Stalagmite-inferred centennial variability of the Asian summer monsoon in southwest China between 58 and 791 ka BP

doi:10.1016/j.quascirev.2017.02.003

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~）

	Stalagmite-inferred centennial variability of the Asian summer monsoon in southwest China between 58 and 791 ka BP
	Shen, Chuan-Chou 3; Spoetl, Christoph 4; Cheng, Hai 6; Zhao, Xin 7; Huang, Chun-Xia 7; Li, Jun-Yun 7; Han, Li-Yin 7; Li, Hong-Chun 3; Edwards, R. Lawrence 5; Zhang, Tao-Tao 1,2,7
刊名	QUATERNARY SCIENCE REVIEWS
	2017-03-15
卷号	160 期号:2017 页码:1-12
关键词	Stalagmite Delta O-18 Asian Summer Monsoon Greenland Interstadials Heinrich Event 6 Southern Hemisphere
DOI	10.1016/j.quascirev.2017.02.003
文献子类	Article
英文摘要	We use a new spliced stalagmite oxygen isotope record from Yangkou Cave and Xinya Cave, Chongqing, southwest China, to reconstruct the centennial-millennial-scale changes in Asian Summer Monsoon (ASM) intensity between 58.0 and 79.3 thousand years before present (ka BP, before AD 1950). This multidecadally resolved record shows four strong ASM periods, corresponding to Greenland Interstadials (GIS) 17-20, and three weak ASM episodes, among which, the one starting at 61.5 +/- 0.2 ka BP and ending at 59.4 +/- 0.2 ka BP that may correlate with Heinrich Event 6. The close agreement of climate events between China and Greenland supports the notion that the ASM is dominantly governed by high-latitude forcings in the Northern Hemisphere. The short-lived interstadial GIS 18, however, lasted for over 3 kyr in the records derived from ASM region, reflecting a gradual decline of ASM intensity, which coincides with a millennial-scale warming trend in Antarctica. This suggests an additional forcing of the ASM by the Southern Hemisphere, which also affected GIS 8-12, H4 and H5, as shown by previous speleothem studies from the ASM region. (C) 2017 Elsevier Ltd. All rights reserved.
WOS关键词	LAST GLACIAL PERIOD ; NORTH-ATLANTIC CLIMATE ; GREENLAND ICE-CORE ; INTERTROPICAL CONVERGENCE ZONE ; MILLENNIAL-SCALE VARIABILITY ; INDIAN-OCEAN CLIMATE ; HIGH-RESOLUTION ; OXYGEN-ISOTOPE ; WINTER MONSOON ; HEINRICH EVENT
WOS研究方向	Physical Geography ; Geology
语种	英语
WOS记录号	WOS:000397374200001
内容类型	期刊论文
源URL	[http://ir.ieecas.cn/handle/361006/5494]
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~）
作者单位	1.Chinese Acad Sci, Inst Earth Environm, State Key Lab Loess & Quaternary Geol, Xian 710075, Peoples R China 2.Minist Land & Resources China, Field Sci Observat & Res Base Karst Ecoenvironm N, Chongqing 408435, Peoples R China 3.Natl Taiwan Univ, Dept Geosci, Taipei 10617, Taiwan 4.Univ Innsbruck, Inst Geol, A-6020 Innsbruck, Austria 5.Univ Minnesota, Dept Earth Sci, Minneapolis, MN 55455 USA 6.Xi An Jiao Tong Univ, Inst Global Environm Change, Xian 710049, Peoples R China 7.Southwest Univ, Chongqing Key Lab Karst Environm, Sch Geog Sci, Chongqing 400715, Peoples R China
推荐引用方式 GB/T 7714	Shen, Chuan-Chou,Spoetl, Christoph,Cheng, Hai,et al. Stalagmite-inferred centennial variability of the Asian summer monsoon in southwest China between 58 and 791 ka BP[J]. QUATERNARY SCIENCE REVIEWS,2017,160(2017):1-12.
APA	Shen, Chuan-Chou.,Spoetl, Christoph.,Cheng, Hai.,Zhao, Xin.,Huang, Chun-Xia.,...&Li, Ting-Yong.(2017).Stalagmite-inferred centennial variability of the Asian summer monsoon in southwest China between 58 and 791 ka BP.QUATERNARY SCIENCE REVIEWS,160(2017),1-12.
MLA	Shen, Chuan-Chou,et al."Stalagmite-inferred centennial variability of the Asian summer monsoon in southwest China between 58 and 791 ka BP".QUATERNARY SCIENCE REVIEWS 160.2017(2017):1-12.