The Eocene-Oligocene boundary climate transition: an Antarctic perspective

Antarctica underwent a complex evolution over the course of the Cenozoic, which influenced the history of the Earth’s climate system. The Eocene-Oligocene boundary is a divide of this history when the ice-free ‘greenhouse world’ transitioned to the ‘icehouse’ with the glaciation of Antarctica. Prior...

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Main Authors: Galeotti, Simone, Bijl, Peter, Brinkuis, Henk, DeConto, Robert M., Escutia, Carlota, Florindo, Fabio, Gasson, Edward G.W., Francis, Jane, Hutchinson, David, Kennedy-Asser, Alan, Lanci, Luca, Sauermilch, Isabel, Sluijs, Appy, Stocchi, Paolo
Other Authors: Siegert, Martin, De Santis, Laura, Naish, Tim
Format: Book Part
Language:unknown
Published: Elsevier 2021
Subjects:
Online Access:http://nora.nerc.ac.uk/id/eprint/531568/
https://doi.org/10.1016/B978-0-12-819109-5.00009-8
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spelling ftnerc:oai:nora.nerc.ac.uk:531568 2023-05-15T13:41:46+02:00 The Eocene-Oligocene boundary climate transition: an Antarctic perspective Galeotti, Simone Bijl, Peter Brinkuis, Henk DeConto, Robert M. Escutia, Carlota Florindo, Fabio Gasson, Edward G.W. Francis, Jane Hutchinson, David Kennedy-Asser, Alan Lanci, Luca Sauermilch, Isabel Sluijs, Appy Stocchi, Paolo Florindo, Fabio Siegert, Martin De Santis, Laura Naish, Tim 2021-10 http://nora.nerc.ac.uk/id/eprint/531568/ https://doi.org/10.1016/B978-0-12-819109-5.00009-8 unknown Elsevier Galeotti, Simone; Bijl, Peter; Brinkuis, Henk; DeConto, Robert M.; Escutia, Carlota; Florindo, Fabio; Gasson, Edward G.W.; Francis, Jane; Hutchinson, David; Kennedy-Asser, Alan; Lanci, Luca; Sauermilch, Isabel; Sluijs, Appy; Stocchi, Paolo. 2021 The Eocene-Oligocene boundary climate transition: an Antarctic perspective. In: Florindo, Fabio; Siegert, Martin; De Santis, Laura; Naish, Tim, (eds.) Antarctic Climate Evolution 2nd edition. Elsevier, 297-361. Publication - Book Section PeerReviewed 2021 ftnerc https://doi.org/10.1016/B978-0-12-819109-5.00009-8 2023-02-04T19:52:47Z Antarctica underwent a complex evolution over the course of the Cenozoic, which influenced the history of the Earth’s climate system. The Eocene-Oligocene boundary is a divide of this history when the ice-free ‘greenhouse world’ transitioned to the ‘icehouse’ with the glaciation of Antarctica. Prior to this, Antarctica experienced warm climates, peaking during Early Eocene when tropical-like conditions existed at the margins of the continent where geological evidence is present. Climate signals in the geological record show that the climate then cooled, but not enough to allow the existence of significant ice until the latest Eocene. Glacial deposits from several areas around the continental margin indicate that ice was present by the earliest Oligocene. This matches the major oxygen isotope positive shift captured by marine records. On land, vegetation was able to persist, but the thermophylic plants of the Eocene were replaced by shrubby vegetation with the southern beech Nothofagus, mosses and ferns, which survived in tundra-like conditions. Coupled climate–ice sheet modelling indicates that changing levels of atmospheric CO2 controlled Antarctica’s climate and the onset of glaciation. Factors such as mountain uplift, vegetation changes, ocean gateway opening and orbital forcing all played a part in cooling the polar climate, but only when CO2 levels reached critical thresholds was Antarctica tipped into an icy glacial world. Book Part Antarc* Antarctic Antarctica Ice Sheet Tundra Natural Environment Research Council: NERC Open Research Archive Antarctic 297 361
institution Open Polar
collection Natural Environment Research Council: NERC Open Research Archive
op_collection_id ftnerc
language unknown
description Antarctica underwent a complex evolution over the course of the Cenozoic, which influenced the history of the Earth’s climate system. The Eocene-Oligocene boundary is a divide of this history when the ice-free ‘greenhouse world’ transitioned to the ‘icehouse’ with the glaciation of Antarctica. Prior to this, Antarctica experienced warm climates, peaking during Early Eocene when tropical-like conditions existed at the margins of the continent where geological evidence is present. Climate signals in the geological record show that the climate then cooled, but not enough to allow the existence of significant ice until the latest Eocene. Glacial deposits from several areas around the continental margin indicate that ice was present by the earliest Oligocene. This matches the major oxygen isotope positive shift captured by marine records. On land, vegetation was able to persist, but the thermophylic plants of the Eocene were replaced by shrubby vegetation with the southern beech Nothofagus, mosses and ferns, which survived in tundra-like conditions. Coupled climate–ice sheet modelling indicates that changing levels of atmospheric CO2 controlled Antarctica’s climate and the onset of glaciation. Factors such as mountain uplift, vegetation changes, ocean gateway opening and orbital forcing all played a part in cooling the polar climate, but only when CO2 levels reached critical thresholds was Antarctica tipped into an icy glacial world.
author2 Florindo, Fabio
Siegert, Martin
De Santis, Laura
Naish, Tim
format Book Part
author Galeotti, Simone
Bijl, Peter
Brinkuis, Henk
DeConto, Robert M.
Escutia, Carlota
Florindo, Fabio
Gasson, Edward G.W.
Francis, Jane
Hutchinson, David
Kennedy-Asser, Alan
Lanci, Luca
Sauermilch, Isabel
Sluijs, Appy
Stocchi, Paolo
spellingShingle Galeotti, Simone
Bijl, Peter
Brinkuis, Henk
DeConto, Robert M.
Escutia, Carlota
Florindo, Fabio
Gasson, Edward G.W.
Francis, Jane
Hutchinson, David
Kennedy-Asser, Alan
Lanci, Luca
Sauermilch, Isabel
Sluijs, Appy
Stocchi, Paolo
The Eocene-Oligocene boundary climate transition: an Antarctic perspective
author_facet Galeotti, Simone
Bijl, Peter
Brinkuis, Henk
DeConto, Robert M.
Escutia, Carlota
Florindo, Fabio
Gasson, Edward G.W.
Francis, Jane
Hutchinson, David
Kennedy-Asser, Alan
Lanci, Luca
Sauermilch, Isabel
Sluijs, Appy
Stocchi, Paolo
author_sort Galeotti, Simone
title The Eocene-Oligocene boundary climate transition: an Antarctic perspective
title_short The Eocene-Oligocene boundary climate transition: an Antarctic perspective
title_full The Eocene-Oligocene boundary climate transition: an Antarctic perspective
title_fullStr The Eocene-Oligocene boundary climate transition: an Antarctic perspective
title_full_unstemmed The Eocene-Oligocene boundary climate transition: an Antarctic perspective
title_sort eocene-oligocene boundary climate transition: an antarctic perspective
publisher Elsevier
publishDate 2021
url http://nora.nerc.ac.uk/id/eprint/531568/
https://doi.org/10.1016/B978-0-12-819109-5.00009-8
geographic Antarctic
geographic_facet Antarctic
genre Antarc*
Antarctic
Antarctica
Ice Sheet
Tundra
genre_facet Antarc*
Antarctic
Antarctica
Ice Sheet
Tundra
op_relation Galeotti, Simone; Bijl, Peter; Brinkuis, Henk; DeConto, Robert M.; Escutia, Carlota; Florindo, Fabio; Gasson, Edward G.W.; Francis, Jane; Hutchinson, David; Kennedy-Asser, Alan; Lanci, Luca; Sauermilch, Isabel; Sluijs, Appy; Stocchi, Paolo. 2021 The Eocene-Oligocene boundary climate transition: an Antarctic perspective. In: Florindo, Fabio; Siegert, Martin; De Santis, Laura; Naish, Tim, (eds.) Antarctic Climate Evolution 2nd edition. Elsevier, 297-361.
op_doi https://doi.org/10.1016/B978-0-12-819109-5.00009-8
container_start_page 297
op_container_end_page 361
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