Abstract

Abstract Benthic fauna assemblages and organic carbon mineralization processes were studied in the northwestern Black Sea along a transect from the well-oxygenated shelf to the (deep) anoxic basin. Bivalves dominated the coenoses at the three oxygenated stations, but with decreasing macrofaunal biomass at increasing water depth. The previously well-described zonation of macrofaunal communities for the northwestern shelf of the Black Sea was also found in this study (Mytilus galloprovincialis coenosis at Station 1 (62 m), Modiolus phaseolinus coenosis at Station 2 (77 m) and 3 (100 m)). The highest meiofauna density was found at the transition from oxic to anoxic bottom waters (Station 4, 130 m, < 5 μM O2). Reduced predation and sufficient food supply are suggested to be of importance at that site. The weight-specific fauna-mediated respiration rate of the mussel community was independent of water depth and always around 14 nmol O2 mg ww-1 d-1. Thus indicating that the mussel communities on the northwester...

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