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  5. Late Pleistocene(MIS 2)Climate Change on the Northern Tibetan Plateau Inferred from Pollen and Geoch

Late Pleistocene(MIS 2)Climate Change on the Northern Tibetan Plateau Inferred from Pollen and Geoch

来源 :The 12th International Conference on Salt Lake Research(第十二届 | 被引量 : 0次 | 上传用户：looksky1989
【摘 要】
：
Introduction A 405-cm sediment section GM02 from Gomo Co salt lake in the northern Tibetan Plateau was used to reconstruct climate changes during marine isotope stage(MIS) 2,including the Last Glacial
【作 者】
：
WANG Yong WANG Jun JI Zhansheng ZHAI Qingguo XIAO Xuchang 
【机 构】
：
Institute of Geology,Chinese Academy of Geological Sciences,Beijing 100037,China
【出 处】
：
The 12th International Conference on Salt Lake Research(第十二届
【发表日期】
：
2014年2期
【关键词】
：
pollen geochemical MIS 2 Last Glacial Maximum Tibetan Plateau 
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Introduction A 405-cm sediment section GM02 from Gomo Co salt lake in the northern Tibetan Plateau was used to reconstruct climate changes during marine isotope stage(MIS) 2,including the Last Glacial Maximum(LGM) and last deglaciation between 23.7 to 12 ka(Fig1).
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