Abstract

Quaternary climate change has been hypothesized to have played a significant role in driving diversification rates in a variety of taxa. We test the hypothesis of increased rates of diversification during the Quaternary in nine groups of New World bats (Chiroptera). The fit of six models of diversification was determined for each group. None experienced an increase in net diversification, rejecting the Quaternary hypothesis. Instead, four groups experienced constant net diversification rates, suggesting no Quaternary climate change impact. Five groups are evolving under a density-dependent model of diversification, suggesting climate cycles may have reduced rates initiated during the Pliocene or late Miocene. The distribution of divergences between sister taxa is consistent with results obtained from avian lineages experiencing declining rates of Quaternary diversification, further discrediting this often invoked hypothesis. Our results suggest that Quaternary climate change did not increase diversification rates in New World bats.

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