Abstract
The ammonia-oxidizing archaea have recently been recognized as a significant component of many microbial communities in the biosphere. Although the overall stoichiometry of archaeal chemoautotrophic growth via ammonia (NH(3)) oxidation to nitrite (NO(2)(-)) is superficially similar to the ammonia-oxidizing bacteria, genome sequence analyses point to a completely unique biochemistry. The only genomic signature linking the bacterial and archaeal biochemistries of NH(3) oxidation is a highly divergent homolog of the ammonia monooxygenase (AMO). Although the presumptive product of the putative AMO is hydroxylamine (NH(2)OH), the absence of genes encoding a recognizable ammonia-oxidizing bacteria-like hydroxylamine oxidoreductase complex necessitates either a novel enzyme for the oxidation of NH(2)OH or an initial oxidation product other than NH(2)OH. We now show through combined physiological and stable isotope tracer analyses that NH(2)OH is both produced and consumed during the oxidation of NH(3) to NO(2)(-) by Nitrosopumilus maritimus, that consumption is coupled to energy conversion, and that NH(2)OH is the most probable product of the archaeal AMO homolog. Thus, despite their deep phylogenetic divergence, initial oxidation of NH(3) by bacteria and archaea appears mechanistically similar. They however diverge biochemically at the point of oxidation of NH(2)OH, the archaea possibly catalyzing NH(2)OH oxidation using a novel enzyme complex.