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Perissopyge (Trilobita) from the lower Cambrian (Series 2, Stage 4) of North America and Greenland

机译:来自北美和格陵兰下寒武统(系列2,第4阶段)的Perissopyge(Trilobita)

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摘要

The distinctive trilobite Perissopyge phenax was originally described from the Henson Gletscher Formation (Cambrian Series 2, Stage 4) of central North Greenland and reported from the Sekwi Formation of Yukon Territory, Canada. This latter material is illustrated herein for the first time. Perissopyge phenax is also currently described from the Paralleldal Formation of Peary Land, North Greenland, some 100 km east of the type locality, where overlying strata correlate with the middle-upper Toyonian Stage of Siberia (Cambrian Stage 4). Perissopyge triangulata, from the Harkless Formation (Cambrian Stage 4) of Nevada, is also discussed and tectonic deformation of the type suite is recognized. An indeterminate species of Perissopyge is identified in the Ella Island Formation of North-East Greenland. The Ella Island Formation yields Olenellus hanseni, which is possibly synonymous with O. cf. truemani from the Henson Gletscher Formation. Together, these occurrences enhance stratigraphical correlation between central North Greenland and North-East Greenland and suggest some utility for Perissopyge in correlation of the lower half of the Laurentian Cambrian.
机译:独特的三叶虫Perissopyge phenax最初是从北格陵兰中部的Henson Gletscher组(寒武纪系列2,第4期)描述的,并从加拿大育空地区的Sekwi组进行了报道。这后一种材料在这里是第一次说明。目前,Perissopyge phenax也可以从北格陵兰的Peary Land的平行地层中描述出来,该地区位于该类型类型以东约100 km,那里的地层与西伯利亚的Toyonian上中段(Cambrian阶段4)相关。还讨论了来自内华达州无the构造(寒武纪第4期)的Perissopyge triangulata,并认识到类型套件的构造变形。在东北格陵兰岛的埃拉岛组中发现了一种不确定的Perissopyge物种。埃拉岛组产生了Olenellus hanseni,它可能与O. cf.同义。 Henman Gletscher组的truemani。这些事件加在一起,增强了北格陵兰中部和东北格陵兰之间的地层学相关性,并暗示了在劳伦底寒武纪下半部的相关性中,佩罗斯佩盖岩具有一定的实用性。

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