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Continuous variation in the pattern of marine v. freshwater foraging in brown trout Salmo trutta L. from Loch Lomond, Scotland

Identifieur interne : 000B37 ( Main/Merge ); précédent : 000B36; suivant : 000B38

Continuous variation in the pattern of marine v. freshwater foraging in brown trout Salmo trutta L. from Loch Lomond, Scotland

Auteurs : E. C. Etheridge [Royaume-Uni] ; C. Harrod [Royaume-Uni] ; C. Bean [Royaume-Uni] ; C. E. Adams [Royaume-Uni]

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RBID : ISTEX:E479729E7487DA99B9620C011DA2D8F01B958B25

English descriptors

Abstract

Carbon stable‐isotope analysis showed that individual brown trout Salmo trutta in Loch Lomond adopted strategies intermediate to that of freshwater residency or anadromy, suggesting either repeated movement between freshwater and marine environments, or estuarine residency. Carbon stable‐isotope (δ13C) values from Loch Lomond brown trout muscle tissue ranged from those indicative of assimilation of purely freshwater‐derived carbon to those reflecting significant utilization of marine‐derived carbon. A single isotope, two‐source mixing model indicated that, on average, marine C made a 33% contribution to the muscle tissue C of Loch Lomond brown trout. Nitrogen stable isotope, δ15N, but not δ13C was correlated with fork length suggesting that larger fish were feeding at a higher trophic level but that marine feeding was not indicated by larger body size. These results are discussed with reference to migration patterns in other species.

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DOI: 10.1111/j.1095-8649.2008.01905.x

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ISTEX:E479729E7487DA99B9620C011DA2D8F01B958B25

Le document en format XML

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<div type="abstract" xml:lang="en">Carbon stable‐isotope analysis showed that individual brown trout Salmo trutta in Loch Lomond adopted strategies intermediate to that of freshwater residency or anadromy, suggesting either repeated movement between freshwater and marine environments, or estuarine residency. Carbon stable‐isotope (δ13C) values from Loch Lomond brown trout muscle tissue ranged from those indicative of assimilation of purely freshwater‐derived carbon to those reflecting significant utilization of marine‐derived carbon. A single isotope, two‐source mixing model indicated that, on average, marine C made a 33% contribution to the muscle tissue C of Loch Lomond brown trout. Nitrogen stable isotope, δ15N, but not δ13C was correlated with fork length suggesting that larger fish were feeding at a higher trophic level but that marine feeding was not indicated by larger body size. These results are discussed with reference to migration patterns in other species.</div>
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