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《Quaternary Sciences》 1999-03
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RE-ORGANIZATION OF ATMOSPHERIC CIRCULATION AT ABOUT 2.6MA OVER NORTHERN CHINA

Ding Zhongli; Yang Shiling; Sun Jimin ;Liu Tungsheng (Institute of Geology, Chinese Academy of Sciences, Beijing 100029)  
Recent studies have shown that the red clay sequence underlying the Quaternary loess of the Chinese LOess Plateau is wind-blown in origin. To address the wind system that tyansported the Tertiary red clay, two north-south transects were studied in the Chinese Loess Plateau.One of the transects was designed to study spatial changes in grain size of the last glacial-nterglasial loess records,and the other to observe particle changes of the Tertiary red clay.The loess transect consists of nine sections, and the red clay transect of four sections. Analyses of closely--spacedsamples show that there is a strong southward decrease in grain size of both loess and palaeosol horizons of the late Pleistocene, which is compatible with the conclusion that the aeolian materials of the Quaternary in the Loess Plateau are transported by the northerly winter monsoonal winds. Grain size distributions of the red clay sequences, however, do not show such a change. From north to south along the red clay transect the particle size distribution is almost identical in the four sections, suggesting that the winter monsoonal winds might have played a less important role in transporting the red clay matarial. It is suggested that the red clay may have been transported by the westerlies from the dust-source-regions of northwestern China onto the Loess Plateau. A remarkable rearrangement of Anospheric patterns at about 2.6Ma, therefore, has been recorded by the red clay-loess shifL It is speculated that this rearrangement of atmospheric patterns may have been caused by the onset of glaciation in the NOrthern Hemisphere.
【Fund】: 国家自然科学基金!49525203
【CateGory Index】: P532
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4 Dong Guang-rong Li Bao-sheng Gao Shang-yu Wu Zheng Shao Ya-jun (Lanzhou Institute of Desert Research, Academia Sinica);THE QUATERNARY ANCIENT EOLIAN SANDS IN THE ORDOS PLATEAU[J];Acta Geographica Sinica;1983-04
5 An Zhisheng Wang Junda Li Huamei;PALEOMAGNETIC RESEARCH OF THE LOCHUAN LOESS SECTION[J];Geochimica;1977-04
6 An Zhisheng (Xi'an Laboratory of Loess and Quaternary Geology, Chinese Academy of Sciences) G. Kukla (Lamont-Doherty Geological Observatory of Columbia University) Liu Tungsheng (Institute of Geology, Chinese Academy of Sciences) (Xi'an Laboratory of Loess and Quaternary Geology, Chinese Academy of Sciences);LOESS STRATIGRAPHY IN LUOCHUAN OF CHINA[J];Quaternary Sciences;1989-02
7 Li Jijun Kang Jiancheng (Department of Geography, Lanzhou University);QUATERNARY GLACIATIONS, PHYSIOGRAPHIC STAGES AND LOESS RECORD IN CHINA[J];Quaternary Sciences;1989-03
8 Han Jiamao (Institute of Geology,Chinese Academy of Sciences) J.J.Hus (Geophysical Center of the Royal Meteorological Institute) Liu Tungsheng (Institute of Geology,Chinese Academy of Sciences) R.Paepe (Earth Technology Institute,Vrije Universiteit Brussel) R.E.Vandenberghe (Laboratory of Magnetism,University of Gent);MAGNETIC PROPERTIES OF THE MALAN AND LISHI FORMATIONS[J];Quaternary Sciences;1991-04
9 Ding Zhongli (Institute of Geology,Chinese Academy of Sciences) (Xi(?)an Laboratory of Loess and Quaternary Geology,Chinese Academy of Sciences) Yu Zhiwei (Department of Geology,China University of Mining and Technology) Liu Tungsheng (Instituse of Geology,Chinese Academy of Sciences);PROGRESS IN LOESS RESEARCH (PART 3):TIME SCALE[J];Quaternary Sciences;1991-04
10 Liu Xiuming (Institute of Geology, Chinese Academy of Sciences) (Geomagnetism Laboratory, University of Liverpool, UK) Liu Tungsheng (Institute of Geology, Chinese Academy of Sciences) John Shaw (Geomagnetism Laboratory, University of Liverpool, UK);MAGNETlC MINERAL CHARACTERISTICS OF CHINESE LOESS AND ITS PALAEOCLIMATIC SIGNIFICANCE[J];Quaternary Sciences;1993-03
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