Abstract
Relatively recently, temperate regions in North America were covered by extensive ice sheets, making them inhospitable to contemporary flora and fauna. Since the retreat of the ice sheets, these regions have been recolonized by a diversity of taxa, some of which have undergone rapid postglacial divergence. Evidence supports the hypothesis that some taxa persisted in unglaciated refugia during the Last Glacial Maximum, such as on Haida Gwaii (formerly the Queen Charlotte Islands). Many taxa on Haida Gwaii are genetically distinct from mainland populations at neutral molecular markers possibly as the result of isolation in refugia or postglacial colonization. The Golden-crowned Kinglet (Regulus satrapa Lichtenstein, 1823) is a continentally distributed, short-distance migratory passerine inhabiting mature conifer forests including those on Haida Gwaii. We used five microsatellite markers and a 568 base-pair fragment of the mitochondrial control region to determine the likelihood that Haida Gwaii region acted as a refugium for this species during the last ice age. We report significant gene flow between Haida Gwaii and the western North American mainland from mitochondrial markers, but significant population genetic differentiation at nuclear markers. We also report genetic divergence between eastern and western Golden-crowned Kinglets, as well as higher genetic diversity and population substructuring within the western population than within the eastern population. The east–west differentiation probably arose due to isolation in separate Pleistocene refugia south of the ice sheets. However, population differences within the west are likely caused by more recent processes; contemporary differentiation of Haida Gwaii Golden-crowned Kinglets most likely occurred postglacially.
Published Version
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