IEECAS OpenIR  > 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
Zhang, Tao-Tao1,2,3; Li, Ting-Yong1,2,3; Cheng, Hai4; Edwards, R. Lawrence5; Shen, Chuan-Chou6; Spoetl, Christoph7; Li, Hong-Chun6; Han, Li-Yin1; Li, Jun-Yun1; Huang, Chun-Xia1; Zhao, Xin1
2017-03-15
Source PublicationQUATERNARY SCIENCE REVIEWS
Volume160Issue:2017Pages:1-12
SubtypeArticle
AbstractWe 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.
KeywordStalagmite Delta O-18 Asian Summer Monsoon Greenland Interstadials Heinrich Event 6 Southern Hemisphere
WOS HeadingsScience & Technology ; Physical Sciences
DOI10.1016/j.quascirev.2017.02.003
WOS KeywordLAST 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
Indexed BySCI
Language英语
WOS Research AreaPhysical Geography ; Geology
WOS SubjectGeography, Physical ; Geosciences, Multidisciplinary
WOS IDWOS:000397374200001
Citation statistics
Document Type期刊论文
Identifierhttp://ir.ieecas.cn/handle/361006/5494
Collection黄土与第四纪地质国家重点实验室(2010~)
Affiliation1.Southwest Univ, Chongqing Key Lab Karst Environm, Sch Geog Sci, Chongqing 400715, Peoples R China
2.Chinese Acad Sci, Inst Earth Environm, State Key Lab Loess & Quaternary Geol, Xian 710075, Peoples R China
3.Minist Land & Resources China, Field Sci Observat & Res Base Karst Ecoenvironm N, Chongqing 408435, Peoples R China
4.Xi An Jiao Tong Univ, Inst Global Environm Change, Xian 710049, Peoples R China
5.Univ Minnesota, Dept Earth Sci, Minneapolis, MN 55455 USA
6.Natl Taiwan Univ, Dept Geosci, Taipei 10617, Taiwan
7.Univ Innsbruck, Inst Geol, A-6020 Innsbruck, Austria
Recommended Citation
GB/T 7714
Zhang, Tao-Tao,Li, Ting-Yong,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 Zhang, Tao-Tao.,Li, Ting-Yong.,Cheng, Hai.,Edwards, R. Lawrence.,Shen, Chuan-Chou.,...&Zhao, Xin.(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 Zhang, Tao-Tao,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.
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