Reduction of Ferric Iron in Anaerobic, Marine Sediment and Interaction with Reduction of Nitrate and Sulfate

Studies were carried out to elucidate the nature and importance of Fe³⁺ reduction in anaerobic slurries of marine surface sediment. A constant accumulation of Fe²⁺ took place immediately after the endogenous NO₃⁻ was depleted. Pasteurized controls showed no activity of Fe³⁺ reduction. Additions of 0.2 mM NO₃⁻ and NO₂⁻ to the active slurries arrested the Fe³⁺ reduction, and the process was resumed only after a depletion of the added compounds. Extended, initial aeration of the sediment did not affect the capacity for reduction of NO₃⁻ and Fe³⁺, but the treatments with NO₃⁻ increased the capacity for Fe³⁺ reduction. Addition of 20 mM MoO₄²⁻ completely inhibited the SO₄²⁻ reduction, but did not affect the reduction of Fe³⁺. The process of Fe³⁺ reduction was most likely associated with the activity of facultative anaerobic, NO₃⁻-reducing bacteria. In surface sediment, the bulk of the Fe³⁺ reduction may be microbial, and the process may be important for mineralization in situ if the availability of NO₃⁻ is low.