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Science 25 November 2005: Vol. 310. no. 5752, pp. 1313 - 1317 DOI: 10.1126/science.1120130
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Reports
Stable Carbon CycleClimate Relationship During the Late Pleistocene
Urs Siegenthaler,1
Thomas F. Stocker,1*
Eric Monnin,1
Dieter Lüthi,1
Jakob Schwander,1
Bernhard Stauffer,1
Dominique Raynaud,2
Jean-Marc Barnola,2
Hubertus Fischer,3
Valérie Masson-Delmotte,4
Jean Jouzel4
A record of atmospheric carbon dioxide (CO 2) concentrations measured on the EPICA (European Project for Ice Coring in Antarctica) Dome Concordia ice core extends the Vostok CO 2 record back to 650,000 years before the present (yr B.P.). Before 430,000 yr B.P., partial pressure of atmospheric CO 2 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 CO 2 remains stable throughout the six glacial cycles, suggesting that the relationship between CO 2 and Antarctic climate remained rather constant over this interval.
1 Climate and Environmental Physics, Physics Institute, University of Bern, Sidlerstrasse 5, CH-3012 Bern, Switzerland.
2 Laboratoire de Glaciologie et de Géophysique de l'Environnement (CNRS), 54 Rue Molières, 38402 St. Martin d'Hères Cedex, France.
3 Alfred Wegener Institute for Polar and Marine Research (AWI), Columbusstrasse, D-27568 Bremerhaven, Germany.
4 Institut Pierre Simon Laplace/Laboratoire des Sciences du Climat et de l'Environnement, CEA-CNRS 1572, CE Saclay, Orme des Merisiers, 91191 Gif-sur-Yvette, France.
* To whom correspondence should be addressed. E-mail: stocker{at}climate.unibe.ch
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