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《Acta Micropalaeontologica Sinica》 2007-01
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ADDITIONAL REMARKS ON VEGETATION TYPES IN SOUTH CHINA DURING THE LAST GLACIAL MAXIMUM (LGM)

LIU Jin-ling (Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, Nanjing 210008)  
A comparative study of pollen floras between two cores: Core 17940 from the northern slope of the South China Sea and a core from the Toushe Basin in central Taiwan Province, reveals that there were three different vegetation types around the two areas during 15—40 kaBP. The first type is characterized with the subtropical evergreen broadleaved forest during MIS2(20—15 kaBP). The second is the Pinus/Alnus-dominated woody plant communitites, corresponding to an interstadial summer monsoon dominated warm and humid climate and higher sea/lake level. The third is the Artemisia/Poaceae(Graminae)-dominated herb communities, corresponding to a stadial winter monsoon dominated warm and dry climate and lower sea/lake level. Alternation of the second and the third vegetation patterns implies cycles of the Asian Monsoon. During the LGM, there were several vegetation types on the northern continental shelves in the South China Sea such as mangrove stands distributed in shallow sea in the front, grassland and shrubs at the front bare parts with the evergreen broadleaved forest behind. The peaks of Artemisia could be comparable to Heinrich events(H events)in the North Atlantic.
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