Oxygen production as an electron overflow pathway in ammonia-oxidizing archaea

Abstract Ammonia-oxidizing archaea (AOA) are widespread in nature and contribute to global carbon and nitrogen cycling. Although their energy production is an aerobic process, AOA occur in environments of low oxygen and in fully anoxic zones. Recently, oxygen production under anoxic conditions was demonstrated, raising the hypothesis that this activity can sustain oxygen dependent ammonia oxidation. In the work presented here, Nitrososphaera viennensis produces high amounts of oxygen in anoxia in dependence of nitrite but not ammonia. Rather than conferring a physiological benefit, oxygen production impaired recovery from anoxia. Produced oxygen is mostly not consumed and therefore cannot sustain ammonia oxidation in the absence of external oxygen. Instead, it is tightly linked to the amount of available redox equivalents. These observations indicate that oxygen production represents a general physiological strategy for alleviating the potential accumulation of reactive intermediates in the ammonia oxidation pathway, analogous to nitrifier denitrification in ammonia-oxidizing bacteria. Teaser Oxygen production in ammonia-oxidizing archaea is not an adaptation to anoxia, but rather an electron overflow pathway that is detectable in anoxic conditions.