Competition between Fe(III)-Reducing and Methanogenic Bacteria for Acetate in Iron-Rich Freshwater Sediments

The kinetics of acetate uptake and the depth distribution of 2-¹⁴C]acetate metabolism were examined in iron-rich sediments from a beaver impoundment in northcentral Alabama. The half-saturation constant (K_m) determined for acetate uptake in slurries of Fe(III)-reducing sediment (0.8 µM) was more than 10-fold lower than that measured in methanogenic slurries (12 µM) which supported comparable rates of bulk organic carbon metabolism and V_max values for acetate uptake. The endogenous acetate concentration (S _n) was also substantially lower (1.7 µM) in Fe(III)-reducing vs methanogenic (9.0 µM) slurries. The proportion of 2-¹⁴C]acetate converted to ¹⁴CH₄ increased with depth from ca 0.1 in the upper 0.5 cm to ca 0.8 below 2 cm and was inversely correlated (r² = 0.99) to a decline in amorphous Fe(III) oxide concentration. The results of the acetate uptake kinetics experiments suggest that differences in the affinity of Fe(III)-reducing bacteria vs methanogens for acetate can account for the preferential conversion of 2-¹⁴C]acetate to ¹⁴CO₂ in Fe(III) oxide-rich surface sediments, and that the downcore increase in conversion of 2-¹⁴C]acetate to ¹⁴CH₄ can be attributed to progressive liberation of methanogens from competition with Fe(III) reducers as Fe(III) oxides are depleted with depth.