The last interglacial–glacial cycle, Clyde foreland, Baffin Island, N.W.T.: stratigraphy, biostratigraphy, and chronology
- 1 December 1977
- journal article
- research article
- Published by Canadian Science Publishing in Canadian Journal of Earth Sciences
- Vol. 14 (12), 2824-2857
- https://doi.org/10.1139/e77-249
Abstract
A study of the stratigraphic sequence (14C and amino acid age control), marine bivalve faunal changes, and palynology of buried soils and organic-rich sediment collected from the Clyde Foreland Formation in the extensive cliff sections of the Clyde foreland, eastern Baffin Island, Northwest Territories [Canada] suggests the following last interglacial-Foxe (last glaciation) glacial-present interglacial sequence: Cape Christian Member (about 130,000 yr BP?); Kuvinilk Member (containing Chlamys islandicus); Kogalu Member (< 35,000 14C yr BP); and the Eglinton Member (10,000 yr BP to present).This publication has 6 references indexed in Scilit:
- Studies of Glacial History in Arctic Canada. II. Interglacial Peat Deposits on Bathurst IslandCanadian Journal of Earth Sciences, 1974
- Wisconsin Glacial Chronology and Relative Sea-level Movements, Narpaing Fiord Broughton Island Area, Eastern Baffin Island, N.W.T.Canadian Journal of Earth Sciences, 1973
- Isostatic response to loading of the crust in CanadaCanadian Journal of Earth Sciences, 1970
- Radiocarbon Isochrones on the Disintegration of the Laurentide Ice SheetArctic and Alpine Research, 1969
- A METHOD OF ABSOLUTE POLLEN COUNTINGNew Phytologist, 1967
- Baffin Island Refugia Older than 54,000 YearsScience, 1966