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8 pages, 2 figures, 4 tablesThe present study assesses the contribution of dark carbon fixation to the primary production in the oxic/anoxic interface of a shallow estuarine environment that develops a salt-water wedge with the presence of sulfide. Primary production was partitioned into oxygenic photosynthesis, anoxygenic photosynthesis and dark fixation. The results show the importance of dark fixation in the oxic/anoxic interface with values higher than 5 mg carbon fixed per cubic meter and per hour in some cases. The average rate of primary production in the dark during the anoxic season for the Ebro River salt wedge resulted in 42 mg C m-2 d-1 in the interface. This represents at least twice the contribution of oxygenic photosynthesis to the primary production in such interface. Because this process is probably important in other salt-wedge or highly stratified estuaries with oxic/anoxic interfaces containing sulfide, the estimates of carbon fixation made so far for these systems may have been underestimated, and should therefore be revised taking into account the contribution of dark processes.This work was financed by DGICyT grant PB87-0183 from the Spanish Ministerio de Educación y Ciencia. J.G.-C. was supported by a FPI scholarship from the Spanish Ministerio de Educación y Ciencia. During the writing of this work, E.O.C. was supported by MIDAS (MIcrobial Diversity in Aquatic Systems, MAS3-CT97-0154) from the European Union.Peer reviewe

Primary production in estuarine oxic/anoxic interfaces: contribution of microbial dark CO2 fixation in the Ebro River Salt Wedge Estuary