2001
DOI: 10.1111/j.1095-8312.2001.tb01368.x
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Patterns of animal dispersal, vicariance and diversification in the Holarctic

Abstract: We analysed patterns of animal dispersal, vicariance and diversification in the Holarctic based on complete phylogenies of 57 extant non-marine taxa, together comprising 770 species, documenting biogeographic events from the Late Mesozoic to the present. Four major areas, each corresponding to a historically persistent landmass, were used in the analyses: eastern Nearctic (EN), western Nearctic (WN), eastern Palaeoarctic (EP) and western Palaeoarctic (WP). Parsimony-based tree fitting showed that there is no s… Show more

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Cited by 405 publications
(531 citation statements)
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References 74 publications
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“…3). These findings are in agreement with broad-scale spatial and temporal analyses of the extant Holarctic fauna (51) and with the timing and pattern of mammalian dispersal indicated by the fossil record (52), both of which suggest that dispersal into the New World in the late Oligocene͞early Miocene was predominantly through Beringia. We infer that divergence of lineages within the extremely diverse subfamily Emberizinae commenced shortly after invasion of the New World (NPRS: 16 Ma, bootstrap SE ϭ 3.3; PL: 18 Ma, SE ϭ 1.6), a timing in close agreement with dates derived from mitochondrial DNA of this group (53).…”
Section: Resultssupporting
confidence: 88%
“…3). These findings are in agreement with broad-scale spatial and temporal analyses of the extant Holarctic fauna (51) and with the timing and pattern of mammalian dispersal indicated by the fossil record (52), both of which suggest that dispersal into the New World in the late Oligocene͞early Miocene was predominantly through Beringia. We infer that divergence of lineages within the extremely diverse subfamily Emberizinae commenced shortly after invasion of the New World (NPRS: 16 Ma, bootstrap SE ϭ 3.3; PL: 18 Ma, SE ϭ 1.6), a timing in close agreement with dates derived from mitochondrial DNA of this group (53).…”
Section: Resultssupporting
confidence: 88%
“…This period was characterised by synchronous speciation in many other terrestrial organisms, as demonstrated by previous works in butterflies (Condamine et al 2013a;Condamine et al 2013b). Such speciation pattern in the late Pliocene and throughout the Pleistocene can be largely attributed to past geological and climatic events such as the change in the Eastern Himalayas or glaciation cycles initiated at the end of the Pliocene (see Sanmartín et al 2001 for a review). Frequent tectonic shifts coupled with climatic oscillations contributed to allopatric (vicariance) divergences either due to physical barriers like mountains and valleys or isolations caused by dispersal within the distribution range of ancestral species.…”
Section: Discussionmentioning
confidence: 56%
“…The land connection between these continents has been present from the mid-Cretaceous up through the late Pliocene 3.5 Mya and several more times during the Pleistocene (Sanmartín et al 2001). Cambefort (1991) suggests the colonization of North America by these ancestors is not older than the Pliocene.…”
Section: Discussionmentioning
confidence: 99%