Bering Sea Figures (IMAGE)
Caption
(a) Rates of local climatic change, (b) expected (bioclimatic velocity) and observed (biotic velocity) distribution responses for the Arctic cod (cold-adapted species) and Flathead sole (warm-water species) across a cold to warm climate transition in the eastern Bering Sea (inset map for geographic reference). Cold to warm transition provides favorable conditions for warm-adapted species while creates unsuitable environment for cold-water taxon.
Credit
Hokkaido University
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