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Conodonts across the Devonian/Carboniferous boundary: a review and implication for the redefinition of the boundary and a proposal for an updated conodont zonation

机译:泥盆纪/石炭纪边界的牙形石:重新定义边界的回顾和意义以及更新牙形石分区的建议

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摘要

This paper is a contribution to the redefinition of the base of Carboniferous system. At present the criterion for the definition of the Devonian–Carboniferous boundary is the first occurrence of a conodont species. In order to evaluate the stratigraphic potential for new criteria for the definition of the Devonian–Carboniferous boundary, the distribution of conodont species of Bispathodus, Branmehla, Palmatolepis, Polygnathus, Protognathodus, Pseudopolygnathus and Siphonodella across the boundary is presented and discussed. An updated biozonation scheme across the boundary based on the First Appearance of Bispathodus ac. aculeatus, Bispathodus costatus, Bispathodus ultimus, Protognathodus kockeli, Siphonodella bransoni and Siphonodella duplicata is proposed, and it is suggested that the new criterion for the definition of the base of the Carboniferous system be the First Appearance Datum of Pr. kockeli or Si. bransoni.
机译:本文为重新定义石炭系的基础做出了贡献。目前,泥盆纪-石炭纪界线的定义标准是牙形石物种的首次出现。为了评估确定泥盆纪-石炭纪界线的新标准的地层潜力,提出并讨论了界线Bispathodus,Brammela,Palmatolepis,Polygnathus,Protognathodus,Pseudopolygnathus和Siphonodella的牙形体分布。基于Bispathodus ac的首次出现,跨越边界的更新的生物分区方案。提出了刺果,双歧双歧杆菌,双歧双歧杆菌,Protognathodus kockeli,巴西细叶拟南芥和双侧拟南芥,并提出了定义石炭系基础的新标准是Pr。的首次出现。 kockeli或Si。布兰索尼。

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