新仙女木事件在罗布泊湖相沉积物中的记录

罗超; 彭子成; 刘卫国; 张兆峰; 贺剑峰; 刘桂建; 张彭熹

Volume 33 Issue 2

Mar. 2008

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Article Navigation > Earth Science > 2008 > 33(2): 190-196

LUO Chao, PENG Zi-cheng, LIU Wei-guo, ZHANG Zhao-feng, HE Jian-feng, LIU Gui-jian, ZHANG Peng-xi, 2008. Evidence from the Lacustrine Sediments of Lop-Nur Lake, Northwest China for the Younger Dryas Event. Earth Science, 33(2): 190-196.

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Evidence from the Lacustrine Sediments of Lop-Nur Lake, Northwest China for the Younger Dryas Event

1.
School of Earth and Space Science, University of Science and Technology of China, Hefei 230026, China
2.
StateKey Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, Xi'an 710054, China
3.
Department of Geology, University of Illinois-Urbana Champaign, Urbana, IL 61801, USA
4.
Qinghai Institute of Salt Lakes, Chinese Academy of Sciences, Xi'an 710043, China

Received Date: 2007-07-16
Publish Date: 2008-03-25

Abstract

Abstract

The environmental proxies of the susceptibility, particle size, and the contents of carbonate and organic carbon in the lacustrine sediments of the CK-2 core from Lop-Nur Lake, Xinjiang, Northwest China are determined in this study.The core section corresponds to the 0.94-5.50 m and 9-14 kaBP.The reconstructed records in Xinjiang, NW China fully demonstrate that the Younger Dryas event occurred within 12.8-11.6 ka BP synchronously with that record in Greenland ice core, and its climate appeared to be cool and humid.These results suggest the rapid response of westerly climate system in the NW China to the climate variability in northern high latitudes in short time.A mechanism involving immigration of westerly winds and the intensity change of the westerly is tentatively proposed to account for this synchronicity.
- Lop-Nur region,
- lacustrine sediments,
- environmental proxies,
- principle component analysis,
- Younger Dryas event

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