Characterization of the nitric oxide reductase from Thermus thermophilus

Nitrous oxide (N₂O) is a powerful greenhouse gas implicated in climate change. The dominant source of atmospheric N₂O is incomplete biological dentrification, and the enzymes responsible for the release of N ₂O are NO reductases. It was recently reported that ambient emissions of N₂O from the Great Boiling Spring in the United States Great Basin are high, and attributed to incomplete denitrification by Thermus thermophilus and related bacterial species [Hedlund BP, et al. (2011) Geobiology 9(6)471-480]. In the present work, we have isolated and characterized the NO reductase (NOR) from T. thermophilus. The enzyme is a member of the cNOR family of enzymes and belongs to a phylogenetic clade that is distinct from previously examined cNORs. Like other characterized cNORs, the T. thermophilus cNOR consists of two subunits, NorB and NorC, and contains a one heme c, one Ca ²⁺, a low-spin heme b, and an active site consisting of a high-spin heme b and FeB. The roles of conserved residues within the cNOR family were investigated by site-directed mutagenesis. The most important and unexpected result is that the glutamic acid ligand to FeB is not essential for function. The E211A mutant retains 68% of wild-type activity. Mutagenesis data and the pattern of conserved residues suggest that there is probably not a single pathway for proton delivery from the periplasm to the active site that is shared by all cNORs, and that there may be multiple pathways within the T. thermophilus cNOR.