Palaeoclimatic evolution recorded by multidicipline in sediments in gahai lake, qaidam basin since late last deglacial  

作　　者：Chen Zhong Ma Haizhou Cao Guangchao Zhang Xiying Zhou Dujun Yao Yuan Yang Guangshu 

机构地区：[1]Faculty of Land Resource Engineering, Kunming University of Science and Technology, Kunming 650093, P.R. China [2]Qinghai Institute of Salt Lake, Chinese Academy of Sciences, Xining 810008, P.R. China [3]School of Life and Geography Science, Qinghai Normal University, Xining 810008, P.R. China [4]East China Geological Exploration Institute of Non-ferrous Metals, Nanjing 210007, P.R. China

出　　处：《High Technology Letters》2010年第3期324-330,共7页高技术通讯（英文版）

摘　　要：Based on the analyses of Loss-on-Ignition （LOI）, carbonate content and sediment characteristics, this paper reconstructs the climatic and environmental evolution of the Gahai lake area since the late Last Deglacial Period. The results cover the late Last Deglacial Period and the Holocene. The climate was very unstable and rather arid during the late Last Deglacial Period. The Holocene can be divided into three periods： the early Holocene （11360-8240 cal aB. P. ）, which was dry but unstable and featured rising temperatures, the mid-Holocene （8240-3200 cal aB. P. ）, which was warm and wet and the late Holocene （ since 3200 cal aBP）, which was cold and dry. Results also show a warm-wet event around 1500 cal aB. P.

关 键 词：Gahai Lake late Last Deglaciation HOLOCENE PALAEOCLIMATE 

分 类 号：P532[天文地球—古生物学与地层学] TS396.7[天文地球—地质学]