中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Millennial-scale Asian summer monsoon variations in South China since the last deglaciation

文献类型:期刊论文

作者Wang, Xisheng1; Chu, Guoqiang2; Sheng, Mei1; Zhang, Shuqin3; Li, Jinhua4; Chen, Yun1; Tang, Ling1; Su, Youliang2; Pei, Junling1; Yang, Zhenyu5
刊名EARTH AND PLANETARY SCIENCE LETTERS
出版日期2016-10-01
卷号451页码:22-30
关键词Asian summer monsoon last deglaciation bond cycles solar insolation diagenesis Chinese speleothem
DOI10.1016/j.epsl.2016.07.006
文献子类Article
英文摘要Characterizing spatiotemporal variability of the Asian summer monsoon (ASM) is critical for full understanding of its behavior, dynamics, and future impacts. The present knowledge about ASM variations since the last glaciation in South China largely relies on several precisely-dated speleothem stable oxygen isotope (delta O-18) records. Although these speleothem delta O-18 signals provide useful evidence for regional past environmental changes, their validity for denoting ASM intensity remains a great controversy. The Huguangyan Maar Lake (HML) provides one of the most complete archives of environmental and climatic changes in the tropical-subtropical South and East Asia since the last glaciation. Here we document a continuous centennial- to millennial-scale ASM record over the past 16 ky BP from the high-sedimentation-rate HML sediments. In contrast with the low-amplitude variations of Chinese speleothem-derived delta O-18 signals and the Chinese loess-based monsoon precipitation proxy indexes, our multi-proxy records reveal a pattern of high-amplitude regional climatic fluctuations, including fine-scale oscillations during the Bolling-Allerod warming, the 8.2 ka cooling event, and an abrupt climate shift from 6.5-5.9 ka. The existence of Bond-like cold/dry events indicates a distinct influence of the North Atlantic circulation on low-latitude monsoon changes. The broad comparability between the HML paleo-proxies, Chinese speleothem delta O-18 records, and the northern hemisphere summer insolation throughout the Holocene, suggests that solar insolation exerts a profound influence on ASM changes. These findings reinforce a model of combined insolation and glacial forcing of the ASM. (C) 2016 Elsevier B.V. All rights reserved.
WOS关键词INTERTROPICAL CONVERGENCE ZONE ; NORTH-ATLANTIC CLIMATE ; MAAR LAKE ; HIGH-RESOLUTION ; WINTER MONSOON ; HUGUANG MAAR ; HOLOCENE ; VARIABILITY ; SEDIMENTS ; RECORDS
WOS研究方向Geochemistry & Geophysics
语种英语
WOS记录号WOS:000382595500003
资助机构NSFC(41274074 ; NSFC(41274074 ; China Geological Survey(1212011120045 ; China Geological Survey(1212011120045 ; 41371219) ; 41371219) ; 121201104000150009) ; 121201104000150009) ; NSFC(41274074 ; NSFC(41274074 ; China Geological Survey(1212011120045 ; China Geological Survey(1212011120045 ; 41371219) ; 41371219) ; 121201104000150009) ; 121201104000150009)
源URL[http://ir.iggcas.ac.cn/handle/132A11/53323]  
专题地质与地球物理研究所_中国科学院新生代地质与环境重点实验室
作者单位1.Chinese Acad Geol Sci, Inst Geomech, MLR Key Lab Paleomagnetism & Paleotecton Reconstr, Beijing 100081, Peoples R China
2.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Cenozo Geol & Environm, Beijing 100029, Peoples R China
3.Jilin Univ, Res Ctr Paleontol & Stratig, Changchun 130021, Peoples R China
4.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Earth & Planetary Phys, Paleomagnetism & Geochronol Lab, Beijing 100029, Peoples R China
5.Capital Normal Univ, Coll Resources Environm & Tourism, Beijing 100048, Peoples R China
推荐引用方式
GB/T 7714
Wang, Xisheng,Chu, Guoqiang,Sheng, Mei,et al. Millennial-scale Asian summer monsoon variations in South China since the last deglaciation[J]. EARTH AND PLANETARY SCIENCE LETTERS,2016,451:22-30.
APA Wang, Xisheng.,Chu, Guoqiang.,Sheng, Mei.,Zhang, Shuqin.,Li, Jinhua.,...&Yang, Zhenyu.(2016).Millennial-scale Asian summer monsoon variations in South China since the last deglaciation.EARTH AND PLANETARY SCIENCE LETTERS,451,22-30.
MLA Wang, Xisheng,et al."Millennial-scale Asian summer monsoon variations in South China since the last deglaciation".EARTH AND PLANETARY SCIENCE LETTERS 451(2016):22-30.

入库方式: OAI收割

来源:地质与地球物理研究所

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