Stable Carbon Cycle: Climate Relationship during the Late Pleistocene
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 CO2record back to 650,000 years before the present (yr B.P.). Before 430,000 yr B.P., partial pressure of atmospheric CO2lies w...
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| Veröffentlicht in: | Science (American Association for the Advancement of Science) 2005-11, Vol.310 (5752), p.1313-1317 |
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| creator | Siegenthaler, Urs Stocker, Thomas F. Monnin, Eric Lüthi, Dieter Schwander, Jakob Stauffer, Bernhard Raynaud, Dominique Barnola, Jean-Marc Fischer, Hubertus Masson-Delmotte, Valérie Jouzel, Jean |
| description | 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 CO2record back to 650,000 years before the present (yr B.P.). Before 430,000 yr B.P., partial pressure of atmospheric CO2lies 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 CO2remains stable throughout the six glacial cycles, suggesting that the relationship between CO2and Antarctic climate remained rather constant over this interval. |
| doi_str_mv | 10.1126/science.1120130 |
| format | Article |
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Before 430,000 yr B.P., partial pressure of atmospheric CO2lies 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 CO2remains stable throughout the six glacial cycles, suggesting that the relationship between CO2and Antarctic climate remained rather constant over this interval.</description><identifier>ISSN: 0036-8075</identifier><identifier>EISSN: 1095-9203</identifier><identifier>DOI: 10.1126/science.1120130</identifier><identifier>PMID: 16311332</identifier><identifier>CODEN: SCIEAS</identifier><language>eng</language><publisher>Washington, DC: American Association for the Advancement of Science</publisher><subject>Analysis ; Atmosphere ; Atmospherics ; Carbon cycle ; Carbon cycle (Biogeochemistry) ; Carbon dioxide ; Climate ; Climate cycles ; Deuterium ; Earth sciences ; Earth, ocean, space ; Exact sciences and technology ; Geological time ; Glacial epoch ; Glaciers ; Greenhouse gases ; Ice ; Ice ages ; Ice cores ; Isotope geochemistry ; Isotope geochemistry. Geochronology ; Marine isotope stages ; Observations ; Ocean, Atmosphere ; Paleoclimatology ; Protection and preservation ; Sampling ; Sciences of the Universe</subject><ispartof>Science (American Association for the Advancement of Science), 2005-11, Vol.310 (5752), p.1313-1317</ispartof><rights>Copyright 2005 American Association for the Advancement of Science</rights><rights>2006 INIST-CNRS</rights><rights>COPYRIGHT 2005 American Association for the Advancement of Science</rights><rights>COPYRIGHT 2005 American Association for the Advancement of Science</rights><rights>Copyright American Association for the Advancement of Science Nov 25, 2005</rights><rights>Distributed under a Creative Commons Attribution 4.0 International License</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a812t-6596b612a0e948f34beefd7a4be3b087ed0806b826d47662ce8e96341447e31c3</citedby><cites>FETCH-LOGICAL-a812t-6596b612a0e948f34beefd7a4be3b087ed0806b826d47662ce8e96341447e31c3</cites><orcidid>0000-0001-8296-381X ; 0000-0002-2787-4221</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://www.jstor.org/stable/pdf/3843209$$EPDF$$P50$$Gjstor$$H</linktopdf><linktohtml>$$Uhttps://www.jstor.org/stable/3843209$$EHTML$$P50$$Gjstor$$H</linktohtml><link.rule.ids>230,314,776,780,799,881,2871,2872,27901,27902,57992,58225</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=17346582$$DView record in Pascal Francis$$Hfree_for_read</backlink><backlink>$$Uhttps://www.ncbi.nlm.nih.gov/pubmed/16311332$$D View this record in MEDLINE/PubMed$$Hfree_for_read</backlink><backlink>$$Uhttps://insu.hal.science/insu-00374945$$DView record in HAL$$Hfree_for_read</backlink></links><search><creatorcontrib>Siegenthaler, Urs</creatorcontrib><creatorcontrib>Stocker, Thomas F.</creatorcontrib><creatorcontrib>Monnin, Eric</creatorcontrib><creatorcontrib>Lüthi, Dieter</creatorcontrib><creatorcontrib>Schwander, Jakob</creatorcontrib><creatorcontrib>Stauffer, Bernhard</creatorcontrib><creatorcontrib>Raynaud, Dominique</creatorcontrib><creatorcontrib>Barnola, Jean-Marc</creatorcontrib><creatorcontrib>Fischer, Hubertus</creatorcontrib><creatorcontrib>Masson-Delmotte, Valérie</creatorcontrib><creatorcontrib>Jouzel, Jean</creatorcontrib><title>Stable Carbon Cycle: Climate Relationship during the Late Pleistocene</title><title>Science (American Association for the Advancement of Science)</title><addtitle>Science</addtitle><description>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 CO2record back to 650,000 years before the present (yr B.P.). Before 430,000 yr B.P., partial pressure of atmospheric CO2lies within the range of 260 and 180 parts per million by volume. 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Geochronology</subject><subject>Marine isotope stages</subject><subject>Observations</subject><subject>Ocean, Atmosphere</subject><subject>Paleoclimatology</subject><subject>Protection and preservation</subject><subject>Sampling</subject><subject>Sciences of the Universe</subject><issn>0036-8075</issn><issn>1095-9203</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2005</creationdate><recordtype>article</recordtype><sourceid>8G5</sourceid><sourceid>BEC</sourceid><sourceid>BENPR</sourceid><sourceid>GUQSH</sourceid><sourceid>M2O</sourceid><recordid>eNqN09Fr1DAcB_Aiijunz76IlIGCQrekSdPEt7PM2-DwxKmvIU1_vcvINWfSivvvzXFl4-RgRx9C-_v8SvprvknyGqNzjHN2EbSBTsP2BmGCniQTjESRiRyRp8kEIcIyjsriJHkRwi1CsSbI8-QEM4IxIfkkubzpVW0hrZSvXZdWd9rCp7SyZq16SL-DVb1xXViZTdoM3nTLtF9BOt8Wv1kwoXcaOniZPGuVDfBqXE-Tn18uf1RX2Xwxu66m80xxnPcZKwSrGc4VAkF5S2gN0DaliiupES-hQRyxmuesoSVjuQYOghGKKS2BYE1Ok4-7966UlRsfN-nvpFNGXk3n0nRhkPGTSypo8QdH_H6HN979HiD0cm2CBmtVB24IknFOaF7wR2HOkRAFJY9CXNI4Vo4iPPsP3rrBd3E0MsekECUWRUTZDi2Vhbj71vVe6WUcp1fWddCa-HiKiRAYs4JFf37Ax6uBtdEHGz7sNUTTw99-qYYQ5PXN1-Pt4tfx9vPsaMtn832bHbLaWQtLkPEkVYt9f7Hz2rsQPLT3RwIjuY2HHOMhx3jEjrfjfxnqNTQPfsxDBO9GoIJWtvWq0yY8uJJQVvCte7NztzEB_r5OOCU5EuQfPpoZPQ</recordid><startdate>20051125</startdate><enddate>20051125</enddate><creator>Siegenthaler, Urs</creator><creator>Stocker, Thomas F.</creator><creator>Monnin, Eric</creator><creator>Lüthi, Dieter</creator><creator>Schwander, Jakob</creator><creator>Stauffer, Bernhard</creator><creator>Raynaud, Dominique</creator><creator>Barnola, Jean-Marc</creator><creator>Fischer, Hubertus</creator><creator>Masson-Delmotte, Valérie</creator><creator>Jouzel, Jean</creator><general>American Association for the Advancement of Science</general><general>The American Association for the Advancement of Science</general><general>American Association for the Advancement of Science (AAAS)</general><scope>IQODW</scope><scope>NPM</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>8GL</scope><scope>IBG</scope><scope>IOV</scope><scope>ISN</scope><scope>0-V</scope><scope>3V.</scope><scope>7QF</scope><scope>7QG</scope><scope>7QL</scope><scope>7QP</scope><scope>7QQ</scope><scope>7QR</scope><scope>7SC</scope><scope>7SE</scope><scope>7SN</scope><scope>7SP</scope><scope>7SR</scope><scope>7SS</scope><scope>7T7</scope><scope>7TA</scope><scope>7TB</scope><scope>7TK</scope><scope>7TM</scope><scope>7U5</scope><scope>7U9</scope><scope>7X2</scope><scope>7X7</scope><scope>7XB</scope><scope>88A</scope><scope>88B</scope><scope>88E</scope><scope>88I</scope><scope>8AF</scope><scope>8BQ</scope><scope>8FD</scope><scope>8FE</scope><scope>8FG</scope><scope>8FH</scope><scope>8FI</scope><scope>8FJ</scope><scope>8FK</scope><scope>8G5</scope><scope>ABJCF</scope><scope>ABUWG</scope><scope>AEUYN</scope><scope>AFKRA</scope><scope>ALSLI</scope><scope>ARAPS</scope><scope>ATCPS</scope><scope>AZQEC</scope><scope>BBNVY</scope><scope>BEC</scope><scope>BENPR</scope><scope>BGLVJ</scope><scope>BHPHI</scope><scope>BKSAR</scope><scope>C1K</scope><scope>CCPQU</scope><scope>CJNVE</scope><scope>D1I</scope><scope>DWQXO</scope><scope>F28</scope><scope>FR3</scope><scope>FYUFA</scope><scope>GHDGH</scope><scope>GNUQQ</scope><scope>GUQSH</scope><scope>H8D</scope><scope>H8G</scope><scope>H94</scope><scope>HCIFZ</scope><scope>JG9</scope><scope>JQ2</scope><scope>K9-</scope><scope>K9.</scope><scope>KB.</scope><scope>KR7</scope><scope>L6V</scope><scope>L7M</scope><scope>LK8</scope><scope>L~C</scope><scope>L~D</scope><scope>M0K</scope><scope>M0P</scope><scope>M0R</scope><scope>M0S</scope><scope>M1P</scope><scope>M2O</scope><scope>M2P</scope><scope>M7N</scope><scope>M7P</scope><scope>M7S</scope><scope>MBDVC</scope><scope>P5Z</scope><scope>P62</scope><scope>P64</scope><scope>PATMY</scope><scope>PCBAR</scope><scope>PDBOC</scope><scope>PQEDU</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PRINS</scope><scope>PTHSS</scope><scope>PYCSY</scope><scope>Q9U</scope><scope>R05</scope><scope>RC3</scope><scope>7TG</scope><scope>7TN</scope><scope>F1W</scope><scope>H96</scope><scope>KL.</scope><scope>L.G</scope><scope>7X8</scope><scope>1XC</scope><scope>VOOES</scope><orcidid>https://orcid.org/0000-0001-8296-381X</orcidid><orcidid>https://orcid.org/0000-0002-2787-4221</orcidid></search><sort><creationdate>20051125</creationdate><title>Stable Carbon Cycle: Climate Relationship during the Late Pleistocene</title><author>Siegenthaler, Urs ; 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the Vostok CO2record back to 650,000 years before the present (yr B.P.). Before 430,000 yr B.P., partial pressure of atmospheric CO2lies 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 CO2remains stable throughout the six glacial cycles, suggesting that the relationship between CO2and Antarctic climate remained rather constant over this interval.</abstract><cop>Washington, DC</cop><pub>American Association for the Advancement of Science</pub><pmid>16311332</pmid><doi>10.1126/science.1120130</doi><tpages>5</tpages><orcidid>https://orcid.org/0000-0001-8296-381X</orcidid><orcidid>https://orcid.org/0000-0002-2787-4221</orcidid><oa>free_for_read</oa></addata></record> |
| fulltext | fulltext |
| identifier | ISSN: 0036-8075 |
| ispartof | Science (American Association for the Advancement of Science), 2005-11, Vol.310 (5752), p.1313-1317 |
| issn | 0036-8075 1095-9203 |
| language | eng |
| recordid | cdi_hal_primary_oai_HAL_insu_00374945v1 |
| source | American Association for the Advancement of Science; Jstor Complete Legacy |
| subjects | Analysis Atmosphere Atmospherics Carbon cycle Carbon cycle (Biogeochemistry) Carbon dioxide Climate Climate cycles Deuterium Earth sciences Earth, ocean, space Exact sciences and technology Geological time Glacial epoch Glaciers Greenhouse gases Ice Ice ages Ice cores Isotope geochemistry Isotope geochemistry. Geochronology Marine isotope stages Observations Ocean, Atmosphere Paleoclimatology Protection and preservation Sampling Sciences of the Universe |
| title | Stable Carbon Cycle: Climate Relationship during the Late Pleistocene |
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