1994Journal of PaleontologyRequires access

Ordovician proetide trilobiteDimeropyge, with a new species from northwestern Canada

Brian D. E. Chatterton

Open publisher page 30 citations

Abstract

Dimeropygeöpik, 1937, is a genus currently composed of at least 14 similar Middle (predominantly) to possibly lowest Upper Ordovician species from Laurentia (13 species) and Baltica (one species). Possible Lower Ordovician specimens have been illustrated by Ross (1951).Dimeropyge clintonensisShaw, 1968, is redescribed, based upon additional material of mature topotypes. A new species ofDimeropyge, D. speyeri, is proposed for material from the Esbataottine Formation in the Mackenzie Mountains, northwestern Canada, previously described asD. clintonensis.A phylogenetic analysis of 10 of the 14 species of this genus is presented (the other species are less completely known, and are related to the analyzed species in a more traditional manner). Ontogenies from protaspid to holaspid stages are provided forD. clintonensis, D. speyeri, andD. virginiensisWhittington and Evitt, 1954. The larval stages of these species are very similar, supporting the close relationship between species assigned toDimeropyge.

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What this paper is about

Dimeropygeöpik, 1937, is a genus currently composed of at least 14 similar Middle (predominantly) to possibly lowest Upper Ordovician species from Laurentia (13 species) and Baltica (one species). Possible Lower Ordovician specimens have been illustrated by Ross (1951).Dimeropyge clintonensisShaw, 1968, is redescribed, based upon additional material of mature topotypes. A new species ofDimeropyge, D. speyeri, is proposed for material from the Esbataottine Formation in the Mackenzie Mountains, northwestern Canada, previously described asD. clintonensis.A phylogenetic analysis of 10 of the 14 species of this genus is presented (the other species are less completely known, and are related to the analyzed species in a more traditional manner). Ontogenies from protaspid to holaspid stages are provided forD. clintonensis, D. speyeri, andD. virginiensisWhittington and Evitt, 1954. The larval stages of these species are very similar, supporting the close relationship between species assigned toDimeropyge.

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Available abstract

Dimeropygeöpik, 1937, is a genus currently composed of at least 14 similar Middle (predominantly) to possibly lowest Upper Ordovician species from Laurentia (13 species) and Baltica (one species). Possible Lower Ordovician specimens have been illustrated by Ross (1951).Dimeropyge clintonensisShaw, 1968, is redescribed, based upon additional material of mature topotypes. A new species ofDimeropyge, D. speyeri, is proposed for material from the Esbataottine Formation in the Mackenzie Mountains, northwestern Canada, previously described asD. clintonensis.A phylogenetic analysis of 10 of the 14 species of this genus is presented (the other species are less completely known, and are related to the analyzed species in a more traditional manner). Ontogenies from protaspid to holaspid stages are provided forD. clintonensis, D. speyeri, andD. virginiensisWhittington and Evitt, 1954. The larval stages of these species are very similar, supporting the close relationship between species assigned toDimeropyge.

Key concepts: Trilobite, Baltica, Ordovician, Laurentia, Genus, Paleontology, Zoology, Geology

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