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Provenance of the upper Miocene–Pliocene Red Clay deposits of the Chinese loess plateau

Nie, Junsheng; Peng, Wenbin; Möller, Andreas; Song, Yougui; Stockli, Daniel F.; Stevens, Thomas; Horton, Brian K.; Liu, Shanpin; Bird, Anna; Oalmann, Jeffrey; Gong, Hujun; Fang, Xiaomin

Authors

Junsheng Nie

Wenbin Peng

Andreas Möller

Yougui Song

Daniel F. Stockli

Thomas Stevens

Brian K. Horton

Shanpin Liu

Jeffrey Oalmann

Hujun Gong

Xiaomin Fang



Abstract

© 2014 Elsevier B.V. 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 (1) the lowermost Red Clay of the late Miocene (depositional age of ~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 (~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.

Journal Article Type Article
Publication Date Dec 1, 2014
Journal Earth and Planetary Science Letters
Print ISSN 0012-821X
Publisher Elsevier
Peer Reviewed Peer Reviewed
Volume 407
Pages 35-47
APA6 Citation Nie, J., Peng, W., Möller, A., Song, Y., Stockli, D. F., Stevens, T., …Fang, X. (2014). Provenance of the upper Miocene–Pliocene Red Clay deposits of the Chinese loess plateau. Earth and planetary science letters, 407, 35-47. https://doi.org/10.1016/j.epsl.2014.09.026
DOI https://doi.org/10.1016/j.epsl.2014.09.026
Keywords Earth and Planetary Sciences (miscellaneous); Space and Planetary Science; Geochemistry and Petrology; Geophysics
Publisher URL https://www.sciencedirect.com/science/article/pii/S0012821X14005810?via%3Dihub
Additional Information This article is maintained by: Elsevier; Article Title: Provenance of the upper Miocene–Pliocene Red Clay deposits of the Chinese loess plateau; Journal Title: Earth and Planetary Science Letters; CrossRef DOI link to publisher maintained version: http://dx.doi.org/10.1016/j.epsl.2014.09.026; Content Type: article; Copyright: Copyright © 2014 Elsevier B.V. All rights reserved.
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