Silurian (Wenlockian) trilobites from Baillie-Hamilton Island, Canadian Arctic Archipelago
- 1 February 1977
- journal article
- research article
- Published by Canadian Science Publishing in Canadian Journal of Earth Sciences
- Vol. 14 (2) , 285-317
- https://doi.org/10.1139/e77-030
Abstract
Wenlockian trilobites representing at least 15 genera are reported from carbonate strata within the Cape Phillips Formation, Baillie-Hamilton Island. The collections are stratigraphically bounded by the graptolite Zones of Cyrtograptus murchisoni and Monograptus testis. The fauna is generically dominated by lichids, odontopleurids, and cheirurids. Scutelluids, phacopids, dalmanitids, and harpids are notable for their absence. At the familial level the fauna corresponds to one recently discovered from similar age beds of the Mackenzie Mountains, Northwest Territories. The limited quantity and fragmental nature of much of the silicified fauna precludes erection of many new taxa, although four new species described are: Sphaerexochus dimorphus, Dicranogmus skinneri, Hemiarges rohri, and Hemiarges mikulici. Dimorphic pygidia are interpreted as probable sexual dimorphs in Sphaerexochus dimorphus n. sp.This publication has 3 references indexed in Scilit:
- Phacops and other trilobites from Emsian age beds of the Delorme Formation, Mackenzie Mountains, Northwest TerritoriesCanadian Journal of Earth Sciences, 1976
- Ordovician Formations and Faunas, Southern Mackenzie MountainsCanadian Journal of Earth Sciences, 1975
- Observations on Dudley TrilobitesQuarterly Journal of the Geological Society, 1850