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《Acta Sedimentologica Sinica》 2012-01
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The Early-Mid Cretaceous Changes of Clay Mineral Composition from Zhejiang and Fujian Provinces,SE China:Indications to paleoclimate changes

LIU Ling1,2 LI Xiang-hui1 WANG Yin1 ZHOU Yong2 CAO Ke3(1.State Key Laboratory of Mineral Deposit Research,School of Earth Sciences and Engineering,Nanjing University,Nanjing 210093; 2.East China Mineral Exploration and Development Bureau,Nanjing 210007; 3.402th Geological Survey,Sichuan Bureau of Geology and Mineral Resources,Chengdu 610213; 4.Qingdao Institute of Marine Geology,Qingdao,Shandong 200092)  
Components of the clay mineral illite,smectite,kaolinite,and chlorite were measured and analyzed at eleven horizons from eleven observed sections to interpret the Early-Mid Cretaceous paleoclimate in western Zhejiang and Fujian provinces,SE China.The results show that in total the relative content of illite is over 80% in average in most of the Lower-Mid Cretaceous;abundant smectite is presented in the Bantou Formation of western Fujian and the upper Shouchang Formation,lower Hengshan Formation,middle Jinhua Formation,and upper Quxian Formation of west Zhejiang,in which the highest value is 49%;kaolinite is few,only high values(up to 38%) ocurring in the middle Quxian Formation in western Zhejiang and upper Shouchang Formation.It is proposed that it was arid-semiarid climate of tropic-subtropic in the Early-Mid Cretaceous in SE China,corresponded to the whole greenhouse(continental) climate in the world;there could be an interruption of hot-humid climate in the early-Aptian and early Cenomanian in western Zhejiang that could be attributed to relatively developed vegetation and larger lacustrine area;and short durations of dry-cold climate could have happened in the Valanginian in western Fujian and in the early Aptian,late Albian,middle Cenomanian in western Zhejiang,which is corresponding to those of the Cretaceous oceanic anoxic events,and is supposed to be caused by regional tectonic uplifts in SE China.
【Fund】: 国家重大基础研究发展规划项目(973)“晚中生代温室气候-气候演变”之课题“晚中生代东西地区古气候重建”(2006CB701401)资助成果
【CateGory Index】: P534.53;P532
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