ZHAO Jinhui, HE Chao, ZHAO Liya, LU Huayu. ATMOSPHERIC DUST LOADS AND SPATIAL DIFFERENCE IN NORTH CHINA SINCE LATE PLEISTOCENE: RECORDS FROM TYPICAL SECTIONS[J]. Marine Geology & Quaternary Geology, 2016, 36(2): 153-160. DOI: 10.16562/j.cnki.0256-1492.2016.02.017
Citation: ZHAO Jinhui, HE Chao, ZHAO Liya, LU Huayu. ATMOSPHERIC DUST LOADS AND SPATIAL DIFFERENCE IN NORTH CHINA SINCE LATE PLEISTOCENE: RECORDS FROM TYPICAL SECTIONS[J]. Marine Geology & Quaternary Geology, 2016, 36(2): 153-160. DOI: 10.16562/j.cnki.0256-1492.2016.02.017
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ATMOSPHERIC DUST LOADS AND SPATIAL DIFFERENCE IN NORTH CHINA SINCE LATE PLEISTOCENE: RECORDS FROM TYPICAL SECTIONS

  • 1. Hubei University College of resources and Environmental Engineering, Wuhan 430062;

  • 2. Geographic and Oceanographic Sciences Nanjing University, Nanjing 210093

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  • Received Date: September 12, 2015
  • Revised Date: November 14, 2015
    Graphical Abstract
    • Abstract
  • Four loess sections of Talede、Panzishan、Yanchang and Kulungou have been selected as typical sections to recover the ancient dust load quantity and their temporal and spatial distributions in this paper. Magnetic susceptibility curve, particle content curve, load curve and δ18O(‰) content curve are used as paleoclimate proxies for study of ancient dust load quantity. The results show that the amount of dust load is higher in glacial stage than that in interglacial stages(A difference may be as high as 1.34-4.34 times),and changes in dust load is characterized by high-frequency fluctuation in the glacial. With regard to the spatial distribution, dust load decreases from the west to the east. The distribution of dust load could be used as a proxy for environmental and climatic reconstruction.
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    • References (23)
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