July 12, 2018

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Mapping species range shifts under recent climatic changes

Environmentally-complex Bering seascape with seasonal seaice cover, 25 June 2018. In the background is NOAA research vessel, Oscar Dyson. Credit: National Oceanic and Atmospheric Administration/Department of Commerce
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Environmentally-complex Bering seascape with seasonal seaice cover, 25 June 2018. In the background is NOAA research vessel, Oscar Dyson. Credit: National Oceanic and Atmospheric Administration/Department of Commerce

Marine species in the eastern Bering Sea are not shifting their distribution ranges fast enough to keep track of current changes in climate, according to a study led by researchers at Hokkaido University.

As global change alters sea temperatures and environmental conditions, need to track these signals at a sufficient pace to remain within their climatic habitat. However, lags in distributional responses to temperature shifts have been documented in terrestrial and aquatic taxa, as species range dynamics are also influenced by factors other than climate.

Irene Alabia, a fisheries oceanographer at Hokkaido University's Arctic Research Center, led a study to evaluate multi-taxa responses to contrasting climatic regimes in the eastern Bering Sea, defined by persistent stanzas of regional warming and cooling. She worked with colleagues at Hokkaido University and the University of Alaska Fairbanks to examine potential distributions of 21 fish and invertebrate species in the eastern Bering Sea between 1993 and 2016. These were generated from multi-ensemble habitat models correlating taxon-specific occurrences to suite of climatic (winter sea surface temperature) and environmental factors (winter sea ice cover and depth).

(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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(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

Using satellite-derived environmental data and species data from bottom trawl surveys, the team compared rates of local climatic change (climatic velocity) to both observed (data-driven) and expected (model-driven) species distributional responses. They found that the climatic velocities were poorly correlated with observed and expected distributional responses, underpinning the importance of incorporating species-specific sensitivity to climate variation when predicting rates of range shifts in to climatic changes. Further, most of the examined were trailing behind climate change, potentially increasing their vulnerability to future climate fluctuations.

"Our results can be useful for reinforcing current conservation and management efforts, and help develop adaptive management strategies to deal with varying impacts of climate changes to marine resources in the region," says Irene Alabia of Hokkaido University. The study was published in the journal Diversity and Distributions.

More information: Irene D. Alabia et al. Distribution shifts of marine taxa in the Pacific Arctic under contemporary climate changes, Diversity and Distributions (2018). DOI: 10.1111/ddi.12788

Journal information: Diversity and Distributions

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