Niche Partitioning of the N Cycling Microbial Community of an Offshore Oxygen Deficient Zone.

Microbial communities in marine oxygen deficient zones (ODZs) are responsible for up to half of marine N loss through conversion of nutrients to NO and N. This N loss is accomplished by a consortium of diverse microbes, many of which remain uncultured. Here, we characterize genes for all steps in the anoxic N cycle in metagenomes from the water column and >30 μm particles from the Eastern Tropical North Pacific (ETNP) ODZ. We use an approach that allows for both phylogenetic identification and semi-quantitative assessment of gene abundances from individual organisms, and place these results in context of chemical measurements and rate data from the same location. Denitrification genes were enriched in >30 μm particles, even in the oxycline, while anammox bacteria were not abundant on particles. Many steps in denitrification were encoded by multiple phylotypes with different distributions. Notably three NO reductases (), each with no cultured relative, inhabited distinct niches; one was free-living, one dominant on particles and one had a C terminal extension found in autotrophic S-oxidizing bacteria. At some depths >30% of the community possessed nitrite reductase . A OTU linked to SAR11 explained much of this abundance. The only bacterial gene found for NO reduction to NO in the ODZ was a form of related to the previously postulated "nitric oxide dismutase," hypothesized to produce N directly while oxidizing methane. However, similar genes are also found in the published genomes of many bacteria that do not oxidize methane, and here the genes did not correlate with the presence of methane oxidation genes. Correlations with NO concentrations indicate that these genes likely facilitate NO reduction to NO in the ODZ. In the oxycline, genes were not detected in the water column, and estimated NO production rates from ammonia oxidation were insufficient to support the observed oxycline NO maximum. However, both and genes were present within particles in the oxycline, suggesting a particulate source of NO and N. Together, our analyses provide a holistic view of the diverse players in the low oxygen nitrogen cycle.