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Givetian and early Frasnian conodonts from the Compte section (Middle-Upper Devonian, Spanish Central Pyrenees)

机译:Compte剖面中的吉文天体和早期弗朗西斯牙形体(中上泥盆统,西班牙中比利牛斯山脉)

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摘要

The Givetian and Frasnian conodont succession investigated in the Compte section (Spanish Pyrenees) is subdivided into nine Givetian standard conodont zones and two Frasnian zones (MN zones). This succession allows precise identification of the lower/middle Givetian, middle/upper Givetian and of the Givetian-Frasnian boundaries by means of index conodonts. The joint entry of Mesotaxis falsiovalis and Skeletognathus norrisi in the same bed shows local isochroneity of the beginning of the falsiovalis and norrisi zones in the latest Givetian. In the earliest Frasnian the sequence of Ancyrodella pristina, A. soluta and A. rotundiloba is observed whilst A. binodosa is lacking. The conodont assemblages consist of key species of the following nine genera: Polygnathus, Icriodus, Tortodus, "Ozarkodina", Schmidtognathus, Klapperina, Mesotaxis, Skeletognathus and Ancyrodella. This is the first conodont report from the Pyrenees showing such a detailed succession of enormous correlation potential.
机译:在“ Compte”部分(西班牙比利牛斯山脉)中研究的吉维天和弗雷斯尼牙形石的继承被细分为九个吉维天标准牙形石带和两个弗拉斯尼恩带(MN带)。此序列允许通过索引牙形体准确识别下/中吉维尼,中/上吉维尼和上吉文-弗拉西尼边界。 Mesotaxis falsiovalis和Skeletognathus norrisi在同一张床中的共同进入显示了最近的吉维田中falsiovalis和norrisi区开始的局部等时性。在最早的弗拉斯尼亚语中,观察到无蓬菌,A。soluta和A. rotundiloba的序列,而缺少A. binodosa。牙形石组合由以下九属的关键种组成:gna属,鸢尾属,龟类,“ Ozarkodina”,Schmidtognathus,Klapperina,Mesotaxis,Skeletognathus和Ancyrodella。这是比利牛斯山脉的第一份牙形石报告,显示了如此巨大的关联潜力的详细演替。

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