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Beebe, B. F. (1980) Pleistocene peccary, Platygonus compressus Le Conte, from Yukon Territory, Canada. Canadian Journal of Earth Sciences, 17 (9) 1204-1209 doi:10.1139/e80-126

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Reference TypeJournal (article/letter/editorial)
TitlePleistocene peccary, Platygonus compressus Le Conte, from Yukon Territory, Canada
JournalCanadian Journal of Earth Sciences
AuthorsBeebe, B. F.Author
Year1980 (September 1)Volume17
Issue9
PublisherCanadian Science Publishing
DOIdoi:10.1139/e80-126Search in ResearchGate
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Mindat Ref. ID476824Long-form Identifiermindat:1:5:476824:5
GUID0
Full ReferenceBeebe, B. F. (1980) Pleistocene peccary, Platygonus compressus Le Conte, from Yukon Territory, Canada. Canadian Journal of Earth Sciences, 17 (9) 1204-1209 doi:10.1139/e80-126
Plain TextBeebe, B. F. (1980) Pleistocene peccary, Platygonus compressus Le Conte, from Yukon Territory, Canada. Canadian Journal of Earth Sciences, 17 (9) 1204-1209 doi:10.1139/e80-126
In(1980, September) Canadian Journal of Earth Sciences Vol. 17 (9) Canadian Science Publishing
Abstract/Notes A fragmented radius of a late Pleistocene peccary, Platygonus compressus Le Conte, has been recovered near Old Crow, Yukon Territory, Canada. The known northern limit of the species is thus extended approximately 3000 km, from the northeastern United States to north of the Arctic Circle in Pleistocene Beringia, and confirms the cold tolerance of the species. The small size of the specimen supports a theory that small size in P. compressus is correlated with periglacial environment. Although the age of the specimen is uncertain, a mid-Wisconsin age is inferred on the basis of availability of a route of dispersal to Beringia and palaeoecological evidence which suggest a largely treeless tundra dominated by sedges and grasses, but with a rich herb component.


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