Stable Carbon Cycle–Climate Relationship During the Late Pleistocene
International audience A record of atmospheric carbon dioxide (CO2) concentrations measured on the EPICA (European Project for Ice Coring in Antarctica) Dome Concordia ice core extends the Vostok CO2 record back to 650,000 years before the present (yr B.P.). Before 430,000 yr B.P., partial pressure...
Published in: | Science |
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Main Authors: | , , , , , , , , , , |
Other Authors: | , , , , , , , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
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2005
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Online Access: | https://insu.hal.science/insu-00374945 https://insu.hal.science/insu-00374945/document https://insu.hal.science/insu-00374945/file/1313.full.pdf https://doi.org/10.1126/science.1120130 |
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English |
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[SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere |
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[SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere Siegenthaler, Urs Stocker, Thomas F. Monnin, Eric Lüthi, Dieter Schwander, Jakob Stauffer, Bernard Raynaud, Dominique Barnola, Jean-Marc Fischer, Hubertus Masson-Delmotte, Valérie Jouzel, Jean Stable Carbon Cycle–Climate Relationship During the Late Pleistocene |
topic_facet |
[SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere |
description |
International audience A record of atmospheric carbon dioxide (CO2) concentrations measured on the EPICA (European Project for Ice Coring in Antarctica) Dome Concordia ice core extends the Vostok CO2 record back to 650,000 years before the present (yr B.P.). Before 430,000 yr B.P., partial pressure of atmospheric CO2 lies within the range of 260 and 180 parts per million by volume. This range is almost 30% smaller than that of the last four glacial cycles; however, the apparent sensitivity between deuterium and CO2 remains stable throughout the six glacial cycles, suggesting that the relationship between CO2 and Antarctic climate remained rather constant over this interval. |
author2 |
Climate and Environmental Physics Bern (CEP) Physikalisches Institut Bern Universität Bern / University of Bern (UNIBE)-Universität Bern / University of Bern (UNIBE) Laboratoire de glaciologie et géophysique de l'environnement (LGGE) Observatoire des Sciences de l'Univers de Grenoble (OSUG) Université Joseph Fourier - Grenoble 1 (UJF)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut national des sciences de l'Univers (INSU - CNRS)-Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)-Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS)-Université Joseph Fourier - Grenoble 1 (UJF)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut national des sciences de l'Univers (INSU - CNRS)-Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)-Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS)-Centre National de la Recherche Scientifique (CNRS) Abteilung Klinische Sozialmedizin, Berufs- und Umweltdermatologie Universität Heidelberg Heidelberg = Heidelberg University Laboratoire des Sciences du Climat et de l'Environnement Gif-sur-Yvette (LSCE) 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)-Direction de Recherche Fondamentale (CEA) (DRF (CEA)) Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA) Glaces et Continents, Climats et Isotopes Stables (GLACCIOS) Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-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)-Direction de Recherche Fondamentale (CEA) (DRF (CEA)) |
format |
Article in Journal/Newspaper |
author |
Siegenthaler, Urs Stocker, Thomas F. Monnin, Eric Lüthi, Dieter Schwander, Jakob Stauffer, Bernard Raynaud, Dominique Barnola, Jean-Marc Fischer, Hubertus Masson-Delmotte, Valérie Jouzel, Jean |
author_facet |
Siegenthaler, Urs Stocker, Thomas F. Monnin, Eric Lüthi, Dieter Schwander, Jakob Stauffer, Bernard Raynaud, Dominique Barnola, Jean-Marc Fischer, Hubertus Masson-Delmotte, Valérie Jouzel, Jean |
author_sort |
Siegenthaler, Urs |
title |
Stable Carbon Cycle–Climate Relationship During the Late Pleistocene |
title_short |
Stable Carbon Cycle–Climate Relationship During the Late Pleistocene |
title_full |
Stable Carbon Cycle–Climate Relationship During the Late Pleistocene |
title_fullStr |
Stable Carbon Cycle–Climate Relationship During the Late Pleistocene |
title_full_unstemmed |
Stable Carbon Cycle–Climate Relationship During the Late Pleistocene |
title_sort |
stable carbon cycle–climate relationship during the late pleistocene |
publisher |
HAL CCSD |
publishDate |
2005 |
url |
https://insu.hal.science/insu-00374945 https://insu.hal.science/insu-00374945/document https://insu.hal.science/insu-00374945/file/1313.full.pdf https://doi.org/10.1126/science.1120130 |
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Antarctic |
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Antarctic |
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Antarc* Antarctic Antarctica EPICA ice core |
genre_facet |
Antarc* Antarctic Antarctica EPICA ice core |
op_source |
ISSN: 0036-8075 EISSN: 1095-9203 Science https://insu.hal.science/insu-00374945 Science, 2005, 310 (5752), pp.1313 à 1317. ⟨10.1126/science.1120130⟩ |
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info:eu-repo/semantics/altIdentifier/doi/10.1126/science.1120130 insu-00374945 https://insu.hal.science/insu-00374945 https://insu.hal.science/insu-00374945/document https://insu.hal.science/insu-00374945/file/1313.full.pdf doi:10.1126/science.1120130 |
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info:eu-repo/semantics/OpenAccess |
op_doi |
https://doi.org/10.1126/science.1120130 |
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Science |
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310 |
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5752 |
container_start_page |
1313 |
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1317 |
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1801383858633965568 |
spelling |
ftsorbonneuniv:oai:HAL:insu-00374945v1 2024-06-09T07:40:27+00:00 Stable Carbon Cycle–Climate Relationship During the Late Pleistocene Siegenthaler, Urs Stocker, Thomas F. Monnin, Eric Lüthi, Dieter Schwander, Jakob Stauffer, Bernard Raynaud, Dominique Barnola, Jean-Marc Fischer, Hubertus Masson-Delmotte, Valérie Jouzel, Jean Climate and Environmental Physics Bern (CEP) Physikalisches Institut Bern Universität Bern / University of Bern (UNIBE)-Universität Bern / University of Bern (UNIBE) Laboratoire de glaciologie et géophysique de l'environnement (LGGE) Observatoire des Sciences de l'Univers de Grenoble (OSUG) Université Joseph Fourier - Grenoble 1 (UJF)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut national des sciences de l'Univers (INSU - CNRS)-Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)-Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS)-Université Joseph Fourier - Grenoble 1 (UJF)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut national des sciences de l'Univers (INSU - CNRS)-Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)-Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS)-Centre National de la Recherche Scientifique (CNRS) Abteilung Klinische Sozialmedizin, Berufs- und Umweltdermatologie Universität Heidelberg Heidelberg = Heidelberg University Laboratoire des Sciences du Climat et de l'Environnement Gif-sur-Yvette (LSCE) 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)-Direction de Recherche Fondamentale (CEA) (DRF (CEA)) Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA) Glaces et Continents, Climats et Isotopes Stables (GLACCIOS) Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-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)-Direction de Recherche Fondamentale (CEA) (DRF (CEA)) 2005 https://insu.hal.science/insu-00374945 https://insu.hal.science/insu-00374945/document https://insu.hal.science/insu-00374945/file/1313.full.pdf https://doi.org/10.1126/science.1120130 en eng HAL CCSD American Association for the Advancement of Science (AAAS) info:eu-repo/semantics/altIdentifier/doi/10.1126/science.1120130 insu-00374945 https://insu.hal.science/insu-00374945 https://insu.hal.science/insu-00374945/document https://insu.hal.science/insu-00374945/file/1313.full.pdf doi:10.1126/science.1120130 info:eu-repo/semantics/OpenAccess ISSN: 0036-8075 EISSN: 1095-9203 Science https://insu.hal.science/insu-00374945 Science, 2005, 310 (5752), pp.1313 à 1317. ⟨10.1126/science.1120130⟩ [SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere info:eu-repo/semantics/article Journal articles 2005 ftsorbonneuniv https://doi.org/10.1126/science.1120130 2024-05-16T23:55:59Z International audience A record of atmospheric carbon dioxide (CO2) concentrations measured on the EPICA (European Project for Ice Coring in Antarctica) Dome Concordia ice core extends the Vostok CO2 record back to 650,000 years before the present (yr B.P.). Before 430,000 yr B.P., partial pressure of atmospheric CO2 lies within the range of 260 and 180 parts per million by volume. This range is almost 30% smaller than that of the last four glacial cycles; however, the apparent sensitivity between deuterium and CO2 remains stable throughout the six glacial cycles, suggesting that the relationship between CO2 and Antarctic climate remained rather constant over this interval. Article in Journal/Newspaper Antarc* Antarctic Antarctica EPICA ice core HAL Sorbonne Université Antarctic Science 310 5752 1313 1317 |