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Pennsylvanian (Desmoinesian-Virgilian) ammonoid zonation for Midcontinent North America

机译:北美中部大陆的宾夕法尼亚州(Desmoinesian-Virgilian)铵盐带

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摘要

The most complete, abundant and diverse Middle-Upper Pennsylvanian ammonoid succession in the world occurs in the North American Midcontinent, where more than 40,000 ammonoids representing 52 genera from at least 42 successive stratigraphic levels have been recovered. The Desmoinesian-Virgilian succession comprises a series of seven substage-scale ammonoid genus zones, in ascending order: Wellerites, Eothalassoceras, Pennoceras, Preshumardites, Pseudaktubites, Shumardites and Subperrinites (new), which are subdivided into 14 ammonoid species- or genus-based subzones. The base of the Eothalassoceras Zone is near the current base of the global Kasimovian Stage, the base of the Pennoceras Zone coincides with the base of the regional Missourian Stage (and likely will be close to the base of a revised Kasimovian Stage when its official base is formally selected), the base of the Pseudaktubites stainbrooki Subzone nearly coincides with the base of the regional Virgilian Stage, and the base of the Shumardites Zone coincides with the base of the global Gzhelian Stage, illustrating the value of this zonation for regional and global correlation.
机译:世界上最完整,最丰富和最多样化的宾夕法尼亚州中上层铵盐类演替发生在北美洲中部大陆,从至少42个连续地层中回收了代表52属的40,000多种铵盐。 Desmoinesian-Virgilian演替包括一系列按升序排列的七个亚阶段规模的氨类属带:Wellerite,Eothalassoceras,Pennoceras,Preshumardites,Pseudaktubites,Shumardite和Subperrinrinite(新),细分为14个以铵盐类或类属分区。 Eothalassoceras区的基础靠近全球Kasimovian阶段的当前基础,Pennoceras区的基础与区域密苏里阶段的基础重合(并且可能接近其官方基础的经修订的Kasimovian阶段的基础。是正式选择的),Pseudaktubites stainbrooki子区的底部与维吉尔地区的基础几乎重合,Shumardites区的基础与全球Gzhelian阶段的基础重合,说明了该分区对于区域和全球范围的价值相关性。

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