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新疆巴楚地区的“Icriodus de formatus”(牙形刺)与巴楚组和东河塘组的时代
引用本文:王成源.新疆巴楚地区的“Icriodus de formatus”(牙形刺)与巴楚组和东河塘组的时代[J].地质论评,2003,49(6):561-566.
作者姓名:王成源
作者单位:中国科学院南京地质古生物研究所,南京,210008;吉林大学古生物学与地层学研究中心,长春,130026
基金项目:国家重点实验室基金,国家重点基础研究发展计划(973计划),023104,G2000077700,,
摘    要:新疆巴楚小海子剖面发现的牙形刺被有关作者鉴定为Icriodus de formatus Han,并将弗拉斯阶-法门阶界线置于巴楚组中段底部,认为东河塘组的时代为弗拉斯期或更老。但巴楚小海子剖面的牙形刺不是Icriodus de formatus,泥盆系-石炭系的界线应划在巴楚组中段下部之内,东河塘组的时代很可能是法门期的。

关 键 词:新疆  Icriodus  de  formatus  巴楚组  东河塘组  泥盆系-石炭系界线  化石

"Icriodus deformatus" from the Bachu Area of Xinjiang and the Ages of the Bachu and Donghetang Formations
WANG Chengyuan Nanjing Institute of Geology and Palaeontology,Chinese Academy of Sciences,Nanjing Research Centre of Palaeontology and Stratigraphy,Jilin University,Changchun."Icriodus deformatus" from the Bachu Area of Xinjiang and the Ages of the Bachu and Donghetang Formations[J].Geological Review,2003,49(6):561-566.
Authors:WANG Chengyuan Nanjing Institute of Geology and Palaeontology  Chinese Academy of Sciences  Nanjing Research Centre of Palaeontology and Stratigraphy  Jilin University  Changchun
Abstract:The conodonts from the Xiaohaizi section of the Bachu area in Xinjiang were identified by some authors as Icriodm deformatus, who placed the Frasnian-Famennian boundary at the base of the Middle Member of the Bachu Formation, and assigned the Donghetang Formation to the Frasnian in age. However, their identification is incorrect; it is not Icriodus deformatus, but may be a new species of Icriodm, in the late Famennian. The Devonian-Carboniferous boundary should fall within the lower part of the Middle Member of the Bachu Formation, and the Donghetang Formation may be Famennian in age.
Keywords:Icriodus  deformatus  Bachu Formation  Donghetang Formation  Devonian-Carboniferous boundary  Xinjiang
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