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The manifestation of the Younger Dryas event in the East Asian summer monsoon margin: New evidence from carbonate geochemistry of the Dali Lake sediments in northern China

文献类型：期刊论文

作者Fan, Jiawei4,5; Xiao, Jule3,4,5; Wen, Ruilin4,5; Zhang, Shengrui4,5; Wang, Xu4,5; Cui, Linlin4,5; Liu, Yanhong2; Li, He2; Yue, Jiaojiao1
刊名HOLOCENE
出版日期2018-07-01
卷号28期号:7页码:1082-1092
关键词East Asian summer monsoon endogenic calcite Northern China paleoprecipitation paleotemperature Younger Dryas
ISSN号0959-6836
DOI10.1177/0959683618761542
英文摘要The processes and mechanisms of the Younger Dryas (YD) event in the modern northern margin of the East Asian summer monsoon (EASM) are still heatedly debated. This study presents new high-resolution (similar to 25 years) records of elements and stable isotopes of <38-mu m calcites from a sediment core from Dali Lake in order to investigate the climatic change in the EASM margin at the last glacial-interglacial transition. The <38-mu m calcites in the Dali Lake sediments are cubical or rhombohedral, implying that they are predominated by endogenic calcites precipitated within the water body of the lake. High values of Ca and Mg concentrations of the endogenic calcites are interpreted as strong evaporation and low dissolved CO2 concentration of the lake water related to high regional temperature. Concurrent increases in C-13 and O-18 values of the endogenic calcites are interpreted as the result of intensified evaporation associated with high temperature or low precipitation in the region. These data indicate that the climate in the Dali Lake region was relatively warm and wet from 15,500 to 12,800 and from 11,550 to 10,000 cal. yr BP, and cold and dry from 12,800 to 11,550 cal. yr BP, which was generally supported by the evidence from the data of sedimentary organic matter from the same sediment core. In addition, the abruptness of the temperature change in the Dali Lake region from 12,800 to 11,550 cal. yr BP could be corresponded, within age uncertainties, to the YD cold reversal occurring over northern high latitudes. The atmospheric coupling between the North Atlantic region and the EASM margin was proposed as the dominant pattern influencing the climatic change in the Dali Lake region during the YD event.
WOS关键词ABRUPT CLIMATE-CHANGE ; TIBETAN PLATEAU ; OXYGEN-ISOTOPE ; INNER-MONGOLIA ; DAIHAI LAKE ; LAST DEGLACIATION ; HOLOCENE ; ATLANTIC ; QINGHAI ; ICE
资助项目National Key Research and Development Program of China[2017YFA0603400] ; National Natural Science Foundation of China[41702179] ; National Natural Science Foundation of China[41130101] ; National Natural Science Foundation of China[41672166] ; China Postdoctoral Science Foundation[2017M610111]
WOS研究方向Physical Geography ; Geology
语种英语
WOS记录号WOS:000438621800004
出版者SAGE PUBLICATIONS LTD
资助机构National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; China Postdoctoral Science Foundation ; China Postdoctoral Science Foundation ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; China Postdoctoral Science Foundation ; China Postdoctoral Science Foundation ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; China Postdoctoral Science Foundation ; China Postdoctoral Science Foundation ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; China Postdoctoral Science Foundation ; China Postdoctoral Science Foundation
源URL[http://ir.iggcas.ac.cn/handle/132A11/94012]  
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
地质与地球物理研究所_岩石圈演化国家重点实验室
通讯作者Fan, Jiawei; Xiao, Jule
作者单位1.China Univ Geosci, Sch Earth Sci, Beijing, Peoples R China
2.Chinese Acad Sci, State Key Lab Lithospher Evolut, Inst Geol & Geophys, Beijing, Peoples R China
3.Univ Chinese Acad Sci, Coll Earth Sci, Beijing, Peoples R China
4.Chinese Acad Sci, Inst Earth Sci, Beijing, Peoples R China
5.Chinese Acad Sci, Key Lab Cenozo Geol & Environm, Inst Geol & Geophys, Beijing 100029, Peoples R China
推荐引用方式
GB/T 7714		 Fan, Jiawei,Xiao, Jule,Wen, Ruilin,et al. The manifestation of the Younger Dryas event in the East Asian summer monsoon margin: New evidence from carbonate geochemistry of the Dali Lake sediments in northern China[J]. HOLOCENE,2018,28(7):1082-1092.
APA Fan, Jiawei.,Xiao, Jule.,Wen, Ruilin.,Zhang, Shengrui.,Wang, Xu.,...&Yue, Jiaojiao.(2018).The manifestation of the Younger Dryas event in the East Asian summer monsoon margin: New evidence from carbonate geochemistry of the Dali Lake sediments in northern China.HOLOCENE,28(7),1082-1092.
MLA Fan, Jiawei,et al."The manifestation of the Younger Dryas event in the East Asian summer monsoon margin: New evidence from carbonate geochemistry of the Dali Lake sediments in northern China".HOLOCENE 28.7(2018):1082-1092.

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来源：地质与地球物理研究所

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