Bedded barites from the Barberton greenstone belt (South Africa and Swaziland) preserve a comprehensive record of atmospheric, oceanic and microbial processes involved in the formation and evolution of the Paleoarchean (3.6–3.2 Ga) oceanic sulfate reservoir. Here, we report multiplesulfur isotopic compositions from four of these barite occurrences. Relatively constant mass-independent signatures (Δ36S/Δ33S = − 1.0 ± 0.2) within deposits support an importantrole for atmospheric photolysis in the production of oxidized sulfur, whereas 34S enrichments relative to the inferred composition of photolytic sulfate suggest drawdown of 34S by microbialsulfatereduction. Strong compositional overlap with barites from India and Western Australia indicates the presence of a large-scale and well-mixed marinesulfate pool. Covariation between δ34S and Δ33S within individual deposits also suggests a role for processes occurring in semi-closed basins fed by this global reservoir. Based on modeling results, we interpret variations in δ34S by local microbialsulfatereduction and correlations with Δ33S by weak inputs of sulfur from magmatic sources, microbial sulfide oxidation or sulfur disproportionation. This agrees with the early occurrence of sulfate reducers in the geological record as inferred from published microscopic pyrite data, and identifies their role as important in both global oceans and local basins in the Paleoarchean