Anaerobic Sulfide Oxidation with Nitrate by a Freshwater Beggiatoa Enrichment Culture

A lithotrophic freshwater Beggiatoa strain was enriched in O₂-H₂S gradient tubes to investigate its ability to oxidize sulfide with NO₃⁻ as an alternative electron acceptor. The gradient tubes contained different NO₃⁻ concentrations, and the chemotactic response of the Beggiatoa mats was observed. The effects of the Beggiatoa sp. on vertical gradients of O₂, H₂S, pH, and NO₃⁻ were determined with microsensors. The more NO₃⁻ that was added to the agar, the deeper the Beggiatoa filaments glided into anoxic agar layers, suggesting that the Beggiatoa sp. used NO₃⁻ to oxidize sulfide at depths below the depth that O₂ penetrated. In the presence of NO₃⁻ Beggiatoa formed thick mats (>8 mm), compared to the thin mats (ca. 0.4 mm) that were formed when no NO₃⁻ was added. These thick mats spatially separated O₂ and sulfide but not NO₃⁻ and sulfide, and therefore NO₃⁻ must have served as the electron acceptor for sulfide oxidation. This interpretation is consistent with a fourfold-lower O₂ flux and a twofold-higher sulfide flux into the NO₃⁻-exposed mats compared to the fluxes for controls without NO₃⁻. Additionally, a pronounced pH maximum was observed within the Beggiatoa mat; such a pH maximum is known to occur when sulfide is oxidized to S⁰ with NO₃⁻ as the electron acceptor.