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A Rb/Sr record of the weathering response to environmental changes in westerly winds across the Tarim Basin in the late Miocene to the early Pleistocene
Chang, H (Chang, Hong)[ 1 ]; An, ZS (An, Zhisheng)[ 1 ]; Wu, F (Wu, Feng)[ 1 ]; Jin, ZD (Jin, Zhangdong)[ 1 ]; Liu, WG (Liu, Weiguo)[ 1 ]; Song, YG (Song, Yougui)[ 1 ]
2013-09-15
发表期刊PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY
卷号386页码:364-373
文章类型期刊论文
摘要

The long-term record of lacustrine deposits in the Tarim Basin seems to provide a record of climate influenced by westerly winds. To characterize the evolution of westerly winds, we analyzed concentrations of Rb, V, Zn, Sc and Sr for the drill core Ls2 from Lop Nor in the eastern Tarim Basin. The Rb/Sr ratio in lacustrine deposits depends primarily on the Sr element activity during weathering, after the influence of source provenance has been removed. We assume that with such a correction, the Rb/Sr ratio is controlled by precipitation, which depends on moisture transport by westerly winds to the Tarim Basin. The Rb/Sr ratio displays a large-amplitude oscillation that generally follows a pattern similar to that of pollen and ostracod assemblages, which support the inference that rainfall amount affects the Rb/Sr ratio, and in turn suggests that it may serve as an index of precipitation that was transported by westerly wind. All these climatic proxies obviously changed since the late Miocene, suggesting stronger aridification that may be attributed to a latitudinal shift in westerly winds since the late Miocene. A southward migration of westerly winds, which then transported more moisture to the southern and eastern parts of the Tibetan Plateau, agrees with modeling results and the geological record during that time. This event may be causally related to the expansion of the northern hemisphere ice and/or regional tectonic uplift of high mountains around the Tarim Basin.

关键词Rb/sr Ratio Weathering Environmental Change The Tarim Basin Westerly Wind The Late Miocene To The Early pleisTocene Expansion Of The North Hemisphere Ice Volume Tectonic Uplift
DOI10.1016/j.palaeo.2013.06.006
收录类别SCI
语种英语
引用统计
文献类型期刊论文
条目标识符http://ir.ieecas.cn/handle/361006/9897
专题古环境研究室
通讯作者Chang, H (Chang, Hong)[ 1 ]
作者单位State Key Laboratory of Loess and Quaternary Geology (SKLLQG), Institute of Earth Environment, Chinese Academy of Sciences, Xi'an 710075, China
推荐引用方式
GB/T 7714
Chang, H ,An, ZS ,Wu, F ,et al. A Rb/Sr record of the weathering response to environmental changes in westerly winds across the Tarim Basin in the late Miocene to the early Pleistocene[J]. PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY,2013,386:364-373.
APA Chang, H ,An, ZS ,Wu, F ,Jin, ZD ,Liu, WG ,&Song, YG .(2013).A Rb/Sr record of the weathering response to environmental changes in westerly winds across the Tarim Basin in the late Miocene to the early Pleistocene.PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY,386,364-373.
MLA Chang, H ,et al."A Rb/Sr record of the weathering response to environmental changes in westerly winds across the Tarim Basin in the late Miocene to the early Pleistocene".PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY 386(2013):364-373.
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