2026 年 42 巻 1 号 p. 1-16
Quantifying the contribution of primary production by sulfur-oxidizing bacteria (SOB) to benthic food webs is important for understanding energy and material flows in aquatic ecosystems, including chemosynthesis-based ecosystems. Sulfur stable isotope ratios (δ34S) are a powerful tool for assessing sulfide utilization by SOB in sediments. In this review, I introduce the methodological approaches (δ34S-based mixing model) used for estimating the contribution of SOB-derived organic matter to the nutrient resources of benthic fauna, and highlight three case studies that used this method in a deep-sea chemosynthesis-based ecosystem, whale-fall ecosystems, and a freshwater lake ecosystem. Finally, I discuss the advantages and limitations of this method for improving evaluations.