Abstract

As the Arctic rapidly warms, sub-Arctic species such as the Atlantic salmon (Salmo salar) are expected to shift their distributions into the Arctic, potentially facilitating interaction with native Arctic species. Here, the possible dispersal and establishment of Atlantic salmon are considered in Canadian Arctic fresh waters containing Arctic char (Salvelinus alpinus), an important subsistence fish species. Available information about Atlantic salmon harvests in the Canadian Arctic was summarized to assess dispersal potential. Review and synthesis of published data were used to assess the suitability of the Canadian Arctic for Atlantic salmon colonization and the interaction potential of Atlantic salmon and Arctic char in Canadian Arctic fresh waters. Establishment of Atlantic salmon in Canadian Arctic thermal habitat was deemed possible, especially with rising freshwater temperatures. Overlap in habitat preferences and life cycles of Atlantic salmon and Arctic char, along with data on resource partitioning in sympatry, implied a possibility for interaction at multiple freshwater life stages. However, many data gaps were identified that inhibit further discussion and analysis. These considerations highlight the need for further study of these two culturally, ecologically, and economically important fish species, to address growing concerns and inform future management efforts.

Highlights

  • Anthropogenic climate warming has brought about distributional shifts and changes in abundance for a wide variety of terrestrial and aquatic species (IPCC 2014; Sunday et al 2015)

  • There is distributional overlap of Atlantic salmon and Arctic char in both North America and in Europe, and sympatric populations are known in Iceland, Norway, Russia, and in Ungava Bay (Grønvik and Klemetsen 1987; Salonius 1973)

  • Riverine and lacustrine habitats may be used by both Atlantic salmon and Arctic char for spawning and rearing, potentially facilitating interaction in both habitats at multiple life stages

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Summary

Introduction

Anthropogenic climate warming has brought about distributional shifts and changes in abundance for a wide variety of terrestrial and aquatic species (IPCC 2014; Sunday et al 2015). This warming is projected to continue increasing beyond 2100 for all but the most severe mitigation scenarios (IPCC 2014). These preferred thermal habitats are moving upward in elevation and to higher latitudes (Parmesan 2006; Sunday et al 2012). Species inhabiting these rapidly changing environments must adapt, shift into more suitable habitat, or risk extirpation (Hein et al 2012)

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