“…Generally, the different magnitudes of divergence can result from differences in divergence time, gene flow, and/or selection regimes (Berner, Roesti, Hendry, & Salzburger, ; Stuart et al., ). In the Little Campbell River, the marine and stream ecotypes are parapatric, with their hybrid zone existing in the midstream (Hagen, ), whereas the stream habitat in Gifu, Japan, is isolated from the sea, making the gene flow between marine and stream ecotypes unlikely (Kitano & Mori, ; Mori, ). The time of freshwater colonization in British Columbia, Canada, is thought to be postglacial (Bell & Foster, ), whereas that of the Japanese stream population was estimated to be much older, such as 0.37–0.43 million years ago, by an analysis of mitochondrial cytochrome b sequence (Watanabe, Mori, & Nishida, ).…”