Detecting pan-Atlantic migration in salmon ( Salmo salar ) using 137 Cs

137 Cs is a globally dispersed radioisotope that is transferred efficiently through the food chain. There is a strong east-west gradient of 137 Cs in the waters of the North Atlantic due to anthropogenic inputs from Europe, with levels exceeding 10 Bq·m -3 in the Irish Sea and concentrations <1.5...

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Bibliographic Details
Published in:Canadian Journal of Fisheries and Aquatic Sciences
Main Authors: Tucker, Strahan, Pazzia, Ivano, Rowan, David, Rasmussen, Joseph B
Format: Article in Journal/Newspaper
Language:English
Published: Canadian Science Publishing 1999
Subjects:
Aquatic Science
Ecology, Evolution, Behavior and Systematics
Canada
Marguerite
Marguerite River
Atlantic salmon
North Atlantic
Salmo salar
Online Access:http://dx.doi.org/10.1139/f99-267
http://www.nrcresearchpress.com/doi/pdf/10.1139/f99-267
Description
Summary:137 Cs is a globally dispersed radioisotope that is transferred efficiently through the food chain. There is a strong east-west gradient of 137 Cs in the waters of the North Atlantic due to anthropogenic inputs from Europe, with levels exceeding 10 Bq·m -3 in the Irish Sea and concentrations <1.5 Bq·m -3 in the West Atlantic. This range in values is subsequently reflected in fish, including Atlantic salmon (Salmo salar), caught in those waters. 137 Cs concentrations in adult salmon, which had returned to the Ste. Marguerite River, Canada, reflected the entire range of values seen previously across the North Atlantic. In fact, 43% of fish had concentrations characteristic of the Faroe, Norwegian, North, and Irish seas. These results are in sharp contrast with what is generally believed about the migration of salmon and suggest that their marine life history is more panoceanic than previously thought.

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