“…Given that the Sr concentration is several hundred times higher in seawater than in freshwater (Rosenthal, Eves, & Cochran, 1970), it is possible to determine the migration history of an individual by evaluating the fluctuations in Sr/Ca ratios in otoliths, where trace elements remain stable for long periods (Campana, 1999;Arai, 2010). The determination of migration history from otolith samples has been performed on many fish species in the past few years, including Japanese dace Tribolodon hakonensis (Günther, 1880) (Ishizaki et al, 2009), Amago salmon Oncorhynchus masou ishikawae (Jordan and McGregor, 1925) (Umino et al, 2001), Dolly Varden trout Salvelinus malma (Walbaum, 1792) (Umatani, Arai, & Maekawa, 2008), and Japanese smelt Hypomesus nipponensis (McAllister, 1963) (Sasaki, Saruwatari, & Watanabe, 2006). The finding that the Sr/Ca ratios of the Sakhalin taimen Hucho perryi (Brevoort, 1856) are between the Sr/Ca ratios of fish in salt water and those in freshwater indicates that they spend time inhabiting brackish areas (Arai, 2010).…”