Pathways of N 2 O production by marine ammonia-oxidizing archaea determined from dual-isotope labeling.

The ocean is a net source of the greenhouse gas and ozone-depleting substance, nitrous oxide (N 2 O), to the atmosphere. Most of that N 2 O is produced as a trace side product during ammonia oxidation, primarily by ammonia-oxidizing archaea (AOA), which numerically dominate the ammonia-oxidizing community in most marine environments. The pathways to N 2 O production and their kinetics, however, are not completely understood. Here, we use 15 N and 18 O isotopes to determine the kinetics of N 2 O production and trace the source of nitrogen (N) and oxygen (O) atoms in N 2 O produced by a model marine AOA species, Nitrosopumilus maritimus . We find that during ammonia oxidation, the apparent half saturation constants of nitrite and N 2 O production are comparable, suggesting that both processes are enzymatically controlled and tightly coupled at low ammonia concentrations. The constituent atoms in N 2 O are derived from ammonia, nitrite, O 2 , and H 2 O via multiple pathways. Ammonia is the primary source of N atoms in N 2 O, but its contribution varies with ammonia to nitrite ratio. The ratio of 45 N 2 O to 46 N 2 O (i.e., single or double labeled N) varies with substrate ratio, leading to widely varying isotopic signatures in the N 2 O pool. O 2 is the primary source for O atoms. In addition to the previously demonstrated hybrid formation pathway, we found a substantial contribution by hydroxylamine oxidation, while nitrite reduction is an insignificant source of N 2 O. Our study highlights the power of dual 15 N- 18 O isotope labeling to disentangle N 2 O production pathways in microbes, with implications for interpretation of pathways and regulation of marine N 2 O sources.