苏格兰西北部Durness群的下奥陶统头足类动物群

D. H. Evans
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引用次数: 1

摘要

摘要:本文描述了苏格兰西北部Durness群下奥陶统的头足类动物组合,涉及6目15科46个分类群。共描述了30个属,其中为新属。有34种被描述,但只有13种被命名;其中,新发现的有桃红绒螯虾、健康绒螯虾和lonachonense绒螯虾。另有9个分类群在目或科水平上采用公开命名法,另有3个分类群目前被认为是不确定的,但为了完整起见,在此包括在内。Durness群(Sailmhor组和Sangomore组)较老的头足类动物组合相对较少,但以ellesmerocerids和basleroceratids为主。相比之下,较年轻的组合(特别是Croisaphuill和Ben Suardal石灰石组)相对丰富,以内角石、石蜡石和正角石为主。头足类动物的组合似乎与纽芬兰西部、魁北克、安大略和纽约州的组合密切相关。正角兽总科的成员出现在Durness群的地平线上,比以前在美国西南部记录的要老一些,与阿瓦洛尼亚(英格兰和威尔士)的成员年龄相似。这表明,无论正角兽总科的早期历史如何,在弗洛ian早期似乎发生了快速的多样化和分散。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
The Lower Ordovician Cephalopod Faunas of the Durness Group, North-West Scotland
ABSTRACT The cephalopod assemblages of the Lower Ordovician portion of the Durness Group of North-West Scotland are described and referred to 46 taxa across six orders and 15 families. A total of 30 genera are described, of which Expandocassinoceras and Augeoceras are new. Thirty-four species are described, although only 13 are named; of these, Pionoceras peachi, Allopiloceras bealachense and Allopiloceras lonachonense are new. A further nine taxa are treated in open nomenclature at the order or family level, and another three are regarded as indeterminate at the present time but are included here for completeness. The older cephalopod assemblages of the Durness Group (Sailmhor and Sangomore formations) are relatively sparse, but dominated by ellesmerocerids and bassleroceratids. By contrast, the younger-assemblages (in particular those of the Croisaphuill and Ben Suardal Limestone formations) are relatively abundant and dominated by endocerids, tarphycerids and orthoceratoids. The cephalopod assemblage appears to be strongly affiliated to those of western Newfoundland, Quebec, Ontario and New York State. Members of the Orthoceratoidea occur in the Durness Group at horizons somewhat older than those previously recorded from the south-western United States and are similar in age to occurrences in Avalonia (England and Wales). This suggests that whatever the earlier history of the Orthoceratoidea, a rapid diversification and dispersal appears to have taken place during the early Floian.
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