“…The melting and recession of glacier ice precipitated a terrestrial rebound of the earth resulting in the formation of several-hundred lake environments that were colonized in parallel by both marine and freshwater fish species at the end of the ice age. The evidence for distinct gene pools in species complexes that evolved within these new environments is widespread and includes Arctic charr (e.g., Jonsson 1993, Corrigan et al 2011), Atlantic salmon (e.g., Verspoor and Cole, 1989;Gilbey et al, 2006), sockeye salmon (e.g., Hamon and Foote, 2005;Pavey et al, 2010b), lake whitefish (e.g., Lindsey, 1963;Fenderson, 1964;Bodaly, 1979;Bernatchez and Dodson, 1990), rainbow smelt (e.g., Taylor and Bentzen, 1993;Shaw and Curry, 2011), stickleback (e.g., Lavin and McPhail, 1993;McPhail, 1993;Thompson et al, 1997;Taylor and McPhail, 1999) and some lampreys (e.g., Docker, 2009). In all of these species, parallel evolution in response to the environment has occurred in multiple environments (Table 1).…”