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Marine Ecology Progress Series

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MEPS 258:283-289 (2003)  -  doi:10.3354/meps258283

Influence of swimming form on otolith δ13C in marine fish

Graham D. Sherwood*, George A. Rose

Fisheries Conservation Chair, Fisheries and Marine Institute of Memorial University of Newfoundland and Labrador, PO Box 4920, St. John¹s, Newfoundland and Labrador, A1C 5R3, Canada

ABSTRACT: While temperature records are available from otolith δ18O profiles in fish, interpreting changes in otolith δ13C remains ambiguous. We compiled a global database of published otolith δ13C values for 60 species representing 30 families of marine fishes. Species¹ mean otolith δ13C ranged from +0.5 to -8.6 ‰. Among-family variance in otoli δ13C was uniquely explained by a morphometric index for aerobic swimming activity (caudal aspect ratio, r2 = 0.61). The models that consistently explained the maximum among-species variance in otolith &symbol;13C included caudal aspect ratio and maximum depth of occurrence. Our analysis supports the use of otolith carbon-isotope ratios to indicate metabolism (primarily active) in marine fish. This information may be applied to studies of fish feeding and related food-web structure, both past and present.

KEY WORDS: Otolith · Stable isotopes · δ13C · Marine fish · Metabolism · Swimming activity · Caudal aspect ratio · Morphometrics

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