“…The Fossa Magna was later filled with thick sediments from the Tertiary (Takeda et al, 2004), and the subsequent elevation of the surrounding land during the Quaternary led to the formation of the high mountain chains in central Honshu. The Fossa Magna and orogenic movements are considered important dispersal barriers for many animal species; recent molecular phylogeographical analyses have indicated deep divergences between inter-and intraspecific vicariants in the Fossa Magna region (Sekiné, Hayashi, & Tojo, 2013;Shoda-Kagaya et al, 2010;Suzuki, Sato, & Ohba, 2002;Tojo et al, 2017;Watanabe et al, 2006;Watanabe, Tominaga, Nakajima, Kakioka, & Tabata, 2017). Furthermore, glacial and interglacial cycles have also been considered to affect genetic structures, mainly through the expansion and contraction of organismal distributions and through migrations from the Asian continent across land bridges during the Quaternary (Millien-Parra & Jaeger, 1999;Motokawa, 2017;Qiu, Fu, & Comes, 2011).…”