中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
12 kaBP lake environment on the Tibetan Plateau

文献类型:期刊论文

作者Li, BY; Wang, SM; Zhu, LP; Li, YF
刊名SCIENCE IN CHINA SERIES D-EARTH SCIENCES
出版日期2001
卷号44期号:supp页码:324-331
关键词glaciers melting period Tibetan Plateau lake environment
英文摘要The systemic analyses have been carried out in this paper to the paleolake shorelines, paleolake sediments and paleoclimatic proxies of 20 lakes, in which there were 12 kaBP dating data on the Tibetan Plateau. The results showed that the paleolake level had apparently risen during 14-11 kaBP, the glaciers melting period, in the Tibetan area and Northwest China. Especially, much more increasing amplitude supplied by thawy glaciers water occurred than in the best period of Holocene. The temperate-humid climate around 12 kaBP appeared in the Tibetan area and even in the whole China. This event may be compared with the Bolling/Allerod warm period which was reflected by Europe and Greenland ice core records. It showed that the B/A event was not a regional one in the North Atlantic area.
公开日期2012-03-02
源URL[http://159.226.73.51/handle/332005/2349]  
专题南京地理与湖泊研究所_湖泊室
推荐引用方式
GB/T 7714
Li, BY,Wang, SM,Zhu, LP,et al. 12 kaBP lake environment on the Tibetan Plateau[J]. SCIENCE IN CHINA SERIES D-EARTH SCIENCES,2001,44(supp):324-331.
APA Li, BY,Wang, SM,Zhu, LP,&Li, YF.(2001).12 kaBP lake environment on the Tibetan Plateau.SCIENCE IN CHINA SERIES D-EARTH SCIENCES,44(supp),324-331.
MLA Li, BY,et al."12 kaBP lake environment on the Tibetan Plateau".SCIENCE IN CHINA SERIES D-EARTH SCIENCES 44.supp(2001):324-331.

入库方式: OAI收割

来源:南京地理与湖泊研究所

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