Hydrazine Oxidoreductase Research Articles

Evolution of an octahaem cytochrome c protein family that is key to aerobic and anaerobic ammonia oxidation by bacteria

The biogeochemical nitrogen cycle is mediated by many groups of microorganisms that harbour octahaem cytochromes c (OCC). In this study molecular evolutionary analyses and the conservation of predicted functional residues and secondary structure were employed to investigate the descent of OCC proteins related to hydroxylamine oxidoreductase (HAO) and hydrazine oxidoreductase (HZO) from pentahaem cytochrome c nitrite reductase (NrfA). An octahaem cytochrome cnitrite reductase (ONR) was shown to be a possible intermediate in the process. Analysis of genomic neighbourhoods of OCC protein-encoding genes revealed adjacent conserved genes whose products, together with HAO, provide a path of electron transfer to quinone and constitute a functional catabolic module. The latter has evolved more than once under a variety of functional pressures on the catabolic lifestyles of their bacterial hosts. Structurally, the archetypical long helices in the large C-terminal domain of the proteins as well as the distal axial ligands to most haems were highly conserved in NrfA and all descendents. Residues known to be involved in the nitrite reductase activity of NrfA including the 'CxxCK' motif at the catalytic haem, the substrate and Ca binding sites, and the nitrite and ammonium channels were conserved in the eight representatives of ONR. In the latter, a unique cysteine has been inserted above the active site. The 64 other OCC proteins differed from ONR by the absence of the 'CxxCK' motif, the channel residues and most of the Ca-binding residues and the conserved presence of an 'Asp-His' pair inserted above the active site as well as the tyrosine that forms an intersubunit cross-link to the catalytic haem of HAO. Our proposed scenario of evolution of OCC proteins in the HAO family from NrfA is supported by (i) homology based on sequence and structure, (ii) its wide distribution among bacterial taxa, (iii) the dedicated interaction with specific proteins, and it is (iv) congruent with geological history.

Global impact and application of the anaerobic ammonium-oxidizing (anammox) bacteria

In the anaerobic ammonium oxidation (anammox) process, ammonia is oxidized with nitrite as primary electron acceptor under strictly anoxic conditions. The reaction is catalysed by a specialized group of planctomycete-like bacteria. These anammox bacteria use a complex reaction mechanism involving hydrazine as an intermediate. The reactions are assumed to be carried out in a unique prokaryotic organelle, the anammoxosome. This organelle is surrounded by ladderane lipids, which make the organelle nearly impermeable to hydrazine and protons. The localization of the major anammox protein, hydrazine oxidoreductase, was determined via immunogold labelling to be inside the anammoxosome. The anammox bacteria have been detected in many marine and freshwater ecosystems and were estimated to contribute up to 50% of oceanic nitrogen loss. Furthermore, the anammox process is currently implemented in water treatment for the low-cost removal of ammonia from high-strength waste streams. Recent findings suggested that the anammox bacteria may also use organic acids to convert nitrate and nitrite into dinitrogen gas when ammonia is in short supply.

1994–2004: 10 years of research on the anaerobic oxidation of ammonium

The obligately anaerobic ammonium oxidation (anammox) reaction with nitrite as primary electron acceptor is catalysed by the planctomycete-like bacteria Brocadia anammoxidans, Kuenenia stuttgartiensis and Scalindua sorokinii. The anammox bacteria use a complex reaction mechanism involving hydrazine as an intermediate. They have a unique prokaryotic organelle, the anammoxosome, surrounded by ladderane lipids, which exclusively contains the hydrazine oxidoreductase as the major protein to combine nitrite and ammonia in a one-to-one fashion. In addition to the peculiar microbiology, anammox was shown to be very important in the oceanic nitrogen cycle, and proved to be a very good alternative for treatment of high-strength nitrogenous waste streams. With the assembly of the K. stuttgartiensis genome at Genoscope, Evry, France, the anammox reaction has entered the genomic and proteomic era, enabling the elucidation of many intriguing aspects of this fascinating microbial process.