1997
DOI: 10.2307/2446615
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Allozyme frequencies in New Jersey and North Carolina populations of Atlantic white‐cedar, Chamaecyparis thyoides (Cupressaceae)

Abstract: The present study was conducted to assess the distribution of genetic variation within and among populations of Chamaecyparis thyoides in both marginal and centrally located populations. Allozyme frequency analyses of ten loci from foliage of four New Jersey populations and two North Carolina populations of C. thyoides showed polymorphic loci = 50%, mean number of alleles per locus = 2.8, effective number of alleles per locus = 1.17, and expected heterozygosity = 0.14. Diversity was highest in two populations … Show more

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Cited by 13 publications
(10 citation statements)
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“…Allelic diversity in the New England and Maritime region was a highly monomorphic subset of the genetic diversity observed in the Atlantic Coastal Plain populations of C. glabra. Similar patterns of reduced genetic variation resulting from putative postglacial range expansion also were observed in Pinus (Cwynar and MacDonald, 1987;Parker et al, 1997) and Chamaecyparis (Kuser et al, 1997). Based on our data, we propose that C. glabra migrated to the New England and Maritime region via an Atlantic coastal route.…”
supporting
confidence: 78%
See 1 more Smart Citation
“…Allelic diversity in the New England and Maritime region was a highly monomorphic subset of the genetic diversity observed in the Atlantic Coastal Plain populations of C. glabra. Similar patterns of reduced genetic variation resulting from putative postglacial range expansion also were observed in Pinus (Cwynar and MacDonald, 1987;Parker et al, 1997) and Chamaecyparis (Kuser et al, 1997). Based on our data, we propose that C. glabra migrated to the New England and Maritime region via an Atlantic coastal route.…”
supporting
confidence: 78%
“…Previous research also demonstrated that the potential for hybridization and polyploidy was influenced greatly by ecohistorical factors, such as the pronounced geoclimatic changes and subsequent plant migrations during the Quaternary Period (Ehrendorfer, 1959;Stebbins, 1971). In eastern North America, the repeated expansion, contraction, fragmentation, and amalgamation of species' ranges during the Pleistocene and Holocene epochs, which began two million years ago (Cain, 1944;Holt and Paterson, 1970;Jacobs, Werth, and Guttman, 1984 court and Delcourt, 1987;Delcourt, 1991), undoubtedly resulted in new contacts between previously isolated populations Kuser et al, 1997), increased the probability of interlineage hybridization and introgression Parker et al, 1997), and led to extinctions of progenitor taxa (Werth, 1991).…”
mentioning
confidence: 99%
“…In several studies, patterns of genetic variation along the geographical range of tree species using isozymes have been explained by Pleistocene environmental changes ( Fowler & Morris, 1977; Cwynar & MacDonald, 1987; Sherman‐Broyles et al. , 1992 ; Zabinski, 1992; Kuser et al. , 1997 ; Parker et al.…”
Section: Introductionmentioning
confidence: 99%
“…Genetic markers such as isozymes have been used to locate glacial refugia and to trace migration routes after glacial retreat of Northern Hemisphere plant taxa yielding comparable results to those gathered from the pollen record (Wheeler & Guries, 1982). In several studies, patterns of genetic variation along the geographical range of tree species using isozymes have been explained by Pleistocene environmental changes (Fowler & Morris, 1977;Cwynar & MacDonald, 1987;Sherman-Broyles et al, 1992;Zabinski, 1992;Kuser et al , 1997;Parker et al , 1997).…”
Section: Introductionmentioning
confidence: 99%
“…Thus, geographical distribution of genetic variation can provide an alternative source of information on past events which in turn is independent from the fossil record (Cwynar & MacDonald, 1987;Lagercrantz & Ryman, 1990;Schnable et al , 1993;Kuser et al , 1997;Ledig, 2000;among others). Thus, geographical distribution of genetic variation can provide an alternative source of information on past events which in turn is independent from the fossil record (Cwynar & MacDonald, 1987;Lagercrantz & Ryman, 1990;Schnable et al , 1993;Kuser et al , 1997;Ledig, 2000;among others).…”
Section: Introductionmentioning
confidence: 99%