Production of oceanic nitrous oxide by ammonia-oxidizing archaea

Abstract

The recent finding that microbial ammonia oxidation in the ocean is performed by archaea to a greater extent than by bacteria has drastically changed the view on oceanic nitrification. The numerical dominance of archaeal ammonia-oxidizers (AOA) over their bacterial counterparts (AOB) in large parts of the ocean leads to the hypothesis that AOA rather than AOB could be the key organisms for the oceanic production of the strong greenhouse gas nitrous oxide (N₂O) that occurs as a by-product of nitrification. Very recently, enrichment cultures of marine ammonia-oxidizing archaea have been reported to produce N₂O. <br><br> Here, we demonstrate that archaeal ammonia monooxygenase genes (<i>amoA</i>) were detectable throughout the water column of the eastern tropical North Atlantic (ETNA) and eastern tropical South Pacific (ETSP) Oceans. Particularly in the ETNA, comparable patterns of abundance and expression of archaeal <i>amoA</i> genes and N₂O co-occurred in the oxygen minimum, whereas the abundances of bacterial <i>amoA</i> genes were negligible. Moreover, selective inhibition of archaea in seawater incubations from the ETNA decreased the N₂O production significantly. In studies with the only cultivated marine archaeal ammonia-oxidizer <i>Nitrosopumilus maritimus</i> SCM1, we provide the first direct evidence for N₂O production in a pure culture of AOA, excluding the involvement of other microorganisms as possibly present in enrichments. <i>N. maritimus</i> showed high N₂O production rates under low oxygen concentrations comparable to concentrations existing in the oxycline of the ETNA, whereas the N₂O production from two AOB cultures was comparably low under similar conditions. Based on our findings, we hypothesize that the production of N₂O in tropical ocean areas results mainly from archaeal nitrification and will be affected by the predicted decrease in dissolved oxygen in the ocean.