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Influence of swimming form on otolith d13C in marine fishGraham D. Sherwood*, George A. RoseFisheries Conservation Chair, Fisheries and Marine Institute of Memorial University of Newfoundland and Labrador, PO Box 4920, St. John's, Newfoundland and Labrador, A1C 5R3, Canada![]() ABSTRACT: While temperature records are available from otolith d18O profiles in fish, interpreting changes in otolith d13C remains ambiguous. We compiled a global database of published otolith d13C values for 60 species representing 30 families of marine fishes. Species' mean otolith d13C ranged from +0.5 to -8.6 ‰. Among-family variance in otoli d13C 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 d13C 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 · d13C · Marine fish · Metabolism · Swimming activity · Caudal aspect ratio · Morphometrics
Published in MEPS Vol.
258
(2003) on August 29
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