The deep ocean during the last interglacial period

被引:53
作者
Duplessy, J. C.
Roche, D. M.
Kageyama, M.
机构
[1] Univ Versailles, CNRS,CEA,UVSQ, LSCE,IPSL, Lab Commissarial Energie Atom, F-91198 Gif Sur Yvette, France
[2] Vrije Univ Amsterdam, Dept Paleoclimatol & Geomorphol, NL-1081 HV Amsterdam, Netherlands
[3] Univ Versailles, CNRS,Lab CEA,UVSQ, LSCE,IPSL, Lab Sci Climat & Environm, F-91198 Gif Sur Yvette, France
关键词
D O I
10.1126/science.1138582
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
Oxygen isotope analysis of benthic foraminifera in deep sea cores from the Atlantic and Southern Oceans shows that during the last interglacial period, North Atlantic Deep Water (NADW) was 0.4 degrees +/- 0.2 degrees C warmer than today, whereas Antarctic Bottom Water temperatures were unchanged. Model simulations show that this distribution of deep water temperatures can be explained as a response of the ocean to forcing by high-latitude insolation. The warming of NADW was transferred to the Circumpolar Deep Water, providing additional heat around Antarctica, which may have been responsible for partial melting of the West Antarctic Ice Sheet.
引用
收藏
页码:89 / 91
页数:3
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