Middle to Upper Ordovician graptolite biostratigraphy of Peel River and other areas of the northern Canadian Cordillera
- 1 February 1985
- journal article
- research article
- Published by Canadian Science Publishing in Canadian Journal of Earth Sciences
- Vol. 22 (2) , 227-239
- https://doi.org/10.1139/e85-020
Abstract
Middle to Upper Ordovician (Darriwilian to Bolindian) graptolite zones of the northern Canadian Cordillera comprise the following: Glyptograptus euglyphus Zone of late Darriwilian (Llandeilo) age, Nemagraptus gracilis Zone of early Gisbornian (late Llandeilo and earliest Caradoc) age, Climacograptus bicornis and Dicranograptus clingani? zones of early to mid-Gisbornian (early to mid-Caradoc) age, Orthograptus quadrimucronatus Zone of Eastonian (late Caradoc) age, and Dicellograptus ornatus zone of Bolindian (Ashgill) age.A prominent biostratigraphic break equivalent to the spiniferus to hians kirki zones (Eastonian) is shown to exist between the clingani? Zone and the overlying quadrimucronatus Zone.Thirty eight common and (or) important species are illustrated, of which one new species, Orthograptus expansus n. sp., is described and figured.This publication has 4 references indexed in Scilit:
- The Ordovician–Silurian boundary, northern Canadian Cordillera: graptolite and conodont correlationCanadian Journal of Earth Sciences, 1982
- Some Pacific Faunal Province graptolites from the Ordovician of northern Yukon, CanadaCanadian Journal of Earth Sciences, 1977
- Middle and Upper Ordovician graptolites from the St. Lawrence Lowlands, Quebec, CanadaCanadian Journal of Earth Sciences, 1977
- Graptolites with Multiple Genicular Spines from the Upper Ordovician of Western North AmericaCanadian Journal of Earth Sciences, 1974