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JOURNAL OF DESERT RESEARCH  2013, Vol. 33 Issue (5): 1314-1323    DOI: 10.7522/j.issn.1000-694X.2013.00195
Paleoclimate and Environment Evolution     
Record for Climate Revolution in Aeolian Deposit of Nabkhas around the Ebinur Lake
JIN Jian-hui1,2, CAO Xiang-dong3, LI Zhi-zhong1,2, CHEN Xiu-ling1,2, HU Fan-gen1, XIA Jing1, WANG Xian-li1
1.Institute of Geography/School of Geography Science/Ministry of Education Key Laboratory of Humid Subtropical Eco-geographycal Process, Fujian Normal University, Fuzhou 350007, China;
2.State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, Xian 710075, China;
3.Xinjiang Education Institute, Urumqi 830000, China
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Abstract  

Analysis on nabkhas around the Ebinur Lake which located in northern Xinjiang of westerly zone show that the aeolian deposit of nabkhas was formed in late Holocene and there was a lack of aeolian deposit in early-mid Holocene. Comparative studies also revealed that the climate in the region had experienced a number of warm-dry and cold-wet (cool-wet)changes since the late Holocene. The nabkhas around Ebinur Lake were well-developed and contained 3 dry periods and 3 wet periods at least since the late glacial epoch. The records of climate revolution in the region are in good agreement with the climate revolution from other Holocene records in northern Xinjiang. The change basically follows in the steps of westerly dominated Holocene climatic model, and also is affected by the sandstorm landscape of Ebinur Lake area.

Key words:  nabkhas      aeolian deposit      grain composition      geochemical elements      climate revolution      Ebinur Lake     
Received:  06 July 2012      Published:  27 July 2012
ZTFLH:  P532  
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Cite this article: 

. Record for Climate Revolution in Aeolian Deposit of Nabkhas around the Ebinur Lake. JOURNAL OF DESERT RESEARCH, 2013, 33(5): 1314-1323.

URL: 

http://www.desert.ac.cn/EN/10.7522/j.issn.1000-694X.2013.00195     OR     http://www.desert.ac.cn/EN/Y2013/V33/I5/1314

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