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《Geological Review》 2006-02
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Conodonts from the Taiyuan Formation and Benxi Formation in the Feicheng Coalfield, Shandong

SU Wei 1),ZHANG Jisheng 2),ZHANG Xiqi 1), WANG Mingzhen 1),LI Zengxue 1) 1) College of Geo-info Science and Engineering,Shandong University of Science and Technology,Taian,271019 2) No.1 Exploration Team, China Administration of Coal Geology,Shandong Provence,Tengzhou,277500  
6 genera 14 species of conodonts have been found from the Taiyuan Formation and Benxi Formation in the Feicheng Coalfield,Shandong Province. Based on the geographical distribution and vertical variation of conodont fossils in the strata, the conodonts may be distinguished into 2 assemblages as following(in descending order):Ⅱ. Streptognathodus barskovi and Ⅰ. Streptognathodus parvus—Idiognothodus magnificus assemblage. Compared with those in nearby regions and some other areas in North China,the geological ages of the fauna in the Feicheng Coalfield should be early Early Permian(assemblage Ⅱ)and late Late Carboniferous(assemblage Ⅰ)respectively,and the Carboniferous— Permian boundary in the Feicheng Coalfield shoulf be at the bottom of No. 4 limestone.
【Fund】: 国家自然基金资助项目(编号49872057)的成果。
【CateGory Index】: Q915
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