MEPS 216:119-127 (2001)  -  doi:10.3354/meps216119

ABSTRACT: In organically enriched sediments of coastal areas, sulfate-reducing bacteria decompose organic matter anaerobically, producing high levels of hydrogen sulfide. Chemoautotrophic sulfur-oxidizing bacteria proliferate at the sulfide/oxygen interface and use hydrogen sulfide as an electron donor. A few species of small polychaete worms, including Capitella sp. I, often dominate the macrofaunal benthic communities in such sulfide-rich environments in the organically enriched sediments. In this study, we conducted 2 laboratory experiments to determine whether Capitella sp. I can benefit trophically through the exploitation of the organic matter chemosynthetically produced by sulfur-oxidizing bacteria. In the first experiment, we reared juveniles of Capitella sp. I with natural sediment of very low organic content, with no additional organic matter, under dark conditions, and exposed them to 3 different levels of sodium sulfide. The worms reared in the sulfide treatments showed better survival, enhanced growth and reproduction. They had lower δ¹³C values (-24.3”, mean) than control worms (-20.1”, mean) and the sediments in which the worms were cultured (-21.4”, mean). The distinctive δ¹³C signature of the worms in the sulfide treatments indicates that they did not share the same carbon source as the control worms. The second experiment was done in the same manner as the first, but the carbonate in the water was replaced with ¹³CO₂ in order to trace the autotrophic fixation of carbon dioxide by chemosynthetic bacteria occurring within the sediments. The results indicate that fixation of ¹³CO₂ was promoted in sediments with Na₂S amendments, and further enhanced by the presence of Capitella sp. I. The worms in these sediments had extremely high δ¹³C values (+5218.2”). The results of this study introduce the possibility of enhanced survival and growth of Capitella sp. I in sulfide-rich environments in the organically enriched sediments, facilitated by its utilization of a novel source of organic matter.

KEY WORDS: Capitella · Chemoautotrophic bacteria · Stable isotope · Organic enrichment · ¹³C · ¹⁵N