Abstract
Based on the presumed nature of regional climates during the late Pleistocene, it is suggested that the climate was inhospitable for P. cinereus on the Del-Mar-Va Peninsula at the Wisconsin maximum. It is postulated that, after the Laurentide ice sheet receded c 14 000 yr BP, the peninsula was invaded by populations of P. cinereus form the N and S. When the 2 forms of P. cinereus met, a secondary zone of contact was produced. -from Author
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CITATION STYLE
Wynn, A. H. (1986). Linkage disequilibrium and a contact zone in Plethodon cinereus on the Del-Mar-Va Peninsula. Evolution, 40(1), 44–54. https://doi.org/10.1111/j.1558-5646.1986.tb05716.x
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