1977
DOI: 10.5962/p.228581
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The Clark’s Cave bone deposit and the late Pleistocene paleoecology of the central Appalachian Mountains of Virginia

Abstract: Remains of 142 species of vertebrates, ca 4,984 individuals, and 35 species of invertebrates, ca 5,547 individuals, were recovered from a late Pleistocene "owl roost" in the entrance talus of Clark's Cave in the central Appalachian Mountains, lat. 38°05'10" N., Bath County, Virginia, U.S.A. Sixty-four percent of the medium-tosmall-sized mammals represented in the cave remains are now found either farther north or conform in size to present boreal population equivalents (Bergmann's Response) and with the New Pa… Show more

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Cited by 39 publications
(14 citation statements)
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“…I have added 33 identifications (all from higher taxa previously listed) for a total of 42 herptile taxa. (Guilday et aL, 1977). The herpetofauna is more similar to that of Natural Chimneys than New Paris No.…”
Section: Clark's Cavementioning
confidence: 89%
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“…I have added 33 identifications (all from higher taxa previously listed) for a total of 42 herptile taxa. (Guilday et aL, 1977). The herpetofauna is more similar to that of Natural Chimneys than New Paris No.…”
Section: Clark's Cavementioning
confidence: 89%
“…Accumulation.-RupXor roost. Fauna.-Clark's Cave herpetofauna was partially reported in Guilday et al (1977). Their list includes 14 taxa, ranging in rank from species to family.…”
Section: Clark's Cavementioning
confidence: 99%
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“…700,000 years BP, slightly older than the late Kansan Cudahy fauna ( Van der Meulen, 1978). Ochotona is not present in any of the numerous Wisconsinan to early Holocene cave faunas from the Appalachians (Guilday et al, 1977(Guilday et al, , 1978…”
Section: Ecology Of Eastern Ochotonamentioning
confidence: 99%
“…Some studies focused on certain morphological features such as size or the complexity of as an aid in identification of Microtus species. The size criterion was used in conjunction with cranial characters from partial skulls and dental variation to identify the remains of M. xanthognathus in the eastern United States (Guilday and Bender, 1960;Hallberg et aL, 1974;Guilday et aL, 1977Guilday et aL, , 1978, but these studies did not consider M. richardsoni, another large species from the northwestern United States. Similarly, the presence of with an additional posterior dentine field is often regarded as positive evidence of the presence of M. pennsylvanicus, yet this morphological feature is irregularly expressed in a number of different North American species, and is a regular feature in at least two others (Bell, 1997;Bell and Repenning, 1999).…”
Section: Systematic Accountsmentioning
confidence: 99%