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《Journal of Jilin University(Earth Science Edition)》 2010-05
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Reconstruction of the Paleo-Environment in Changchun Area,Northeast China during the Late Mid-Pleistocene:Evidences from Sedimentary Geochemistry and Palynology

WANG Dan-ping1,2,WANG Xi-kui2,JIANG Yu-biao31.School of Ocean and Earth Sciences,Tongji University,Shanghai 200092,China2.College of Earth Sciences,Jilin University,Changchun 130061,China3.Zhejiang Institute of Geophysical Exploration,Hangzhou 310005,China  
On the basis of TL dating and grain size analysis of the Core HDBZK-1 samples in the Changchun Area,the authors employ K2O,Na2O,MgO,CaO,Al2O3 and their ratios,K2O/Na2O and Al2O3/(Al2O3+CaO+Na2O),which are sensitive to environmental changes,combined with pollen analysis,to analyze the climate environment change of the Changchun area during the late Mid-Pleistocene(probably from 280 to 120 kaB.P.).The results show that the Changchun area has experienced four distinctive cold-dry and warm-wet paleo-climate changes during the late Mid-Pleistocene:cold and dry(281.6-244.0 kaB.P.)-moderate warm and slightly wet(244.0-215.0 kaB.P.)-cold and dry(215.0-131.8 kaB.P.)-the climate turned warm and wet again,with an obvious sign of a sudden increase of freshwater algae(131.8-126.4 kaB.P.),which probably comply with the climate cycles reflected by deep-sea oxygen isotope curves.
【Fund】: 国家自然科学基金项目(40621063);; 吉林省地震局项目(105147-2);; 吉林大学“211”工程三期建设项目
【CateGory Index】: P595;P532
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