Correlation of climatic events between East Asia and Norwegian Sea during last deglaciation
Zhou, WJ; An, ZS; Porter, SC; Donahue, D; Jull, AJT
1997-10
发表期刊SCIENCE IN CHINA SERIES D-EARTH SCIENCES
卷号40期号:5页码:496-501
文章类型Article
摘要Using a high resolution C-14 chronology, delta(13)C values and organic carbon content, from loess/paleosol and peat profiles in China, we can demonstrate century scale warm-cold East Asian monsoon paleoclimatic fluctuation events and significant precipitation variability within the last deglaciation. The major climatic events recognized are the Bolling (1 300-12 500 a B. P.), Older Dryas (12 500-11 750 a B. P.), Allerod (11 750-11 200 a B. P.) and Younger Dryas (11 200-10 000 a B. P.). The stratigraphic structure of the last deglaciation sediments is characterized by frequent changes in sedimentation phases reflecting climatic instability. These high frequency, rapid climatic events can correlate with fluctuations recorded by sea surface temperatures in the Norwegian Sea. This indicates a pale oclimate teleconnection between polar, high latitude areas and East Asian monsoon areas through westerlies and the related atmospheric pressure system.
关键词last deglaciation East Asian monsoon paleoclimatic fluctuation loess-paleosol
学科领域Geology
DOI10.1007/BF02877615
关键词[WOS]ATLANTIC ; OCEAN ; LOESS ; CHINA
收录类别SCI ; SCIE
语种英语
WOS研究方向Geosciences, Multidisciplinary
WOS记录号WOS:A1997XU77300008
出版者SCIENCE CHINA PRESS
引用统计
被引频次:4[WOS]   [WOS记录]     [WOS相关记录]
文献类型期刊论文
条目标识符http://ir.ieecas.cn/handle/361006/12093
专题黄土与第四纪地质国家重点实验室(1985-2004)
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Zhou, WJ,An, ZS,Porter, SC,et al. Correlation of climatic events between East Asia and Norwegian Sea during last deglaciation[J]. SCIENCE IN CHINA SERIES D-EARTH SCIENCES,1997,40(5):496-501.
APA Zhou, WJ,An, ZS,Porter, SC,Donahue, D,&Jull, AJT.(1997).Correlation of climatic events between East Asia and Norwegian Sea during last deglaciation.SCIENCE IN CHINA SERIES D-EARTH SCIENCES,40(5),496-501.
MLA Zhou, WJ,et al."Correlation of climatic events between East Asia and Norwegian Sea during last deglaciation".SCIENCE IN CHINA SERIES D-EARTH SCIENCES 40.5(1997):496-501.
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