Nitrite (NO
2
–
) is a central intermediate for various metabolic pathways within the biogeochemical nitrogen cycle. In dissimilatory nitrate ammonification, NO
2
–
is reduced to ammonia in a remarkable six‐electron reaction, catalyzed by the multiheme enzyme cytochrome
c
NO
2
–
reductase. The protein is a homodimer with a monomer mass of 58 kDa and five covalently attached heme cofactors, one of which features a free coordination site at the distal axial position of its central iron atom and an unusual and unique lysine ligand on the opposing, proximal axial position. The substrate NO
2
−
binds to this iron atom through the free electron pair on the nitrogen atom and is then reduced consecutively to ammonia, without any detectable release of reaction intermediates or by‐products. In the bacterial cell, many NO
2
−
reductases form a membrane‐associated complex with a small protein, NrfH, which is able to couple the oxidation of menaquinone from within the membrane to electron transfer to the catalytically active NO
2
−
reductase. A proton gradient is generated in a Q‐loop mechanism on NrfH, making NO
2
−
reduction an effective energy metabolism in anaerobic environments.