The roles of possible geographic barriers and geological events on the phylogeographic structure of the Eastern broad toothed field mouse (Apodemus mystacinus)

The Eastern broad toothed field mouse, Apodemus mystacinus, is a rodent species distributed in Turkey, the Middle East, and a few Aegean Islands. The aim of this study is to analyse the phylogeographic structure of A. mystacinus and possible causes of its differentiation, on the basis of mitochondrial and nuclear DNA sequences using a large number of new samples from Turkey. In this context, partial mitochondrial sequences of cytochrome b (Cytb), control region (D-loop) and a nuclear interphotoreceptor retinoid-binding protein (IRBP) gene were used to reveal the geographical differentiation among A. mystacinus populations and the validity of its subspecies. The estimated divergence times revealed that the first separation of A. mystacinus into three distinct groups (subspecies of A. mystacinus: A. m. mystacinus, A. m. smyrnensis, and A. m. euxinus) begun 0.641 Mya. The possible physical barriers in Anatolia such as high mountains and rivers could interrupt the gene flow between A. mystacinus populations. The results of the present study indicated that A. mystacinus might have used the high rocky areas along the Anatolian Diagonal as a dispersal way. Moreover, mitochondrial data in this study suggested for the first time that A. m. rhodius is synonymous with the nominative subspecies A. m. mystacinus.

Plate tectonics and biogeographical patterns of the Pseudophoxinus (Pisces: Cypriniformes) species complex of central Anatolia, Turkey

We investigated the phylogenetic relationships of Pseudophoxinus (Cyprinidae: Leuciscinae) species from central Anatolia, Turkey to test the hypothesis of geographic speciation driven by early Pliocene orogenic events. We analyzed 1141 aligned base pairs of the complete cytochrome b mitochondrial gene. Phylogenetic relationships reconstructed by maximum likelihood, Bayesian likelihood, and maximum parsimony methods are identical, and generally well supported. Species and clades are restricted to geologically well-defined units, and are deeply divergent from each other. The basal diversification of central Anatolian Pseudophoxinus is estimated to have occurred approximately 15 million years ago. Our results are in agreement with a previous study of the Anatolian fish genus Aphanius that also shows a diversification pattern driven by the Pliocene orogenic events. The distribution of clades of Aphanius and Pseudophoxinus overlap, and areas of distribution comprise the same geological units. The geological history of Anatolia is likely to have had a major impact on the diversification history of many taxa occupying central Anatolia; many of these taxa are likely to be still unrecognized as distinct.