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- W2038725256 abstract "Abstract January Cave, in the Rocky Mountains of southwestern Alberta, has yielded vertebrate remains from a coprocenosis of mid-Wisconsinan-age. Taphonomic analysis indicates accumulation by raptors, mostly owls, and mammalian carnivores. The vertebrate record, together with pollen analysis, indicates that cool, dry conditions prevailed in an extensive tundra-like environment, with prairie elements in the valleys below. Thirty-four mammalian taxa have been recovered from January Cave. Today, some of these species (e.g., Lemmus sibiricus and Dicrostonyx torquatus ) do not coexist with others (e.g., Cynomys sp., Mustela nigripes, Vulpes velox , and Lagurus curtatus ). Therefore, the January Cave local fauna represents a “nonanalog” mammalian community characteristic of the late Pleistocene. It suggests that the region enjoyed an equable climate, with reduced climatic extremes but still cool, further supporting a mid-Wisconsinan age estimate for the fauna. It is the first major, small vertebrate fauna of its age to be reported from Alberta." @default.
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- W2038725256 date "1991-01-01" @default.
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- W2038725256 title "Mid-Wisconsinan Vertebrates and their Environment from January Cave, Alberta, Canada" @default.
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- W2038725256 doi "https://doi.org/10.1016/0033-5894(91)90100-j" @default.
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