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A new Metapolygnathus platform conodont species and its implications for Upper Carnian global correlations

机译:一个新的Metapolygnathus平台牙形石物种及其对上卡尼期全球相关性的启示

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摘要

A rich conodont fauna from two Neotethyan sections, Pizzo Mondello (western Sicily, Italy) and Pignola 2 sections (southern Apennines, Italy) includes conodonts described herein as a new species. Metapolygnathus praecommunisti sp. nov. is transitional between Paragondolella noah and Metapolygnathus communisti. The genus Metapolygnathus (in− cluding M. praecommunisti) is now characterised by posterior prolongation of the keel termination, associated with a cen− trally located pit and with a weak ornamentation confined to the anterior part of the platform margins. The establishment of M. praecommunisti addresses the problems related to the origin and the peculiar, probably facies−controlled, distribu− tion of its descendant species M. communisti. Since M. praecommunisti occurs in the entire Tethys and in North America, we propose the species as a good guide fossil for global correlations, characterised by a short temporal range limited to the uppermost Tuvalian (upper Carnian). The stratigraphic occurrence of the genus Metapolygnathus is restricted to the Tuvalian–Lacian (upper Carnian–lower Norian), excluding its presence in the Julian substage (lower Carnian).
机译:来自两个新特提斯山脉部分的丰富牙形动物区系,包括Pizzo Mondello(意大利西西里岛西部)和Pignola 2区域(意大利南亚平宁山脉),包括本文中描述为新物种的牙形体。南美白poly十一月是帕拉贡多拉诺亚(Paragondolella noah)和Metapolygnathus communisti之间的过渡。 Metapolygnathus属(包括M. praecommunisti)的特征是龙骨末端的后部延长,与中央凹坑相关联,并受限于平台边缘的前部。 pra.communististi的建立解决了与它的后代M.communisti的起源和特殊的,可能是由相控制的分布有关的问题。由于praecommunististi发生在整个特提斯和北美洲,我们建议将该物种作为全球相关性的良好指导化石,其特征是时间范围仅限于最高的图瓦勒阶(上卡尼阶)。 Metapolygnathus属的地层仅限于Tuvalian–Lacian(上部Carnian–下部Norian),但不存在于Julian阶段(下部Carnian)。

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    MAZZA M; M. RIGO; NICORA A;

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  • 年度 2011
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  • 正文语种 eng
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