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Phylogeography of Fischer’s blue,Tongeia fischeri,in Japan: Evidence for introgressive hybridization
Authors:Ekgachai Jeratthitikul  Takehiro Hara  Masaya Yago  Tateo Itoh  Min Wang  Shin-ichi Usami  Tsutomu Hikida
Institution:1. Laboratory of Systematic Zoology, Department of Zoology, Graduate School of Science, Kyoto University, Kitashirakawa-Oiwakecho, Sakyo-ku, Kyoto 606-8502, Japan;2. Division of Science and Technology, Shinshu University, 3-1-1 Asahi, Matsumoto 390-8621, Japan;3. The University Museum, The University of Tokyo, 7-3-1 Hongo, Bunkyo-ku, Tokyo 113-0033, Japan;4. Department of Biology, Faculty of Science, Shinshu University, 3-1-1 Asahi, Matsumoto 390-8621, Japan;5. Laboratory of Insect Ecology, South China Agricultural University, Guangzhou, China;6. Institute of Mountain Sciences, Shinshu University, 3-1-1 Asahi, Matsumoto 390-8621, Japan
Abstract:The widespread lycaenid butterfly Tongeia fischeri is distributed from eastern Europe to northeastern Asia and represented by three geographically isolated populations in Japan. In order to clarify the phylogeographic history of the species, we used sequences of three mitochondrial (COI, Cyt b and ND5) and two nuclear (Rpl5 and Ldh) genes of 207 individuals collected from 55 sites throughout Japan and five sites on the Asian continent. Phylogenetic trees and the median-joining network revealed six evolutionary mitochondrial haplotype clades, which corresponded to the geographic distribution of the species. Common ancestors of Japanese T. fischeri might have come to Japan during the mid-Pleistocene by multiple dispersals of continental populations, probably via a land bridge or narrow channel between western Japan and the Korean Peninsula. The geographical patterns of variation of mitochondrial and nuclear markers are discordant in northeastern Kyushu, possibly as a result of introgressive hybridization during the ancient contact between the Kyushu and Shikoku populations in the last glacial maximum. The phylogeographic pattern of T. fischeri in Japan are probably related to the geological history, Pleistocene climatic oscillations and distribution of the host plant.
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