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Olenid-dominated trilobite fauna from the Shallow Bay Formation (Cow Head Group), Cambrian-Ordovician boundary interval, western Newfoundland

机译:来自纽芬兰西部寒武纪-奥陶纪边界区间的浅湾组(牛群)的油状三叶虫动物群

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摘要

A single boulder (PH 8.14), recovered from unit 8 on the Point of Head, Cow Head Peninsula, Shallow Bay Formation (Cow Head Group), contains a unique olenid-dominated trilobite fauna composed of the following taxa: Boeckaspis geordii n. sp., Leiobienvillia terranovica (Rasetti, 1954), hystricurid n. gen. n. sp., Tulepyge sp. A, Tulepyge sp. B, Tulepyge? sp. C, and Symphysurina sp. The pelturine trilobite aB. geordii dominates the assemblage. Boulder PH 8.14 consists of light grey-brown packstone to grainstone. This is atypical for olenid-dominated faunas, which usually occur in dark laminated limestones and shales. The fauna is likely earliest Ordovician in age, but a latest Cambrian age cannot be entirely ruled out. Regardless, this assemblage is unique in that it is the only known olenid-dominated fauna from Cambrian-Ordovicianaboundary sediments in Laurentia. A phylogenetic analysis of Boeckaspis and other putatively closely related taxa (Westergaardia Raymond, 1924 and Jujuyaspis Kobayashi, 1936) was conducted. The results of the analysis indicate that Westergaardia is not monophyletic and as such it is considered a junior synonym of Boeckaspis herein.
机译:从牛头半岛牛头半岛浅湾组(牛头群)的第8单元中回收的一块巨石(PH 8.14)包含由以下类群组成的独特的以油类为主的三叶虫动物群:Boeckaspis geordii n。 ,Leiobienvillia terranovica(Rasetti,1954年),hystricurid n。 gen。 。 ,Tulepyge sp。 A,图莱比格sp。 B,图莱比奇? sp。 C和Symphysurina sp。 pelturine三叶虫aB。 geordii占主导地位。博尔德PH 8.14由浅灰褐色的堆积石到颗粒岩组成。这对于以油类为主的动物来说是非典型的,它们通常发生在深色的层状石灰岩和页岩中。该动物可能是最早的奥陶纪,但不能完全排除最近的寒武纪。无论如何,这种组合是独特的,因为它是劳伦西亚(Camerian-Ordoviciana)边界沉积物中唯一已知的以油类为主的动物。进行了Boeckaspis和其他假定密切相关的类群(Westergaardia Raymond,1924年和Jujuyaspis Kobayashi,1936年)的系统发育分析。分析结果表明Westergaardia不是单系的,因此在本文中被认为是Boeckaspis的初级同义词。

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