Molecular evidence for dispersal rather than vicariance as the origin of flightless insect species on the Chatham Islands, New Zealand

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Driven by the West Wind Drift? A synthesis of southern temperate marine biogeography, with new directions for dispersalism (2008, background): “His reservations have proven to be well founded to date, as subsequent molecular phylogenetic analyses have enabled researchers to reject southern panbiogeographic hypotheses (e.g. Trewick, 2000; Trewick & Wallis, 2001; Paterson et al., 2006).”
Hello New Zealand (2006, background): “, 1994, 2006; Campbell, 1998), taxonomic (Emberson, 1998) and molecular data (Trewick, 2000; Trewick et al., 2005; Paterson et al., 2006) that the extant Chathams emerged from the sea 1– 3 Ma.”
Directional asymmetry of long‐distance dispersal and colonization could mislead reconstructions of biogeography (2005, background): “1, a molecular date suggests that the most terminal node is too recent to be explained by vicariance then a dispersal explanation is typically inferred (e.g. Leys et al., 2000; Trewick, 2000).”
The resurrection of oceanic dispersal in historical biogeography. (2005, background): “Other taxa for which molecular dating has supported oceanic dispersal over tectonic vicariance include freshwater teleosts [15,16] ,c arnivores[17] ,l emurs[17], monkeys [18], squamate reptiles [19,20] ,f rogs[21], flightless insects [ 22 ], and angiosperms in the Malpighiaceae [23], Rapateaceae [24”