Otolith carbon isotope δ 13 C values may provide temporally resolved diet proxies in fish. If otolith δ 13 C values reflect diet, isotope values from recent otolith and muscle tissue should correlate and known ontogenetic diet shifts should be reflected in comparisons between otolith material deposited during different life history stages. We analyzed paired otolith and muscle samples for δ 13 C from black rockfish Sebastes melanops to examine the potential of otoliths to reflect diet in small

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... 200−299 mm fork length) and large (≥300 mm) fish. We found a significant positive regression between δ 13 C values from recent (~12 mo) otolith material and muscle in large fish, but not in small fish. Within individual otoliths, δ 13 C values were enriched by ~3 ‰ in recent otolith edge material compared to age-0 otolith core material and were consistent with known nearshore−offshore gradients in δ 13 C values at the base of the food web. Bulk otolith δ 13 C appeared to provide a broad indicator of dietary carbon sources, but variation in metabolism and dissolved inorganic carbon δ 13 C among and within individuals likely influences otolith δ 13 C as well and limits precision. Nevertheless, the results are promising and bulk otolith δ 13 C may be an appropriate tool to examine large trophic and ecosystem level shifts that have occurred concurrently with changes in habitat, commercial fishing, invasive species, climate change, and other direct or indirect human impacts using historic or ancient otoliths. Future studies should continue to consider the utility of bulk otolith δ 13 C to describe diet in other marine fish using this simple approach.