Denitrification byAnaeromyxobacter dehalogenans, a Common Soil Bacterium Lacking the Nitrite Reductase GenesnirSandnirK
ABSTRACTThe versatile soil bacteriumAnaeromyxobacter dehalogenanslacks the hallmark denitrification genesnirSandnirK(encoding NO2−→NO reductases) and couples growth to NO3−reduction to NH4+(respiratory ammonification) and to N2O reduction to N2.A. dehalogenansalso grows by reducing Fe(III) to Fe(II), which chemically reacts with NO2−to form N2O (i.e., chemodenitrification). Following the addition of 100 μmol of NO3−or NO2−to Fe(III)-grown axenic cultures ofA. dehalogenans, 54 (±7) μmol and 113 (±2) μmol N2O-N, respectively, were produced and subsequently consumed. The conversion of NO3−to N2in the presence of Fe(II) through linked biotic-abiotic reactions represents an unrecognized ecophysiology ofA. dehalogenans. The new findings demonstrate that the assessment of gene content alone is insufficient to predict microbial denitrification potential and N loss (i.e., the formation of gaseous N products). A survey of complete bacterial genomes in the NCBI Reference Sequence database coupled with available physiological information revealed that organisms lackingnirSornirKbut with Fe(III) reduction potential and genes for NO3−and N2O reduction are not rare, indicating that NO3−reduction to N2through linked biotic-abiotic reactions is not limited toA. dehalogenans. Considering the ubiquity of iron in soils and sediments and the broad distribution of dissimilatory Fe(III) and NO3−reducers, denitrification independent of NO-forming NO2−reductases (through combined biotic-abiotic reactions) may have substantial contributions to N loss and N2O flux.IMPORTANCECurrent attempts to gauge N loss from soils rely on the quantitative measurement ofnirKandnirSgenes and/or transcripts. In the presence of iron, the common soil bacteriumAnaeromyxobacter dehalogenansis capable of denitrification and the production of N2without the key denitrification genesnirKandnirS. Such chemodenitrifiers denitrify through combined biotic and abiotic reactions and have potentially large contributions to N loss to the atmosphere and fill a heretofore unrecognized ecological niche in soil ecosystems. The findings emphasize that the comprehensive understanding of N flux and the accurate assessment of denitrification potential can be achieved only when integrated studies of interlinked biogeochemical cycles are performed.