Exceptionally high biosphere productivity at the beginning of Marine Isotopic Stage 11
Abstract 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...
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crspringernat:10.1038/s41467-020-15739-2 2023-05-15T14:09:40+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 Agence Nationale de la Recherche Institut National des Sciences de l'Univers, Centre National de la Recherche Scientifique 2020 http://dx.doi.org/10.1038/s41467-020-15739-2 http://www.nature.com/articles/s41467-020-15739-2.pdf http://www.nature.com/articles/s41467-020-15739-2 en eng Springer Science and Business Media LLC https://creativecommons.org/licenses/by/4.0 https://creativecommons.org/licenses/by/4.0 CC-BY Nature Communications volume 11, issue 1 ISSN 2041-1723 General Physics and Astronomy General Biochemistry, Genetics and Molecular Biology General Chemistry journal-article 2020 crspringernat https://doi.org/10.1038/s41467-020-15739-2 2022-01-04T15:41:02Z Abstract 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 Springer Nature (via Crossref) Antarctic Southern Ocean The Antarctic Nature Communications 11 1 |
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Open Polar |
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Springer Nature (via Crossref) |
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crspringernat |
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English |
topic |
General Physics and Astronomy General Biochemistry, Genetics and Molecular Biology General Chemistry |
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General Physics and Astronomy General Biochemistry, Genetics and Molecular Biology General Chemistry 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 |
General Physics and Astronomy General Biochemistry, Genetics and Molecular Biology General Chemistry |
description |
Abstract 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 |
Agence Nationale de la Recherche Institut National des Sciences de l'Univers, Centre National de la Recherche Scientifique |
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 |
Springer Science and Business Media LLC |
publishDate |
2020 |
url |
http://dx.doi.org/10.1038/s41467-020-15739-2 http://www.nature.com/articles/s41467-020-15739-2.pdf http://www.nature.com/articles/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 |
Nature Communications volume 11, issue 1 ISSN 2041-1723 |
op_rights |
https://creativecommons.org/licenses/by/4.0 https://creativecommons.org/licenses/by/4.0 |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.1038/s41467-020-15739-2 |
container_title |
Nature Communications |
container_volume |
11 |
container_issue |
1 |
_version_ |
1766281694717935616 |