The Anatolian glacial refugium and human-mediated colonization: a phylogeographical study of the stone marten (Martes foina) in Turkey

The Anatolian Peninsula, comprising most of modern Turkey, is situated at the junction of Europe, the Middle East and Asia. Together with its complex geomorphological and climatic history, this has given rise to a rich fauna and flora, which exhibits a wide range of historical biogeographical patterns. The stone marten (Martes foina) is a small carnivore that is found across the temperate Palaearctic region including Anatolia, where it is often associated with habitats modified by humans, but few genetic data exist for this species. We sequenced a 1840-bp region of the mitochondrial genome from 97 martens sampled across the peninsula and intron 7 of the nuclear β-fibrinogen gene from 53 of these. Two mitochondrial lineages were recovered, with overlapping eastern and western distributions, but there was no geographical structure for the autosomal marker. Coalescent analyses indicated that both of the lineages originated during the Last Glacial Maximum, one of them within an eastern Anatolian refugium and the other in a western Anatolian or Balkan refugium. The western lineage colonized most of Europe in the Holocene, while the eastern lineage may be endemic to Anatolia, from where it colonized the Iberian Peninsula via human translocation. The presence of at least one refugial stone marten population highlights the importance of Anatolia to the preservation of genetic variation and biodiversity.

A mitogenomic phylogeny and genetic history of sable (Martes zibellina)

We assessed phylogeny of sable (Martes zibellina, Linnaeus, 1758) by sequence analysis of nearly complete, new mitochondrial genomes in 36 specimens from different localities in northern Eurasia (Primorye, Khabarovsk and Krasnoyarsk regions, the Kamchatka Peninsula, the Kuril Islands and the Urals). Phylogenetic analysis of mtDNA sequences demonstrates that two clades, A and BC, radiated about 200-300 thousandyears ago (kya) according to results of Bayesian molecular clock and RelTime analyses of different mitogenome alignments (nearly complete mtDNA sequences, protein-coding region, and synonymous sites), while the age estimates of clades A, B and C fall within the Late Pleistocene (~50-140 kya). Bayesian skyline plots (BSPs) of sable population size change based on analysis of nearly complete mtDNAs show an expansion around 40 kya in the warm Karganian time, without a decline of population size around the Last Glacial Maximum (21 kya). The BSPs based on synonymous clock rate indicate that M. zibellina experienced demographic expansions later, approximately 22 kya. The A2a clade that colonized Kamchatka ~23-50 kya (depending on the mutation rate used) survived the last glaciation there as demonstrated by the BSP analysis. In addition, we have found evidence of positive selection acting at ND4 and cytochrome b genes, thereby suggesting adaptive evolution of the A2a clade in Kamchatka.