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《Journal of Chongqing Normal University(Natural Science)》 2012-04
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Climate Change Indicated by Quaternary Red Earth Trace Elements at Changle in Fujian Province

ZHAO Qian1,2,LI Zhi-zhong1,2,JIN Jian-hui1,2,ZHU Shu-ya1,2,HU Fan-gen,ZHANG Hui(1.School of Geography Science;2.Institute of Geography Research,Fujian Normal University,Fuzhou 350007,China)  
Based on the field investigation and combined with the OSL and ESR dating,this paper focuses on the research of red earth profile of Changle(CL) in Fujian province.The results show that: the content of trace element at CL profile has a regular fluctuation change in their concentration and distribution.It is suggested that there are different geochemical behaviors between these element during weathering and pedogenesis.Higher content of Mn,Nb,Rb,Cr,Pb or lower Ni,As,Sr,Zn,V in CL profile means a warm and wet climate,and luxuriant vegetation.Lower content of Mn,Nb,Rb,Cr,Pb or Higher content of Ni,As,Sr,Zn,V in CL profile means a cold and dry climate.Since the early Pleistocene the climate of Changle has experienced 4~5 times climates changes in dry-wet and cold-warm fluctuations.It shows that since the late early-Pleistocene,the climate changes recorded by the content and their ratio of trace element at CL profile is the specific response to the global climatic changes,and meanwhile it displays special zonality at the subtropical monsoon region.
【Fund】: 福建省自然科学基金(No.2009JO1208);; 福建省公益类科研院所专项基金(No.2009R10039-4);; 福建省大学生创新性实验计划项目(No.FJNU2011-034)
【CateGory Index】: P532
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