it comes to Earth system change, what does “anthropogenic” mean? The ongoing debate over pre-twentieth-century markers shows the challenge of attributing evidence of such change unambiguously to collective human agency. Starting from a review of the Orbis Spike hypothesis, this essay by the Anthropocene historian Franz Mauelshagen compares the early modern “Agrarian Acceleration” during the Little Ice Age with the material world of the twentieth century, a century when industrial outputs replaced biomass as the dominant extracted material. This great metabolic anomaly signifies no less than a shift in the meaning of “anthropogenic” itself.

[post_title] => Historical Assessment of the “Anthropogenic” Factor [post_excerpt] => [post_status] => publish [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => historical-assessment-of-the-anthropogenic-factor [to_ping] => [pinged] => [post_modified] => 2022-06-01 10:59:12 [post_modified_gmt] => 2022-06-01 08:59:12 [post_content_filtered] => [post_parent] => 0 [guid] => https://www.anthropocene-curriculum.org/?post_type=contribution&p=45001 [menu_order] => 0 [post_type] => contribution [post_mime_type] => [comment_count] => 0 [filter] => raw ) [691] => Array ( [ID] => 44606 [post_author] => 130 [post_date] => 2022-04-22 09:51:01 [post_date_gmt] => 2022-04-22 07:51:01 [post_content] =>

Geographer and writer Adam Bobbette describes the reciprocal and porous relationship between society and geology in early twentieth-century Java, and Julia Adeney Thomas argues that the novelty of the Anthropocene lies in the shift from local geology to the chronicling of the Earth system

Aren’t we overlooking important traditions when we assert the novelty of a geology that deals with human forces? Geographer and writer Adam Bobbette describes the reciprocal and porous relationship between society and geology in early twentieth-century Java, where volcanological activities were seen as a fundamental expression of social history and vice versa.

 

In a follow-up comment, Japan historian Julia Adeney Thomas points out that the historical and cultural resources that we bring to bear on the unprecedented challenge of the Anthropocene must first recognize our altered reality.

[post_title] => A Javanese Anthropocene? [post_excerpt] => [post_status] => publish [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => a-javanese-anthropocene [to_ping] => [pinged] => [post_modified] => 2022-05-16 12:09:24 [post_modified_gmt] => 2022-05-16 10:09:24 [post_content_filtered] => [post_parent] => 0 [guid] => https://www.anthropocene-curriculum.org/?post_type=contribution&p=44606 [menu_order] => 0 [post_type] => contribution [post_mime_type] => [comment_count] => 0 [filter] => raw ) [692] => Array ( [ID] => 45188 [post_author] => 105 [post_date] => 2022-04-22 09:49:50 [post_date_gmt] => 2022-04-22 07:49:50 [post_content] =>

Constellating three documents that mark a story of changing hopes for a better future, historian Julia Adeney Thomas advocates to recognize the immaterial power of ideas that gave birth to the Anthropocene.

We cannot trace the development of the Anthropocene without understanding the immaterial markers—the hopes as well as the greed—behind the Anthropocene’s physical manifestations. This essay by historian Julia Adeney Thomas argues that modern political ideals of ever-growing liberty, justice, and prosperity shaped Earth’s geology as definitively as did powerful technologies.

[post_title] => Modern Political Hopes as Immaterial Markers of the Anthropocene [post_excerpt] => [post_status] => publish [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => modern-political-hopes-as-immaterial-markers-of-the-anthropocene [to_ping] => [pinged] => [post_modified] => 2022-05-16 12:09:48 [post_modified_gmt] => 2022-05-16 10:09:48 [post_content_filtered] => [post_parent] => 0 [guid] => https://www.anthropocene-curriculum.org/?post_type=contribution&p=45188 [menu_order] => 0 [post_type] => contribution [post_mime_type] => [comment_count] => 0 [filter] => raw ) [693] => Array ( [ID] => 44330 [post_author] => 130 [post_date] => 2022-04-22 09:45:10 [post_date_gmt] => 2022-04-22 07:45:10 [post_content] =>

How can an archaeology of the present address molecules as driving elements of the “Great Acceleration”? Benjamin Steininger contends that the apparatus of catalytic chemistry has triggered a cascade of accelerations which lead to the Anthropocene.

How can an archaeology of the present address molecules as driving elements of the “Great Acceleration”? Benjamin Steininger, cultural theorist and also cultural practitioner, contends that the mobilization of combustion fuel molecules through the technical apparatus of catalytic chemistry has triggered a cascade of accelerations which lead to the fundamental transformation we now call the Anthropocene.

[post_title] => Molecular Mobilization [post_excerpt] => [post_status] => publish [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => molecular-mobilization [to_ping] => [pinged] => [post_modified] => 2022-05-31 14:13:47 [post_modified_gmt] => 2022-05-31 12:13:47 [post_content_filtered] => [post_parent] => 0 [guid] => https://www.anthropocene-curriculum.org/?post_type=contribution&p=44330 [menu_order] => 0 [post_type] => contribution [post_mime_type] => [comment_count] => 0 [filter] => raw ) [694] => Array ( [ID] => 47231 [post_author] => 105 [post_date] => 2022-04-22 09:42:34 [post_date_gmt] => 2022-04-22 07:42:34 [post_content] =>

Christoph Rosol reflects on the disturbing schism between geoscientific insights and the info-capitalist modus operandi diluting these insights to mere noise. Are we ready to comprehend what the Earth has already recorded?

Geology of a Floating Present

There is no clear signal-to-noise ratio when it comes to classifying and reacting to the existential shift now underway. In this political commentary, Anthropocene historian and curator Christoph Rosol reflects on the disturbing schism between geoscientific insights and the info-capitalist modus operandi diluting these insights to mere noise. Are we ready to comprehend what the Earth has already recorded? Are we structurally equipped for what is already happening?

 

[post_title] => When the Signal Disappears in the Noise [post_excerpt] => [post_status] => publish [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => when-the-signal-disappears-in-the-noise [to_ping] => [pinged] => [post_modified] => 2022-05-16 12:10:26 [post_modified_gmt] => 2022-05-16 10:10:26 [post_content_filtered] => [post_parent] => 0 [guid] => https://www.anthropocene-curriculum.org/?post_type=contribution&p=47231 [menu_order] => 0 [post_type] => contribution [post_mime_type] => [comment_count] => 0 [filter] => raw ) [695] => Array ( [ID] => 45654 [post_author] => 103 [post_date] => 2022-04-22 09:41:04 [post_date_gmt] => 2022-04-22 07:41:04 [post_content] => [post_title] => The Technofossil Record: Where Archaeology and Paleontology Meet [post_excerpt] => [post_status] => publish [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => the-technofossil-record-where-archaeology-and-paleontology-meet [to_ping] => [pinged] => [post_modified] => 2022-06-01 15:03:19 [post_modified_gmt] => 2022-06-01 13:03:19 [post_content_filtered] => [post_parent] => 0 [guid] => https://www.anthropocene-curriculum.org/?post_type=contribution&p=45654 [menu_order] => 0 [post_type] => contribution [post_mime_type] => [comment_count] => 0 [filter] => raw ) [696] => Array ( [ID] => 45364 [post_author] => 105 [post_date] => 2022-04-22 09:41:01 [post_date_gmt] => 2022-04-22 07:41:01 [post_content] =>

Venice’s critical environment is a paradigmatic case for comprehending socio-environmental history in dialogue with the Earth sciences.

A Fuzzy Anthropocene Boundary

Venice’s critical environment is a paradigmatic case for comprehending socio-environmental history in dialogue with the Earth sciences. Venice, the water city, and its lagoon offer a multi-layered and very telling case for studying the longue durée of human interventions in local settings, a scale on which natural causes and human agency are usually not so easily separated. The diachronic and cross-disciplinary investigation that Venice invites is what the historian and philosopher Pietro Daniel Omodeo and the applied geologist Sebastiano Trevisani advocate in order to understand the forces that have led the globe to transition into the Anthropocene.

[post_title] => The Critical Environment of the Venice Lagoon [post_excerpt] => [post_status] => publish [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => the-critical-environment-of-the-venice-lagoon [to_ping] => [pinged] => [post_modified] => 2022-05-31 15:16:02 [post_modified_gmt] => 2022-05-31 13:16:02 [post_content_filtered] => [post_parent] => 0 [guid] => https://www.anthropocene-curriculum.org/?post_type=contribution&p=45364 [menu_order] => 0 [post_type] => contribution [post_mime_type] => [comment_count] => 0 [filter] => raw ) [697] => Array ( [ID] => 47030 [post_author] => 105 [post_date] => 2022-04-22 09:40:58 [post_date_gmt] => 2022-04-22 07:40:58 [post_content] => Nuclear winter and other disasters

According to the Nuclear Winter theory, a thermonuclear conflict between the United States and the Soviet Union could cool down the Earth’s temperature to such an extent that it would alter the atmospheric processes as well as the biological components of the planet. Books, articles, and reports on this topic appeared in the 1980s. Films and visuals attracted media attention. But the Nuclear Winter soon became controversial. Lying at the intersection of climate science and biosphere studies, Giulia Rispoli shows how research on the Nuclear Winter became the subject of extensive smear campaigns, missing the occasion to offer a visual prophecy of the Anthropocene.

[post_title] => The Moment We Visualized the Anthropocene [post_excerpt] => [post_status] => publish [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => the-moment-we-visualized-the-anthropocene [to_ping] => [pinged] => [post_modified] => 2022-06-01 13:13:20 [post_modified_gmt] => 2022-06-01 11:13:20 [post_content_filtered] => [post_parent] => 0 [guid] => https://www.anthropocene-curriculum.org/?post_type=contribution&p=47030 [menu_order] => 0 [post_type] => contribution [post_mime_type] => [comment_count] => 0 [filter] => raw ) [698] => Array ( [ID] => 44953 [post_author] => 130 [post_date] => 2022-04-22 09:36:56 [post_date_gmt] => 2022-04-22 07:36:56 [post_content] =>

Literary scholar Eva Horn unpacks air as an environing medium that has always entangled human life and the environment in very specific ways.

Anthropogenic markers signal disruptions, and the disruptions to the atmosphere are one of the most emblematic in this regard. Literary scholar Eva Horn unpacks air as an environing medium that has always entangled human life and the environment in very specific ways. She argues that the manifestations of a disrupted atmosphere—in the form of air pollution, contagion, and as artificial climates and climatic changes—reveal an entire history of multiple models of characterizing human-made transformations.

[post_title] => The Case of Air [post_excerpt] => [post_status] => publish [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => the-case-of-air [to_ping] => [pinged] => [post_modified] => 2022-05-16 12:11:43 [post_modified_gmt] => 2022-05-16 10:11:43 [post_content_filtered] => [post_parent] => 0 [guid] => https://www.anthropocene-curriculum.org/?post_type=contribution&p=44953 [menu_order] => 0 [post_type] => contribution [post_mime_type] => [comment_count] => 0 [filter] => raw ) [699] => Array ( [ID] => 47054 [post_author] => 105 [post_date] => 2022-04-22 09:35:21 [post_date_gmt] => 2022-04-22 07:35:21 [post_content] =>

Christoph Rosol sketches out the marriage of paleoceanography with isotope chemistry in the middle of the twentieth century, part of a synchronism between the onset of the Anthropocene and the emergence of the technical means of understanding it.

There is an astounding synchronism between the onset of the Anthropocene and the emergence of the technical means of registering and understanding it. Science historian Christoph Rosol sketches out the marriage of paleoceanography with isotope chemistry that took place in the middle of the twentieth century, highlighting the interdisciplinary co-evolution of an epistemic practice that sits at the heart of contemporary chronostratigraphy.

[post_title] => A Mid-Twentieth Century Start Date for Anthropocene Geology [post_excerpt] => [post_status] => publish [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => a-mid-twentieth-century-start-date-for-anthropocene-geology [to_ping] => [pinged] => [post_modified] => 2022-06-01 13:12:30 [post_modified_gmt] => 2022-06-01 11:12:30 [post_content_filtered] => [post_parent] => 0 [guid] => https://www.anthropocene-curriculum.org/?post_type=contribution&p=47054 [menu_order] => 0 [post_type] => contribution [post_mime_type] => [comment_count] => 0 [filter] => raw ) [700] => Array ( [ID] => 45648 [post_author] => 103 [post_date] => 2022-04-22 09:33:40 [post_date_gmt] => 2022-04-22 07:33:40 [post_content] => [post_title] => Combustion Products as Markers for the Anthropocene [post_excerpt] => [post_status] => publish [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => combustion-products-as-markers-for-the-anthropocene [to_ping] => [pinged] => [post_modified] => 2022-06-01 14:57:50 [post_modified_gmt] => 2022-06-01 12:57:50 [post_content_filtered] => [post_parent] => 0 [guid] => https://www.anthropocene-curriculum.org/?post_type=contribution&p=45648 [menu_order] => 0 [post_type] => contribution [post_mime_type] => [comment_count] => 0 [filter] => raw ) [701] => Array ( [ID] => 45637 [post_author] => 103 [post_date] => 2022-04-22 09:21:40 [post_date_gmt] => 2022-04-22 07:21:40 [post_content] => [post_title] => Anthropogenic Threats to Ecosystems in the Anthropocene [post_excerpt] => [post_status] => publish [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => anthropogenic-threats-to-ecosystems-in-the-anthropocene [to_ping] => [pinged] => [post_modified] => 2022-06-01 15:04:24 [post_modified_gmt] => 2022-06-01 13:04:24 [post_content_filtered] => [post_parent] => 0 [guid] => https://www.anthropocene-curriculum.org/?post_type=contribution&p=45637 [menu_order] => 0 [post_type] => contribution [post_mime_type] => [comment_count] => 0 [filter] => raw ) [702] => Array ( [ID] => 47081 [post_author] => 105 [post_date] => 2022-04-22 09:20:48 [post_date_gmt] => 2022-04-22 07:20:48 [post_content] =>

We live to burn and we burn to live. Artist Matthew C. Wilson pieces together the pyrogenic deep time of rifts, violent changes that also always produce new possibilities.

We live to burn and we burn to live. Reflecting on the making of a film in a dual excavation site—an archaic hominin archeological site, situated in an open cast coal mine—artist Matthew C. Wilson pieces together the pyrogenic deep time of rifts, violent changes that also always produce new possibilities.

[post_title] => Geological Evidences [post_excerpt] => [post_status] => publish [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => geological-evidences [to_ping] => [pinged] => [post_modified] => 2022-05-31 12:31:10 [post_modified_gmt] => 2022-05-31 10:31:10 [post_content_filtered] => [post_parent] => 0 [guid] => https://www.anthropocene-curriculum.org/?post_type=contribution&p=47081 [menu_order] => 0 [post_type] => contribution [post_mime_type] => [comment_count] => 0 [filter] => raw ) [703] => Array ( [ID] => 45570 [post_author] => 105 [post_date] => 2022-04-22 09:14:58 [post_date_gmt] => 2022-04-22 07:14:58 [post_content] =>

The following essay and mapping exercise on whales reflects on the natural-cultural history of these creatures whose non-human bodies allow for thinking across different aesthetic and epistemic registers.

Aesthetics and the Anthropocene

The following essay and mapping exercise emerge from the conversations and visual research of the Carbon Aesthetics group, which consists of artists and scholars exploring carbon and its relations in the artistic research project of the “Carbon Catalogue.” Focusing on whales—and the way whales are considered as an environmental archive and “no-tech” carbon storage by marine biologists and sustainability economists alike—the group reflects on the natural-cultural history of these creatures whose non-human bodies allow for thinking across different aesthetic and epistemic registers.

Following the essay is a reflection by Bernadette Bensaude-Vincent on how carbon’s ubiquity, connectivity, and scalability allow its aesthetics to open up a new way of “being in-the-world.”

[post_title] => Whale Falls, Carbon Sinks [post_excerpt] => [post_status] => publish [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => whale-falls-carbon-sinks [to_ping] => [pinged] => [post_modified] => 2022-05-31 14:20:48 [post_modified_gmt] => 2022-05-31 12:20:48 [post_content_filtered] => [post_parent] => 0 [guid] => https://www.anthropocene-curriculum.org/?post_type=contribution&p=45570 [menu_order] => 0 [post_type] => contribution [post_mime_type] => [comment_count] => 0 [filter] => raw ) [704] => Array ( [ID] => 44101 [post_author] => 130 [post_date] => 2022-04-22 09:13:42 [post_date_gmt] => 2022-04-22 07:13:42 [post_content] =>

The control of fire plays a fundamental role in human history and cultural evolution. However, with increased anthropogenic combustion of fossil fuels—and, indeed, decreased combustion of biomass—fire acquires novel significance as a potent instrument of geo-technological agency. In this essay, human geographer Nigel Clark discusses fire as an integrative marker of the Anthropocene, positioning it at the momentous interface between Earth system changes and lithic strata.

[post_title] => Anthropogenic Fire as the Hinge between Earth System and Strata [post_excerpt] => [post_status] => publish [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => anthropogenic-fire-as-the-hinge-between-earth-system-and-strata [to_ping] => [pinged] => [post_modified] => 2022-05-31 13:59:21 [post_modified_gmt] => 2022-05-31 11:59:21 [post_content_filtered] => [post_parent] => 0 [guid] => https://www.anthropocene-curriculum.org/?post_type=contribution&p=44101 [menu_order] => 0 [post_type] => contribution [post_mime_type] => [comment_count] => 0 [filter] => raw ) [705] => Array ( [ID] => 44792 [post_author] => 105 [post_date] => 2022-04-22 09:08:54 [post_date_gmt] => 2022-04-22 07:08:54 [post_content] =>

Sebastián Ureta gives a thick description of Anthropocene landscapes where vast, stratified dumps of chemical residues that largely outlive their creators.

On a journey through Chile, Sebastián Ureta gives a thick description of Anthropocene landscapes in which the never-ending pursuit of mineral value extraction leads to environmental devastation and long-term damage of health and well-being. In his multi-part presentation, tailings enact a “geological now” in mining regions, an anthropogenic stratigraphy based not on the remains of large cities or infrastructures, but on vast, stratified dumps of chemical residues that largely outlive their creators.

[post_title] => Tailings and the Onset of a Chilean Anthropocene [post_excerpt] => [post_status] => publish [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => tailings-and-the-onset-of-a-chilean-anthropocene [to_ping] => [pinged] => [post_modified] => 2022-05-16 12:14:00 [post_modified_gmt] => 2022-05-16 10:14:00 [post_content_filtered] => [post_parent] => 0 [guid] => https://www.anthropocene-curriculum.org/?post_type=contribution&p=44792 [menu_order] => 0 [post_type] => contribution [post_mime_type] => [comment_count] => 0 [filter] => raw ) [706] => Array ( [ID] => 45301 [post_author] => 105 [post_date] => 2022-04-22 09:08:00 [post_date_gmt] => 2022-04-22 07:08:00 [post_content] =>

We are live in the venerable International Court of Stratigraphic Arbitration, and on trial is the question whether concrete, the unparalleled material, is indeed an admissible marker for defining the onset of the Anthropocene.

We are live in room number 2022 of the venerable International Court of Stratigraphic Arbitration where two esteemed scholars—an archaeologist and an anthropologist—appeared before the jury. On trial is the question whether concrete, the unparalleled material, is indeed an admissible marker for defining the onset of the Anthropocene. Here is a record of the first day of the hearing.

[post_title] => Concrete: A Stratigraphic Marker for the Anthropocene [post_excerpt] => [post_status] => publish [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => concrete-a-stratigraphic-marker-for-the-anthropocene [to_ping] => [pinged] => [post_modified] => 2022-06-01 12:54:48 [post_modified_gmt] => 2022-06-01 10:54:48 [post_content_filtered] => [post_parent] => 0 [guid] => https://www.anthropocene-curriculum.org/?post_type=contribution&p=45301 [menu_order] => 0 [post_type] => contribution [post_mime_type] => [comment_count] => 0 [filter] => raw ) [707] => Array ( [ID] => 44729 [post_author] => 130 [post_date] => 2022-04-22 09:05:31 [post_date_gmt] => 2022-04-22 07:05:31 [post_content] =>

Faced with the Anthropocene, Marcia Bjornerud sees a set of grave ironies at play that make it hard for any geologist to capture its real meaning. We can only acknowledge these ironies and use them wisely to restore a lost alliance with the Earth.

With the dawning Anthropocene crisis how should we tell the story of our planet? The Earth’s biography is usually described through punctuated events, seeming to alternate between evolution and extinction. However, faced with our proposed new epoch, geologist and writer Marcia Bjornerud sees a set of grave ironies at play that make it hard for any geologist to capture its real meaning. We can only acknowledge these ironies and use them wisely to restore a lost alliance with the Earth.

[post_title] => Ironies of the Anthropocene [post_excerpt] => [post_status] => publish [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => ironies-of-the-anthropocene [to_ping] => [pinged] => [post_modified] => 2022-05-16 12:14:32 [post_modified_gmt] => 2022-05-16 10:14:32 [post_content_filtered] => [post_parent] => 0 [guid] => https://www.anthropocene-curriculum.org/?post_type=contribution&p=44729 [menu_order] => 0 [post_type] => contribution [post_mime_type] => [comment_count] => 0 [filter] => raw ) [708] => Array ( [ID] => 45651 [post_author] => 103 [post_date] => 2022-04-22 09:03:36 [post_date_gmt] => 2022-04-22 07:03:36 [post_content] => [post_title] => Radioactive Fallout as a Marker for the Anthropocene [post_excerpt] => [post_status] => publish [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => radioactive-fallout-as-a-marker-for-the-anthropocene [to_ping] => [pinged] => [post_modified] => 2022-06-01 13:10:08 [post_modified_gmt] => 2022-06-01 11:10:08 [post_content_filtered] => [post_parent] => 0 [guid] => https://www.anthropocene-curriculum.org/?post_type=contribution&p=45651 [menu_order] => 0 [post_type] => contribution [post_mime_type] => [comment_count] => 0 [filter] => raw ) [709] => Array ( [ID] => 45261 [post_author] => 130 [post_date] => 2022-04-22 09:00:45 [post_date_gmt] => 2022-04-22 07:00:45 [post_content] =>

Maria Rentetzi shares a personal encounter during a research trip to Hiroshima. What can we learn from the intense humanity inscribed in gestures of respect and apology to the survivors of the atomic bomb, an event at the dawn of the Anthropocene?

Hiroshima signifies the end of a worldview and the beginning of a different form of civilization. In this contribution, historian of technoscience and gender Maria Rentetzi shares the story of a personal encounter during a research trip to the city that fell victim to the 1945 dropping of the atomic bomb. Can we learn from the intense humanity that is inscribed in gestures of deep respect and apology to the survivors of this horrific event at the dawn of the Anthropocene?

[post_title] => The Japanese Art of Bowing and the Nuclear Anthropocene [post_excerpt] => [post_status] => publish [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => the-japanese-art-of-bowing-and-the-nuclear-anthropocene [to_ping] => [pinged] => [post_modified] => 2022-05-16 12:15:14 [post_modified_gmt] => 2022-05-16 10:15:14 [post_content_filtered] => [post_parent] => 0 [guid] => https://www.anthropocene-curriculum.org/?post_type=contribution&p=45261 [menu_order] => 0 [post_type] => contribution [post_mime_type] => [comment_count] => 0 [filter] => raw ) [710] => Array ( [ID] => 47250 [post_author] => 105 [post_date] => 2022-04-21 23:24:15 [post_date_gmt] => 2022-04-21 21:24:15 [post_content] => Courtesy spurloser [post_title] => adcdc6a96a4f196fcfc9cdcd604e78c5d3c9b178 [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => adcdc6a96a4f196fcfc9cdcd604e78c5d3c9b178 [to_ping] => [pinged] => [post_modified] => 2022-04-21 23:24:49 [post_modified_gmt] => 2022-04-21 21:24:49 [post_content_filtered] => [post_parent] => 47231 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/adcdc6a96a4f196fcfc9cdcd604e78c5d3c9b178.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [711] => Array ( [ID] => 47238 [post_author] => 105 [post_date] => 2022-04-21 22:52:57 [post_date_gmt] => 2022-04-21 20:52:57 [post_content] => [post_title] => Keogh – Ephemeral Biosphere [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => keogh-ephemeral-biosphere [to_ping] => [pinged] => [post_modified] => 2022-04-21 22:52:57 [post_modified_gmt] => 2022-04-21 20:52:57 [post_content_filtered] => [post_parent] => 44887 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/Keogh-–-Ephemeral-Biosphere.pdf [menu_order] => 0 [post_type] => attachment [post_mime_type] => application/pdf [comment_count] => 0 [filter] => raw ) [712] => Array ( [ID] => 47235 [post_author] => 105 [post_date] => 2022-04-21 22:30:47 [post_date_gmt] => 2022-04-21 20:30:47 [post_content] => Source: Jan Zalasiewicz et al., The Anthropocene as a Geological Time Unit, Cambridge University Press, 2019, Figure 2.4.2 [post_title] => Figure 2.4.2 [post_excerpt] => Historical variations of concentrations and mass-accumulation rates of black carbon (BC), char, soot, parent-PAHs, oxygenated PAHs (OPAHs) and azaarenes (AZAs) in the Huguangyan Maar Lake. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => figure-2-4-2 [to_ping] => [pinged] => [post_modified] => 2022-04-22 09:01:27 [post_modified_gmt] => 2022-04-22 07:01:27 [post_content_filtered] => [post_parent] => 47231 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/Figure-2.4.2-.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [713] => Array ( [ID] => 47232 [post_author] => 105 [post_date] => 2022-04-21 21:53:43 [post_date_gmt] => 2022-04-21 19:53:43 [post_content] => Source: Martin J. Head et al., “The Great Acceleration is real and provides a quantitative basis for the proposed Anthropocene Series/Epoch,” Episodes (2021) [post_title] => Key-trends-and-drivers-for-the-Anthropocene-from-the-Late-Pleistocene-to-present-based [post_excerpt] => Key geochemical trends for the Anthropocene from the Late Pleistocene to present, based on ice core records from Greenland, Antarctica, and instrumental data. Panels show prominent deflections of a) carbon dioxide concentrations and isotopic ratio of carbon-13 to carbon 12 (δ13C), b) methane concentration, and c) nitrous oxide concentration together with the nitrogen isotopic composition of nitrate (δ15N-NO3) at the proposed onset of the Anthropocene after a relatively stable period of the Holocene. Panel d) shows global temperature anomalies relative to the 1980–2004 mean. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => key-trends-and-drivers-for-the-anthropocene-from-the-late-pleistocene-to-present-based [to_ping] => [pinged] => [post_modified] => 2022-04-21 23:34:34 [post_modified_gmt] => 2022-04-21 21:34:34 [post_content_filtered] => [post_parent] => 47231 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/Key-trends-and-drivers-for-the-Anthropocene-from-the-Late-Pleistocene-to-present-based.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [714] => Array ( [ID] => 47208 [post_author] => 105 [post_date] => 2022-04-21 20:49:51 [post_date_gmt] => 2022-04-21 18:49:51 [post_content] => Chart by Kira Lappé, © All rights reserved Kira Lappé [post_title] => Fig3 [post_excerpt] => Materials documented in the anthropogenic sediments of the Viennese well logs. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => fig3 [to_ping] => [pinged] => [post_modified] => 2022-04-21 20:54:23 [post_modified_gmt] => 2022-04-21 18:54:23 [post_content_filtered] => [post_parent] => 47201 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/Fig3.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [715] => Array ( [ID] => 47207 [post_author] => 105 [post_date] => 2022-04-21 20:49:49 [post_date_gmt] => 2022-04-21 18:49:49 [post_content] => Map by Kira Lappé, © All rights reserved Kira Lappé [post_title] => Fig2 [post_excerpt] => Thickness of anthropogenic deposits documented in the Viennese well logs (vertical exaggeration by 100). Waste disposal sites are marked in blue, and the historic city center is marked in yellow. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => fig2 [to_ping] => [pinged] => [post_modified] => 2022-04-21 20:50:51 [post_modified_gmt] => 2022-04-21 18:50:51 [post_content_filtered] => [post_parent] => 47201 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/Fig2.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [716] => Array ( [ID] => 47202 [post_author] => 105 [post_date] => 2022-04-21 20:43:13 [post_date_gmt] => 2022-04-21 18:43:13 [post_content] => [post_title] => Hornek : Lappe – Latent Soils [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => hornek-lappe-latent-soils [to_ping] => [pinged] => [post_modified] => 2022-04-21 20:43:13 [post_modified_gmt] => 2022-04-21 18:43:13 [post_content_filtered] => [post_parent] => 46415 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/Hornek-Lappe-–-Latent-Soils.pdf [menu_order] => 0 [post_type] => attachment [post_mime_type] => application/pdf [comment_count] => 0 [filter] => raw ) [717] => Array ( [ID] => 47145 [post_author] => 105 [post_date] => 2022-04-21 16:24:24 [post_date_gmt] => 2022-04-21 14:24:24 [post_content] => Courtesy Stratagrids [post_title] => 6c3f14d5-94ab-4d8c-babb-e2c65f9e522a [post_excerpt] => Stratagrids (Max Stocklosa and Daniel Wolter) 2016 [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 6c3f14d5-94ab-4d8c-babb-e2c65f9e522a [to_ping] => [pinged] => [post_modified] => 2022-04-26 12:30:07 [post_modified_gmt] => 2022-04-26 10:30:07 [post_content_filtered] => [post_parent] => 47078 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2000/04/6c3f14d5-94ab-4d8c-babb-e2c65f9e522a.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [718] => Array ( [ID] => 47125 [post_author] => 105 [post_date] => 2022-04-21 16:00:22 [post_date_gmt] => 2022-04-21 14:00:22 [post_content] => Courtesy NASA, Public Domain [post_title] => 1979px-STS032-72-033_-_View_of_Earth_(Raw_scan)_rescale [post_excerpt] => View of Earth with the SYNCOM IV communications satellite, January 10, 1990. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 1979px-sts032-72-033_-_view_of_earth_raw_scan_rescale [to_ping] => [pinged] => [post_modified] => 2022-04-21 16:44:26 [post_modified_gmt] => 2022-04-21 14:44:26 [post_content_filtered] => [post_parent] => 47078 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/1979px-STS032-72-033_-_View_of_Earth_Raw_scan_rescale.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [719] => Array ( [ID] => 47122 [post_author] => 105 [post_date] => 2022-04-21 15:14:11 [post_date_gmt] => 2022-04-21 13:14:11 [post_content] => Courtesy Museum of New Zealand - Te Papa Tongarewa, CC BY-NC-ND 4.0 [post_title] => 27035734 [post_excerpt] => Plastic cereal collectible Stegosaurus (1962). [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 27035734 [to_ping] => [pinged] => [post_modified] => 2022-04-21 16:45:40 [post_modified_gmt] => 2022-04-21 14:45:40 [post_content_filtered] => [post_parent] => 47078 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/27035734.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [720] => Array ( [ID] => 47121 [post_author] => 105 [post_date] => 2022-04-21 15:12:51 [post_date_gmt] => 2022-04-21 13:12:51 [post_content] => Courtesy Stratagrids [post_title] => 3078ba31-a689-4d4a-ae91-e583e05ab203 [post_excerpt] => Stratagrids (Max Stocklosa and Daniel Wolter) 2016 [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 3078ba31-a689-4d4a-ae91-e583e05ab203 [to_ping] => [pinged] => [post_modified] => 2022-04-26 12:30:02 [post_modified_gmt] => 2022-04-26 10:30:02 [post_content_filtered] => [post_parent] => 47078 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/3078ba31-a689-4d4a-ae91-e583e05ab203.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [721] => Array ( [ID] => 47095 [post_author] => 105 [post_date] => 2022-04-21 13:16:56 [post_date_gmt] => 2022-04-21 11:16:56 [post_content] => © All rights reserved Matthew C. Wilson [post_title] => Geological Evidences_50 [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => geological-evidences_50 [to_ping] => [pinged] => [post_modified] => 2022-04-21 13:19:34 [post_modified_gmt] => 2022-04-21 11:19:34 [post_content_filtered] => [post_parent] => 47081 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/Geological-Evidences_50.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [722] => Array ( [ID] => 47094 [post_author] => 105 [post_date] => 2022-04-21 13:16:48 [post_date_gmt] => 2022-04-21 11:16:48 [post_content] => © All rights reserved Matthew C. Wilson [post_title] => Geological Evidences_47 [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => geological-evidences_47 [to_ping] => [pinged] => [post_modified] => 2022-04-21 13:18:28 [post_modified_gmt] => 2022-04-21 11:18:28 [post_content_filtered] => [post_parent] => 47081 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/Geological-Evidences_47.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [723] => Array ( [ID] => 47093 [post_author] => 105 [post_date] => 2022-04-21 13:16:41 [post_date_gmt] => 2022-04-21 11:16:41 [post_content] => © All rights reserved Matthew C. Wilson [post_title] => Geological Evidences_35 [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => geological-evidences_35 [to_ping] => [pinged] => [post_modified] => 2022-04-21 13:18:25 [post_modified_gmt] => 2022-04-21 11:18:25 [post_content_filtered] => [post_parent] => 47081 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/Geological-Evidences_35.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [724] => Array ( [ID] => 47092 [post_author] => 105 [post_date] => 2022-04-21 13:16:33 [post_date_gmt] => 2022-04-21 11:16:33 [post_content] => © All rights reserved Matthew C. Wilson [post_title] => Geological Evidences_31 [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => geological-evidences_31 [to_ping] => [pinged] => [post_modified] => 2022-04-21 13:19:22 [post_modified_gmt] => 2022-04-21 11:19:22 [post_content_filtered] => [post_parent] => 47081 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/Geological-Evidences_31.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [725] => Array ( [ID] => 47091 [post_author] => 105 [post_date] => 2022-04-21 13:16:25 [post_date_gmt] => 2022-04-21 11:16:25 [post_content] => © All rights reserved Matthew C. Wilson [post_title] => Geological Evidences_26 [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => geological-evidences_26 [to_ping] => [pinged] => [post_modified] => 2022-04-21 13:18:12 [post_modified_gmt] => 2022-04-21 11:18:12 [post_content_filtered] => [post_parent] => 47081 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/Geological-Evidences_26.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [726] => Array ( [ID] => 47090 [post_author] => 105 [post_date] => 2022-04-21 13:16:17 [post_date_gmt] => 2022-04-21 11:16:17 [post_content] => © All rights reserved Matthew C. Wilson [post_title] => Geological Evidences_24 [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => geological-evidences_24 [to_ping] => [pinged] => [post_modified] => 2022-04-21 13:18:58 [post_modified_gmt] => 2022-04-21 11:18:58 [post_content_filtered] => [post_parent] => 47081 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/Geological-Evidences_24.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [727] => Array ( [ID] => 47089 [post_author] => 105 [post_date] => 2022-04-21 13:16:10 [post_date_gmt] => 2022-04-21 11:16:10 [post_content] => © All rights reserved Matthew C. Wilson [post_title] => Geological Evidences_15 [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => geological-evidences_15 [to_ping] => [pinged] => [post_modified] => 2022-04-21 13:18:19 [post_modified_gmt] => 2022-04-21 11:18:19 [post_content_filtered] => [post_parent] => 47081 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/Geological-Evidences_15.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [728] => Array ( [ID] => 47088 [post_author] => 105 [post_date] => 2022-04-21 13:16:02 [post_date_gmt] => 2022-04-21 11:16:02 [post_content] => © All rights reserved Matthew C. Wilson [post_title] => Geological Evidences_12 [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => geological-evidences_12 [to_ping] => [pinged] => [post_modified] => 2022-04-21 13:19:16 [post_modified_gmt] => 2022-04-21 11:19:16 [post_content_filtered] => [post_parent] => 47081 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/Geological-Evidences_12.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [729] => Array ( [ID] => 47087 [post_author] => 105 [post_date] => 2022-04-21 13:15:55 [post_date_gmt] => 2022-04-21 11:15:55 [post_content] => © All rights reserved Matthew C. Wilson [post_title] => Geological Evidences_07 [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => geological-evidences_07 [to_ping] => [pinged] => [post_modified] => 2022-04-21 13:20:37 [post_modified_gmt] => 2022-04-21 11:20:37 [post_content_filtered] => [post_parent] => 47081 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/Geological-Evidences_07.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [730] => Array ( [ID] => 47086 [post_author] => 105 [post_date] => 2022-04-21 13:15:45 [post_date_gmt] => 2022-04-21 11:15:45 [post_content] => © All rights reserved Matthew C. Wilson [post_title] => Geological Evidences_01 [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => geological-evidences_01 [to_ping] => [pinged] => [post_modified] => 2022-04-21 13:18:14 [post_modified_gmt] => 2022-04-21 11:18:14 [post_content_filtered] => [post_parent] => 47081 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/Geological-Evidences_01.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [731] => Array ( [ID] => 47067 [post_author] => 105 [post_date] => 2022-04-20 22:14:53 [post_date_gmt] => 2022-04-20 20:14:53 [post_content] => Photos by Jérôme Kaiser, © all rights reserved Jérôme Kaiser [post_title] => IMG_0877_2 [post_excerpt] => The water-sediment interface in a short sediment core recovered by the multicorer used at the candidate GSSP site of the Baltic Sea. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => img_0877_2 [to_ping] => [pinged] => [post_modified] => 2022-04-20 22:15:40 [post_modified_gmt] => 2022-04-20 20:15:40 [post_content_filtered] => [post_parent] => 45654 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2000/04/IMG_0877_2.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [732] => Array ( [ID] => 47057 [post_author] => 105 [post_date] => 2022-04-20 21:13:18 [post_date_gmt] => 2022-04-20 19:13:18 [post_content] => Courtesy University of Chicago Photographic Archive, Special Collections Research Center, University of Chicago Library [post_title] => urey_emiliani [post_excerpt] => Gerald J. Wasserburg, Cesare Emiliani, and Harold C. Urey in front of a mass spectrometer in Urey’s lab at the University of Chicago, ca. 1953. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => urey_emiliani [to_ping] => [pinged] => [post_modified] => 2022-04-20 21:29:51 [post_modified_gmt] => 2022-04-20 19:29:51 [post_content_filtered] => [post_parent] => 47054 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/urey_emiliani.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [733] => Array ( [ID] => 47056 [post_author] => 105 [post_date] => 2022-04-20 21:13:07 [post_date_gmt] => 2022-04-20 19:13:07 [post_content] => Emil Phillippi, Die Grundproben der Deutschen Südpolar-Expedition 1901–1903, vol. 2. Reimer Verlag, Berlin, 1912, © All rights original publisher [post_title] => Deutsche Suedpolarexpedition_cropped [post_excerpt] => Drilling sites of the “Gauß Expedition” of 1901–1903 in the Southern Atlantic and Indian Ocean. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => deutsche-suedpolarexpedition_cropped [to_ping] => [pinged] => [post_modified] => 2022-04-20 21:14:07 [post_modified_gmt] => 2022-04-20 19:14:07 [post_content_filtered] => [post_parent] => 47054 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/Deutsche-Suedpolarexpedition_cropped.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [734] => Array ( [ID] => 47055 [post_author] => 105 [post_date] => 2022-04-20 21:12:56 [post_date_gmt] => 2022-04-20 19:12:56 [post_content] => Taken from Schott 1952, p. 26, © All rights reserved the original publisher [post_title] => albatross_bohrkerne [post_excerpt] => Schott’s paleotemperature plot, derived from foraminifer quantities. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => albatross_bohrkerne [to_ping] => [pinged] => [post_modified] => 2022-04-20 21:16:49 [post_modified_gmt] => 2022-04-20 19:16:49 [post_content_filtered] => [post_parent] => 47054 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/albatross_bohrkerne.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [735] => Array ( [ID] => 47037 [post_author] => 105 [post_date] => 2022-04-20 19:59:05 [post_date_gmt] => 2022-04-20 17:59:05 [post_content] => copyright unknown [post_title] => Picture4 [post_excerpt] => Cover of the Soviet Journal Priroda, vol. 10. (1983). [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => picture4-4 [to_ping] => [pinged] => [post_modified] => 2022-04-22 08:47:15 [post_modified_gmt] => 2022-04-22 06:47:15 [post_content_filtered] => [post_parent] => 47030 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/Picture4.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [736] => Array ( [ID] => 47036 [post_author] => 105 [post_date] => 2022-04-20 19:59:01 [post_date_gmt] => 2022-04-20 17:59:01 [post_content] => Courtesy CIA, public domain [post_title] => Picture3 [post_excerpt] => Diagram obtained by the CIA from the International Seminar on Nuclear War in Italy 1984. It depicts the findings of Soviet 3-D computer model research on nuclear winter from 1983, and although it contains similar errors as earlier Western models, it was the first 3-D model of nuclear winter. (The three dimensions in the model are longitude, latitude and altitude.) The diagram shows the model’s predictions of global temperature changes after a global nuclear exchange. The top image shows effects after 40 days, the bottom after 243 days. A co-author was Nuclear Winter modeling pioneer Vladimir Alexandrov. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => picture3-4 [to_ping] => [pinged] => [post_modified] => 2022-04-20 20:16:12 [post_modified_gmt] => 2022-04-20 18:16:12 [post_content_filtered] => [post_parent] => 47030 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/Picture3-1.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [737] => Array ( [ID] => 47035 [post_author] => 105 [post_date] => 2022-04-20 19:58:57 [post_date_gmt] => 2022-04-20 17:58:57 [post_content] => © All rights reserved original publisher [post_title] => Picture2 [post_excerpt] => Carl Sagan, et al.'s diagram of the greenhouse effect in "The Climatic Effects of Nuclear War," Scientific American, 251/2 (1984). [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => picture2-4 [to_ping] => [pinged] => [post_modified] => 2022-04-22 08:47:03 [post_modified_gmt] => 2022-04-22 06:47:03 [post_content_filtered] => [post_parent] => 47030 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/Picture2.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [738] => Array ( [ID] => 47034 [post_author] => 105 [post_date] => 2022-04-20 19:58:55 [post_date_gmt] => 2022-04-20 17:58:55 [post_content] => © All rights reserved original publisher [post_title] => Picture1 [post_excerpt] => Cover of The Cold and the Dark by Paul R. Ehrlich et al. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => picture1-6 [to_ping] => [pinged] => [post_modified] => 2022-04-22 08:46:57 [post_modified_gmt] => 2022-04-22 06:46:57 [post_content_filtered] => [post_parent] => 47030 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/Picture1.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [739] => Array ( [ID] => 47033 [post_author] => 105 [post_date] => 2022-04-20 19:58:54 [post_date_gmt] => 2022-04-20 17:58:54 [post_content] => Courtesy John W. Birks, © All rights reserved original publisher [post_title] => Fig.3 [post_excerpt] => Cover of the article co-authored by Paul Crutzen and John W. Birks “The Atmosphere After a Nuclear War: Twilight at Noon.” [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => fig-3 [to_ping] => [pinged] => [post_modified] => 2022-04-22 08:46:51 [post_modified_gmt] => 2022-04-22 06:46:51 [post_content_filtered] => [post_parent] => 47030 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/Fig.3.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [740] => Array ( [ID] => 47018 [post_author] => 105 [post_date] => 2022-04-20 17:03:36 [post_date_gmt] => 2022-04-20 15:03:36 [post_content] => Diagram redesigned by Luis Melendrez Zehfuss [post_title] => critical_environments_Fig1_V2-CORRECTED-01 [post_excerpt] => Major steps in chemostratigraphic studies of environmental change during the Anthropocene. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => critical_environments_fig1_v2-corrected-01 [to_ping] => [pinged] => [post_modified] => 2022-04-21 17:47:19 [post_modified_gmt] => 2022-04-21 15:47:19 [post_content_filtered] => [post_parent] => 45637 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2000/04/critical_environments_Fig1_V2-CORRECTED-01.svg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/svg+xml [comment_count] => 0 [filter] => raw ) [741] => Array ( [ID] => 47008 [post_author] => 99 [post_date] => 2022-04-20 17:00:53 [post_date_gmt] => 2022-04-20 15:00:53 [post_content] => [post_title] => Markers: Material Delineations of the Present [post_excerpt] => [post_status] => publish [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => markers-material-delineations-of-the-present [to_ping] => [pinged] => [post_modified] => 2022-05-17 17:49:57 [post_modified_gmt] => 2022-05-17 15:49:57 [post_content_filtered] => [post_parent] => 0 [guid] => https://www.anthropocene-curriculum.org/?post_type=event&p=47008 [menu_order] => 0 [post_type] => event [post_mime_type] => [comment_count] => 0 [filter] => raw ) [742] => Array ( [ID] => 47009 [post_author] => 105 [post_date] => 2022-04-20 16:10:48 [post_date_gmt] => 2022-04-20 14:10:48 [post_content] => Graph redesigned by Luis Melendrez Zehfuss [post_title] => Anthrobiogeochemcial_Fig3_V3-CORRECTED-01 [post_excerpt] => δ13C variability from Loader et al. 2013 (see footnote 10) for the period 1500–2008 CE measured in tree-ring cellulose for a composite tree ring stable isotope chronology developed using Pinus sylvestris trees from northern Fennoscandia. Fine line represents annually-resolved δ13C variability, thick solid line presents the annual data smoothed with a centrally-weighted 51-year moving average. Dashed line represents the mean δ13C value for the “pre-industrial” period 1500–1799 CE. Mean annual replication for the record is >13 trees. Analytical precision = 0.12 per mil. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => anthrobiogeochemcial_fig3_v3-corrected-01 [to_ping] => [pinged] => [post_modified] => 2022-04-21 16:51:22 [post_modified_gmt] => 2022-04-21 14:51:22 [post_content_filtered] => [post_parent] => 45645 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2000/04/Anthrobiogeochemcial_Fig3_V3-CORRECTED-01.svg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/svg+xml [comment_count] => 0 [filter] => raw ) [743] => Array ( [ID] => 47004 [post_author] => 12 [post_date] => 2022-04-20 15:58:07 [post_date_gmt] => 2022-04-20 13:58:07 [post_content] => [post_title] => Screenshot 2022-04-20 at 15.55.59 [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => screenshot-2022-04-20-at-15-55-59 [to_ping] => [pinged] => [post_modified] => 2022-04-20 15:58:07 [post_modified_gmt] => 2022-04-20 13:58:07 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/Screenshot-2022-04-20-at-15.55.59.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [744] => Array ( [ID] => 46989 [post_author] => 99 [post_date] => 2022-04-20 15:43:47 [post_date_gmt] => 2022-04-20 13:43:47 [post_content] => [post_title] => Postcards from the Anthropocene: Unsettling the Geopolitics of Representation [post_excerpt] => [post_status] => publish [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => postcards-from-the-anthropocene-unsettling-the-geopolitics-of-representation [to_ping] => [pinged] => [post_modified] => 2022-04-20 16:00:29 [post_modified_gmt] => 2022-04-20 14:00:29 [post_content_filtered] => [post_parent] => 0 [guid] => https://www.anthropocene-curriculum.org/?post_type=event&p=46989 [menu_order] => 0 [post_type] => event [post_mime_type] => [comment_count] => 0 [filter] => raw ) [745] => Array ( [ID] => 46992 [post_author] => 105 [post_date] => 2022-04-20 15:39:06 [post_date_gmt] => 2022-04-20 13:39:06 [post_content] => Diagram modified from Gushulak et al. (2021). Photo credit for SEMs of representative benthic and planktonic taxa: Paul Hamilton, Canadian Museum of Nature © All rights reserved [post_title] => BioticChange2-01 [post_excerpt] => Stratigraphically constrained cluster analysis (CONISS) reveals assemblage changes in key benthic (total sum) and planktonic diatom taxa from varved sediments from Crawford Lake. The greatest dissimilarity (total sum of squares) between successive samples distinguishes Zone B (since the early 1980s) from Zone A, which can be divided into subzones A2 and A1 above and below the varves deposited in 1930 CE, with significant changes around 1950 and 1870, respectively. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => bioticchange2-01 [to_ping] => [pinged] => [post_modified] => 2022-05-31 11:50:18 [post_modified_gmt] => 2022-05-31 09:50:18 [post_content_filtered] => [post_parent] => 45642 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2000/04/BioticChange2-01.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [746] => Array ( [ID] => 46991 [post_author] => 105 [post_date] => 2022-04-20 15:36:33 [post_date_gmt] => 2022-04-20 13:36:33 [post_content] => [post_title] => BioticChange24 [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => bioticchange24 [to_ping] => [pinged] => [post_modified] => 2022-04-20 15:36:33 [post_modified_gmt] => 2022-04-20 13:36:33 [post_content_filtered] => [post_parent] => 45642 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2000/04/BioticChange24.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [747] => Array ( [ID] => 46990 [post_author] => 99 [post_date] => 2022-04-20 15:28:19 [post_date_gmt] => 2022-04-20 13:28:19 [post_content] => [post_title] => image [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => image-8 [to_ping] => [pinged] => [post_modified] => 2022-04-20 15:28:19 [post_modified_gmt] => 2022-04-20 13:28:19 [post_content_filtered] => [post_parent] => 46989 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/image.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [748] => Array ( [ID] => 46982 [post_author] => 105 [post_date] => 2022-04-20 15:24:11 [post_date_gmt] => 2022-04-20 13:24:11 [post_content] => Diagram modified from Gushulak et al. (2021). Photo credit for SEMs of representative benthic and planktonic taxa: Paul Hamilton, Canadian Museum of Nature. [post_title] => Biotic-change-01 [post_excerpt] => Stratigraphically constrained cluster analysis (CONISS) reveals assemblage changes in key benthic (total sum) and planktonic diatom taxa from varved sediments from Crawford Lake. The greatest dissimilarity (total sum of squares) between successive samples distinguishes Zone B (since the early 1980s) from Zone A, which can be divided into subzones A2 and A1 above and below the varves deposited in 1930 CE, with significant changes around 1950 and 1870, respectively. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => biotic-change-01 [to_ping] => [pinged] => [post_modified] => 2022-04-20 15:25:54 [post_modified_gmt] => 2022-04-20 13:25:54 [post_content_filtered] => [post_parent] => 45642 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2000/04/Biotic-change-01.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [749] => Array ( [ID] => 46979 [post_author] => 99 [post_date] => 2022-04-20 15:23:54 [post_date_gmt] => 2022-04-20 13:23:54 [post_content] => [post_title] => Landscapes of Injustice [post_excerpt] => [post_status] => publish [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => landscapes-of-injustice-2 [to_ping] => [pinged] => [post_modified] => 2022-04-20 16:01:17 [post_modified_gmt] => 2022-04-20 14:01:17 [post_content_filtered] => [post_parent] => 0 [guid] => https://www.anthropocene-curriculum.org/?post_type=event&p=46979 [menu_order] => 0 [post_type] => event [post_mime_type] => [comment_count] => 0 [filter] => raw ) [750] => Array ( [ID] => 46977 [post_author] => 99 [post_date] => 2022-04-20 15:22:02 [post_date_gmt] => 2022-04-20 13:22:02 [post_content] => [post_title] => image001 [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => image001-3 [to_ping] => [pinged] => [post_modified] => 2022-04-20 15:22:02 [post_modified_gmt] => 2022-04-20 13:22:02 [post_content_filtered] => [post_parent] => 46967 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/image001.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [751] => Array ( [ID] => 46969 [post_author] => 105 [post_date] => 2022-04-20 15:18:20 [post_date_gmt] => 2022-04-20 13:18:20 [post_content] => Diagram modified from Gushulak et al. (2021). Photo credit for SEMs of representative benthic and planktonic taxa: Paul Hamilton, Canadian Museum of Nature. [post_title] => Biotic-change1 [post_excerpt] => Stratigraphically constrained cluster analysis (CONISS) reveals assemblage changes in key benthic (total sum) and planktonic diatom taxa from varved sediments from Crawford Lake. The greatest dissimilarity (total sum of squares) between successive samples distinguishes Zone B (since the early 1980s) from Zone A, which can be divided into subzones A2 and A1 above and below the varves deposited in 1930 CE, with significant changes around 1950 and 1870, respectively. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => biotic-change1 [to_ping] => [pinged] => [post_modified] => 2022-04-20 15:20:28 [post_modified_gmt] => 2022-04-20 13:20:28 [post_content_filtered] => [post_parent] => 45642 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2000/04/Biotic-change1.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [752] => Array ( [ID] => 46967 [post_author] => 99 [post_date] => 2022-04-20 15:17:55 [post_date_gmt] => 2022-04-20 13:17:55 [post_content] => [post_title] => Landscapes of Injustice [post_excerpt] => [post_status] => publish [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => landscapes-of-injustice [to_ping] => [pinged] => [post_modified] => 2022-04-20 16:01:36 [post_modified_gmt] => 2022-04-20 14:01:36 [post_content_filtered] => [post_parent] => 0 [guid] => https://www.anthropocene-curriculum.org/?post_type=event&p=46967 [menu_order] => 0 [post_type] => event [post_mime_type] => [comment_count] => 0 [filter] => raw ) [753] => Array ( [ID] => 46964 [post_author] => 105 [post_date] => 2022-04-20 15:01:08 [post_date_gmt] => 2022-04-20 13:01:08 [post_content] => Photos by Jérôme Kaiser, © all rights reserved Jérôme Kaiser [post_title] => Bjornerud-2 [post_excerpt] => Left: The multicorer used at the candidate GSSP site of the Baltic Sea. Right: The water-sediment interface in a short sediment core recovered by the multicorer. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => bjornerud-2 [to_ping] => [pinged] => [post_modified] => 2022-04-20 15:02:38 [post_modified_gmt] => 2022-04-20 13:02:38 [post_content_filtered] => [post_parent] => 44729 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2000/04/Bjornerud-2.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [754] => Array ( [ID] => 46949 [post_author] => 103 [post_date] => 2022-04-20 12:52:54 [post_date_gmt] => 2022-04-20 10:52:54 [post_content] => [post_title] => amd_landing-teaser_no-text_white [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => amd_landing-teaser_no-text_white [to_ping] => [pinged] => [post_modified] => 2022-04-20 12:52:54 [post_modified_gmt] => 2022-04-20 10:52:54 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/amd_landing-teaser_no-text_white.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [755] => Array ( [ID] => 46948 [post_author] => 103 [post_date] => 2022-04-20 12:49:52 [post_date_gmt] => 2022-04-20 10:49:52 [post_content] => [post_title] => amd_landing-teaser_no-text [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => amd_landing-teaser_no-text [to_ping] => [pinged] => [post_modified] => 2022-04-20 12:49:52 [post_modified_gmt] => 2022-04-20 10:49:52 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/amd_landing-teaser_no-text.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [756] => Array ( [ID] => 46945 [post_author] => 103 [post_date] => 2022-04-20 12:17:55 [post_date_gmt] => 2022-04-20 10:17:55 [post_content] => [post_title] => amd_landing-teaser_white [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => amd_landing-teaser_white [to_ping] => [pinged] => [post_modified] => 2022-04-20 12:17:55 [post_modified_gmt] => 2022-04-20 10:17:55 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/amd_landing-teaser_white.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [757] => Array ( [ID] => 46906 [post_author] => 105 [post_date] => 2022-04-19 16:59:37 [post_date_gmt] => 2022-04-19 14:59:37 [post_content] => Map redesigned by Luis Melendrez Zehfuss [post_title] => Steininger_Fig2_V2_newmap [post_excerpt] => “Location of shipwrecks that were classified to have considerable pollution risk to the environment. The oil has been removed from the wrecks marked with a red circle. Map from NCA.” From: Liv-Guri Faksness, Dag Altin, Per Daling, and Kristin Rist Sørheim, “Report. Potential oil product leakages from World War II shipwrecks- Assessment of possible environmental risk,” SINTEF Materials and Chemistry. Environmental Technology, (September 1, 2016): p. 4. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => steininger_fig2_v2_newmap [to_ping] => [pinged] => [post_modified] => 2022-05-31 14:10:53 [post_modified_gmt] => 2022-05-31 12:10:53 [post_content_filtered] => [post_parent] => 44330 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2000/04/Steininger_Fig2_V2_newmap.svg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/svg+xml [comment_count] => 0 [filter] => raw ) [758] => Array ( [ID] => 46905 [post_author] => 105 [post_date] => 2022-04-19 16:48:53 [post_date_gmt] => 2022-04-19 14:48:53 [post_content] => Chart redesigned by Luis Melendrez Zehfuss [post_title] => Steininger_Fig3_V1_export [post_excerpt] => From: Liv-Guri Faksness, Dag Altin, Per Daling, Kristin Rist Sørheim, “Report. Potential oil product leakages from World War II shipwrecks,” p. 24. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => steininger_fig3_v1_export [to_ping] => [pinged] => [post_modified] => 2022-04-21 19:48:13 [post_modified_gmt] => 2022-04-21 17:48:13 [post_content_filtered] => [post_parent] => 44330 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2000/04/Steininger_Fig3_V1_export.svg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/svg+xml [comment_count] => 0 [filter] => raw ) [759] => Array ( [ID] => 46878 [post_author] => 99 [post_date] => 2022-04-19 16:06:55 [post_date_gmt] => 2022-04-19 14:06:55 [post_content] => [post_title] => Unearthing the Present Full Program [post_excerpt] => [post_status] => publish [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => unearthing-the-present [to_ping] => [pinged] => [post_modified] => 2022-05-23 16:39:15 [post_modified_gmt] => 2022-05-23 14:39:15 [post_content_filtered] => [post_parent] => 0 [guid] => https://www.anthropocene-curriculum.org/?post_type=event&p=46878 [menu_order] => 0 [post_type] => event [post_mime_type] => [comment_count] => 0 [filter] => raw ) [760] => Array ( [ID] => 46872 [post_author] => 105 [post_date] => 2022-04-19 09:48:01 [post_date_gmt] => 2022-04-19 07:48:01 [post_content] => [post_title] => Thames molluscs [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => thames-molluscs [to_ping] => [pinged] => [post_modified] => 2022-04-19 09:48:01 [post_modified_gmt] => 2022-04-19 07:48:01 [post_content_filtered] => [post_parent] => 45642 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2000/04/Thames-molluscs.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [761] => Array ( [ID] => 46869 [post_author] => 105 [post_date] => 2022-04-19 01:05:24 [post_date_gmt] => 2022-04-18 23:05:24 [post_content] => Data sourced from UNSCEAR, 2000 and modified from Waters et al. 2015. Satellite equirectangular projection courtesy NASA. [post_title] => Latitudinal variation_Nasa [post_excerpt] => Figure 2. The locations of significant human contributions to radionuclide signals. The distribution and total fission and fusion yields, in megatons, of atmospheric nuclear weapons tests (those in purple predating the first H-bomb test on November 1, 1952 and those in red following that event) emphasizes the relatively limited scale of the first seven years of testing. The location of significant nuclear accidents/discharges are shown in blue. Superimposed is the latitudinal variation of global strontium-90 fallout, in becquerels per square meter. Note that the yield of tests and hence magnitude of the Sr-90 signal is greatest in the Northern Hemisphere—the mid-latitude Sr-90 peak is controlled by natural atmospheric circulation cells rather than the latitude of maximum detonations. A similar but much smaller peak is seen in the Southern Hemisphere. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => latitudinal-variation_nasa-2 [to_ping] => [pinged] => [post_modified] => 2022-04-19 01:05:50 [post_modified_gmt] => 2022-04-18 23:05:50 [post_content_filtered] => [post_parent] => 45651 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2000/04/Latitudinal-variation_Nasa.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [762] => Array ( [ID] => 46859 [post_author] => 105 [post_date] => 2022-04-19 00:06:10 [post_date_gmt] => 2022-04-18 22:06:10 [post_content] => [post_title] => CC-graphic [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => cc-graphic [to_ping] => [pinged] => [post_modified] => 2022-04-19 00:06:10 [post_modified_gmt] => 2022-04-18 22:06:10 [post_content_filtered] => [post_parent] => 46013 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/CC-graphic.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [763] => Array ( [ID] => 46857 [post_author] => 105 [post_date] => 2022-04-18 22:38:23 [post_date_gmt] => 2022-04-18 20:38:23 [post_content] => [post_title] => Markers-Artworks-Meta-Grey [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => markers-artworks-meta-grey [to_ping] => [pinged] => [post_modified] => 2022-04-18 22:38:38 [post_modified_gmt] => 2022-04-18 20:38:38 [post_content_filtered] => [post_parent] => 45966 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/Markers-Artworks-Meta-Grey.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [764] => Array ( [ID] => 46850 [post_author] => 105 [post_date] => 2022-04-18 12:57:34 [post_date_gmt] => 2022-04-18 10:57:34 [post_content] => Photo by Stephen Himson © All rights reserved Stephen Himson [post_title] => Picture1 [post_excerpt] => The mollusc assemblage of the River Thames near Teddington Lock, Richmond-upon-Thames, UK. Two species of non-native molluscs dominate the river in this area: the zebra mussel, Dreissena polymorpha, and the Asian clam, Corbicula fluminea. C. fluminea was introduced to Europe in 1980 (it entered the Thames in 2004). D. polymorpha was widespread in Europe from the nineteenth century, but only introduced to North America in 1986. Therefore, the first occurrence of D. polymorpha in North America, and the first co-occurrence of C. fluminea with D. polymorpha in Europe, illustrate a potential late-twentieth century chain of correlation. Many other species can be used in this way. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => picture1-5 [to_ping] => [pinged] => [post_modified] => 2022-05-31 11:50:26 [post_modified_gmt] => 2022-05-31 09:50:26 [post_content_filtered] => [post_parent] => 45642 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2000/04/Picture1.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [765] => Array ( [ID] => 46829 [post_author] => 105 [post_date] => 2022-04-15 20:11:50 [post_date_gmt] => 2022-04-15 18:11:50 [post_content] => Image courtesy NASA [post_title] => 207401main_image_989_full [post_excerpt] => A giant brown cloud storm over Asia which appeared over China in April, 2001. The dense portion of air pollution travelled over Japan and the Pacific Ocean, reaching the United States just within a week. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 207401main_image_989_full [to_ping] => [pinged] => [post_modified] => 2022-04-15 20:12:39 [post_modified_gmt] => 2022-04-15 18:12:39 [post_content_filtered] => [post_parent] => 46812 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/207401main_image_989_full.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [766] => Array ( [ID] => 46828 [post_author] => 105 [post_date] => 2022-04-15 20:09:48 [post_date_gmt] => 2022-04-15 18:09:48 [post_content] => Image courtesy Jeff Schmaltz/NASA via Wikimedia, public domain [post_title] => Haze_over_Eastern_China_(15602396765) [post_excerpt] => Haze accumulated over the North China Plain in October, 2014. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => haze_over_eastern_china_15602396765 [to_ping] => [pinged] => [post_modified] => 2022-04-15 20:11:23 [post_modified_gmt] => 2022-04-15 18:11:23 [post_content_filtered] => [post_parent] => 46812 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/Haze_over_Eastern_China_15602396765.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [767] => Array ( [ID] => 46827 [post_author] => 105 [post_date] => 2022-04-15 20:07:30 [post_date_gmt] => 2022-04-15 18:07:30 [post_content] => Courtesy Wikimedia [post_title] => 2448px-Burned_Stubble_in_a_Paddy_Field_After_the_Harvest_in_West,_Bengal,_India [post_excerpt] => Ashes of burnt stubble in a paddy field in harvesting in West Bengal, India. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 2448px-burned_stubble_in_a_paddy_field_after_the_harvest_in_west_bengal_india [to_ping] => [pinged] => [post_modified] => 2022-04-15 20:08:33 [post_modified_gmt] => 2022-04-15 18:08:33 [post_content_filtered] => [post_parent] => 46812 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/2448px-Burned_Stubble_in_a_Paddy_Field_After_the_Harvest_in_West_Bengal_India.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [768] => Array ( [ID] => 46826 [post_author] => 105 [post_date] => 2022-04-15 20:06:44 [post_date_gmt] => 2022-04-15 18:06:44 [post_content] => Image courtesy Jeff Schmaltz/NASA via Wikimedia, public domain [post_title] => Aerial_view_of_Air_Pollution_in_North_India,_Agriculture_Fires,_November_2013 [post_excerpt] => Smoke from agricultural fires in Punjab, north of India, being carried along the Himalayas and accumulating over the National Capital Region (Delhi with urban areas of State neighbors), mixing with urban and industrial smog. (November, 2013) [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => aerial_view_of_air_pollution_in_north_india_agriculture_fires_november_2013 [to_ping] => [pinged] => [post_modified] => 2022-04-15 20:09:32 [post_modified_gmt] => 2022-04-15 18:09:32 [post_content_filtered] => [post_parent] => 46812 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/Aerial_view_of_Air_Pollution_in_North_India_Agriculture_Fires_November_2013.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [769] => Array ( [ID] => 46825 [post_author] => 105 [post_date] => 2022-04-15 20:01:09 [post_date_gmt] => 2022-04-15 18:01:09 [post_content] => Feburary 15, 2019 Sentinel data via Wikimedia, CC BY-SA IGO 3.0 [post_title] => 2560px-Palm_oil_plantations_ESA19484729 [post_excerpt] => Palm oil plantations in East Kalimantan (the Indonesian part of the island Borneo) showing various stages of deforestation—the green patches show the established plantations and the brown ones show the newly-harvested land. Tropical rainforests are cleared in the area to make room for palm oil production. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 2560px-palm_oil_plantations_esa19484729 [to_ping] => [pinged] => [post_modified] => 2022-04-15 20:06:08 [post_modified_gmt] => 2022-04-15 18:06:08 [post_content_filtered] => [post_parent] => 46812 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/2560px-Palm_oil_plantations_ESA19484729.jpeg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [770] => Array ( [ID] => 46824 [post_author] => 105 [post_date] => 2022-04-15 19:58:40 [post_date_gmt] => 2022-04-15 17:58:40 [post_content] => Image courtesy Wakx via >a href="https://en.wikipedia.org/wiki/File:Riau_deforestation_2006.jpg">Wikimedia, cc-by-sa-2.0 [post_title] => Riau_deforestation_2006 [post_excerpt] => Remains of sawn wood from the deforestation in Indragiri Hulu, the Riau Province of Indonesia, for palm oil production (2006). [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => riau_deforestation_2006 [to_ping] => [pinged] => [post_modified] => 2022-04-15 20:00:54 [post_modified_gmt] => 2022-04-15 18:00:54 [post_content_filtered] => [post_parent] => 46812 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/Riau_deforestation_2006.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [771] => Array ( [ID] => 46823 [post_author] => 105 [post_date] => 2022-04-15 19:56:09 [post_date_gmt] => 2022-04-15 17:56:09 [post_content] => Image courtesy Joshua Stevens/NASA, Wikimedia, public domain [post_title] => Satellite_image_of_2019_Southeast_Asian_haze_in_Borneo_-_20190915 [post_excerpt] => Another satellite image of Kalimantan (as part of Borneo) on fire with the resulting haze from Sumatra and Kalimantan forest fires hanging over the surrounding areas (September 15, 2019). [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => satellite_image_of_2019_southeast_asian_haze_in_borneo_-_20190915 [to_ping] => [pinged] => [post_modified] => 2022-04-15 19:58:01 [post_modified_gmt] => 2022-04-15 17:58:01 [post_content_filtered] => [post_parent] => 46812 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/Satellite_image_of_2019_Southeast_Asian_haze_in_Borneo_-_20190915.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [772] => Array ( [ID] => 46822 [post_author] => 105 [post_date] => 2022-04-15 19:56:08 [post_date_gmt] => 2022-04-15 17:56:08 [post_content] => Image courtesy Jeff Schmaltz/NASA, Wikimedia, public domain [post_title] => Satellite_image_of_2013_Southeast_Asian_haze_-_20130619_(annotated) [post_excerpt] => A satellite image capturing smoke blowing from forest fires on the island of Sumatra in Indonesia, crossing over to Singapore and Malaysia due to seasonal wind (June 19, 2013). The fires were lit, despite local laws prohibiting it, to clear the forests during the dry season to prepare the soil for a new crop cycle. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => satellite_image_of_2013_southeast_asian_haze_-_20130619_annotated [to_ping] => [pinged] => [post_modified] => 2022-04-15 19:58:07 [post_modified_gmt] => 2022-04-15 17:58:07 [post_content_filtered] => [post_parent] => 46812 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/Satellite_image_of_2013_Southeast_Asian_haze_-_20130619_annotated.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [773] => Array ( [ID] => 46821 [post_author] => 105 [post_date] => 2022-04-15 19:54:41 [post_date_gmt] => 2022-04-15 17:54:41 [post_content] => Image courtesy Jeff Schmaltz/NASA, Wikimedia, public domain [post_title] => Borneo_fires_October_2006 [post_excerpt] => A satellite image of the island Borneo (shared by Malaysia, Brunei, and Indonesia) in Southeast Asia engulfed by smoke on October 5, 2006. The locations marked in red (in the south) are fires detected in Kalimantan, the Indonesian portion of the island. The haze from the fires is blown northwards by the regional wind, giving rise to transboundary pollution. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => borneo_fires_october_2006 [to_ping] => [pinged] => [post_modified] => 2022-04-15 19:58:11 [post_modified_gmt] => 2022-04-15 17:58:11 [post_content_filtered] => [post_parent] => 46812 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/Borneo_fires_October_2006.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [774] => Array ( [ID] => 46818 [post_author] => 105 [post_date] => 2022-04-15 19:52:39 [post_date_gmt] => 2022-04-15 17:52:39 [post_content] => Courtesy Wikimedia [post_title] => [post_excerpt] => Smog (measured as tropospheric ozone) over Indonesia and the Indian Ocean on October 22, 1997. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => idl-tiff-file-3 [to_ping] => [pinged] => [post_modified] => 2022-04-15 19:53:16 [post_modified_gmt] => 2022-04-15 17:53:16 [post_content_filtered] => [post_parent] => 46812 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/TOMS_indonesia_smog_lrg.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [775] => Array ( [ID] => 46817 [post_author] => 105 [post_date] => 2022-04-15 19:50:36 [post_date_gmt] => 2022-04-15 17:50:36 [post_content] => Courtesy Wikimedia [post_title] => Peatland Burn [post_excerpt] => A guard extinguishing a peat fire, which can last for months as smoldering fire in the underground peat layer, remaining undetected and reigniting once an oxygen source is present. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => peatland-burn [to_ping] => [pinged] => [post_modified] => 2022-04-15 19:51:26 [post_modified_gmt] => 2022-04-15 17:51:26 [post_content_filtered] => [post_parent] => 46812 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/Marking_the_Fire.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [776] => Array ( [ID] => 46816 [post_author] => 105 [post_date] => 2022-04-15 19:49:30 [post_date_gmt] => 2022-04-15 17:49:30 [post_content] => Courtesy Library of Congress, public domain [post_title] => donora_mill [post_excerpt] => A wire mill on the banks of the Monongahela River in Donora, Pennsylvania in 1910. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => donora_mill [to_ping] => [pinged] => [post_modified] => 2022-04-15 19:49:57 [post_modified_gmt] => 2022-04-15 17:49:57 [post_content_filtered] => [post_parent] => 46812 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/donora_mill.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [777] => Array ( [ID] => 46815 [post_author] => 105 [post_date] => 2022-04-15 19:46:38 [post_date_gmt] => 2022-04-15 17:46:38 [post_content] => Courtesy Igors Jefimovs, Wikimedia, CC-BY-3.0 [post_title] => Smog over Almaty [post_excerpt] => Smog trapped over Almaty, Kazakhstan (January 2014). [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => smog-over-almaty [to_ping] => [pinged] => [post_modified] => 2022-04-21 19:50:41 [post_modified_gmt] => 2022-04-21 17:50:41 [post_content_filtered] => [post_parent] => 46812 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/Smog_over_Almaty.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [778] => Array ( [ID] => 46814 [post_author] => 105 [post_date] => 2022-04-15 19:43:16 [post_date_gmt] => 2022-04-15 17:43:16 [post_content] => Photograph courtesy Wikimedia, public domain [post_title] => Tokyo_Jinzo_Hiryo [post_excerpt] => Factories in Tokyo (1908). [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => tokyo_jinzo_hiryo [to_ping] => [pinged] => [post_modified] => 2022-05-31 14:00:48 [post_modified_gmt] => 2022-05-31 12:00:48 [post_content_filtered] => [post_parent] => 46812 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/Tokyo_Jinzo_Hiryo.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [779] => Array ( [ID] => 46813 [post_author] => 105 [post_date] => 2022-04-15 19:43:14 [post_date_gmt] => 2022-04-15 17:43:14 [post_content] => Photograph courtesy Wikimedia, public domain [post_title] => Osaka_Ryuso [post_excerpt] => Factories in Osaka (1908). [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => osaka_ryuso [to_ping] => [pinged] => [post_modified] => 2022-05-31 14:00:51 [post_modified_gmt] => 2022-05-31 12:00:51 [post_content_filtered] => [post_parent] => 46812 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/Osaka_Ryuso.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [780] => Array ( [ID] => 46809 [post_author] => 105 [post_date] => 2022-04-14 21:51:29 [post_date_gmt] => 2022-04-14 19:51:29 [post_content] => Poster by Henry Eveleigh, Wikimedia, public domain; World Trade Week poster Courtesy of the US National Archives and Records Administration, Wikimedia, public domain [post_title] => Thomas-1 [post_excerpt] => Left: Henry Eveleigh’s 1947 “tree of peace” poster, which won first prize at an international poster contest organized by the United Nations. Right: A 1947 poster stressing the role of global trade in international cooperation created by the US Chamber of Commerce. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => thomas-1 [to_ping] => [pinged] => [post_modified] => 2022-04-14 21:51:58 [post_modified_gmt] => 2022-04-14 19:51:58 [post_content_filtered] => [post_parent] => 45188 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/Thomas-1.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [781] => Array ( [ID] => 46800 [post_author] => 105 [post_date] => 2022-04-14 21:17:36 [post_date_gmt] => 2022-04-14 19:17:36 [post_content] => Photo by Jerome Kaiser, © all rights reserved Jerome Kaiser [post_title] => Bjornerud-1 [post_excerpt] => Left: The multicorer used at the GSSP site in the Baltic Sea. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => bjornerud-1 [to_ping] => [pinged] => [post_modified] => 2022-04-19 21:17:31 [post_modified_gmt] => 2022-04-19 19:17:31 [post_content_filtered] => [post_parent] => 44729 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/Bjornerud-1.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [782] => Array ( [ID] => 46791 [post_author] => 105 [post_date] => 2022-04-14 20:57:54 [post_date_gmt] => 2022-04-14 18:57:54 [post_content] => Courtesy Colin Donihue, © all rights reserved Colin Donihue [post_title] => Anolis_Carolinensis_trio_crop [post_excerpt] => An Anolis carolinensis lizard, holding on to a branch during a strong gust of wind. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => anolis_carolinensis_trio_crop [to_ping] => [pinged] => [post_modified] => 2022-04-20 15:07:57 [post_modified_gmt] => 2022-04-20 13:07:57 [post_content_filtered] => [post_parent] => 44729 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/Anolis_Carolinensis_trio_crop.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [783] => Array ( [ID] => 46784 [post_author] => 105 [post_date] => 2022-04-14 20:43:49 [post_date_gmt] => 2022-04-14 18:43:49 [post_content] => Photo by Sebastiano Trevisani [post_title] => outletMalamoccoA [post_excerpt] => A detail of the Malamocco inlet, in the area of deployment of the 19 mobile barriers. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => outletmalamoccoa [to_ping] => [pinged] => [post_modified] => 2022-04-14 20:45:17 [post_modified_gmt] => 2022-04-14 18:45:17 [post_content_filtered] => [post_parent] => 45364 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/outletMalamoccoA.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [784] => Array ( [ID] => 46781 [post_author] => 105 [post_date] => 2022-04-14 20:15:47 [post_date_gmt] => 2022-04-14 18:15:47 [post_content] => Photo by Photoholgic via Unsplash [post_title] => photoholgic-wZTiKB6rQYY-unsplash [post_excerpt] => Aerial view of high-rise buildings covered with smoke in Shanghai, China. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => photoholgic-wztikb6rqyy-unsplash [to_ping] => [pinged] => [post_modified] => 2022-04-14 20:23:08 [post_modified_gmt] => 2022-04-14 18:23:08 [post_content_filtered] => [post_parent] => 44953 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/03/photoholgic-wZTiKB6rQYY-unsplash.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [785] => Array ( [ID] => 46778 [post_author] => 105 [post_date] => 2022-04-14 19:57:32 [post_date_gmt] => 2022-04-14 17:57:32 [post_content] => Diagram from Gerhard H. Lehmann, ABC des Erdöls, Band 5, Heidelberg: Shell-Bücherei, 1955, p. 35 © all rights reserved original publisher [post_title] => 7_Molekulare-Mobilisierung-rescaled [post_excerpt] => “Molecular Mobilization,” a “simplified flowchart of the SHELL Oil company Montreal East Refinery,” showing the intermediate stage between crude oil (far left) and various applications (far right), including tap and vacuum distillation units [Tapdistillation and Vakuumdestillation], catalytic and thermal cracking units [Katal. Krackanlage/Therm. Krackanlage], gas separation [Gastrennung], and polymerization. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 7_molekulare-mobilisierung-rescaled [to_ping] => [pinged] => [post_modified] => 2022-05-31 14:10:31 [post_modified_gmt] => 2022-05-31 12:10:31 [post_content_filtered] => [post_parent] => 44330 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/7_Molekulare-Mobilisierung-rescaled.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [786] => Array ( [ID] => 46755 [post_author] => 105 [post_date] => 2022-04-14 18:24:13 [post_date_gmt] => 2022-04-14 16:24:13 [post_content] => [post_title] => Walker_cover [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => walker_cover [to_ping] => [pinged] => [post_modified] => 2022-04-14 18:24:13 [post_modified_gmt] => 2022-04-14 16:24:13 [post_content_filtered] => [post_parent] => 44879 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/Walker_cover.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [787] => Array ( [ID] => 46753 [post_author] => 105 [post_date] => 2022-04-14 18:21:44 [post_date_gmt] => 2022-04-14 16:21:44 [post_content] => [post_title] => CIRCUMV_lead [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => circumv_lead [to_ping] => [pinged] => [post_modified] => 2022-04-14 18:21:44 [post_modified_gmt] => 2022-04-14 16:21:44 [post_content_filtered] => [post_parent] => 46431 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/CIRCUMV_lead.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [788] => Array ( [ID] => 46751 [post_author] => 105 [post_date] => 2022-04-14 18:20:02 [post_date_gmt] => 2022-04-14 16:20:02 [post_content] => [post_title] => Salome Rodeck and Matthew C. Wilson in Conversation [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => salome-rodeck-and-matthew-c-wilson-in-conversation [to_ping] => [pinged] => [post_modified] => 2022-04-14 18:20:02 [post_modified_gmt] => 2022-04-14 16:20:02 [post_content_filtered] => [post_parent] => 45047 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/03/Salome-Rodeck-and-Matthew-C.-Wilson-in-Conversation.pdf [menu_order] => 0 [post_type] => attachment [post_mime_type] => application/pdf [comment_count] => 0 [filter] => raw ) [789] => Array ( [ID] => 46746 [post_author] => 105 [post_date] => 2022-04-14 18:07:24 [post_date_gmt] => 2022-04-14 16:07:24 [post_content] => Photo by Jens Ziehe. Julian Charrière, VG Bild-Kunst, Bonn, Germany © all rights reserved [post_title] => HAM 2021 [post_excerpt] => Weight of Shadows, 2021, installation view, Weight of Shadows, Prix Marcel Duchamp, Centre Pompidou, Paris, France, 2021. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => ham-2021-3 [to_ping] => [pinged] => [post_modified] => 2022-05-31 11:38:42 [post_modified_gmt] => 2022-05-31 09:38:42 [post_content_filtered] => [post_parent] => 44795 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/07_JulianCharriere_WeightOfShadows_2021_PureWaste_2021_REPLACE.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [790] => Array ( [ID] => 46739 [post_author] => 105 [post_date] => 2022-04-14 17:40:28 [post_date_gmt] => 2022-04-14 15:40:28 [post_content] => [post_title] => Revolutionaceae [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => revolutionaceae [to_ping] => [pinged] => [post_modified] => 2022-04-14 17:40:28 [post_modified_gmt] => 2022-04-14 15:40:28 [post_content_filtered] => [post_parent] => 46738 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/Revolutionaceae.pdf [menu_order] => 0 [post_type] => attachment [post_mime_type] => application/pdf [comment_count] => 0 [filter] => raw ) [791] => Array ( [ID] => 46736 [post_author] => 105 [post_date] => 2022-04-14 17:39:54 [post_date_gmt] => 2022-04-14 15:39:54 [post_content] => [post_title] => Circumvehoraceae [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => circumvehoraceae [to_ping] => [pinged] => [post_modified] => 2022-04-14 17:39:54 [post_modified_gmt] => 2022-04-14 15:39:54 [post_content_filtered] => [post_parent] => 46735 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/Circumvehoraceae.pdf [menu_order] => 0 [post_type] => attachment [post_mime_type] => application/pdf [comment_count] => 0 [filter] => raw ) [792] => Array ( [ID] => 46733 [post_author] => 105 [post_date] => 2022-04-14 17:38:10 [post_date_gmt] => 2022-04-14 15:38:10 [post_content] => [post_title] => Terraformidaea [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => terraformidaea [to_ping] => [pinged] => [post_modified] => 2022-04-14 17:38:10 [post_modified_gmt] => 2022-04-14 15:38:10 [post_content_filtered] => [post_parent] => 46732 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/Terraformidaea.pdf [menu_order] => 0 [post_type] => attachment [post_mime_type] => application/pdf [comment_count] => 0 [filter] => raw ) [793] => Array ( [ID] => 46730 [post_author] => 105 [post_date] => 2022-04-14 17:37:34 [post_date_gmt] => 2022-04-14 15:37:34 [post_content] => [post_title] => Obscureae [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => obscureae [to_ping] => [pinged] => [post_modified] => 2022-04-14 17:37:34 [post_modified_gmt] => 2022-04-14 15:37:34 [post_content_filtered] => [post_parent] => 46729 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/Obscureae.pdf [menu_order] => 0 [post_type] => attachment [post_mime_type] => application/pdf [comment_count] => 0 [filter] => raw ) [794] => Array ( [ID] => 46727 [post_author] => 105 [post_date] => 2022-04-14 17:37:02 [post_date_gmt] => 2022-04-14 15:37:02 [post_content] => [post_title] => Colombianae:Praedoraceae [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => colombianaepraedoraceae [to_ping] => [pinged] => [post_modified] => 2022-04-14 17:37:02 [post_modified_gmt] => 2022-04-14 15:37:02 [post_content_filtered] => [post_parent] => 46726 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/ColombianaePraedoraceae.pdf [menu_order] => 0 [post_type] => attachment [post_mime_type] => application/pdf [comment_count] => 0 [filter] => raw ) [795] => Array ( [ID] => 46724 [post_author] => 105 [post_date] => 2022-04-14 17:36:21 [post_date_gmt] => 2022-04-14 15:36:21 [post_content] => [post_title] => Colonariales [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => colonariales [to_ping] => [pinged] => [post_modified] => 2022-04-14 17:36:21 [post_modified_gmt] => 2022-04-14 15:36:21 [post_content_filtered] => [post_parent] => 46723 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/Colonariales.pdf [menu_order] => 0 [post_type] => attachment [post_mime_type] => application/pdf [comment_count] => 0 [filter] => raw ) [796] => Array ( [ID] => 46721 [post_author] => 105 [post_date] => 2022-04-14 17:35:32 [post_date_gmt] => 2022-04-14 15:35:32 [post_content] => [post_title] => Capitalospermae [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => capitalospermae [to_ping] => [pinged] => [post_modified] => 2022-04-14 17:35:32 [post_modified_gmt] => 2022-04-14 15:35:32 [post_content_filtered] => [post_parent] => 46720 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/Capitalospermae.pdf [menu_order] => 0 [post_type] => attachment [post_mime_type] => application/pdf [comment_count] => 0 [filter] => raw ) [797] => Array ( [ID] => 46718 [post_author] => 105 [post_date] => 2022-04-14 17:34:00 [post_date_gmt] => 2022-04-14 15:34:00 [post_content] => [post_title] => Atmosphanae [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => atmosphanae [to_ping] => [pinged] => [post_modified] => 2022-04-14 17:34:00 [post_modified_gmt] => 2022-04-14 15:34:00 [post_content_filtered] => [post_parent] => 46717 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/Atmosphanae.pdf [menu_order] => 0 [post_type] => attachment [post_mime_type] => application/pdf [comment_count] => 0 [filter] => raw ) [798] => Array ( [ID] => 46715 [post_author] => 105 [post_date] => 2022-04-14 17:29:36 [post_date_gmt] => 2022-04-14 15:29:36 [post_content] => [post_title] => Autosuffocoaceae [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => autosuffocoaceae [to_ping] => [pinged] => [post_modified] => 2022-04-14 17:29:36 [post_modified_gmt] => 2022-04-14 15:29:36 [post_content_filtered] => [post_parent] => 45043 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/03/Autosuffocoaceae.pdf [menu_order] => 0 [post_type] => attachment [post_mime_type] => application/pdf [comment_count] => 0 [filter] => raw ) [799] => Array ( [ID] => 46712 [post_author] => 105 [post_date] => 2022-04-14 17:10:31 [post_date_gmt] => 2022-04-14 15:10:31 [post_content] => Reproduced from Stephen J. Pyne, The Pyrocene: How we Created an Age of Fire, and what Happens Next. University of California Press: Oakland, CA, 2021 © all rights reserved UC Press [post_title] => Pyne_Clark-final [post_excerpt] => Two fires, competing: US burned area (in 1,000 acres, left axis) and fossil fuel emissions (in metric tons carbon, right axis). Data is from Carbon Dioxide Information Analysis Center, US Department of Energy and National Interagency Fire Center. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => pyne_clark-final [to_ping] => [pinged] => [post_modified] => 2022-05-31 13:51:03 [post_modified_gmt] => 2022-05-31 11:51:03 [post_content_filtered] => [post_parent] => 44101 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/Pyne_Clark-final.svg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/svg+xml [comment_count] => 0 [filter] => raw ) [800] => Array ( [ID] => 46702 [post_author] => 105 [post_date] => 2022-04-14 16:11:11 [post_date_gmt] => 2022-04-14 14:11:11 [post_content] => [post_title] => IMAGE-1-Kew-WC [post_excerpt] => The Wardian case was a portable airtight greenhouse developed by Nathaniel Bagshaw Ward to protect live plant material during transportation [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => image-1-kew-wc [to_ping] => [pinged] => [post_modified] => 2022-04-14 16:11:11 [post_modified_gmt] => 2022-04-14 14:11:11 [post_content_filtered] => [post_parent] => 44887 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/03/IMAGE-1-Kew-WC.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [801] => Array ( [ID] => 46670 [post_author] => 105 [post_date] => 2022-04-14 14:09:22 [post_date_gmt] => 2022-04-14 12:09:22 [post_content] => Photo courtesy National Nuclear Security Administration / Nevada Site Office via wikimedia, public domain [post_title] => Nuclear_spectators [post_excerpt] => NATO observers attending an above-ground nuclear test in the Nevada desert, May 28, 1957. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => nuclear_spectators [to_ping] => [pinged] => [post_modified] => 2022-04-14 14:11:53 [post_modified_gmt] => 2022-04-14 12:11:53 [post_content_filtered] => [post_parent] => 45651 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/Nuclear_spectators.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [802] => Array ( [ID] => 46669 [post_author] => 105 [post_date] => 2022-04-14 14:04:43 [post_date_gmt] => 2022-04-14 12:04:43 [post_content] => Photo courtesy National Nuclear Security Administration / Nevada Site Office via wikimedia, public domain [post_title] => Operation_Plumbbob_-_Hood [post_excerpt] => An above-ground nuclear test on Yucca Flat in the Nevada desert, July 5, 1957. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => operation_plumbbob_-_hood [to_ping] => [pinged] => [post_modified] => 2022-04-14 14:11:31 [post_modified_gmt] => 2022-04-14 12:11:31 [post_content_filtered] => [post_parent] => 45651 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/Operation_Plumbbob_-_Hood.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [803] => Array ( [ID] => 46629 [post_author] => 105 [post_date] => 2022-04-13 17:59:54 [post_date_gmt] => 2022-04-13 15:59:54 [post_content] => Photo by Strat188, wikimedia [post_title] => Plastics_in_strata [post_excerpt] => As high tides and storm surges erode the landfill deposits at East Tilbury, sheet plastics dumped in the 1980s emerge from the low receding cliffs, to be swept out onto the river and eventually out to sea. Such modern forms of plastic are found only in the upper layers. Lower layers contain earlier forms of plastic such as bakelite. In fact this landfill, started in the late nineteenth century, may comprise a stratigraphic record of almost the entire history of plastics. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => plastics_in_strata [to_ping] => [pinged] => [post_modified] => 2022-04-21 18:25:51 [post_modified_gmt] => 2022-04-21 16:25:51 [post_content_filtered] => [post_parent] => 45654 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/Plastics_in_strata.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [804] => Array ( [ID] => 46624 [post_author] => 105 [post_date] => 2022-04-13 17:46:07 [post_date_gmt] => 2022-04-13 15:46:07 [post_content] => Photo by LeRoy Woodson for the EPA DOCUMERICA program (1972–1977), Wikimedia, public domain [post_title] => CHIMNEYS_OF_U.S._STEEL_PLANT_EMIT_SMOKE_24_HOURS_A_DAY_-_NARA_-_545435 [post_excerpt] => Chimneys of the U.S. Steel Plant, Birmingham, Alabama, 1972. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => chimneys_of_u-s-_steel_plant_emit_smoke_24_hours_a_day_-_nara_-_545435 [to_ping] => [pinged] => [post_modified] => 2022-04-14 11:44:04 [post_modified_gmt] => 2022-04-14 09:44:04 [post_content_filtered] => [post_parent] => 45648 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/CHIMNEYS_OF_U.S._STEEL_PLANT_EMIT_SMOKE_24_HOURS_A_DAY_-_NARA_-_545435.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [805] => Array ( [ID] => 46605 [post_author] => 105 [post_date] => 2022-04-13 16:44:18 [post_date_gmt] => 2022-04-13 14:44:18 [post_content] => © all rights reserved Fred Dott/Greenpeace [post_title] => German Plastic Waste Found in MalaysiaPlastikmuell aus Deutschland in Malaysia [post_excerpt] => When control mechanisms fail: German plastic waste is not sent to Malaysia for recycling purposes only. It also lands in local landfills. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => german-plastic-waste-found-in-malaysiaplastikmuell-aus-deutschland-in-malaysia [to_ping] => [pinged] => [post_modified] => 2022-04-13 16:45:29 [post_modified_gmt] => 2022-04-13 14:45:29 [post_content_filtered] => [post_parent] => 44742 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/GP1STUJ5_PressMedia.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [806] => Array ( [ID] => 46587 [post_author] => 103 [post_date] => 2022-04-13 10:12:08 [post_date_gmt] => 2022-04-13 08:12:08 [post_content] =>
Anthropogenic Markers:
Stratigraphy and Context
[post_title] => amd_landing_teaser [post_excerpt] =>
PUBLICATION
[post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => amd_landing_teaser [to_ping] => [pinged] => [post_modified] => 2022-05-18 11:54:29 [post_modified_gmt] => 2022-05-18 09:54:29 [post_content_filtered] => [post_parent] => 0 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/amd_landing_teaser.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [807] => Array ( [ID] => 46563 [post_author] => 105 [post_date] => 2022-04-11 18:13:55 [post_date_gmt] => 2022-04-11 16:13:55 [post_content] => Courtesy Arturo Volantines, public domain [post_title] => Picture3 [post_excerpt] => Portrait of Teresa Blanco. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => picture3-3 [to_ping] => [pinged] => [post_modified] => 2022-04-11 18:23:14 [post_modified_gmt] => 2022-04-11 16:23:14 [post_content_filtered] => [post_parent] => 44778 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/Picture3.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [808] => Array ( [ID] => 46562 [post_author] => 105 [post_date] => 2022-04-11 18:13:51 [post_date_gmt] => 2022-04-11 16:13:51 [post_content] => Courtesy Fundación Terram [post_title] => Picture5 [post_excerpt] => An “animita” or popular memorial built in memory of the Chamorro Galvez family near their submerged home. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => picture5 [to_ping] => [pinged] => [post_modified] => 2022-04-12 15:16:32 [post_modified_gmt] => 2022-04-12 13:16:32 [post_content_filtered] => [post_parent] => 44778 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/Picture5.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [809] => Array ( [ID] => 46557 [post_author] => 105 [post_date] => 2022-04-11 17:49:03 [post_date_gmt] => 2022-04-11 15:49:03 [post_content] => © all rights reserved Julian Charrière, VG Bild-Kunst, Bonn, Germany [post_title] => Julian Charrière - Able - First Light, 2016 (copyright the artist; VG Bild-Kunst, Bonn, Germany)-scaled [post_excerpt] => Able - First Light, 2016. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => julian-charriere-able-first-light-2016-copyright-the-artist-vg-bild-kunst-bonn-germany-scaled [to_ping] => [pinged] => [post_modified] => 2022-04-11 17:49:30 [post_modified_gmt] => 2022-04-11 15:49:30 [post_content_filtered] => [post_parent] => 45260 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/Julian-Charrière-Able-First-Light-2016-copyright-the-artist-VG-Bild-Kunst-Bonn-Germany-scaled-1.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [810] => Array ( [ID] => 46556 [post_author] => 105 [post_date] => 2022-04-11 17:46:13 [post_date_gmt] => 2022-04-11 15:46:13 [post_content] => © all rights reserved Julian Charrière, VG Bild-Kunst, Bonn, Germany [post_title] => Julian Charrière - Sycamore - First Light, 2016 (copyright the artist; VG Bild-Kunst, Bonn, Germany) [post_excerpt] => Sycamore - First Light, 2016. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => julian-charriere-sycamore-first-light-2016-copyright-the-artist-vg-bild-kunst-bonn-germany [to_ping] => [pinged] => [post_modified] => 2022-04-11 17:46:31 [post_modified_gmt] => 2022-04-11 15:46:31 [post_content_filtered] => [post_parent] => 45260 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/Julian-Charrière-Sycamore-First-Light-2016-copyright-the-artist-VG-Bild-Kunst-Bonn-Germany.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [811] => Array ( [ID] => 46555 [post_author] => 105 [post_date] => 2022-04-11 17:40:25 [post_date_gmt] => 2022-04-11 15:40:25 [post_content] => © all rights reserved Julian Charrière, VG Bild-Kunst, Bonn, Germany [post_title] => JulianCharriere_Enyu-IV-TerminalBeach_2016_CopyrightTheArtist_VGBildKunstBonnGermany [post_excerpt] => Enyu IV - Terminal Beach, 2016 [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => juliancharriere_enyu-iv-terminalbeach_2016_copyrighttheartist_vgbildkunstbonngermany [to_ping] => [pinged] => [post_modified] => 2022-04-11 17:45:39 [post_modified_gmt] => 2022-04-11 15:45:39 [post_content_filtered] => [post_parent] => 45260 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/JulianCharriere_Enyu-IV-TerminalBeach_2016_CopyrightTheArtist_VGBildKunstBonnGermany.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [812] => Array ( [ID] => 46554 [post_author] => 105 [post_date] => 2022-04-11 17:40:07 [post_date_gmt] => 2022-04-11 15:40:07 [post_content] => © all rights reserved Julian Charrière, VG Bild-Kunst, Bonn, Germany [post_title] => JulianCharriere_Eneman-III-TerminalBeach_2016_CopyrightTheArtist_VGBildKunstBonnGermany [post_excerpt] => Eneman III – Terminal Beach, 2016 [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => juliancharriere_eneman-iii-terminalbeach_2016_copyrighttheartist_vgbildkunstbonngermany [to_ping] => [pinged] => [post_modified] => 2022-04-11 17:45:32 [post_modified_gmt] => 2022-04-11 15:45:32 [post_content_filtered] => [post_parent] => 45260 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/JulianCharriere_Eneman-III-TerminalBeach_2016_CopyrightTheArtist_VGBildKunstBonnGermany.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [813] => Array ( [ID] => 46553 [post_author] => 105 [post_date] => 2022-04-11 17:39:49 [post_date_gmt] => 2022-04-11 15:39:49 [post_content] => © all rights reserved Julian Charrière, VG Bild-Kunst, Bonn, Germany [post_title] => JulianCharriere_Aomen-III-TerminalBeach_2016_CopyrightTheArtist_VGBildKunstBonnGermany [post_excerpt] => Aomen III - Terminal Beach, 2016. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => juliancharriere_aomen-iii-terminalbeach_2016_copyrighttheartist_vgbildkunstbonngermany [to_ping] => [pinged] => [post_modified] => 2022-04-11 17:45:22 [post_modified_gmt] => 2022-04-11 15:45:22 [post_content_filtered] => [post_parent] => 45260 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/JulianCharriere_Aomen-III-TerminalBeach_2016_CopyrightTheArtist_VGBildKunstBonnGermany.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [814] => Array ( [ID] => 46545 [post_author] => 105 [post_date] => 2022-04-11 17:03:20 [post_date_gmt] => 2022-04-11 15:03:20 [post_content] => Julian Charrière, VG Bild-Kunst, Bonn, Germany © all rights reserved [post_title] => JulianCharriere_PureWaste_2021_VideoStill_CopyrightTheArtist_VGBildKunstBonnGermany_Scale [post_excerpt] => Video still from Pure Waste, 2021. Pure Waste (FHD color video, 16:10 aspect ratio, stereo sound, 05 minutes 30 seconds). [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => juliancharriere_purewaste_2021_videostill_copyrighttheartist_vgbildkunstbonngermany_scale [to_ping] => [pinged] => [post_modified] => 2022-05-31 11:39:04 [post_modified_gmt] => 2022-05-31 09:39:04 [post_content_filtered] => [post_parent] => 44795 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/JulianCharriere_PureWaste_2021_VideoStill_CopyrightTheArtist_VGBildKunstBonnGermany_Scale.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [815] => Array ( [ID] => 46535 [post_author] => 105 [post_date] => 2022-04-11 16:35:53 [post_date_gmt] => 2022-04-11 14:35:53 [post_content] => Courtesy Christoph Rosol [post_title] => IMG_3184 [post_excerpt] => The Raffineria Porto Marghera, across the lagoon from Venice. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => img_3184 [to_ping] => [pinged] => [post_modified] => 2022-04-11 16:39:15 [post_modified_gmt] => 2022-04-11 14:39:15 [post_content_filtered] => [post_parent] => 45364 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/IMG_3184.m4v [menu_order] => 0 [post_type] => attachment [post_mime_type] => video/mp4 [comment_count] => 0 [filter] => raw ) [816] => Array ( [ID] => 46534 [post_author] => 105 [post_date] => 2022-04-11 16:35:40 [post_date_gmt] => 2022-04-11 14:35:40 [post_content] => Photograph courtesy Christoph Rosol [post_title] => IMG_3182 [post_excerpt] => The Raffineria Porto Marghera, across the lagoon from Venice. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => img_3182 [to_ping] => [pinged] => [post_modified] => 2022-05-31 15:15:56 [post_modified_gmt] => 2022-05-31 13:15:56 [post_content_filtered] => [post_parent] => 45364 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/IMG_3182.jpeg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [817] => Array ( [ID] => 46533 [post_author] => 105 [post_date] => 2022-04-11 16:35:36 [post_date_gmt] => 2022-04-11 14:35:36 [post_content] => Courtesy Christoph Rosol [post_title] => IMG_3392 [post_excerpt] => The MOSE structure. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => img_3392 [to_ping] => [pinged] => [post_modified] => 2022-04-11 16:38:33 [post_modified_gmt] => 2022-04-11 14:38:33 [post_content_filtered] => [post_parent] => 45364 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/IMG_3392.jpeg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [818] => Array ( [ID] => 46511 [post_author] => 105 [post_date] => 2022-04-11 14:31:38 [post_date_gmt] => 2022-04-11 12:31:38 [post_content] => Sentinel data 2022, CC BY-SA IGO 3.0 [post_title] => T20LLR_20210920T143729_TCI_crop3 [post_excerpt] => Agricultural section in western Amazonia. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => t20llr_20210920t143729_tci_crop3 [to_ping] => [pinged] => [post_modified] => 2022-04-22 10:53:32 [post_modified_gmt] => 2022-04-22 08:53:32 [post_content_filtered] => [post_parent] => 45201 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/03/T20LLR_20210920T143729_TCI_crop3.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [819] => Array ( [ID] => 46510 [post_author] => 105 [post_date] => 2022-04-11 14:30:57 [post_date_gmt] => 2022-04-11 12:30:57 [post_content] => Sentinel data 2022, CC BY-SA IGO 3.0 [post_title] => T20LLR_20210920T143729_TCI_crop2 [post_excerpt] => Agricultural section in western Amazonia. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => t20llr_20210920t143729_tci_crop2 [to_ping] => [pinged] => [post_modified] => 2022-04-22 10:53:20 [post_modified_gmt] => 2022-04-22 08:53:20 [post_content_filtered] => [post_parent] => 45201 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/03/T20LLR_20210920T143729_TCI_crop2.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [820] => Array ( [ID] => 46509 [post_author] => 105 [post_date] => 2022-04-11 14:30:14 [post_date_gmt] => 2022-04-11 12:30:14 [post_content] => Sentinel data 2022, CC BY-SA IGO 3.0 [post_title] => T20LLR_20210920T143729_TCI_crop1 [post_excerpt] => Agricultural section in western Amazonia. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => t20llr_20210920t143729_tci_crop1 [to_ping] => [pinged] => [post_modified] => 2022-04-22 10:53:13 [post_modified_gmt] => 2022-04-22 08:53:13 [post_content_filtered] => [post_parent] => 45201 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/03/T20LLR_20210920T143729_TCI_crop1.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [821] => Array ( [ID] => 46507 [post_author] => 105 [post_date] => 2022-04-11 13:50:56 [post_date_gmt] => 2022-04-11 11:50:56 [post_content] => [post_title] => HOURGLASS_COVER [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => screenshot-2022-04-11-at-13-49-51-anthropocene-curriculum-%e2%86%92-home [to_ping] => [pinged] => [post_modified] => 2022-04-11 13:51:11 [post_modified_gmt] => 2022-04-11 11:51:11 [post_content_filtered] => [post_parent] => 46363 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/Screenshot-2022-04-11-at-13-49-51-Anthropocene-Curriculum-→-Home.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [822] => Array ( [ID] => 46503 [post_author] => 105 [post_date] => 2022-04-11 13:41:47 [post_date_gmt] => 2022-04-11 11:41:47 [post_content] => [post_title] => Screenshot 2022-04-11 at 13-41-07 hourglass river [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => screenshot-2022-04-11-at-13-41-07-hourglass-river [to_ping] => [pinged] => [post_modified] => 2022-04-11 13:41:47 [post_modified_gmt] => 2022-04-11 11:41:47 [post_content_filtered] => [post_parent] => 46365 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/Screenshot-2022-04-11-at-13-41-07-hourglass-river.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [823] => Array ( [ID] => 46453 [post_author] => 105 [post_date] => 2022-04-10 08:41:54 [post_date_gmt] => 2022-04-10 06:41:54 [post_content] => [post_title] => COL_key [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => screenshot-2022-04-10-at-08-29-49-anthropocene-curriculum-%e2%86%92-home [to_ping] => [pinged] => [post_modified] => 2022-04-10 08:42:30 [post_modified_gmt] => 2022-04-10 06:42:30 [post_content_filtered] => [post_parent] => 46427 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/Screenshot-2022-04-10-at-08-29-49-Anthropocene-Curriculum-→-Home.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png 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[post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => screenshot-2022-04-10-at-08-38-50-anthropocene-curriculum-%e2%86%92-home [to_ping] => [pinged] => [post_modified] => 2022-04-10 08:40:35 [post_modified_gmt] => 2022-04-10 06:40:35 [post_content_filtered] => [post_parent] => 46433 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/Screenshot-2022-04-10-at-08-38-50-Anthropocene-Curriculum-→-Home.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [826] => Array ( [ID] => 46421 [post_author] => 105 [post_date] => 2022-04-09 18:56:46 [post_date_gmt] => 2022-04-09 16:56:46 [post_content] => [post_title] => Vienna-Materials [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => vienna-materials [to_ping] => [pinged] => [post_modified] => 2022-04-09 18:56:46 [post_modified_gmt] => 2022-04-09 16:56:46 [post_content_filtered] => [post_parent] => 46420 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/Vienna-Materials.xlsx [menu_order] => 0 [post_type] => attachment [post_mime_type] => application/vnd.openxmlformats-officedocument.spreadsheetml.sheet [comment_count] => 0 [filter] => raw ) [827] => Array ( [ID] => 46417 [post_author] => 105 [post_date] => 2022-04-09 18:50:19 [post_date_gmt] => 2022-04-09 16:50:19 [post_content] => [post_title] => 4_Vienna_Lappé_page_proof_1 [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 4_vienna_lappe_page_proof_1 [to_ping] => [pinged] => [post_modified] => 2022-04-09 18:50:19 [post_modified_gmt] => 2022-04-09 16:50:19 [post_content_filtered] => [post_parent] => 46415 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/4_Vienna_Lappé_page_proof_1.pdf [menu_order] => 0 [post_type] => attachment [post_mime_type] => application/pdf [comment_count] => 0 [filter] => raw ) [828] => Array ( [ID] => 46416 [post_author] => 105 [post_date] => 2022-04-09 18:49:02 [post_date_gmt] => 2022-04-09 16:49:02 [post_content] => Public domain [post_title] => Suess_Vienna_Map [post_excerpt] => The first geological map of Vienna by Eduard Suess (1862), already including anthropogenic deposits (Schutt). [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => suess_vienna_map [to_ping] => [pinged] => [post_modified] => 2022-04-11 13:30:21 [post_modified_gmt] => 2022-04-11 11:30:21 [post_content_filtered] => [post_parent] => 46415 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/Suess_Vienna_Map.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [829] => Array ( [ID] => 46404 [post_author] => 105 [post_date] => 2022-04-09 18:18:33 [post_date_gmt] => 2022-04-09 16:18:33 [post_content] => [post_title] => Aspanggruende [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => aspanggruende [to_ping] => [pinged] => [post_modified] => 2022-04-09 18:18:33 [post_modified_gmt] => 2022-04-09 16:18:33 [post_content_filtered] => [post_parent] => 44540 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/02/Aspanggruende.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [830] => Array ( [ID] => 46401 [post_author] => 105 [post_date] => 2022-04-09 18:16:43 [post_date_gmt] => 2022-04-09 16:16:43 [post_content] => [post_title] => Boden_von_Wien [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => boden_von_wien [to_ping] => [pinged] => [post_modified] => 2022-04-09 18:16:43 [post_modified_gmt] => 2022-04-09 16:16:43 [post_content_filtered] => [post_parent] => 44514 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/02/Boden_von_Wien.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [831] => Array ( [ID] => 46396 [post_author] => 105 [post_date] => 2022-04-09 17:55:18 [post_date_gmt] => 2022-04-09 15:55:18 [post_content] => [post_title] => Rennweg52 [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => rennweg52 [to_ping] => [pinged] => [post_modified] => 2022-04-09 17:55:18 [post_modified_gmt] => 2022-04-09 15:55:18 [post_content_filtered] => [post_parent] => 44545 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/Rennweg52.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [832] => Array ( [ID] => 46394 [post_author] => 105 [post_date] => 2022-04-09 17:53:43 [post_date_gmt] => 2022-04-09 15:53:43 [post_content] => [post_title] => Knocken_Rennweg [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => knocken_rennweg [to_ping] => [pinged] => [post_modified] => 2022-04-09 17:53:43 [post_modified_gmt] => 2022-04-09 15:53:43 [post_content_filtered] => [post_parent] => 44543 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/Knocken_Rennweg.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [833] => Array ( [ID] => 46389 [post_author] => 105 [post_date] => 2022-04-09 17:44:02 [post_date_gmt] => 2022-04-09 15:44:02 [post_content] => [post_title] => Wipplingerstrasse [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => wipplingerstrasse [to_ping] => [pinged] => [post_modified] => 2022-04-09 17:44:02 [post_modified_gmt] => 2022-04-09 15:44:02 [post_content_filtered] => [post_parent] => 44547 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/02/Wipplingerstrasse.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [834] => Array ( [ID] => 46386 [post_author] => 105 [post_date] => 2022-04-09 08:15:01 [post_date_gmt] => 2022-04-09 06:15:01 [post_content] => Photo by Brian Holmes [post_title] => Upper_Old_River [post_excerpt] => Cypress swamp, Upper Old River. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => upper_old_river [to_ping] => [pinged] => [post_modified] => 2022-04-22 09:53:33 [post_modified_gmt] => 2022-04-22 07:53:33 [post_content_filtered] => [post_parent] => 46379 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/Upper_Old_River.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [835] => Array ( [ID] => 46385 [post_author] => 105 [post_date] => 2022-04-09 08:14:48 [post_date_gmt] => 2022-04-09 06:14:48 [post_content] => Photo by Brian Holmes [post_title] => Overbank_Structure [post_excerpt] => Overbank structure. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => overbank_structure [to_ping] => [pinged] => [post_modified] => 2022-04-22 09:53:27 [post_modified_gmt] => 2022-04-22 07:53:27 [post_content_filtered] => [post_parent] => 46379 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/Overbank_Structure.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [836] => Array ( [ID] => 46384 [post_author] => 105 [post_date] => 2022-04-09 08:14:35 [post_date_gmt] => 2022-04-09 06:14:35 [post_content] => Photo by Brian Holmes [post_title] => Overbank_sign [post_excerpt] => Signage for Old River complex. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => overbank_sign [to_ping] => [pinged] => [post_modified] => 2022-04-22 09:53:21 [post_modified_gmt] => 2022-04-22 07:53:21 [post_content_filtered] => [post_parent] => 46379 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/Overbank_sign.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [837] => Array ( [ID] => 46383 [post_author] => 105 [post_date] => 2022-04-09 08:14:07 [post_date_gmt] => 2022-04-09 06:14:07 [post_content] => Photo by Brian Holmes [post_title] => Auxilliary_Structure [post_excerpt] => Auxiliary structure. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => auxilliary_structure [to_ping] => [pinged] => [post_modified] => 2022-05-17 14:28:56 [post_modified_gmt] => 2022-05-17 12:28:56 [post_content_filtered] => [post_parent] => 46379 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/Auxilliary_Structure.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [838] => Array ( [ID] => 46382 [post_author] => 105 [post_date] => 2022-04-09 08:12:16 [post_date_gmt] => 2022-04-09 06:12:16 [post_content] => Photo by Brian Holmes [post_title] => Lock_and_dam [post_excerpt] => Lock and dam. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => lock_and_dam [to_ping] => [pinged] => [post_modified] => 2022-04-22 09:53:11 [post_modified_gmt] => 2022-04-22 07:53:11 [post_content_filtered] => [post_parent] => 46379 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/Lock_and_dam.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [839] => Array ( [ID] => 46381 [post_author] => 105 [post_date] => 2022-04-09 08:12:03 [post_date_gmt] => 2022-04-09 06:12:03 [post_content] => Photo by Brian Holmes [post_title] => Control_structure [post_excerpt] => Control structure. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => control_structure [to_ping] => [pinged] => [post_modified] => 2022-04-22 09:53:03 [post_modified_gmt] => 2022-04-22 07:53:03 [post_content_filtered] => [post_parent] => 46379 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/Control_structure.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [840] => Array ( [ID] => 46380 [post_author] => 105 [post_date] => 2022-04-09 08:11:04 [post_date_gmt] => 2022-04-09 06:11:04 [post_content] => Map by the authors [post_title] => ORCS [post_excerpt] => 1. Hydroelectric dam, constructed by City of Vidalia, US Army Corps of Engineers (USACE), and Catalyst Old River Hydroelectric, 1985-89. 2. Overbank structure, constructed by USACE, 1956-59. 3. Low sill structure, constructed by USACE, 1955-59. 4. Auxiliary structure, constructed by USACE, 1981-86. 5. Lock and Dam, constructed by USACE, 1958-1962. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => orcs [to_ping] => [pinged] => [post_modified] => 2022-04-22 09:52:56 [post_modified_gmt] => 2022-04-22 07:52:56 [post_content_filtered] => [post_parent] => 46379 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/ORCS.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [841] => Array ( [ID] => 46377 [post_author] => 105 [post_date] => 2022-04-09 08:08:17 [post_date_gmt] => 2022-04-09 06:08:17 [post_content] => [post_title] => HourglassRiver-Part3 [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => hourglassriver-part3 [to_ping] => [pinged] => [post_modified] => 2022-04-09 08:08:17 [post_modified_gmt] => 2022-04-09 06:08:17 [post_content_filtered] => [post_parent] => 46376 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/HourglassRiver-Part3.pdf [menu_order] => 0 [post_type] => attachment [post_mime_type] => application/pdf [comment_count] => 0 [filter] => raw ) [842] => Array ( [ID] => 46374 [post_author] => 105 [post_date] => 2022-04-09 08:06:30 [post_date_gmt] => 2022-04-09 06:06:30 [post_content] => [post_title] => HourglassRiver-Part2 [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => hourglassriver-part2 [to_ping] => [pinged] => [post_modified] => 2022-04-09 08:06:30 [post_modified_gmt] => 2022-04-09 06:06:30 [post_content_filtered] => [post_parent] => 46373 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/HourglassRiver-Part2.pdf [menu_order] => 0 [post_type] => attachment [post_mime_type] => application/pdf [comment_count] => 0 [filter] => raw ) [843] => Array ( [ID] => 46371 [post_author] => 105 [post_date] => 2022-04-09 08:04:18 [post_date_gmt] => 2022-04-09 06:04:18 [post_content] => [post_title] => HourglassRiver-Part1 [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => hourglassriver-part1 [to_ping] => [pinged] => [post_modified] => 2022-04-09 08:04:18 [post_modified_gmt] => 2022-04-09 06:04:18 [post_content_filtered] => [post_parent] => 46370 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/HourglassRiver-Part1.pdf [menu_order] => 0 [post_type] => attachment [post_mime_type] => application/pdf [comment_count] => 0 [filter] => raw ) [844] => Array ( [ID] => 46368 [post_author] => 105 [post_date] => 2022-04-09 07:58:03 [post_date_gmt] => 2022-04-09 05:58:03 [post_content] => [post_title] => Screenshot 2022-04-09 at 07-57-32 an anthropocene river [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => screenshot-2022-04-09-at-07-57-32-an-anthropocene-river [to_ping] => [pinged] => [post_modified] => 2022-04-09 07:58:03 [post_modified_gmt] => 2022-04-09 05:58:03 [post_content_filtered] => [post_parent] => 46365 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/Screenshot-2022-04-09-at-07-57-32-an-anthropocene-river.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [845] => Array ( [ID] => 46359 [post_author] => 105 [post_date] => 2022-04-08 16:49:47 [post_date_gmt] => 2022-04-08 14:49:47 [post_content] => Courtesy Die Äußere-Kennzeichen-Sammlung von Abraham-Gottlob Werner, TU Bergakademie Freiberg. [post_title] => 111244_001-a [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 111244_001-a [to_ping] => [pinged] => [post_modified] => 2022-04-22 10:24:03 [post_modified_gmt] => 2022-04-22 08:24:03 [post_content_filtered] => [post_parent] => 44798 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/111244_001-a.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [846] => Array ( [ID] => 46358 [post_author] => 105 [post_date] => 2022-04-08 16:49:46 [post_date_gmt] => 2022-04-08 14:49:46 [post_content] => Courtesy Die Äußere-Kennzeichen-Sammlung von Abraham-Gottlob Werner, TU Bergakademie Freiberg. Gerhard Heide, Andreas Massanek, Beata Heide, Photography: Susanne Paskoff, Freiberg (Inv.-Nr.: 111021 / 111050 / 111105 / 111114 / 111125 / 111244) [post_title] => 111125_001-a [post_excerpt] => 6 of 249 brightly colored plates, which helped to classify minerals according to criteria which were still accessible to human sensual perception. Fabricated from Meissen porcelain after 1814, the plates now form an important part of Abraham Gottlob Werner’s comprehensive object collection on “outward criteria” of minerals. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 111125_001-a [to_ping] => [pinged] => [post_modified] => 2022-04-22 10:24:01 [post_modified_gmt] => 2022-04-22 08:24:01 [post_content_filtered] => [post_parent] => 44798 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/111125_001-a.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [847] => Array ( [ID] => 46357 [post_author] => 105 [post_date] => 2022-04-08 16:49:45 [post_date_gmt] => 2022-04-08 14:49:45 [post_content] => Courtesy Die Äußere-Kennzeichen-Sammlung von Abraham-Gottlob Werner, TU Bergakademie Freiberg. [post_title] => 111114_001-a [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 111114_001-a [to_ping] => [pinged] => [post_modified] => 2022-04-22 10:24:04 [post_modified_gmt] => 2022-04-22 08:24:04 [post_content_filtered] => [post_parent] => 44798 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/111114_001-a.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [848] => Array ( [ID] => 46356 [post_author] => 105 [post_date] => 2022-04-08 16:49:44 [post_date_gmt] => 2022-04-08 14:49:44 [post_content] => Courtesy Die Äußere-Kennzeichen-Sammlung von Abraham-Gottlob Werner, TU Bergakademie Freiberg. [post_title] => 111105_003-a [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 111105_003-a [to_ping] => [pinged] => [post_modified] => 2022-04-22 10:24:06 [post_modified_gmt] => 2022-04-22 08:24:06 [post_content_filtered] => [post_parent] => 44798 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/111105_003-a.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [849] => Array ( [ID] => 46355 [post_author] => 105 [post_date] => 2022-04-08 16:49:43 [post_date_gmt] => 2022-04-08 14:49:43 [post_content] => Courtesy Die Äußere-Kennzeichen-Sammlung von Abraham-Gottlob Werner, TU Bergakademie Freiberg. [post_title] => 111050_001-a [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 111050_001-a [to_ping] => [pinged] => [post_modified] => 2022-04-22 10:24:08 [post_modified_gmt] => 2022-04-22 08:24:08 [post_content_filtered] => [post_parent] => 44798 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/111050_001-a.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [850] => Array ( [ID] => 46354 [post_author] => 105 [post_date] => 2022-04-08 16:49:42 [post_date_gmt] => 2022-04-08 14:49:42 [post_content] => Courtesy Die Äußere-Kennzeichen-Sammlung von Abraham-Gottlob Werner, TU Bergakademie Freiberg. [post_title] => 111021_001-a [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => 111021_001-a [to_ping] => [pinged] => [post_modified] => 2022-04-22 10:24:09 [post_modified_gmt] => 2022-04-22 08:24:09 [post_content_filtered] => [post_parent] => 44798 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/111021_001-a.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [851] => Array ( [ID] => 46349 [post_author] => 105 [post_date] => 2022-04-08 16:44:31 [post_date_gmt] => 2022-04-08 14:44:31 [post_content] => Courtesy Collections patrimoniales numérisées des bibliothèques de l'Université de Strasbourg, public domain [post_title] => coll12_95006_crop3 [post_excerpt] => Section of a larger broadsheet showing a classification of minerals according criteria that are accessible to human sensual perception. Abraham Gottlob Werner grouped according to species, families and “clanship.” Broadsheet 530 x 730 mm by Joseph Lindauer entitled “Werner's neuestes Mineral-Sistem [sic].“ München 1816. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => coll12_95006_crop3 [to_ping] => [pinged] => [post_modified] => 2022-04-22 10:20:30 [post_modified_gmt] => 2022-04-22 08:20:30 [post_content_filtered] => [post_parent] => 44798 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/coll12_95006_crop3.jpeg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [852] => Array ( [ID] => 46338 [post_author] => 105 [post_date] => 2022-04-08 15:13:22 [post_date_gmt] => 2022-04-08 13:13:22 [post_content] => [post_title] => critical_environments_Table-v1-outlines [post_excerpt] => Table 1. Typical trends in historic copper, lead, mercury, and zinc pollution recorded in different natural archives. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => critical_environments_table-v1-outlines [to_ping] => [pinged] => [post_modified] => 2022-04-21 17:46:58 [post_modified_gmt] => 2022-04-21 15:46:58 [post_content_filtered] => [post_parent] => 45637 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/critical_environments_Table-v1-outlines.svg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/svg+xml [comment_count] => 0 [filter] => raw ) [853] => Array ( [ID] => 46335 [post_author] => 105 [post_date] => 2022-04-08 15:11:07 [post_date_gmt] => 2022-04-08 13:11:07 [post_content] => [post_title] => critical_environments_Tablev1-outline [post_excerpt] => Table 1. Typical trends in historic copper, lead, mercury, and zinc pollution recorded in different natural archives. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => critical_environments_tablev1-outline-3 [to_ping] => [pinged] => [post_modified] => 2022-04-08 15:11:33 [post_modified_gmt] => 2022-04-08 13:11:33 [post_content_filtered] => [post_parent] => 45637 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/critical_environments_Tablev1-outline-2.svg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/svg+xml [comment_count] => 0 [filter] => raw ) [854] => Array ( [ID] => 46330 [post_author] => 105 [post_date] => 2022-04-08 14:13:21 [post_date_gmt] => 2022-04-08 12:13:21 [post_content] => [post_title] => critical_environments_Tablev1-outline [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => critical_environments_tablev1-outline-2 [to_ping] => [pinged] => [post_modified] => 2022-04-08 14:13:21 [post_modified_gmt] => 2022-04-08 12:13:21 [post_content_filtered] => [post_parent] => 45637 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/critical_environments_Tablev1-outline-1.svg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/svg+xml [comment_count] => 0 [filter] => raw ) [855] => Array ( [ID] => 46327 [post_author] => 105 [post_date] => 2022-04-08 14:12:11 [post_date_gmt] => 2022-04-08 12:12:11 [post_content] => Diagram redesigned by Luis Melendrez Zehfuss [post_title] => critical_environments_Fig3_page-proof-outline [post_excerpt] => Dating methods of the samples collected in environmental archives of the Anthropocene. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => critical_environments_fig3_page-proof-outline [to_ping] => [pinged] => [post_modified] => 2022-04-21 17:47:37 [post_modified_gmt] => 2022-04-21 15:47:37 [post_content_filtered] => [post_parent] => 45637 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/critical_environments_Fig3_page-proof-outline.svg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/svg+xml [comment_count] => 0 [filter] => raw ) [856] => Array ( [ID] => 46326 [post_author] => 105 [post_date] => 2022-04-08 14:11:50 [post_date_gmt] => 2022-04-08 12:11:50 [post_content] => Diagram redesigned by Luis Melendrez Zehfuss [post_title] => critical_environments_Fig2_page-proof-outlines [post_excerpt] => Environmental archives of the Anthropocene Epoch. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => critical_environments_fig2_page-proof-outlines [to_ping] => [pinged] => [post_modified] => 2022-04-21 17:47:30 [post_modified_gmt] => 2022-04-21 15:47:30 [post_content_filtered] => [post_parent] => 45637 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/critical_environments_Fig2_page-proof-outlines.svg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/svg+xml [comment_count] => 0 [filter] => raw ) [857] => Array ( [ID] => 46325 [post_author] => 105 [post_date] => 2022-04-08 14:11:25 [post_date_gmt] => 2022-04-08 12:11:25 [post_content] => Redesigned by Luis Melendrez Zehfuss [post_title] => critical_environments_Fig1_page-proof-outlines [post_excerpt] => Major steps in chemostratigraphic studies of environmental change during the Anthropocene. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => critical_environments_fig1_page-proof-outlines [to_ping] => [pinged] => [post_modified] => 2022-04-08 14:11:37 [post_modified_gmt] => 2022-04-08 12:11:37 [post_content_filtered] => [post_parent] => 45637 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/critical_environments_Fig1_page-proof-outlines.svg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/svg+xml [comment_count] => 0 [filter] => raw ) [858] => Array ( [ID] => 46324 [post_author] => 105 [post_date] => 2022-04-08 14:10:39 [post_date_gmt] => 2022-04-08 12:10:39 [post_content] => [post_title] => critical_environments_Tablev1-outline [post_excerpt] => Table 1. Typical trends in historic copper, lead, mercury, and zinc pollution recorded in different natural archives. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => critical_environments_tablev1-outline [to_ping] => [pinged] => [post_modified] => 2022-04-08 14:10:46 [post_modified_gmt] => 2022-04-08 12:10:46 [post_content_filtered] => [post_parent] => 45637 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/critical_environments_Tablev1-outline.svg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/svg+xml [comment_count] => 0 [filter] => raw ) [859] => Array ( [ID] => 46321 [post_author] => 105 [post_date] => 2022-04-08 14:06:01 [post_date_gmt] => 2022-04-08 12:06:01 [post_content] => Graph redesigned from Wagreich and Draganits 2018 (footnote 15) by Luis Melendrez Zehfuss [post_title] => Anthrobiogeochemical_Fig5_page-proof-outlines [post_excerpt] => Holocene Pb concentration and 206Pb/207Pb ratios from the Arctic ice core section at Devon Island, Canada (D1999 core, Devon Island Ice Cap, Nunavut). Grey rectangles mark levels of anthropogenic lead input around 3000 BP, 2000 BP, medieval times and the Industrial Revolution and Great Acceleration lead peak. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => anthrobiogeochemical_fig5_page-proof-outlines [to_ping] => [pinged] => [post_modified] => 2022-04-21 16:51:53 [post_modified_gmt] => 2022-04-21 14:51:53 [post_content_filtered] => [post_parent] => 45645 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/Anthrobiogeochemical_Fig5_page-proof-outlines.svg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/svg+xml [comment_count] => 0 [filter] => raw ) [860] => Array ( [ID] => 46320 [post_author] => 105 [post_date] => 2022-04-08 14:04:39 [post_date_gmt] => 2022-04-08 12:04:39 [post_content] => Graph redesigned by Luis Melendrez Zehfuss [post_title] => Anthrobiogeochemical_Fig4_page-proof-outlines [post_excerpt] => Examples of δ15N profiles in different environmental archives; Greenland Summit ice core (blue); coral skeleton (orange); alpine lake Beauty (green). Data compiled from Holtgrieve et al. 2011 (ice core, lake sediment) and Duprey et al. 2020 (coral skeleton). See footnote 12. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => anthrobiogeochemical_fig4_page-proof-outlines [to_ping] => [pinged] => [post_modified] => 2022-04-21 16:51:46 [post_modified_gmt] => 2022-04-21 14:51:46 [post_content_filtered] => [post_parent] => 45645 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/Anthrobiogeochemical_Fig4_page-proof-outlines.svg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/svg+xml [comment_count] => 0 [filter] => raw ) [861] => Array ( [ID] => 46319 [post_author] => 105 [post_date] => 2022-04-08 14:03:45 [post_date_gmt] => 2022-04-08 12:03:45 [post_content] => Redesigned from Waters et al. 2018 by Luis Melendrez Zehfuss [post_title] => Anthrobiogeochemcial_Fig3_page-proof-outlines [post_excerpt] => δ13C variability from Loader et al. 2013 (see footnote 10) for the period 1500–2008 CE measured in tree-ring cellulose for a composite tree ring stable isotope chronology developed using Pinus sylvestris trees from northern Fennoscandia. Fine line represents annually-resolved δ13C variability, thick solid line presents the annual data smoothed with a centrally-weighted 51-year moving average. Dashed line represents the mean δ13C value for the “pre-industrial” period 1500–1799 CE. Mean annual replication for the record is >13 trees. Analytical precision = 0.12 per mil. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => anthrobiogeochemcial_fig3_page-proof-outlines [to_ping] => [pinged] => [post_modified] => 2022-04-19 00:54:06 [post_modified_gmt] => 2022-04-18 22:54:06 [post_content_filtered] => [post_parent] => 45645 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/Anthrobiogeochemcial_Fig3_page-proof-outlines.svg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/svg+xml [comment_count] => 0 [filter] => raw ) [862] => Array ( [ID] => 46318 [post_author] => 105 [post_date] => 2022-04-08 14:03:12 [post_date_gmt] => 2022-04-08 12:03:12 [post_content] => Diagram redesigned from Stenni et al. 2017 (footnote 9) by Luis Melendrez Zehfuss [post_title] => Anthrobiogeochemical_Fig2_page-proof-image [post_excerpt] => Regional composites of stable oxygen isotope values, in each case calculated using two different methods. All anomalies are expressed relative to the 1960–1990 CE interval. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => anthrobiogeochemical_fig2_page-proof-image [to_ping] => [pinged] => [post_modified] => 2022-04-21 16:51:02 [post_modified_gmt] => 2022-04-21 14:51:02 [post_content_filtered] => [post_parent] => 45645 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/Anthrobiogeochemical_Fig2_page-proof-image.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [863] => Array ( [ID] => 46312 [post_author] => 105 [post_date] => 2022-04-08 13:31:00 [post_date_gmt] => 2022-04-08 11:31:00 [post_content] => Graph from Warneke 2002 (see footnote 9) and table from Wu et al. 2011 (see footnote 7), redesigned by Luis Melendrez Zehfuss [post_title] => Nuclear_fig4_V3_page_proof-outline [post_excerpt] => Figure 4. Pu isotope ratios present in a sediment core collected near Sellafield which record a shift from plutonium production for nuclear weapons manufacture (lower part of graph) to the reprocessing of spent nuclear reactor fuel (upper part of graph). The sediment core is 65cm long, and the dates shown on the left have been determined for each sediment layer by matching the profiles of the various radionuclides present in the core with their known history of release from Sellafield. The inset table shows typical plutonium isotopic ratios of various sources in the environment. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => nuclear_fig4_v3_page_proof-outline [to_ping] => [pinged] => [post_modified] => 2022-04-14 13:55:02 [post_modified_gmt] => 2022-04-14 11:55:02 [post_content_filtered] => [post_parent] => 45651 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/Nuclear_fig4_V3_page_proof-outline.svg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/svg+xml [comment_count] => 0 [filter] => raw ) [864] => Array ( [ID] => 46311 [post_author] => 105 [post_date] => 2022-04-08 13:29:46 [post_date_gmt] => 2022-04-08 11:29:46 [post_content] => Data on aggregate test numbers sourced from UNSCEAR (2000) (footnote 4), atmospheric C-14 concentrations from Hua et al. 2013 and for Pu from Hancock et al. 2014 (footnote 5). Redesigned from Waters et al. 2015 (footnote 1) by Luis Melendrez Zehfuss [post_title] => Nuclear_fig3_V3-page-proof-outline [post_excerpt] => Figure 3. Timeline of key events that have influenced anthropogenic radiogenic signatures. The frequency of atmospheric and underground nuclear weapons testing is compared with the fallout signals detected for plutonium and radiocarbon (C-14). Note that fallout follows the aggregate number of tests, with a time lag of 6 months–2 years, with the C-14 peak lagging and at reduced levels in the Southern Hemisphere compared with the Northern Hemisphere. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => nuclear_fig3_v3-page-proof-outline [to_ping] => [pinged] => [post_modified] => 2022-04-14 14:02:48 [post_modified_gmt] => 2022-04-14 12:02:48 [post_content_filtered] => [post_parent] => 45651 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/04/Nuclear_fig3_V3-page-proof-outline.svg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/svg+xml [comment_count] => 0 [filter] => raw ) [865] => Array ( [ID] => 46305 [post_author] => 105 [post_date] => 2022-04-08 13:17:55 [post_date_gmt] => 2022-04-08 11:17:55 [post_content] => Data sourced from UNSCEAR, 2000 and modified from Waters et al. 2015. Satellite equirectangular projection courtesy NASA. [post_title] => Latitudinal variation_Nasa [post_excerpt] => Figure 2. The locations of significant human contributions to radionuclide signals. The distribution and total fission and fusion yields, in megatons, of atmospheric nuclear weapons tests (those in purple predating the first H-bomb test on November 1, 1952 and those in red following that event) emphasizes the relatively limited scale of the first seven years of testing. The location of significant nuclear accidents/discharges are shown in blue. Superimposed is the latitudinal variation of global strontium-90 fallout, in becquerels per square meter. Note that the yield of tests and hence magnitude of the Sr-90 signal is greatest in the Northern Hemisphere—the mid-latitude Sr-90 peak is controlled by natural atmospheric circulation cells rather than the latitude of maximum detonations. A similar but much smaller peak is seen in the Southern Hemisphere. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => latitudinal-variation_nasa [to_ping] => [pinged] => [post_modified] => 2022-04-14 13:50:03 [post_modified_gmt] => 2022-04-14 11:50:03 [post_content_filtered] => [post_parent] => 45651 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/03/Latitudinal-variation_Nasa.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [866] => Array ( [ID] => 46304 [post_author] => 105 [post_date] => 2022-04-08 13:16:07 [post_date_gmt] => 2022-04-08 11:16:07 [post_content] => Diagram adapted by Nathaniel LaCelle-Peterson from original http://www.zamandayolculuk.com/ [post_title] => Nuclear_fig1_V3_page_proof_outlines [post_excerpt] => Figure 1. The nuclear fission process. The splitting of the U-235 atom generates a burst of energy and fires out neutrons which can generate further fission events in a chain reaction. The fragments generated by the fission process form fission products, which decay to a stable isotope form by emission of beta and gamma radiation. If a neutron is absorbed (shown here with U-238) without causing a fission event, then heavier actinides, such as Pu-239, are produced. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => nuclear_fig1_v3_page_proof_outlines [to_ping] => [pinged] => [post_modified] => 2022-04-21 18:28:56 [post_modified_gmt] => 2022-04-21 16:28:56 [post_content_filtered] => [post_parent] => 45651 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/03/Nuclear_fig1_V3_page_proof_outlines.svg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/svg+xml [comment_count] => 0 [filter] => raw ) [867] => Array ( [ID] => 46296 [post_author] => 105 [post_date] => 2022-04-08 12:59:05 [post_date_gmt] => 2022-04-08 10:59:05 [post_content] => [post_title] => Anthropocene-GSSP sediment core_ EGotland Basin [post_excerpt] => [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => anthropocene-gssp-sediment-core_-egotland-basin [to_ping] => [pinged] => [post_modified] => 2022-04-08 12:59:17 [post_modified_gmt] => 2022-04-08 10:59:17 [post_content_filtered] => [post_parent] => 45654 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/03/Anthropocene-GSSP-sediment-core_-EGotland-Basin.jpg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/jpeg [comment_count] => 0 [filter] => raw ) [868] => Array ( [ID] => 46295 [post_author] => 105 [post_date] => 2022-04-08 12:56:54 [post_date_gmt] => 2022-04-08 10:56:54 [post_content] => Graphs redesigned from Ceballos et al. 2015 and Behrens and Luksch 2006 by Luis Melendrez Zehfuss [post_title] => Technofossil_page_proof-test-01 [post_excerpt] => Two quite different kinds of data—biological species extinction rates taken from Ceballos et al. 2015, and rates of growth of new synthetic inorganic crystalline compounds (i.e. minerals in all but formal name) taken from the 2006 study of Behrens and Luksch. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => technofossil_page_proof-test-01 [to_ping] => [pinged] => [post_modified] => 2022-04-21 18:24:27 [post_modified_gmt] => 2022-04-21 16:24:27 [post_content_filtered] => [post_parent] => 45654 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/03/Technofossil_page_proof-test-01.png [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/png [comment_count] => 0 [filter] => raw ) [869] => Array ( [ID] => 46294 [post_author] => 105 [post_date] => 2022-04-08 12:52:27 [post_date_gmt] => 2022-04-08 10:52:27 [post_content] => Photo by Strat188, wikimedia [post_title] => close-up3 [post_excerpt] => Twentieth-century technofossils in inundated landfill deposits at East Tilbury on the River Thames estuary. The landfill is being eroded by tidal surges as sea level rises. Here are objects of glass, ceramic, brick, tile, concrete, etc. Lighter materials such as plastics have been carried away by the tides, leaving heavier items behind. 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[post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => critical_environments_fig3_page-proof [to_ping] => [pinged] => [post_modified] => 2022-04-08 12:11:29 [post_modified_gmt] => 2022-04-08 10:11:29 [post_content_filtered] => [post_parent] => 45637 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/03/critical_environments_Fig3_page-proof.svg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/svg+xml [comment_count] => 0 [filter] => raw ) [874] => Array ( [ID] => 46276 [post_author] => 105 [post_date] => 2022-04-08 12:10:14 [post_date_gmt] => 2022-04-08 10:10:14 [post_content] => Redesigned by Luis Melendrez Zehfuss [post_title] => critical_environments_Fig2_page-proof [post_excerpt] => Environmental archives of the Anthropocene Epoch. [post_status] => inherit [comment_status] => closed [ping_status] => closed [post_password] => [post_name] => critical_environments_fig2_page-proof [to_ping] => [pinged] => [post_modified] => 2022-04-08 12:10:31 [post_modified_gmt] => 2022-04-08 10:10:31 [post_content_filtered] => [post_parent] => 45637 [guid] => https://content.anthropocene-curriculum.org/wp-content/uploads/2022/03/critical_environments_Fig2_page-proof.svg [menu_order] => 0 [post_type] => attachment [post_mime_type] => image/svg+xml [comment_count] => 0 [filter] => raw ) [875] => Array ( [ID] => 46275 [post_author] => 105 [post_date] => 2022-04-08 12:08:56 [post_date_gmt] => 2022-04-08 10:08:56 [post_content] => Redesigned by Luis Melendrez Zehfuss [post_title] => critical_environments_Fig1_page-proof [post_excerpt] => Major steps in chemostratigraphic studies of environmental change during the Anthropocene. 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