Exceptionally high biosphere productivity at the beginning of Marine Isotopic Stage 11

International audience Significant changes in atmospheric CO 2 over glacial-interglacial cycles have mainly been attributed to the Southern Ocean through physical and biological processes. However, little is known about the contribution of global biosphere productivity, associated with important CO...

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Published in:Nature Communications
Main Authors: Brandon, Margaux, LANDAIS, AMAELLE, Duchamp-Alphonse, Stéphanie, Favre, Violaine, Schmitz, Léa, Abrial, Héloïse, Prié, Frédéric, Extier, Thomas, Blunier, Thomas
Other Authors: Laboratoire des Sciences du Climat et de l'Environnement Gif-sur-Yvette (LSCE), Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ), Glaces et Continents, Climats et Isotopes Stables (GLACCIOS), Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ), Géosciences Paris Saclay (GEOPS), Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS), Centre for Ice and Climate Copenhagen, Niels Bohr Institute Copenhagen (NBI), Faculty of Science Copenhagen, University of Copenhagen = Københavns Universitet (KU)-University of Copenhagen = Københavns Universitet (KU)-Faculty of Science Copenhagen, University of Copenhagen = Københavns Universitet (KU)-University of Copenhagen = Københavns Universitet (KU)
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2020
Subjects:
Online Access:https://hal.archives-ouvertes.fr/hal-02765978
https://hal.archives-ouvertes.fr/hal-02765978/document
https://hal.archives-ouvertes.fr/hal-02765978/file/s41467-020-15739-2.pdf
https://doi.org/10.1038/s41467-020-15739-2
id ftccsdartic:oai:HAL:hal-02765978v1
record_format openpolar
institution Open Polar
collection Archive ouverte HAL (Hyper Article en Ligne, CCSD - Centre pour la Communication Scientifique Directe)
op_collection_id ftccsdartic
language English
topic [SDU.OCEAN]Sciences of the Universe [physics]/Ocean
Atmosphere
[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces
environment
spellingShingle [SDU.OCEAN]Sciences of the Universe [physics]/Ocean
Atmosphere
[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces
environment
Brandon, Margaux
LANDAIS, AMAELLE
Duchamp-Alphonse, Stéphanie
Favre, Violaine
Schmitz, Léa
Abrial, Héloïse
Prié, Frédéric
Extier, Thomas
Blunier, Thomas
Exceptionally high biosphere productivity at the beginning of Marine Isotopic Stage 11
topic_facet [SDU.OCEAN]Sciences of the Universe [physics]/Ocean
Atmosphere
[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces
environment
description International audience Significant changes in atmospheric CO 2 over glacial-interglacial cycles have mainly been attributed to the Southern Ocean through physical and biological processes. However, little is known about the contribution of global biosphere productivity, associated with important CO 2 fluxes. Here we present the first high resolution record of Δ 17 O of O 2 in the Antarctic EPICA Dome C ice core over Termination V and Marine Isotopic Stage (MIS) 11 and reconstruct the global oxygen biosphere productivity over the last 445 ka. Our data show that compared to the younger terminations, biosphere productivity at the end of Termination V is 10 to 30 % higher. Comparisons with local palaeo observations suggest that strong terrestrial productivity in a context of low eccentricity might explain this pattern. We propose that higher biosphere productivity could have maintained low atmospheric CO 2 at the beginning of MIS 11, thus highlighting its control on the global climate during Termination V.
author2 Laboratoire des Sciences du Climat et de l'Environnement Gif-sur-Yvette (LSCE)
Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)
Glaces et Continents, Climats et Isotopes Stables (GLACCIOS)
Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)
Géosciences Paris Saclay (GEOPS)
Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)
Centre for Ice and Climate Copenhagen
Niels Bohr Institute Copenhagen (NBI)
Faculty of Science Copenhagen
University of Copenhagen = Københavns Universitet (KU)-University of Copenhagen = Københavns Universitet (KU)-Faculty of Science Copenhagen
University of Copenhagen = Københavns Universitet (KU)-University of Copenhagen = Københavns Universitet (KU)
format Article in Journal/Newspaper
author Brandon, Margaux
LANDAIS, AMAELLE
Duchamp-Alphonse, Stéphanie
Favre, Violaine
Schmitz, Léa
Abrial, Héloïse
Prié, Frédéric
Extier, Thomas
Blunier, Thomas
author_facet Brandon, Margaux
LANDAIS, AMAELLE
Duchamp-Alphonse, Stéphanie
Favre, Violaine
Schmitz, Léa
Abrial, Héloïse
Prié, Frédéric
Extier, Thomas
Blunier, Thomas
author_sort Brandon, Margaux
title Exceptionally high biosphere productivity at the beginning of Marine Isotopic Stage 11
title_short Exceptionally high biosphere productivity at the beginning of Marine Isotopic Stage 11
title_full Exceptionally high biosphere productivity at the beginning of Marine Isotopic Stage 11
title_fullStr Exceptionally high biosphere productivity at the beginning of Marine Isotopic Stage 11
title_full_unstemmed Exceptionally high biosphere productivity at the beginning of Marine Isotopic Stage 11
title_sort exceptionally high biosphere productivity at the beginning of marine isotopic stage 11
publisher HAL CCSD
publishDate 2020
url https://hal.archives-ouvertes.fr/hal-02765978
https://hal.archives-ouvertes.fr/hal-02765978/document
https://hal.archives-ouvertes.fr/hal-02765978/file/s41467-020-15739-2.pdf
https://doi.org/10.1038/s41467-020-15739-2
geographic Antarctic
Southern Ocean
The Antarctic
geographic_facet Antarctic
Southern Ocean
The Antarctic
genre Antarc*
Antarctic
EPICA
ice core
Southern Ocean
genre_facet Antarc*
Antarctic
EPICA
ice core
Southern Ocean
op_source ISSN: 2041-1723
EISSN: 2041-1723
Nature Communications
https://hal.archives-ouvertes.fr/hal-02765978
Nature Communications, Nature Publishing Group, 2020, 11 (1), ⟨10.1038/s41467-020-15739-2⟩
op_relation info:eu-repo/semantics/altIdentifier/doi/10.1038/s41467-020-15739-2
hal-02765978
https://hal.archives-ouvertes.fr/hal-02765978
https://hal.archives-ouvertes.fr/hal-02765978/document
https://hal.archives-ouvertes.fr/hal-02765978/file/s41467-020-15739-2.pdf
doi:10.1038/s41467-020-15739-2
op_rights http://creativecommons.org/licenses/by/
info:eu-repo/semantics/OpenAccess
op_doi https://doi.org/10.1038/s41467-020-15739-2
container_title Nature Communications
container_volume 11
container_issue 1
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spelling ftccsdartic:oai:HAL:hal-02765978v1 2023-05-15T13:54:56+02:00 Exceptionally high biosphere productivity at the beginning of Marine Isotopic Stage 11 Brandon, Margaux LANDAIS, AMAELLE Duchamp-Alphonse, Stéphanie Favre, Violaine Schmitz, Léa Abrial, Héloïse Prié, Frédéric Extier, Thomas Blunier, Thomas Laboratoire des Sciences du Climat et de l'Environnement Gif-sur-Yvette (LSCE) Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ) Glaces et Continents, Climats et Isotopes Stables (GLACCIOS) Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ) Géosciences Paris Saclay (GEOPS) Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS) Centre for Ice and Climate Copenhagen Niels Bohr Institute Copenhagen (NBI) Faculty of Science Copenhagen University of Copenhagen = Københavns Universitet (KU)-University of Copenhagen = Københavns Universitet (KU)-Faculty of Science Copenhagen University of Copenhagen = Københavns Universitet (KU)-University of Copenhagen = Københavns Universitet (KU) 2020-12 https://hal.archives-ouvertes.fr/hal-02765978 https://hal.archives-ouvertes.fr/hal-02765978/document https://hal.archives-ouvertes.fr/hal-02765978/file/s41467-020-15739-2.pdf https://doi.org/10.1038/s41467-020-15739-2 en eng HAL CCSD Nature Publishing Group info:eu-repo/semantics/altIdentifier/doi/10.1038/s41467-020-15739-2 hal-02765978 https://hal.archives-ouvertes.fr/hal-02765978 https://hal.archives-ouvertes.fr/hal-02765978/document https://hal.archives-ouvertes.fr/hal-02765978/file/s41467-020-15739-2.pdf doi:10.1038/s41467-020-15739-2 http://creativecommons.org/licenses/by/ info:eu-repo/semantics/OpenAccess ISSN: 2041-1723 EISSN: 2041-1723 Nature Communications https://hal.archives-ouvertes.fr/hal-02765978 Nature Communications, Nature Publishing Group, 2020, 11 (1), ⟨10.1038/s41467-020-15739-2⟩ [SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere [SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environment info:eu-repo/semantics/article Journal articles 2020 ftccsdartic https://doi.org/10.1038/s41467-020-15739-2 2021-12-19T00:55:17Z International audience Significant changes in atmospheric CO 2 over glacial-interglacial cycles have mainly been attributed to the Southern Ocean through physical and biological processes. However, little is known about the contribution of global biosphere productivity, associated with important CO 2 fluxes. Here we present the first high resolution record of Δ 17 O of O 2 in the Antarctic EPICA Dome C ice core over Termination V and Marine Isotopic Stage (MIS) 11 and reconstruct the global oxygen biosphere productivity over the last 445 ka. Our data show that compared to the younger terminations, biosphere productivity at the end of Termination V is 10 to 30 % higher. Comparisons with local palaeo observations suggest that strong terrestrial productivity in a context of low eccentricity might explain this pattern. We propose that higher biosphere productivity could have maintained low atmospheric CO 2 at the beginning of MIS 11, thus highlighting its control on the global climate during Termination V. Article in Journal/Newspaper Antarc* Antarctic EPICA ice core Southern Ocean Archive ouverte HAL (Hyper Article en Ligne, CCSD - Centre pour la Communication Scientifique Directe) Antarctic Southern Ocean The Antarctic Nature Communications 11 1