Sulfur cycling of intertidal Wadden Sea sediments (Konigshafen, Island of Sylt, Germany): sulfate reduction and sulfur gas emission

Sulfate reduction rates (SRRt) and reduced inorganic sulfur pools (RIS) in Wadden Sea sediment as well as sulfur gas emissions directly to the atmosph ere were measured at intervals of 2 to 12 months from 1991 to 1994. Three s tations were chosen in the intertidal embayment, Konigshafen, representing the: range of sediments found in the Wadden Sea: Organic-poor coarse sand, organic-poor and Arenicola marina inhabited medium sand, and organic-rich m uddy sand. Maximum SRRt were 2 to 5 times higher in muddy sand than in the sandy sediments. The depth-integrated SRRt varied 12 to 13-fold on a season al basis at the three stations. Although temperature controls biochemical p rocesses, the overall control is more complex due to the simultaneous influ ence of other seasonal factors such as availability of organic matter and o xidation level of surface sediment. The sedimentary RIS pools were low due to iron limitation and contained only 30% acid volatile sulfur (AVS). Muddy sand had up to an order of magnitude more RIS than the two sandy sediments . The turnover of RIS was rapid (turnover time from similar to 1 to 32 h), fastest during summer and at the sandy stations. The emission of S-gases wa s dominated by H2S during summer (45-67% of the total), and was highest in muddy and lowest in coarse sand. H2S was less important in early spring (3- 49% of the total). Other sulfur gases, such as COS, DMS and CS2, each accou nted for less than 20% of the total sulfur emissions with no specific tempo ral and spatial pattern. Due to the low content of metals in the sediment, the reduced sulfur pools are cycled rapidly with chemical and biological re oxidation at oxic-anoxic boundaries as a major sink. Thus, the emissions of H2S account for less than 1 parts per thousand of the sulfide produced. (C ) 2000 Elsevier Science B.V, All rights reserved.