Orbital and millennial Antarctic climate variability over the past 800,000 years

被引：1594

作者：

Jouzel, J. ^{[1
]}

Masson-Delmotte, V.

Cattani, O.

Dreyfus, G.

Falourd, S.

Hoffmann, G.

Minster, B.

Nouet, J.

Barnola, J. M.

Chappellaz, J.

Fischer, H.

Gallet, J. C.

Johnsen, S.

Leuenberger, M.

Loulergue, L.

Luethi, D.

Oerter, H.

Parrenin, F.

Raisbeck, G.

Raynaud, D.

Schilt, A.

Schwander, J.

Selmo, E.

Souchez, R.

Spahni, R.

Stauffer, B.

Steffensen, J. P.

Stenni, B.

Stocker, T. F.

Tison, J. L.

Werner, M.

Wolff, E. W.

机构：

[1] Univ Versailles St Quentin Yvelines, CE Saclay, Lab Sci Climat & Environn, Inst Pierre Simon Laplace,CEA,CNRS, F-91191 Gif Sur Yvette, France

[2] Univ Grenoble 1, Lab Glaciol & Geophys Environm, CNRS, F-38402 St Martin Dheres, France

[3] Alfred Wegener Inst Polar & Marine Res, D-27568 Bremerhaven, Germany

[4] Univ Copenhagen, Dept Geophys, DK-2100 Copenhagen, Denmark

[5] Univ Reykjavik, Inst Sci, IS-107 Reykjavik, Iceland

[6] Univ Bern, Inst Phys, CH-3012 Bern, Switzerland

[7] CNRS, Ctr Spectrometrie Nucl & Spectrometrie Masse, F-91405 Orsay, France

[8] Univ Parma, Dept Earth Sci, I-43100 Parma, Italy

[9] Univ Libre Bruxelles, Dept Sci Terre & Environm, Brussels, Belgium

[10] Univ Trieste, Dept Geol Environm & Marine Sci, I-34127 Trieste, Italy

[11] Max Planck Inst Biogeochem, D-7701 Jena, Germany

[12] British Antarctic Survey, Cambridge CB3 0ET, England

来源：

SCIENCE | 2007年 / 317卷 / 5839期

基金：

英国自然环境研究理事会;

关键词：

D O I：

10.1126/science.1141038

中图分类号：

O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];

学科分类号：

07 ; 0710 ; 09 ;

摘要：

A high-resolution deuterium profile is now available along the entire European Project for Ice Coring in Antarctica Dome C ice core, extending this climate record back to marine isotope stage 20.2, similar to 800,000 years ago. Experiments performed with an atmospheric general circulation model including water isotopes support its temperature interpretation. We assessed the general correspondence between Dansgaard-Oeschger events and their smoothed Antarctic counterparts for this Dome C record, which reveals the presence of such features with similar amplitudes during previous glacial periods. We suggest that the interplay between obliquity and precession accounts for the variable intensity of interglacial periods in ice core records.

引用

页码：793 / 796

页数：4

共 41 条

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