In organically enriched sediments of coastal areas, sulfate-reducing bacter
ia decompose organic matter anaerobically, producing high levels of hydroge
n sulfide. Chemoautotrophic sulfur-oxidizing bacteria proliferate at the su
lfide/oxygen interface and use hydrogen sulfide as an electron donor. A few
species of small polychaete worms, including Capitella sp. 1, often domina
te the macrofaunal benthic communities in such sulfide-rich environments in
the organically enriched sediments. In this study, we conducted 2 laborato
ry 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 treatm
ents showed better survival, enhanced growth and reproduction. They had low
er delta C-13 values (-24.3 parts per thousand, mean) than control worms (-
20.1 parts per thousand, mean) and the sediments in which the worms were cu
ltured (-21.4 parts per thousand, mean). The distinctive delta C-13 signatu
re 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 don
e in the same manner as the first, but the carbonate in the water was repla
ced with (CO2)-C-13 in order to trace the autotrophic fixation of carbon di
oxide by chemosynthetic bacteria occurring within the sediments. The result
s indicate that fixation of (CO2)-C-13 was promoted in sediments with Na2S
amendments, and further enhanced by the presence of Capitella sp. 1. The wo
rms in these sediments had extremely high delta C-13 values (+5218.2 parts
per thousand). The results of this study introduce the possibility of enhan
ced survival and growth of Capitella sp. I in sulfide-rich environments in
the organically enriched sediments, facilitated by its utilization of a nov
el source of organic matter.