Multi-proxy evidence for sea level fall at the onset of the Eocene-Oligocene transition
Abstract Continental-scale expansion of the East Antarctic Ice Sheet during the Eocene-Oligocene Transition (EOT) is one of the largest non-linear events in Earth’s climate history. Declining atmospheric carbon dioxide concentrations and orbital variability triggered glacial expansion and strong fee...
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Online Access: | https://doi.org/10.1038/s41467-023-39806-6 https://doaj.org/article/5b2552d28b5a4c4b8e1ccc7bc7e9a59e |
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ftdoajarticles:oai:doaj.org/article:5b2552d28b5a4c4b8e1ccc7bc7e9a59e 2023-09-05T13:14:07+02:00 Multi-proxy evidence for sea level fall at the onset of the Eocene-Oligocene transition Marcelo A. De Lira Mota Tom Dunkley Jones Nursufiah Sulaiman Kirsty M. Edgar Tatsuhiko Yamaguchi Melanie J. Leng Markus Adloff Sarah E. Greene Richard Norris Bridget Warren Grace Duffy Jennifer Farrant Masafumi Murayama Jonathan Hall James Bendle 2023-08-01T00:00:00Z https://doi.org/10.1038/s41467-023-39806-6 https://doaj.org/article/5b2552d28b5a4c4b8e1ccc7bc7e9a59e EN eng Nature Portfolio https://doi.org/10.1038/s41467-023-39806-6 https://doaj.org/toc/2041-1723 doi:10.1038/s41467-023-39806-6 2041-1723 https://doaj.org/article/5b2552d28b5a4c4b8e1ccc7bc7e9a59e Nature Communications, Vol 14, Iss 1, Pp 1-13 (2023) Science Q article 2023 ftdoajarticles https://doi.org/10.1038/s41467-023-39806-6 2023-08-20T00:36:15Z Abstract Continental-scale expansion of the East Antarctic Ice Sheet during the Eocene-Oligocene Transition (EOT) is one of the largest non-linear events in Earth’s climate history. Declining atmospheric carbon dioxide concentrations and orbital variability triggered glacial expansion and strong feedbacks in the climate system. Prominent among these feedbacks was the repartitioning of biogeochemical cycles between the continental shelves and the deep ocean with falling sea level. Here we present multiple proxies from a shallow shelf location that identify a marked regression and an elevated flux of continental-derived organic matter at the earliest stage of the EOT, a time of deep ocean carbonate dissolution and the extinction of oligotrophic phytoplankton groups. We link these observations using an Earth System model, whereby this first regression delivers a pulse of organic carbon to the oceans that could drive the observed patterns of deep ocean dissolution and acts as a transient negative feedback to climate cooling. Article in Journal/Newspaper Antarc* Antarctic Ice Sheet Directory of Open Access Journals: DOAJ Articles Antarctic East Antarctic Ice Sheet Nature Communications 14 1 |
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Directory of Open Access Journals: DOAJ Articles |
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ftdoajarticles |
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Science Q |
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Science Q Marcelo A. De Lira Mota Tom Dunkley Jones Nursufiah Sulaiman Kirsty M. Edgar Tatsuhiko Yamaguchi Melanie J. Leng Markus Adloff Sarah E. Greene Richard Norris Bridget Warren Grace Duffy Jennifer Farrant Masafumi Murayama Jonathan Hall James Bendle Multi-proxy evidence for sea level fall at the onset of the Eocene-Oligocene transition |
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Science Q |
description |
Abstract Continental-scale expansion of the East Antarctic Ice Sheet during the Eocene-Oligocene Transition (EOT) is one of the largest non-linear events in Earth’s climate history. Declining atmospheric carbon dioxide concentrations and orbital variability triggered glacial expansion and strong feedbacks in the climate system. Prominent among these feedbacks was the repartitioning of biogeochemical cycles between the continental shelves and the deep ocean with falling sea level. Here we present multiple proxies from a shallow shelf location that identify a marked regression and an elevated flux of continental-derived organic matter at the earliest stage of the EOT, a time of deep ocean carbonate dissolution and the extinction of oligotrophic phytoplankton groups. We link these observations using an Earth System model, whereby this first regression delivers a pulse of organic carbon to the oceans that could drive the observed patterns of deep ocean dissolution and acts as a transient negative feedback to climate cooling. |
format |
Article in Journal/Newspaper |
author |
Marcelo A. De Lira Mota Tom Dunkley Jones Nursufiah Sulaiman Kirsty M. Edgar Tatsuhiko Yamaguchi Melanie J. Leng Markus Adloff Sarah E. Greene Richard Norris Bridget Warren Grace Duffy Jennifer Farrant Masafumi Murayama Jonathan Hall James Bendle |
author_facet |
Marcelo A. De Lira Mota Tom Dunkley Jones Nursufiah Sulaiman Kirsty M. Edgar Tatsuhiko Yamaguchi Melanie J. Leng Markus Adloff Sarah E. Greene Richard Norris Bridget Warren Grace Duffy Jennifer Farrant Masafumi Murayama Jonathan Hall James Bendle |
author_sort |
Marcelo A. De Lira Mota |
title |
Multi-proxy evidence for sea level fall at the onset of the Eocene-Oligocene transition |
title_short |
Multi-proxy evidence for sea level fall at the onset of the Eocene-Oligocene transition |
title_full |
Multi-proxy evidence for sea level fall at the onset of the Eocene-Oligocene transition |
title_fullStr |
Multi-proxy evidence for sea level fall at the onset of the Eocene-Oligocene transition |
title_full_unstemmed |
Multi-proxy evidence for sea level fall at the onset of the Eocene-Oligocene transition |
title_sort |
multi-proxy evidence for sea level fall at the onset of the eocene-oligocene transition |
publisher |
Nature Portfolio |
publishDate |
2023 |
url |
https://doi.org/10.1038/s41467-023-39806-6 https://doaj.org/article/5b2552d28b5a4c4b8e1ccc7bc7e9a59e |
geographic |
Antarctic East Antarctic Ice Sheet |
geographic_facet |
Antarctic East Antarctic Ice Sheet |
genre |
Antarc* Antarctic Ice Sheet |
genre_facet |
Antarc* Antarctic Ice Sheet |
op_source |
Nature Communications, Vol 14, Iss 1, Pp 1-13 (2023) |
op_relation |
https://doi.org/10.1038/s41467-023-39806-6 https://doaj.org/toc/2041-1723 doi:10.1038/s41467-023-39806-6 2041-1723 https://doaj.org/article/5b2552d28b5a4c4b8e1ccc7bc7e9a59e |
op_doi |
https://doi.org/10.1038/s41467-023-39806-6 |
container_title |
Nature Communications |
container_volume |
14 |
container_issue |
1 |
_version_ |
1776205169235591168 |