湖北恩施志留系秀山组顶部的牙形刺及其地层意义
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  • 英文篇名:SILURIAN CONODONTS FROM THE UPPERMOST PART OF THE XIUSHAN FORMATION,ENSHI,HUBEI PROVINCE,CHINA AND THEIR STRATIGRAPHICAL SIGNIFICANCE
  • 作者:闫冠州 ; 吴荣昌 ; 王怿 ; 唐鹏
  • 英文作者:YAN Guanzhou;WU Rongchang;WANG Yi;TANG Peng;Key Laboratory of Economic Stratigraphy and Palaeogeography,Nanjing Institute of Geology and Palaeontology,Chinese Academy of Sciences;Adimission of Graduate Student of University of Science and Technology of China;State Key Laboratory of Palaeobiology and Stratigraphy,Nanjing Institute of Geology and Palaeontology,Chinese Academy of Sciences;
  • 关键词:牙形刺 ; 志留系 ; 兰多维列统 ; 秀山组 ; 恩施 ; 湖北
  • 英文关键词:Conodonts;;Xiushan Formation;;Telychian;;Enshi;;Hubei Province;;China
  • 中文刊名:WSGT
  • 英文刊名:Acta Micropalaeontologica Sinica
  • 机构:中国科学院南京地质古生物研究所中国科学院资源地层学与古地理学重点实验室;中国科学技术大学研究生院;中国科学院南京地质古生物研究所现代古生物学和地层学国家重点实验室;
  • 出版日期:2018-06-15
  • 出版单位:微体古生物学报
  • 年:2018
  • 期:v.35
  • 基金:国家自然科学基金委(41672008、41521061)的资助~~
  • 语种:中文;
  • 页:WSGT201802004
  • 页数:13
  • CN:02
  • ISSN:32-1189/Q
  • 分类号:49-61
摘要
本文描述了湖北恩施太阳河灯草坪剖面志留系秀山组顶部灰岩夹层中的牙形刺。秀山组顶部的灰岩产出较丰富的牙形刺化石,共10属14种,包括Pterospathodus eopennatus,P.a.cf.angulatus,Apsidognathus sp.,Ozakodina paraplanussima,Ozakodina sp.,?Distomodus sp.,?Tuberocostadontus sp.,Coryssagnathus shaannanensis,Wurmiella recave,Wurmiella sp.,Oulodus shiqianensis,Oulodus sp.,Pseudooneotodus beckmanni,Distomodus sp.。根据牙形刺的产出情况,可识别出两个牙形刺带。秀山组顶部灰岩可归入Pterospathodus eopennatus超带的P.eopennatus ssp.n.2带。需要指出的是,秀山组最顶部样品发现了P.a.cf.angulatus,因此,秀山组顶部的时代延伸至Pterospathodus celloni超带的P.a.angulatus带,时代为兰多维列世特列奇早-中期。
        This study reports the conodont fauna from the uppermost part of the Xiushan Formation at the Dengcaoping section in Enshi,Hubei Province,China.Abundant Telychian(Lower Silurian)conodonts have been recovered from this section including Pterospathodus eopennatus,P.a.cf.angulatus,Apsidognathus sp.,Ozakodina paraplanussima,Ozakodina sp.,?Distomodus sp.,?Tuberocostadontus sp.,Coryssagnathus shaannanensis,Wurmiella recave,W.sp.,Oulodus shiqianensis,Oulodus sp.,Pseudooneotodus beckmanni and Distomodus sp.This conodont fauna can be referred to Silurian Telychian Pterospathodus eopennatus ssp.n.2 Zone of P.eopennatus Superzone.It is worthy to note that the presence of Pterospathodus amorphognathus cf.angulatus indicates the uppermost of the Xiushan Formation can be assigned to the Pterospathodus amorphognathus angulatus Zone of Pterospathodus celloni Superzone.
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