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《Acta Scicentiarum Naturalum Universitis Pekinesis》 2003-04
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Reconstruction of the Paleoenvironment in Central North China During 5000aBP to 4000aBP: Evidence from Mollusks Fossils

LIANG Liang XIA Zhengkai LIU Decheng (Dept.of Resources and Environmental Geosciences,College of Environmental Sciences, Peking University, Beijing, 100871)  
The discovery of the Holocene lacustrine sediment in the Central North Chin a has provided acceptable records of the paleoenvironment during approximately 5 ?660?aBP to 3?500?aBP. The vertical distribution and fluctuation of aquatic, amphibian and terrestrial mollusks remains in Sihenan Profile represent the physical en vironmental history of this area. The process of birth, expansion, and vanishmen t of the ancient lake was well recorded through the presence and absence of aqua tic species. And from the abundance variation of hygrophilous—warmth-and moist u re-loving species, It can be known that the Central North China was warm er and moister than the present during the period of 5?000?aBP to 4?000?aBP.
【Fund】: 国家自然科学基金 ( 40 1710 96 );; 国家十五攻关预研究 ( 2 0 0 1BA80 5B0 5 )资助项目
【CateGory Index】: P532;Q915
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