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Late Miocene- early Pleistocene paleoclimate history of the Chinese Loess Plateau revealed by remanence unmixing

文献类型：期刊论文

作者Nie, Junsheng1,2; Zhang, Rui1; Necula, Cristian3; Heslop, David4; Liu, Qingsong2; Gong, Lisha1; Banerjee, Subir5
刊名GEOPHYSICAL RESEARCH LETTERS
出版日期2014-03-28
卷号41期号:6页码:2163-2168
关键词loess red clay Pliocene environmental magnetism
ISSN号0094-8276
DOI10.1002/2014GL059379
文献子类Article
英文摘要Previous studies show that the Quaternary loess sequence and the late Miocene-Pliocene red clay sequence on the Chinese Loess Plateau (CLP) share similar magnetic properties despite their being deposited under different climate conditions. To solve this paradox, we apply a novel remanence unmixing technique and demonstrate that loess and red clay on the central CLP contain a similar low-coercivity pedogenic component, but their high-coercivity components differ dramatically, reflecting different oxidation and temperature conditions. We infer that temperatures on the Chinese Loess Plateau cooled from the late Miocene to the Quaternary, in a manner similar to sea surface temperature records for the same time interval. This coherency between marine and terrestrial records argues for a CO2 forcing on long-term paleoclimatic variations.
WOS关键词REVERSAL CURVE DIAGRAMS ; RED-CLAY SEQUENCE ; ENVIRONMENTAL MAGNETISM ; LOESS/PALEOSOL SEQUENCES ; CLIMATE ; PEDOGENESIS ; MA ; SUSCEPTIBILITY ; EVOLUTION ; MONSOON
WOS研究方向Geology
语种英语
WOS记录号WOS:000334264900047
出版者AMER GEOPHYSICAL UNION
资助机构(973) National Basic Research Program of China(2013CB956400) ; (973) National Basic Research Program of China(2013CB956400) ; (973) National Basic Research Program of China(2013CB956400) ; (973) National Basic Research Program of China(2013CB956400) ; Chinese Academy of Sciences(XDB03020400) ; Chinese Academy of Sciences(XDB03020400) ; Chinese Academy of Sciences(XDB03020400) ; Chinese Academy of Sciences(XDB03020400) ; National Natural Science Foundation(41172329 ; National Natural Science Foundation(41172329 ; National Natural Science Foundation(41172329 ; National Natural Science Foundation(41172329 ; Research Fund for the Doctoral Program of Higher Education of China(20110211110012) ; Research Fund for the Doctoral Program of Higher Education of China(20110211110012) ; Research Fund for the Doctoral Program of Higher Education of China(20110211110012) ; Research Fund for the Doctoral Program of Higher Education of China(20110211110012) ; Fundamental Research Funds for the Central Universities ; Fundamental Research Funds for the Central Universities ; Fundamental Research Funds for the Central Universities ; Fundamental Research Funds for the Central Universities ; CNCS(ID31/2010) ; CNCS(ID31/2010) ; CNCS(ID31/2010) ; CNCS(ID31/2010) ; 41321061 ; 41321061 ; 41321061 ; 41321061 ; 41021091) ; 41021091) ; 41021091) ; 41021091) ; (973) National Basic Research Program of China(2013CB956400) ; (973) National Basic Research Program of China(2013CB956400) ; (973) National Basic Research Program of China(2013CB956400) ; (973) National Basic Research Program of China(2013CB956400) ; Chinese Academy of Sciences(XDB03020400) ; Chinese Academy of Sciences(XDB03020400) ; Chinese Academy of Sciences(XDB03020400) ; Chinese Academy of Sciences(XDB03020400) ; National Natural Science Foundation(41172329 ; National Natural Science Foundation(41172329 ; National Natural Science Foundation(41172329 ; National Natural Science Foundation(41172329 ; Research Fund for the Doctoral Program of Higher Education of China(20110211110012) ; Research Fund for the Doctoral Program of Higher Education of China(20110211110012) ; Research Fund for the Doctoral Program of Higher Education of China(20110211110012) ; Research Fund for the Doctoral Program of Higher Education of China(20110211110012) ; Fundamental Research Funds for the Central Universities ; Fundamental Research Funds for the Central Universities ; Fundamental Research Funds for the Central Universities ; Fundamental Research Funds for the Central Universities ; CNCS(ID31/2010) ; CNCS(ID31/2010) ; CNCS(ID31/2010) ; CNCS(ID31/2010) ; 41321061 ; 41321061 ; 41321061 ; 41321061 ; 41021091) ; 41021091) ; 41021091) ; 41021091) ; (973) National Basic Research Program of China(2013CB956400) ; (973) National Basic Research Program of China(2013CB956400) ; (973) National Basic Research Program of China(2013CB956400) ; (973) National Basic Research Program of China(2013CB956400) ; Chinese Academy of Sciences(XDB03020400) ; Chinese Academy of Sciences(XDB03020400) ; Chinese Academy of Sciences(XDB03020400) ; Chinese Academy of Sciences(XDB03020400) ; National Natural Science Foundation(41172329 ; National Natural Science Foundation(41172329 ; National Natural Science Foundation(41172329 ; National Natural Science Foundation(41172329 ; Research Fund for the Doctoral Program of Higher Education of China(20110211110012) ; Research Fund for the Doctoral Program of Higher Education of China(20110211110012) ; Research Fund for the Doctoral Program of Higher Education of China(20110211110012) ; Research Fund for the Doctoral Program of Higher Education of China(20110211110012) ; Fundamental Research Funds for the Central Universities ; Fundamental Research Funds for the Central Universities ; Fundamental Research Funds for the Central Universities ; Fundamental Research Funds for the Central Universities ; CNCS(ID31/2010) ; CNCS(ID31/2010) ; CNCS(ID31/2010) ; CNCS(ID31/2010) ; 41321061 ; 41321061 ; 41321061 ; 41321061 ; 41021091) ; 41021091) ; 41021091) ; 41021091) ; (973) National Basic Research Program of China(2013CB956400) ; (973) National Basic Research Program of China(2013CB956400) ; (973) National Basic Research Program of China(2013CB956400) ; (973) National Basic Research Program of China(2013CB956400) ; Chinese Academy of Sciences(XDB03020400) ; Chinese Academy of Sciences(XDB03020400) ; Chinese Academy of Sciences(XDB03020400) ; Chinese Academy of Sciences(XDB03020400) ; National Natural Science Foundation(41172329 ; National Natural Science Foundation(41172329 ; National Natural Science Foundation(41172329 ; National Natural Science Foundation(41172329 ; Research Fund for the Doctoral Program of Higher Education of China(20110211110012) ; Research Fund for the Doctoral Program of Higher Education of China(20110211110012) ; Research Fund for the Doctoral Program of Higher Education of China(20110211110012) ; Research Fund for the Doctoral Program of Higher Education of China(20110211110012) ; Fundamental Research Funds for the Central Universities ; Fundamental Research Funds for the Central Universities ; Fundamental Research Funds for the Central Universities ; Fundamental Research Funds for the Central Universities ; CNCS(ID31/2010) ; CNCS(ID31/2010) ; CNCS(ID31/2010) ; CNCS(ID31/2010) ; 41321061 ; 41321061 ; 41321061 ; 41321061 ; 41021091) ; 41021091) ; 41021091) ; 41021091)
源URL[http://ir.iggcas.ac.cn/handle/132A11/85885]  
专题中国科学院地质与地球物理研究所
通讯作者Nie, Junsheng
作者单位1.Lanzhou Univ, Collaborat Innovat Ctr Arid Environm & Climate Ch, MOE Key Lab Western Chinas Environm Syst, Lanzhou 730000, Peoples R China
2.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing, Peoples R China
3.Univ Bucharest, Paleomagnetism Lab, Fac Phys, Bucharest, Romania
4.Australian Natl Univ, Res Sch Earth Sci, Canberra, ACT, Australia
5.Univ Minnesota, Dept Geol & Geophys, Inst Rock Magnetism, Minneapolis, MN USA
推荐引用方式
GB/T 7714		 Nie, Junsheng,Zhang, Rui,Necula, Cristian,et al. Late Miocene- early Pleistocene paleoclimate history of the Chinese Loess Plateau revealed by remanence unmixing[J]. GEOPHYSICAL RESEARCH LETTERS,2014,41(6):2163-2168.
APA Nie, Junsheng.,Zhang, Rui.,Necula, Cristian.,Heslop, David.,Liu, Qingsong.,...&Banerjee, Subir.(2014).Late Miocene- early Pleistocene paleoclimate history of the Chinese Loess Plateau revealed by remanence unmixing.GEOPHYSICAL RESEARCH LETTERS,41(6),2163-2168.
MLA Nie, Junsheng,et al."Late Miocene- early Pleistocene paleoclimate history of the Chinese Loess Plateau revealed by remanence unmixing".GEOPHYSICAL RESEARCH LETTERS 41.6(2014):2163-2168.

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来源：地质与地球物理研究所

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