Abstract
A fragmented radius of a Late Pleistocene peccary, P. compressus Le Conte, was recovered near Old Crow, Yukon Territory, Canada. The known northern limit of the species is extended .apprx. 3000 km, from the northeastern USA 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 paleoecological evidence which suggest a largely treeless tundra dominated by sedges and grasses, but with a rich herb component.