期刊
EARTH AND PLANETARY SCIENCE LETTERS
卷 407, 期 -, 页码 35-47出版社
ELSEVIER
DOI: 10.1016/j.epsl.2014.09.026
关键词
provenance; Red Clay; loess; Pliocene; U-Pb geochronology; zircon
资金
- (973) National Basic Research Program of China [2013CB956400]
- Strategic Priority Research Program of the Chinese Academy of Sciences [XDB03020400]
- National Natural Science Foundation of China [41172329, 41372036, 41321061, 41021091, 41290253]
- Research Fund for the Doctoral Program of Higher Education of China [20110211110012]
- Scientific and Technological Innovation Team of Chinese Academy of Sciences
- China Postdoctoral Science Foundation [20100470538]
- Natural Environment Research Council (NERC) [NE/I008837/1]
- Natural Science Basis Research Plan in Shaanxi Province of China [2012JM5002]
- NERC [NE/I008837/1] Funding Source: UKRI
- STFC [ST/J001600/1] Funding Source: UKRI
- Natural Environment Research Council [NE/I008837/1] Funding Source: researchfish
- Science and Technology Facilities Council [ST/J001600/1] Funding Source: researchfish
A clear understanding of the provenance of late Cenozoic Chinese loess and the underlying Red Clay deposits will shed light on the history and mechanisms of Asian aridification. Although much progress has been made in understanding the source of Quaternary loess on the Chinese Loess Plateau (CLP), the provenance of the underlying upper Miocene-Pliocene Red Clay sequence is largely unknown. Here we present the first provenance history of the Red Clay sequence based on zircon U-Pb ages from the central CLP. Visual and statistical analyses of the U-Pb age populations and comparison with results from potential source regions reveals that (I) the lowermost Red Clay of the late Miocene (depositional age of similar to 8 Ma) is likely sourced from the nearby Liupan Mountains and the Qaidam Basin; (2) the middle Red Clay (5.5-4 Ma) of the early-mid Pliocene is sourced mainly from the Taklamakan desert, transported via lower-level westerly winds; (3) the upper Red Clay of the late Pliocene (similar to 3 Ma) is sourced from mixed areas, although western source materials from middle-northern Tibetan plateau (including Qaidam Desert sediments and materials eroded from the Qilian Mountains) sediments appear to dominate; and (4) the Quaternary loess is also sourced from mixed source regions, albeit with dominant northern CLP proximal desert sediments transported via winter monsoon winds, which in turn may be transported from mountain source regions of the northeastern Tibet and Gobi Altai via major river systems. This long term shift in sources suggests a progressive eastward aridification during the Pliocene in Asia with the specific timing of provenance shifts synchronous with large-scale climatic transitions and Tibetan uplift, demonstrating that Asian desertification is controlled by both factors. (C) 2014 Elsevier B.V. All rights reserved.
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