Stable isotope analysis of marine feeding signatures of Atlantic salmon in the North Atlantic

<qd> Dempson, J. B., Braithwaite, V. A., Doherty, D., and Power, M. 2010. Stable isotope analysis of marine feeding signatures of Atlantic salmon in the North Atlantic. – ICES Journal of Marine Science, 67: 52–61. </qd>Differences in the marine feeding of three geographically distinct po...

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Bibliographic Details
Published in:ICES Journal of Marine Science
Main Authors: Dempson, J. Brian, Braithwaite, Victoria A., Doherty, Denis, Power, Michael
Format: Text
Language:English
Published: Oxford University Press 2010
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Online Access:http://icesjms.oxfordjournals.org/cgi/content/short/67/1/52
https://doi.org/10.1093/icesjms/fsp227
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Summary:<qd> Dempson, J. B., Braithwaite, V. A., Doherty, D., and Power, M. 2010. Stable isotope analysis of marine feeding signatures of Atlantic salmon in the North Atlantic. – ICES Journal of Marine Science, 67: 52–61. </qd>Differences in the marine feeding of three geographically distinct populations of Atlantic salmon ( Salmo salar ) in the North Atlantic (Conne River, Newfoundland; Koksoak River, Ungava Bay, Québec; River Erne, northwest Ireland) were examined using analyses of stable isotopes of carbon and nitrogen (δ13C and δ15N) and contrasted with isotope signatures obtained from a sample of salmon of unknown origin captured in the Labrador Sea. Although the overall range of δ13C and δ15N values (δ13C: <f> </f> from −22.42 to −19.37; δ15N: <f> </f> from 10.70 to 13.38) was similar to that reported by others, significant differences were found among populations and between different sea-age life-history groups. Reported differences in marine feeding between populations from the Northeast and Northwest Atlantic corroborated the stable isotope results. A surrogate measure of lipid content, the C:N ratio, was also compared among 1-sea-winter salmon. The highest levels were associated with the Koksoak River, suggesting that Subarctic populations may require higher energy reserves to contend with their longer migrations and more-severe environmental conditions.