Air–sea temperature decoupling in western Europe during the last interglacial–glacial transition

被引：0

作者：

María Fernanda Sánchez Goñi

Edouard Bard

Amaelle Landais

Linda Rossignol

Francesco d’Errico

机构：

[1] Ecole Pratique des Hautes Etudes,Department of Archaeology

[2] UMR-CNRS 5805 EPOC,undefined

[3] Université Bordeaux 1,undefined

[4] Aix Marseille Université,undefined

[5] CNRS,undefined

[6] IRD,undefined

[7] Collège de France,undefined

[8] UM CEREGE,undefined

[9] IPSL / Laboratoire des Sciences du Climat et de l’Environnement CEA CNRS UVSQ UMR 8212,undefined

[10] Université Bordeaux 1,undefined

[11] UMR-CNRS 5805 EPOC,undefined

[12] CNRS UMR 5199 PACEA-PPP,undefined

[13] Université Bordeaux 1,undefined

[14] History,undefined

[15] Cultural Studies and Religion,undefined

[16] University of Bergen,undefined

来源：

Nature Geoscience | 2013年 / 6卷

关键词：

D O I：

暂无

中图分类号：

学科分类号：

摘要：

Between 80,000 and 70,000 years ago, climate cooled and ice sheets in the high northern latitudes expanded. Pollen and microfossil data from marine sediments indicate that an increasing thermal gradient between cold air and warmer oceans could have supported continental ice growth.

引用

页码：837 / 841

页数：4

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