Pleistocene Bison Skeleton (Bison bison cf. occidentalis) from Clayhurst Crossing, British Colombia

Author:

Apland Brian,Harington Charles R.

Abstract

Remains of a large old male bison skeleton from a gravel pit near Clayhurst Crossing are tentatively referred to the extinct western bison (Bison bison cf. occidentalis). It is the most complete late Pleistocene "medium-horned" bison so far reported from Canada, and is therefore described in detail. Four accelerator mass spectrometry (AMS) radiocarbon dates on bone from the specimen provide a weighted average age of 10,500±90 yr BP, supporting an earlier suggestion that river terraces in the mid-Peace area began developing before 10,000 years ago. Evidently Bison bison antiquus occurred in southern Alberta about 11,000 years ago, and both it and Bison bison occidentalis occupied the Peace River area shortly before 10,000 years ago. It is hypothesised that by at least 9700 BP, B. b. occidentalis had spread southern Alberta. These data suggest that biotic interchange between the former Beringian refugium and the southern interior Plains of North America occurred prior to 10,500 years ago.

Publisher

Consortium Erudit

Subject

Paleontology,Geology

Reference38 articles.

1. Bobrowsky, P.T., Catto, N. and Levson, V., 1991. Reconnaissance Quaternary geological investigations in Peace River District, British Columbia (93P, 94A). British Columbia Geological Survey Branch, Geological Fieldwork 1990, Paper 1991-1: 345-358.

2. Bobrowsky, P.T. and Rutter, N., 1990. Geologic evidence for an ice-free corridor in northeastern British Columbia, Canada. In Current Research in the Pleistocene, 7: 133-135.

3. Bobrowsky, P.T. and Rutter, N., 1992. The Quaternary geologic history of the Canadian Rocky Mountains. Géographie physique et Quaternaire, 46(1): 5-50.

4. Churcher, C.S., 1968. Pleistocene ungulates from the Bow Rivergravels at Cochrane, Alberta. Canadian Journal of Earth Sciences, 5(6): 1467-1488.

5. Churcher, C.S., 1975. Additional evidence of Pleistocene ungulates from the Bow River gravels at Cochrane, Alberta. Canadian Journal of Earth Sciences, 12: 68-76.

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