Stalagmite evidence for the onset of the Last Interglacial in southern Europe at 129±1 ka -: art. no. L24708

被引：146

作者：

Drysdale, RN

Zanchetta, G

Hellstrom, JC

Fallick, AE

Zhao, JX

机构：

[1] Univ Newcastle, Environm & Climate Change Res Grp, Sch Environm & Life Sci, Callaghan, NSW 2308, Australia

[2] Scottish Univ Environm Res Ctr, E Kilbride G75 0QF, Lanark, Scotland

[3] Univ Pisa, Dipartimento Sci Terra, I-56126 Pisa, Italy

[4] Univ Melbourne, Sch Earth Sci, Parkville, Vic 3010, Australia

[5] Univ Queensland, Dept Earth Sci, St Lucia, Qld 4072, Australia

来源：

GEOPHYSICAL RESEARCH LETTERS | 2005年 / 32卷 / 24期

关键词：

D O I：

10.1029/2005GL024658

中图分类号：

P [天文学、地球科学];

学科分类号：

07 ;

摘要：

Multi-proxy data from an Italian stalagmite constrain the commencement of full Last Interglacial conditions in southern Europe at 129 +/- 1 ka, consistent with absolutely dated records currently available from both hemispheres. The post-glacial transition towards warmer and wetter conditions commenced at 134 +/- 2 ka. Oxygen isotope evidence suggests this was interrupted briefly at 130 +/- 2 ka, an event probably related to the 'Termination II pause' associated with Heinrich Event 11. For most of the stalagmite, the pattern of delta(18)O variation mimics the air temperature record from the Vostok ice core, especially through marine isotope stage 5. There is no obvious evidence for substantial 'early interglacial' warming.

引用

页码：1 / 4

页数：4

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