Figure 3.

Origin and diversification pattern of Neotropical Troidini. The uppermost panel shows the evolution of paleoclimate as estimated by proxy Benthic δO18[20]. Major climate events are indicated. The lineages-through-time plot is placed next, with the 95% confidence interval indicated by a dotted red line. Most likely biogeographic reconstructions (inferred by the DEC model) are shown on the median-age BEAST chronogram of Neotropical Troidini. Major geological events are also indicated to show congruence between speciation and possible factors of diversification.

Condamine et al. BMC Evolutionary Biology 2012 12:82   doi:10.1186/1471-2148-12-82
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