Stable Carbon CycleClimate Relationship During the Late Pleistocene-Reference-Cited by-同舟云学术

Stable Carbon CycleClimate Relationship During the Late Pleistocene

Published:2005-11-25 Issue:5752 Volume:310 Page:1313-1317
ISSN:0036-8075
Container-title:Science
language:en
Short-container-title:Science

Author:

Siegenthaler Urs¹²³⁴,Stocker Thomas F.¹²³⁴,Monnin Eric¹²³⁴,Lüthi Dieter¹²³⁴,Schwander Jakob¹²³⁴,Stauffer Bernhard¹²³⁴,Raynaud Dominique¹²³⁴,Barnola Jean-Marc¹²³⁴,Fischer Hubertus¹²³⁴,Masson-Delmotte Valérie¹²³⁴,Jouzel Jean¹²³⁴

Affiliation:

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.

Abstract

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.

Publisher

American Association for the Advancement of Science (AAAS)

Subject

Multidisciplinary

Reference34 articles.

1. Eight glacial cycles from an Antarctic ice core

2. Vostok ice core provides 160,000-year record of atmospheric CO2

3. Natural and anthropogenic changes in atmospheric CO2over the last 1000 years from air in Antarctic ice and firn

4. Atmospheric CO2 concentration and millennial-scale climate change during the last glacial period

5. Ice Core Records of Atmospheric CO 2 Around the Last Three Glacial Terminations

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