Source-to-sink fluctuations of Asian aeolian deposits since the late Oligocene

doi:10.1016/j.earscirev.2019.102963

	Source-to-sink fluctuations of Asian aeolian deposits since the late Oligocene
	Sun, Youbin 3,4,7; Yan, Yan 2; Nie, Junsheng 1; Li, Gaojun 5; Shi, Zhengguo 4,6,7; Qiang, Xiaoke 4,7; Chang, Hong 4,7; An, Zhisheng 4,6,7
刊名	EARTH-SCIENCE REVIEWS
	2020
卷号	200 页码:19
关键词	Asian aeolian deposits Primary and secondary sources Provenance tracers Source-to-sink fluctuations Tectonic and climatic impacts
ISSN号	0012-8252
DOI	10.1016/j.earscirev.2019.102963
通讯作者	Sun, Youbin(sunyb@ieecas.cn) ; Yan, Yan(yanyan@gig.ac.cn)
英文摘要	The source-to-sink fluctuations of Asian aeolian deposits have been investigated over the past two decades using multiple mineralogical and geochemical tracers. These source tracers have substantially improved our understanding of the processes of production, transport and deposition of Asian dust cycling from the Asian inland basins to the North Pacific Ocean. However, due to differences in the sensitivity and interpretation of these various tracers, there is controversy about which regions were the dominant dust sources and whether the dust provenances were stable at tectonic and glacial-interglacial timescales. Here we comprehensively review the source-to-sink system of Asian aeolian deposits on the Chinese Loess Plateau since the late Oligocene. By assessing the utility of recently employed provenance tracers, we conclude that integrating different tracers can effectively distinguish major primary and secondary dust sources. The combination of Sr-Nd isotopes, quartz ESR-CI-delta O-18 data, and zircon age spectra can decipher the source-to-sink fluctuations of Asian aeolian deposits at tectonic and glacial-interglacial timescales. Comparison of these sensitive source tracers with tectonic and climatic evidence indicates that the phased growth of the northern Tibetan Plateau played a key role in Asian dust production and transport during the late Oligocene to Miocene, while the onset and expansion of the Northern Hemisphere ice-sheets had a substantial impact on the source-to-sink fluctuations since the late Pliocene.
资助项目	Ministry of Science and Technology of China[2016YFA0601902] ; Chinese Academy of Sciences[132B61KYSB20170005] ; National Natural Science Foundation of China[41525008]
WOS关键词	APATITE FISSION-TRACK ; NORTHERN TIBETAN PLATEAU ; CHINESE LOESS PLATEAU ; CENOZOIC TECTONIC EVOLUTION ; ALTYN-TAGH FAULT ; RESOLUTION MAGNETO STRATIGRAPHY ; RARE-EARTH-ELEMENTS ; RED CLAY DEPOSITS ; PAST 8 MA ; U-PB
WOS研究方向	Geology
语种	英语
出版者	ELSEVIER
WOS记录号	WOS:000514749100009
资助机构	Ministry of Science and Technology of China ; Chinese Academy of Sciences ; National Natural Science Foundation of China
内容类型	期刊论文
源URL	[http://ir.ieecas.cn/handle/361006/12528]
专题	地球环境研究所_古环境研究室第四纪科学与全球变化卓越创新中心
通讯作者	Sun, Youbin; Yan, Yan
作者单位	1.Lanzhou Univ, Coll Earth & Environm Sci, MOE Key Lab Western Chinas Environm Syst, Lanzhou 73000, Peoples R China 2.Chinese Acad Sci, Guangzhou Inst Geochem, Key Lab Ocean & Marginal Sea Geol, Guangzhou 510640, Peoples R China 3.Xi An Jiao Tong Univ, Inst Global Environm Change, Xian 710049, Peoples R China 4.CAS Ctr Excellence Quaternary Sci & Global Change, Xian 710061, Peoples R China 5.Nanjing Univ, Dept Earth & Planetary Sci, MOE Key Lab Surficial Geochem, Nanjing 210023, Peoples R China 6.Pilot Natl Lab Marine Sci & Technol Qingdao, Open Studio Ocean Continental Climate & Environm, Qingdao 266200, Peoples R China 7.Chinese Acad Sci, Inst Earth Environm, State Key Lab Loess & Quaternary Geol, Xian 710061, Peoples R China
推荐引用方式 GB/T 7714	Sun, Youbin,Yan, Yan,Nie, Junsheng,et al. Source-to-sink fluctuations of Asian aeolian deposits since the late Oligocene[J]. EARTH-SCIENCE REVIEWS,2020,200:19.
APA	Sun, Youbin.,Yan, Yan.,Nie, Junsheng.,Li, Gaojun.,Shi, Zhengguo.,...&An, Zhisheng.(2020).Source-to-sink fluctuations of Asian aeolian deposits since the late Oligocene.EARTH-SCIENCE REVIEWS,200,19.
MLA	Sun, Youbin,et al."Source-to-sink fluctuations of Asian aeolian deposits since the late Oligocene".EARTH-SCIENCE REVIEWS 200(2020):19.