Sulfur, carbon, and nitrogen stable isotope ratios in soft tissues and trophic relationships of fish from the near-shore waters of the peter the great bay in the Sea of Japan
S. I. Kiyashko, T. A. Velivetskaya, A. V. Ignatiev
Abstract
S. I. Kiyashko, T. A. Velivetskaya, A. V. Ignatiev
Abstract
Stable isotope ratios of sulfur ( 34 S/ 32 S), carbon ( 13 C/ 12 C), and nitrogen ( 15 N/ 14 N) were analyzed in the soft tissues of 12 common species of fish from the near-shore waters of the Peter the Great Bay in the Sea of Japan. The average δ 13 C values of individual species varied from −20.7‰ for planktivorous fish to −16.8‰ for benthivorous fish, reflecting the growing relative contribution of benthic primary producers to fish nutrition. The majority of the various species representatives studied can be assigned to one trophic level, as indicated by their narrow range of δ 15 N values (9.9 to 12.6‰). Large interspecific variations were found in the sulfur stable isotope ratios of fish (the mean δ 34 S values ranged from 11.2 to 19.5‰). This is the result of the different contributions to fish nutrition of infaunal invertebrates that are depleted in 34 S due to the microbial food chain of the bottom sediments.
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Stable isotope ratios of sulfur ( 34 S/ 32 S), carbon ( 13 C/ 12 C), and nitrogen ( 15 N/ 14 N) were analyzed in the soft tissues of 12 common species of fish from the near-shore waters of the Peter the Great Bay in the Sea of Japan. The average δ 13 C values of individual species varied from −20.7‰ for planktivorous fish to −16.8‰ for benthivorous fish, reflecting the growing relative contribution of benthic primary producers to fish nutrition. The majority of the various species representatives studied can be assigned to one trophic level, as indicated by their narrow range of δ 15 N values (9.9 to 12.6‰). Large interspecific variations were found in the sulfur stable isotope ratios of fish (the mean δ 34 S values ranged from 11.2 to 19.5‰). This is the result of the different contributions to fish nutrition of infaunal invertebrates that are depleted in 34 S due to the microbial food chain of the bottom sediments.
Key concepts: δ34S, Trophic level, δ15N, δ13C, Benthic zone, Bay, Sulfur, Stable isotope ratio