Timing and structure of the Younger Dryas event in northern China

doi:10.1016/j.quascirev.2012.03.006

CORC > 地球环境研究所 > 中国科学院地球环境研究所 > 黄土与第四纪地质国家重点实验室（2010~）

	Timing and structure of the Younger Dryas event in northern China
	Ma, ZB (Ma, Zhi-Bang)[1,2]; Cheng, H (Cheng, Hai)[3,4,5]; Tan, M (Tan, Ming)[1]; Edwards, RL (Edwards, R. Lawrence)[4]; Li, HC (Li, Hong-Chun)[6]; You, CF (You, Chen-Feng)[7]; Duan, WH (Duan, Wu-Hui)[1]; Wang, X (Wang, Xu)[1]; Kelly, MJ (Kelly, Megan J.)[4]
刊名	QUATERNARY SCIENCE REVIEWS
	2012-05-18
卷号	41 页码:83-93
关键词	Asymmetrical Younger Dryas Structure Abrupt Climate Change Asian Monsoon Kulishu Cave Northern China
DOI	10.1016/j.quascirev.2012.03.006
文献子类	期刊论文
英文摘要	A high-resolution and absolute-dated stalagmite record from Kulishu Cave, Beijing characterizes Asian Monsoon (AM) history in northern China between ca 14 and 10.5 ka BP (thousand yrs before present, present = 1950), including the entire Younger Dryas (YD) event. Using Th-230 dates and counting of annual-layers, the shift into the YD began at 12,850 +/- 40 yr BP and took similar to 340 yrs and the shift out of the YD began at 11,560 +/- 40 yr BP and took <38 yrs (best estimate similar to 20 yrs), broadly similar to previously reported AM records from central and southeastern China. The more gradual nature of the start of the YD event as observed in the AM records appears to contrast with the more abrupt beginning observed in the Greenland ice records. The total amplitude of the AM YD event is also smaller than the amplitude of the AM Heinrich Stadial 1 event. In addition, the general rising trend of the AM during the Bolling-Allerod period contrasts with the general cooling trend in Greenland temperature during that time. The influence of rising insolation on the AM may explain this observation.
语种	英语
内容类型	期刊论文
源URL	[http://ir.ieecas.cn/handle/361006/10210]
专题	地球环境研究所_黄土与第四纪地质国家重点实验室（2010~）
通讯作者	Ma, ZB (Ma, Zhi-Bang)[1,2]
作者单位	1.Key Laboratory of Cenozoic Geology and Environment, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China; 2.Key Laboratory of Saline Lake Resources and Environment, Ministry of Land and Resources, Beijing 100037, China; 3.Institute of Global Environmental Change, Xi’an Jiaotong University, Xi’an 710049, China; 4.Department of Earth Sciences, University of Minnesota, Minneapolis, MN 55455, USA; 5.State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, Xi’an 710075, China; 6.Department of Geosciences, National Taiwan University, Taipei 617, Taiwan; 7.Department of Earth Sciences, National Cheng Kung University, Tainan 701, Taiwan
推荐引用方式 GB/T 7714	Ma, ZB ,Cheng, H ,Tan, M ,et al. Timing and structure of the Younger Dryas event in northern China[J]. QUATERNARY SCIENCE REVIEWS,2012,41:83-93.
APA	Ma, ZB .,Cheng, H .,Tan, M .,Edwards, RL .,Li, HC .,...&Kelly, MJ .(2012).Timing and structure of the Younger Dryas event in northern China.QUATERNARY SCIENCE REVIEWS,41,83-93.
MLA	Ma, ZB ,et al."Timing and structure of the Younger Dryas event in northern China".QUATERNARY SCIENCE REVIEWS 41(2012):83-93.