山东济宁煤田东区太原组■类动物群  

STUDY ON THE FUSULINIDA FAUNA IN THE TAIYUAN FORMATION FROM THE EAST AREA OF JINING COALFIELD, SHANDONG PROVINCE

作　　者：蒋汉朝[1] 王明镇[2] 张锡麒[2] 李增学[2] 

机构地区：[1]中国科学院地质与地球物理研究所,北京100029 [2]山东科技大学地球科学系,山东泰安271019

出　　处：《古生物学报》2001年第4期514-522,共9页Acta Palaeontologica Sinica

基　　金：国家自然科学基金资助项目 (No .49872 0 5 7)

摘　　要：通过对山东济宁煤田东区太原组类动物群的系统研究 ,共鉴定出类化石 15属 10 8种。根据类化石在地层中的分布和垂向的变化规律 ,自上而下建立一个带三个亚带 :Pseudoschwagerina带 ,3)Boultoniawillsi Schwagerinacervicalis亚带 ,2 )Pseudofusulinasphaeroidea Schwagerinaneolata亚带 ,1)Rugosofusulinacom plicata Quasifusulinalongissima亚带。通过与邻区及华北部分地区对比 ,本区太原组类动物群的地质时代为早二叠世早期 ,本区石炭By a systematic study of the fusulinida fauna in the Taiyuan Formation from the east area of Jining coalfield, Shandong Province, 15 genera and 108 species of Fusulinida fossils have been found. According to the geographical distribution and vertical variation of fusulinid fossils in the strata, the fusulinids may be distinguished into 1 assemblage and 3 subassemblages as following(in descending order): Ⅰ. Pseudoschwagerina assemblage,3). Boultonia willsi Schwagerina cervicalis subassemblage, 2). Pseudofusulina sphaeroidea Schwagerina neolata subassemblage, 1). Rugosofusulina complicata Quasifusulina longissima subassemblage. Compared with those in nearby regions and some other areas in North China, the geological age of the fusulinid fauna in the Taiyuan Formation of Jining coalfield should be early Early Permian, and the boundary between Carboniferous and Permian in the east area of Jining coalfield should be placed at the bottom of NO.11 limestone in the lower portion of the Taiyuan Formation.

关 键 词：TING类动物群 太原组 二叠系 济宁 山东 煤田 

分 类 号：Q915[天文地球—古生物学与地层学]