Southern Ocean biogenic blooms freezing-in Oligocene colder climates

<jats:title>Abstract</jats:title><jats:p>Crossing a key atmospheric CO<jats:sub>2</jats:sub> threshold triggered a fundamental global climate reorganisation ~34 million years ago (Ma) establishing permanent Antarctic ice sheets. Curiously, a more dramatic CO<jats:sub...

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Published in:Nature Communications
Main Authors: Hochmuth, Katharina, Whittaker, Joanne M, Sauermilch, Isabel, Klocker, Andreas, Gohl, Karsten, LaCasce, Joseph H
Format: Article in Journal/Newspaper
Language:unknown
Published: Springer Nature 2022
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Online Access:https://epic.awi.de/id/eprint/57557/
https://epic.awi.de/id/eprint/57557/1/Hochmuth-etal_Southern-Ocean-biogenic-blooms-freezing-in-Oligocene-colder-climates_NatureComms_2022.pdf
https://hdl.handle.net/10013/epic.c0f08c8c-789c-4ffe-a1d5-600ac791e6f1
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spelling ftawi:oai:epic.awi.de:57557 2024-09-15T17:47:29+00:00 Southern Ocean biogenic blooms freezing-in Oligocene colder climates Hochmuth, Katharina Whittaker, Joanne M Sauermilch, Isabel Klocker, Andreas Gohl, Karsten LaCasce, Joseph H 2022-11-09 application/pdf https://epic.awi.de/id/eprint/57557/ https://epic.awi.de/id/eprint/57557/1/Hochmuth-etal_Southern-Ocean-biogenic-blooms-freezing-in-Oligocene-colder-climates_NatureComms_2022.pdf https://hdl.handle.net/10013/epic.c0f08c8c-789c-4ffe-a1d5-600ac791e6f1 unknown Springer Nature https://epic.awi.de/id/eprint/57557/1/Hochmuth-etal_Southern-Ocean-biogenic-blooms-freezing-in-Oligocene-colder-climates_NatureComms_2022.pdf Hochmuth, K. , Whittaker, J. M. , Sauermilch, I. , Klocker, A. , Gohl, K. orcid:0000-0002-9558-2116 and LaCasce, J. H. (2022) Southern Ocean biogenic blooms freezing-in Oligocene colder climates , Nature Communications, 13 (1), pp. 1-10 . doi:10.1038/s41467-022-34623-9 <https://doi.org/10.1038/s41467-022-34623-9> , hdl:10013/epic.c0f08c8c-789c-4ffe-a1d5-600ac791e6f1 EPIC3Nature Communications, Springer Nature, 13(1), pp. 1-10, ISSN: 2041-1723 Article isiRev 2022 ftawi https://doi.org/10.1038/s41467-022-34623-9 2024-06-24T04:30:12Z <jats:title>Abstract</jats:title><jats:p>Crossing a key atmospheric CO<jats:sub>2</jats:sub> threshold triggered a fundamental global climate reorganisation ~34 million years ago (Ma) establishing permanent Antarctic ice sheets. Curiously, a more dramatic CO<jats:sub>2</jats:sub> decline (~800–400 ppm by the Early Oligocene(~27 Ma)), postdates initial ice sheet expansion but the mechanisms driving this later, rapid drop in atmospheric carbon during the early Oligocene remains elusive and controversial. Here we use marine seismic reflection and borehole data to reveal an unprecedented accumulation of early Oligocene strata (up to 2.2 km thick over 1500 × 500 km) with a major biogenic component in the Australian Southern Ocean. High-resolution ocean simulations demonstrate that a tectonically-driven, one-off reorganisation of ocean currents, caused a unique period where current instability coincided with high nutrient input from the Antarctic continent. This unrepeated and short-lived environment favoured extreme bioproductivity and enhanced sediment burial. The size and rapid accumulation of this sediment package potentially holds ~1.067 × 10<jats:sup>15</jats:sup> kg of the ‘missing carbon’ sequestered during the decline from an Eocene high CO<jats:sub>2</jats:sub>-world to a mid-Oligocene medium CO<jats:sub>2</jats:sub>-world, highlighting the exceptional role of the Southern Ocean in modulating long-term climate.</jats:p> Article in Journal/Newspaper Antarc* Antarctic Ice Sheet Southern Ocean Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center) Nature Communications 13 1
institution Open Polar
collection Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center)
op_collection_id ftawi
language unknown
description <jats:title>Abstract</jats:title><jats:p>Crossing a key atmospheric CO<jats:sub>2</jats:sub> threshold triggered a fundamental global climate reorganisation ~34 million years ago (Ma) establishing permanent Antarctic ice sheets. Curiously, a more dramatic CO<jats:sub>2</jats:sub> decline (~800–400 ppm by the Early Oligocene(~27 Ma)), postdates initial ice sheet expansion but the mechanisms driving this later, rapid drop in atmospheric carbon during the early Oligocene remains elusive and controversial. Here we use marine seismic reflection and borehole data to reveal an unprecedented accumulation of early Oligocene strata (up to 2.2 km thick over 1500 × 500 km) with a major biogenic component in the Australian Southern Ocean. High-resolution ocean simulations demonstrate that a tectonically-driven, one-off reorganisation of ocean currents, caused a unique period where current instability coincided with high nutrient input from the Antarctic continent. This unrepeated and short-lived environment favoured extreme bioproductivity and enhanced sediment burial. The size and rapid accumulation of this sediment package potentially holds ~1.067 × 10<jats:sup>15</jats:sup> kg of the ‘missing carbon’ sequestered during the decline from an Eocene high CO<jats:sub>2</jats:sub>-world to a mid-Oligocene medium CO<jats:sub>2</jats:sub>-world, highlighting the exceptional role of the Southern Ocean in modulating long-term climate.</jats:p>
format Article in Journal/Newspaper
author Hochmuth, Katharina
Whittaker, Joanne M
Sauermilch, Isabel
Klocker, Andreas
Gohl, Karsten
LaCasce, Joseph H
spellingShingle Hochmuth, Katharina
Whittaker, Joanne M
Sauermilch, Isabel
Klocker, Andreas
Gohl, Karsten
LaCasce, Joseph H
Southern Ocean biogenic blooms freezing-in Oligocene colder climates
author_facet Hochmuth, Katharina
Whittaker, Joanne M
Sauermilch, Isabel
Klocker, Andreas
Gohl, Karsten
LaCasce, Joseph H
author_sort Hochmuth, Katharina
title Southern Ocean biogenic blooms freezing-in Oligocene colder climates
title_short Southern Ocean biogenic blooms freezing-in Oligocene colder climates
title_full Southern Ocean biogenic blooms freezing-in Oligocene colder climates
title_fullStr Southern Ocean biogenic blooms freezing-in Oligocene colder climates
title_full_unstemmed Southern Ocean biogenic blooms freezing-in Oligocene colder climates
title_sort southern ocean biogenic blooms freezing-in oligocene colder climates
publisher Springer Nature
publishDate 2022
url https://epic.awi.de/id/eprint/57557/
https://epic.awi.de/id/eprint/57557/1/Hochmuth-etal_Southern-Ocean-biogenic-blooms-freezing-in-Oligocene-colder-climates_NatureComms_2022.pdf
https://hdl.handle.net/10013/epic.c0f08c8c-789c-4ffe-a1d5-600ac791e6f1
genre Antarc*
Antarctic
Ice Sheet
Southern Ocean
genre_facet Antarc*
Antarctic
Ice Sheet
Southern Ocean
op_source EPIC3Nature Communications, Springer Nature, 13(1), pp. 1-10, ISSN: 2041-1723
op_relation https://epic.awi.de/id/eprint/57557/1/Hochmuth-etal_Southern-Ocean-biogenic-blooms-freezing-in-Oligocene-colder-climates_NatureComms_2022.pdf
Hochmuth, K. , Whittaker, J. M. , Sauermilch, I. , Klocker, A. , Gohl, K. orcid:0000-0002-9558-2116 and LaCasce, J. H. (2022) Southern Ocean biogenic blooms freezing-in Oligocene colder climates , Nature Communications, 13 (1), pp. 1-10 . doi:10.1038/s41467-022-34623-9 <https://doi.org/10.1038/s41467-022-34623-9> , hdl:10013/epic.c0f08c8c-789c-4ffe-a1d5-600ac791e6f1
op_doi https://doi.org/10.1038/s41467-022-34623-9
container_title Nature Communications
container_volume 13
container_issue 1
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