依据牙形刺来确定纳庆(纳水)剖面巴什基尔阶与莫斯科阶界线的三个潜在方案
In the Carboniferous,the endemism of biota,the strong glacial-eustatic control over sedimentation and consequent widespread disconformities hamper theselection of acceptabk GSSPs for the Carboniferous stages,including the Serpuldlovian,Moscovian,Kasimovian and Gzhehan.Those relatively deeper-water,carbonate-slope and basinal sections can be served as potential candidate sections for GSSPs.The Naqing Section,which was formerly named as the Nashui section in Luosu,Luodian,Guizhou Province.South China,iS such a slope facies section.More detailed conodont biostratigraphy mainly for the GSSP of the Moscovian Stage has been carried out in recent two years.
Bashkirian/Moscovian boundary conodont Naqing section South China
祁玉平 王向东 Lance L.Lambert James E.Barrick 王志浩 胡科毅
Nanjing Institute of Geology and Paleontology,the Chinese Academy of Sciences,Nanjing,210008,P.R.Chi Department of Geological Sciences of the University of Texas at San Antonio,San Antonio,TX 78249,USA Department of Geosciences of Texas Tech University,Lubbock,TX 79409,USA
国内会议
贵州
中文
87-89
2011-10-01(万方平台首次上网日期,不代表论文的发表时间)