Intercontinental disjunctions between eastern Asia and western North America in vascular plants highlight the biogeographic importance of the Bering land bridge from late Cretaceous to Neogene

Abstract This review shows a close biogeographic connection between eastern Asia and western North America from the late Cretaceous to the late Neogene in major lineages of vascular plants (flowering plants, gymnosperms, ferns and lycophytes). Of the eastern Asian–North American disjuncts, conifers...

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Bibliographic Details
Published in:Journal of Systematics and Evolution
Main Authors: Wen, Jun, Nie, Ze‐Long, Ickert‐Bond, Stefanie M.
Other Authors: Arnold Arboretum of Harvard University, Field Museum and the Smithsonian Institution
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2016
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Online Access:http://dx.doi.org/10.1111/jse.12222
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fjse.12222
https://onlinelibrary.wiley.com/doi/pdf/10.1111/jse.12222
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Summary:Abstract This review shows a close biogeographic connection between eastern Asia and western North America from the late Cretaceous to the late Neogene in major lineages of vascular plants (flowering plants, gymnosperms, ferns and lycophytes). Of the eastern Asian–North American disjuncts, conifers exhibit a high proportion of disjuncts between eastern Asia and western North America. Several lineages of ferns also show a recent disjunct pattern in the two areas. In flowering plants, the pattern is commonly shown in temperate elements between northeastern Asia and northwestern North America, as well as elements of the relict boreotropical and Neogene mesophytic and coniferous floras. The many cases of intercontinental biogeographic disjunctions between eastern Asia and western North America in plants supported by recent phylogenetic analyses highlight the importance of the Bering land bridge and/or the plant migrations across the Beringian region from the late Cretaceous to the late Neogene, especially during the Miocene. The Beringian region has permitted the filtering and migration of certain plant taxa since the Pliocene after the opening of the Bering Strait, as many conspecific taxa or closely related species occur on both sides of Beringia.