Zr/Rb ratio in the Chinese loess sequences and its implication for changes in the East Asian winter monsoon strength

被引:139
作者
Chen, J [1 ]
Chen, Y
Liu, LW
Ji, JF
Balsam, W
Sun, YB
Lu, HY
机构
[1] Nanjing Univ, Dept Earth Sci, Inst Surf Geochem, State Key Lab Mineral Deposit Res, Nanjing 210093, Peoples R China
[2] Univ Texas, Dept Earth & Environm Sci, Arlington, TX 76019 USA
[3] CAS, Inst Earth Environm, State Key Lab Loess & Quaternary Geol, Xian 710075, Peoples R China
基金
中国国家自然科学基金;
关键词
D O I
10.1016/j.gca.2005.11.029
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
The long-term dust accumulation sequences on the Chinese Loess Plateau (CLP) provide a valuable opportunity to study the evolution of East Asian winter monsoon strength. Grain size of bulk samples of loess deposits, though widely used, is a modified measure of the strength of winter monsoon wind due to modification by post-depositional weathering and pedogenesis. This study proposes a new and reliable geochemical climate proxy that records the variability of the East Asian winter monsoon on the CLP. Six loess-paleosol sections on the Plateau were selected for measuring concentrations of the trace elements Zr and Rb as well as grain size. Variations of the Zr/Rb ratio in all the sections encompassing the last 130 ka display a generally similar pattern to that of mean grain size of bulk samples (MGSB). Though a positive correlation exists between the Zr/Rb ratio and MGSB, the correlation coefficient decreases in southern and eastern sections where intense pedogenesis occurred in the relatively warm and humid climates. Long-term Zr/Rb variation in the Lingtai section exhibits amplitudes and frequencies similar to those in MGSB and the mean grain size of quartz particles (MGSQ, accepted as a more reliable proxy than MGSB) in the upper loess-paleosol. sequence over the past 2.6 Ma. However, for the underlying Red Clay formation, in the interval from about 7-2.6 Ma B.P., the MGSB record is relatively stable, whereas both the Zr/Rb ratio and MGSQ show distinct variability and display amplitudes similar to those observed in the overlying loess-paleosol sequence. These results demonstrate that the Zr/Rb ratio reflects original eolian grain size and may serve as a reliable index of the strength of East Asian winter monsoon winds. (c) 2005 Elsevier Inc. All rights reserved.
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页码:1471 / 1482
页数:12
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