Denitrification by Anaeromyxobacter dehalogenans, a Common Soil Bacterium Lacking Nitrite Reductase Genes (nirS/nirK).

ABSTRACT: The versatile soil bacterium Anaeromyxobacter dehalogenans lacks the hallmark denitrification genes nirS and nirK (NO2-?NO), and couples growth to NO3- reduction to NH4+ (respiratory ammonification) and to N2O reduction to N2A. dehalogenans also grows by reducing Fe(III) to Fe(II), which chemically reacts with NO2- to form N2O (i.e., chemodenitrification). Following the addition of 100 ?moles of NO3- or NO2- to Fe(III)-grown, axenic cultures of A. dehalogenans, 54 (±7) ?moles and 113 (±2) ?moles N2O-N, respectively, were produced and subsequently consumed. The conversion of NO3- to N2 in the presence of Fe(II) through linked biotic-abiotic reactions represents an unrecognized ecophysiology of A. 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 lacking nirS/nirK but with Fe(III) reduction potential and genes for NO3- and N2O reduction are not rare, indicating that NO3- reduction to N2 through linked biotic-abiotic reactions is not limited to A. 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.Importance Current attempts to gauge N loss from soils rely on the quantitative measurement of nirK and nirS genes and/or transcripts. In the presence of iron, the common soil bacterium Anaeromyxobacter dehalogenans is capable of denitrification and producing N2 without the key denitrification genes nirK/nirS 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 comprehensive understanding of N flux and accurate assessment of denitrification potential can only be achieved when integrated studies of interlinked biogeochemical cycles are performed.

SUBMITTER: Onley JR 

PROVIDER: S-EPMC5795083 | biostudies-other | 2017 Dec

REPOSITORIES: biostudies-other