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
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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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