We measured surface 0, uptake, 35S0.,2-reduction, and total sediment metabolism (CO, production) in sediments (O-30 cm) supporting stands of short Spartina alterniflora in a New England salt marsh. Sediment CO, production was highest at the surface where 0, was present and declined rapidly with depth. In deeper sediments (below 5 cm) CO, production was equal to 35S0,2-reduction as determined by the Cr2+ reduction technique. Time-course experiments using CO, production and 35S04?-reduction (by Cr2+ reduction and aqua regia digest) indicate that the aqua regia technique is not reliable for measuring SOd2-reduction and that the rate ofSOd2-reduction is much less than previously reported for this marsh.Our estimates of annual 0, uptake conform with those for CO, production and belowground production. We estimate carbon mineralization to average about 180 mmol C.m-2.d-1, among the highest measured for marine sediments. Our simultaneous measurements of 0, uptake, CO2 production, and SOd2-reduction suggest that at least half of this decomposition occurs via SOd2-reduction. We conclude that the mechanisms underlying carbon and sulfur cycling in salt marsh sediments are much more similar to subtidal sediments than previously recognized.