Mitochondrial DNA analysis confirms the existence of two glacial races of rainbow smelt Osmerus mordax and their reproductive isolation in the St Lawrence River estuary (Quebec, Canada)

A phylogeographic analysis of mitochondrial DNA variation was performed in order to test the hypothesis that north-eastern North America has been postglacially recolonized by two races of rainbow smelt Osmerus mordax. This was accomplished by documenting the geographical distribution of two major mtDNA phylogenetic clades among 1290 smelt from 49 lacustrine and anadromous populations covering most of the species' native range. The data set was built by combining previously published results with those generated in this study. The two mtDNA clades showed a geographical dichotomy, independent of life-history types, whereby the more eastern populations were either fixed or largely dominated by one clade and western populations for the other. Such geographical pattern implying a phylogenetic discontinuity provided strong evidence for the persistence of smelt in two distinct glacial refugia as well as their differential postglacial dispersal. The most likely refugium for the so-called Atlantic race was the Atlantic coastal plains, whereas that of the so-called Acadian race was the exundated Grand Banks area. Patterns of postglacial dispersal interpreted from palaeogeographic events suggested that the Atlantic race recolonized northern regions about 5000 years prior the Acadian race. Both races came into contact in the St Lawrence River estuary. While gene flow has been possible, the sympatric occurrence in the estuary of anadromous populations alternatively dominated by one mtDNA clade or the other indicated that reproductive isolation mechanisms between the two races developed within this contact zone. This represents the first evidence of secondary intergradation among distinct races of aquatic organisms in an estuarine environment.