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《Arid Land Geography》 1995-04
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ENVIRONMENTAL EVOLUTION OF THE DESERT-LOESS TRANSITIONAL ZONE OVER THE LAST 0.5Ma

Sun Jimin; Ding Zhongli; Liu Tungsheng(Institute of Geology, Chinese Academy of Sciences. Bejijng. China)  
Besed of studying the sand-loess-palacosol series of Shboao profile, which is located in the desert-loess transitional zone of north China, the Mu Us Descrt evolution and the climatic flunctuations over the last 0.5Ma have been discussed, Our result indicated that:1. According to the sedimental records of Shimao profile, the oldest aeolian sand of desert-loess transitional zone formed at 0.5Ma B.P., so this probably means the earliest occuring time of Mu Us desert.2. The evolution of Mu Us Desert is controlled by the Quatcrnary climatic oscillation,and underwent changes from desert to non-desert or non-desert to desert. During the past 0.5Ma, at least 13 times of desert extension occurred, which are inferred by the 13palaeoeolian sand layers of Shimao profile.3. The strahgraphic sequence of the desert-loess transitional zone can be correlated with that of the Loess Plateau, but shows more sensitive to the past climatic changes: the sand layers sandwiched in glacial loess sediments and the loess or sand layers interbedded in interglacial palaeosols, all suggest that the sedimental succcssions in the transitional zone have a high resolution potential for recognozing not only the glacial-interglacial stages but also the within-stage climatic fluctuations.
【Fund】: 国家自然科学基金
【CateGory Index】: P931
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