The age of North America’s youngest Paleozoic continental vertebrates: a review of data from the Middle Permian Pease River (Texas) and El Reno (Oklahoma) Groups

M. Laurin, R. W. Hook
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引用次数: 1

Abstract

The youngest Paleozoic vertebrate-bearing continental deposits of North America are Middle Permian (Guadalupian) in age and occur in the Chickasha Formation (El Reno Group) of central Oklahoma and the lithostratigraphically lower San Angelo Formation (Pease River Group) of North-Central Texas. Although regarded originally as Guadalupian, these deposits have been assigned recently to the Early Permian on the basis of marine fossils and questionable lithostratigraphic extrapolations from marine to continental strata. A review of ammonoid genera recovered from the Blaine Formation, which overlies both the Chickasha and San Angelo in Oklahoma and Texas, shows that they range globally in age from the Early to Late Permian but most occur in the Guadalupian or Middle Permian. A modest but intensively studied paleobotanical record of compression fossils from the San Angelo, as well as palynomorphs in rocks associated with the Chickasha, presents an unquestionably Middle to Late Permian flora dominated by voltzian conifers. The Chickasha and San Angelo vertebrate assemblages are overwhelmingly dominated by large caseid synapsids and indicate a biostratigraphic signal of early Guadalupian. The occurrence of the tupilakosaurid temnospondyl Slaugenhopia, the parareptile Macroleter, and the eureptile Rothianiscus suggest a Roadian age (lowermost Guadalupian) given the global records of closely related forms. These plant and vertebrate assemblages contrast sharply with those of underlying Cisuralian rocks of the Hennessey Formation of Oklahoma and the Clear Fork Formation of Texas, both of which are much more fossiliferous than those of the Guadalupian in the region. A barren interval of up to 300 m in thickness separates these fossil-bearing intervals. This true void, first reported a half century ago by E.C. Olson, has not been recognized in recent biochronology studies. These findings, as well as those of other vertebrate paleontologists who have evaluated the San Angelo and Chickasha data by other means, strongly refute the notion of “Olson’s Gap” as currently entertained.
北美最年轻的古生代大陆脊椎动物的年龄:对中二叠纪Pease河(德克萨斯州)和El Reno(俄克拉荷马州)群数据的回顾
北美最年轻的古生代脊椎动物大陆矿床年龄为中二叠世(Guadalupian),分布在俄克拉荷马州中部的切克沙组(El Reno群)和德克萨斯州中北部的圣安吉洛组(Pease River群)的岩石地层下部。虽然这些矿床最初被认为是瓜达鲁普系,但最近根据海相化石和从海相到陆相地层的可疑岩石地层推断,这些矿床被划分为早二叠世。对覆盖俄克拉何马州和德克萨斯州切克沙和圣安吉洛的Blaine组中发现的氨属进行了回顾,发现它们的年龄从早到晚二叠纪不等,但大多数出现在瓜达卢普统或中二叠纪。对来自圣安吉洛的压缩化石的古植物学记录,以及与切克沙有关的岩石中的岩石形态进行了适度但深入的研究,毫无疑问地显示了一个以voltzian针叶树为主的二叠纪中晚期植物群。切克沙和圣安吉洛脊椎动物组合绝大多数以大型caseid synapsid为主,显示了瓜达鲁普世早期的生物地层信号。考虑到全球记录的密切相关的形式,tupilakosaurid temnospondyl Slaugenhopia, parparptile Macroleter和爬行动物Rothianiscus的出现表明了一个道路时代(最低的瓜达卢普时代)。这些植物和脊椎动物的组合与俄克拉何马州Hennessey组和德克萨斯州Clear Fork组的下伏顺苏拉系岩石形成鲜明对比,后者比该地区瓜达鲁普系的化石要多得多。厚达300米的贫瘠层将这些含化石层隔开。半个世纪前,E.C.奥尔森(E.C. Olson)首次报道了这种真正的空白,但在最近的生物年代学研究中却没有得到承认。这些发现,以及其他脊椎动物古生物学家通过其他方式评估圣安吉洛和切克沙数据的发现,强烈驳斥了目前人们所接受的“奥尔森缺口”的概念。
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