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DOI	10.1016/j.yqres.2009.11.004
	Climate change since 11.5 ka on the Diancang Massif on the southeastern margin of the Tibetan Plateau
	Yang, Jiangqiang; Zhang, Wei; Cui, Zhijiu; Yi, Chaolu; Chen, Yixin; Xu, Xiangke
通讯作者	Yang, JQ (通讯作者)
发表日期	2010
ISSN	0033-5894
EISSN	1096-0287
起始页码	304
结束页码	312
卷号	73 期号:2
英文摘要	The Diancang Massif is located in a region linking the Tibetan and Yungui Plateaus. Climatically, it is in a transition belt between the south and middle subtropical zones, controlled by Indian monsoon and westerlies. Thus, this study provides more evidences on the evolution of Indian monsoon since the Holocene. We reconstruct the history of climate on the Diancang Massif since 11.5 ka, using integrated correlation of glacial activities, early human settlement sites, and climate proxies abstracted from variations in grain size, magnetic susceptibility, geochemical composition, and pollen in lacustrine sediments. Six climatic stages have been identified. Stage 1, from 11.5 ka to 9.0 ka, is a relatively wet period, corresponding to the onset of the Holocene; from 9.5 ka to 6.0 ka, the climate is arid; a cold period follows from 6.0 ka to 5.3 ka, and this is Succeeded by a temperate stage from 5.3 ka to 4.0 ka; from 4.0 ka to 0.73 ka the climate is again arid. Compared with other regions dominated by the Indian monsoon, there is a delay in response of the climate on the Diancang Massif to the onset of the Holocene. (C) 2009 University of Washington. Published by Elsevier Inc. All Fights reserved.
关键词	ASIAN MONSOON HIGH-RESOLUTION SUMMER MONSOON POLLEN EVIDENCE HOLOCENE GLACIATION EVOLUTION SEDIMENTS HIMALAYA RECORD
英文关键词	Diancang Massif; Climate change; Indian Monsoon; Holocene
语种	英语
WOS研究方向	Physical Geography ; Geology
WOS类目	Geography, Physical ; Geosciences, Multidisciplinary
WOS记录号	WOS:000275246700015
来源期刊	QUATERNARY RESEARCH
来源机构	中国科学院青藏高原研究所
文献类型	期刊论文
条目标识符	http://gcip.llas.ac.cn/handle/2XKMVOVA/257784
推荐引用方式 GB/T 7714	Yang, Jiangqiang,Zhang, Wei,Cui, Zhijiu,et al. Climate change since 11.5 ka on the Diancang Massif on the southeastern margin of the Tibetan Plateau[J]. 中国科学院青藏高原研究所,2010,73(2).
APA	Yang, Jiangqiang,Zhang, Wei,Cui, Zhijiu,Yi, Chaolu,Chen, Yixin,&Xu, Xiangke.(2010).Climate change since 11.5 ka on the Diancang Massif on the southeastern margin of the Tibetan Plateau.QUATERNARY RESEARCH,73(2).
MLA	Yang, Jiangqiang,et al."Climate change since 11.5 ka on the Diancang Massif on the southeastern margin of the Tibetan Plateau".QUATERNARY RESEARCH 73.2(2010).