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《Acta Palaeontologica Sinica》 2008-02
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SPORE-POLLEN ASSEMBLAGE AND ENVIRONMENTAL CHANGES OF THE CHENGDU PLAIN DURING THE LATE HOLOCENE

LUO Li-ping 1),ZHU Li-dong 2),XIANG Fang 2),YANG Wen-guang 3),KAN Ai-ke 4),LUO Hong 2),ZHANG Qin 5) and ZHU Zhang-yi 5) 1) Institute of Multipurpose Utilization of Mineral Resources,the Chinese Academy of Geological Sciences,Chengdu 610041,China,2) Institute of Sedimentary Geology,Chengdu University of Technology,Chengdu 610059,China;3) Laboratory of Marine Geology,Tongji University,Shanghai 200092,China;4) Institute of information engineering,Chengdu University of Technology,Chengdu,Sichuan 610059,China;5) The Institute of Archaeology of Chengdu City,Chengdu,Sichuan 610072,China  
On the Chengdu Plain,a four-meter thick sedimentary succession has accumulated during the past 4 000a of Holocene.In this study,82 samples were collected at 5cm intervals.Based on the characteristics of spore-pollen and 6 datasets from 14 C analysis,the vegetation-climatic changes on the Chengdu Plain during the last 4 000a are discussed.Five phases of paleovegetation successions and climatic fluctuations are revealed for the past 4 000 years,and five climate periods can be recognized and correlated regionally and globally.The results of this study suggest that the climate on Chengdu Plain has been affected by global climate to a certain degree.
【Fund】: 国家十五科技攻关项目(2004BA810B05);; 现代古生物学和地层学国家重点实验室基金(063110)联合资助
【CateGory Index】: Q914
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