A 1000-year record of Mg/Li and Li/Ca ratios of ostracod shells in Lake Qinghai,NE Tibetan Plateau  

作　　者：ZHU Zhengjie XIANG Yu LI Yanjun 

机构地区：[1]Chongqing Key Laboratory of Exogenic Mineralization and Mine Environment, Chongqing Institute of Geology and Mineral Resources [2]Chongqing Research Center of State Key Laboratory of Coal Resources and Safe Mining

出　　处：《Acta Geologica Sinica(English Edition)》2014年第S1期39-40,共2页地质学报（英文版）

基　　金：financially supported by the project of National Natural Science Foundation of China (Grant No. 41073097);the project of Natural Science Foundation of Chongqing, China (Grant NO. cstc2013jcyja20001)

摘　　要：1 Introduction Lake Qinghai,famous as the largest inland saline lake in China,located on the high-altitude northeastern Tibetan Plateau,and four junctional zones of the East Asian summer monsoon(EASM),Indian summer monsoon(ISM),East Asian winter monsoon and the westerly jet stream prevail,making it sensitive to global climate change1 Introduction Lake Qinghai,famous as the largest inland saline lake in China,located on the high-altitude northeastern Tibetan Plateau,and four junctional zones of the East Asian summer monsoon(EASM),Indian summer monsoon(ISM),East Asian winter monsoon and the westerly jet stream prevail,making it sensitive to global climate change

关 键 词：Lake Qinghai Li/Ca ratios Mg/Li ratios temperature variations 

分 类 号：Q958[生物学—动物学]