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《Geology-geochemistry》 2001-02
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Xu Hai(Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550002)  
Research on climatic changes in the Holocene plays an important role in palaeoclimatology. Much work has been done by Chinese scientists, which makes great contributions to the reconstruction of the Holocene palaeoclimate in China. Divergences on some typical times such as the Megathermal, the Suitang warm period, the Medieval Warm Epoch and the Little Ice Age, have been presented by many researchers because of the complex influence by levity topography and by quick oscillation of the East Asian monsoon. Among those interpretations, solar irradiance is more effective to interpret the fluctuations of climate on a long-term scale.;
【Fund】: 国家自然科学基金重点项目 (编 :49733130 )
【CateGory Index】: P532
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