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DOI10.1016/j.quaint.2013.03.012
Evolution of the arid climate in High Asia since similar to 1 Ma: Evidence from loess deposits on the surface and rims of the Tibetan Plateau
Zan, Jinbo; Fang, Xiaomin; Yang, Shengli; Yan, Maodu
通讯作者Zan, JB (通讯作者)
发表日期2013
ISSN1040-6182
EISSN1873-4553
起始页码210
结束页码217
卷号313
英文摘要The formation and development of the arid climate in High Asia remain controversial. This is largely because of the scarcity of continuous high-resolution geological records from the Asian interior region. Thick loess sequences deposited on the surface of the Tibetan Plateau and its rims provide great potential to reconstruct a high-resolution history of the formation and evolution of High Asia arid climate. Based on detailed investigations of the grain size and carbonate content of representative loess sequences in High Asia, a persistent drying of High Asia occurred in the past 1 Ma, and two major rapid drying events occurred at about 0.9-0.8 Ma and 0.5 Ma. Persistent and rapid stepwise uplifts of the Tibetan Plateau since the Mid-Pleistocene might play a dominant role in the drying of High Asia, although the Mid-Pleistocene global cooling may partially contribute to the event. (C) 2013 Elsevier Ltd and INQUA. All rights reserved.
关键词WESTERN QAIDAM BASINCHINESE LOESSMAGNETIC-SUSCEPTIBILITYASTRONOMICAL CALIBRATIONNORTHERN-HEMISPHERESOUTHERN ASIATARIM BASINUPLIFTMONSOONMOUNTAINS
语种英语
WOS研究方向Physical Geography ; Geology
WOS类目Geography, Physical ; Geosciences, Multidisciplinary
WOS记录号WOS:000327171200021
来源期刊QUATERNARY INTERNATIONAL
来源机构中国科学院青藏高原研究所
文献类型期刊论文
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/258123
推荐引用方式
GB/T 7714
Zan, Jinbo,Fang, Xiaomin,Yang, Shengli,et al. Evolution of the arid climate in High Asia since similar to 1 Ma: Evidence from loess deposits on the surface and rims of the Tibetan Plateau[J]. 中国科学院青藏高原研究所,2013,313.
APA Zan, Jinbo,Fang, Xiaomin,Yang, Shengli,&Yan, Maodu.(2013).Evolution of the arid climate in High Asia since similar to 1 Ma: Evidence from loess deposits on the surface and rims of the Tibetan Plateau.QUATERNARY INTERNATIONAL,313.
MLA Zan, Jinbo,et al."Evolution of the arid climate in High Asia since similar to 1 Ma: Evidence from loess deposits on the surface and rims of the Tibetan Plateau".QUATERNARY INTERNATIONAL 313(2013).
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