中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Holocene climatic evolution at the Chinese Loess Plateau: Testing sensitivity to the global warming-cooling events

文献类型:期刊论文

作者Anwar, Taslima1,2; Kravchinsky, Vadim A.1,2; Zhang, Rui1,2,3; Koukhar, Lioudmila P.1; Yang, Lirong2; Yue, Leping2,3
刊名JOURNAL OF ASIAN EARTH SCIENCES
出版日期2018-10-15
卷号166页码:223-232
关键词Climate change Chinese loess-paleosol sequence Holocene Magnetic susceptibility Petromagnetism Soil
ISSN号1367-9120
DOI10.1016/j.jseaes.2018.07.032
通讯作者Kravchinsky, Vadim A.(vadim@ualberta.ca) ; Zhang, Rui(ruizhang@nwu.edu.cn)
英文摘要A high resolution petromagnetic analysis demonstrates that pedogenic alterations in Holocene loess (sand) sequences from the regions of the Guanzhong Basin and the Mu Us Desert on the Chinese Loess Plateau (CLP) were affected by climatic variations in temperature and precipitation. Three warm-humid intervals (similar to 8.4-3.7, similar to 2.4-1.2, and similar to 0.81-0.48 ka), associated with soil formation and relatively high values of petromagnetic parameters, occurred during the Holocene. A substantial paleosol development from similar to 8.4 to 3.7 ka and higher petromagnetic parameter values indicate a generally strong warm-humid phase in the mid-Holocene which can be attributed to the Holocene climatic optimum. Our study demonstrates that the Holocene climate in the eastern part of the CLP is sensitive to warming and cooling events linked to global changes in temperature and precipitation. A complete Holocene climate record is constructed, correlating well with the other regional climate records along the south-to-north profile on eastern CLP, and suggesting that similar climatic changes occurred in eastern monsoonal China during the Holocene. Results are supported by other climate records in different regions of the world, and imply that the Holocene climatic optimum in the northern hemisphere probably took place at the same time.
WOS关键词TEMPERATURE-DEPENDENT SUSCEPTIBILITY ; GLACIAL-INTERGLACIAL CYCLE ; QINGHAI-TIBETAN PLATEAU ; NORTH-ATLANTIC CLIMATE ; HIGH-RESOLUTION ; ENVIRONMENTAL-CHANGES ; LATE PLEISTOCENE ; TIME-SCALE ; MAGNETIC-SUSCEPTIBILITY ; PALEOCLIMATIC RECORD
资助项目National Science Foundation of China[41772027] ; National Science Foundation of China[41372037] ; Natural Sciences and Engineering Research Council of Canada (NSERC)
WOS研究方向Geology
语种英语
WOS记录号WOS:000450379800018
出版者PERGAMON-ELSEVIER SCIENCE LTD
资助机构National Science Foundation of China ; Natural Sciences and Engineering Research Council of Canada (NSERC)
源URL[http://ir.ieecas.cn/handle/361006/14574]  
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Kravchinsky, Vadim A.; Zhang, Rui
作者单位1.Univ Alberta, Dept Phys, Edmonton, AB T6G 2E1, Canada
2.Northwest Univ, Dept Geol, State Key Lab Continental Dynam, Xian 710069, Shaanxi, Peoples R China
3.Chinese Acad Sci, State Key Lab Loess & Quaternary Geol, Inst Earth Environm, Xian 710075, Shaanxi, Peoples R China
推荐引用方式
GB/T 7714
Anwar, Taslima,Kravchinsky, Vadim A.,Zhang, Rui,et al. Holocene climatic evolution at the Chinese Loess Plateau: Testing sensitivity to the global warming-cooling events[J]. JOURNAL OF ASIAN EARTH SCIENCES,2018,166:223-232.
APA Anwar, Taslima,Kravchinsky, Vadim A.,Zhang, Rui,Koukhar, Lioudmila P.,Yang, Lirong,&Yue, Leping.(2018).Holocene climatic evolution at the Chinese Loess Plateau: Testing sensitivity to the global warming-cooling events.JOURNAL OF ASIAN EARTH SCIENCES,166,223-232.
MLA Anwar, Taslima,et al."Holocene climatic evolution at the Chinese Loess Plateau: Testing sensitivity to the global warming-cooling events".JOURNAL OF ASIAN EARTH SCIENCES 166(2018):223-232.

入库方式: OAI收割

来源:地球环境研究所

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