“…Mounting evidence have verified the involvement of ammonia-oxidizing archaea (AOA) in N 2 O production. , Multiple studies showed that AOA might compete over AOB and became the important N 2 O-producer under specific environmental conditions, particularly such as low-fertility, oxygen-limited and acidic conditions. − The mechanisms for N 2 O production by AOA are still not fully understood. By far, several AOA-driven N 2 O production pathways have been proposed as follows: (1) akin to AOB, the archaeal ammonia monooxygenase (AMO) catalyzes the aerobic oxidation of NH 3 to NH 2 OH, followed by the conversion to N 2 O by putative enzymes in AOA; ,, (2) with HNO working as the intermediate of AMO, N 2 O might be formed by an archaeal putative enzyme such as nitroxyl oxidoreductase (NXOR); , (3) by the aid of nitrite reductase (NIR), NO is produced and may serve as an electron delivery mechanism to assist the activation of AMO and the associated NH 2 OH output for N 2 O production; , (4) through putative nitrifier denitrification pathway, AOA utilize nitrite and nitric oxide as the alternative electron acceptors to produce N 2 O; − and (5) abiotic reactions, in which N 2 O is produced with one N source from NH 4 + and the other one from NO 2 – or NH 2 OH. ,,, Some of the archaeal N 2 O production pathways still need further investigation, since no conclusive homologue or substitute of the key enzymes [e.g., hydroxylamine dehydrogenase (HAO) and nitric reductase (NOR)] involved in N 2 O formation has been found. , …”