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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Published in:Nature Communications
Main Authors: 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
Format: Article in Journal/Newspaper
Language:English
Published: Nature Portfolio 2023
Subjects:
Q
Online Access:https://doi.org/10.1038/s41467-023-39806-6
https://doaj.org/article/5b2552d28b5a4c4b8e1ccc7bc7e9a59e
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spelling 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
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Science
Q
spellingShingle 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
topic_facet 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
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