Phylogeny recapitulates geography, or why New Zealand has so many species of skinks

The evolutionary history of 25 New Zealand scincid lizards in the endemic genera Oligosoma andCyclodina was examined using 12S rRNA sequence data. Phylogenetic resolution was poor, despite there being up to 9% sequence divergence between taxa. Lack of resolution was not attributable to biases in the data, such as site saturation or differences in sites free to vary, so we infer that New Zealand skinks underwent two relatively rapid phases of divergence. The rate of substitution for the skink sequences appears to be similar to some bird and mammal groups for which times of divergence have been estimated. Using these calibrations diversification of Oligosoma skinks probably began at least 23 million years ago (Mya). The pattern of relationships and the timing of this diversification are interpreted as resulting from rapid allopatric speciation during the Oligocene (25–35 Mya) when New Zealand was fragmented into many low lying islands. A second major phase of speciation involving the Cyclodina seems to have occurred during the Miocene (15–24 Mya), probably as a consequence of increasing land area and habitat diversity. This pattern of skink evolution contrasts with the Oligocene «environmental crisis» hypothesis of Cooper & Cooper (Proc. R. Soc. Lond. B. 261 , 293–302), but can be attributed to differences in the ecology of different taxa. This can be tested by examination of other groups, such as land snails and geckos. The large number of lizard species in New Zealand can be considered a legacy both of past geography as well as the absence of small mammals which would have been both competitors and predators.