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Versantvoort, W.

Publications and source records attributed to Versantvoort, W..

2 recordsLinked to original sources

Spectroscopic insights into the mechanism of anammox hydrazine synthase

Anaerobic ammonium oxidizing bacteria make a living oxidizing ammonium with nitrite as electron acceptor, intermediates nitric oxide and hydrazine, and end product dinitrogen gas. Hydrazine is a biologically unique free intermediate in this metabolism, and is produced by the enzyme hydrazine synthase. Crystallization of Candidatus Kuenenia stuttgartiensis hydrazine synthase allowed for an initial hypothesis of its reaction mechanism. In this hypothesis, nitric oxide is first reduced to hydroxylamine after which hydroxylamine is condensed with ammonium to form hydrazine. Hydrazine synthase is a tetraheme cytochrome c, containing two proposed active site hemes ({gamma}I & I) in the {gamma}- and -subunit, respectively, connected by an intra-enzymatic tunnel. Here we combined the data from electrochemistry-induced Fourier transform infrared (FTIR) spectroscopy, EPR and optical spectroscopy to shed light on the redox properties and protein dynamics of hydrazine synthase in the context of its reaction mechanism. Redox titrations revealed two low potential low spin hemes with midpoint potentials of [~]-360 mV and [~]-310 mV for heme II and {gamma}II, respectively. Heme {gamma}I showed redox transitions in the range of 0 mV, consisting of both low spin and high spin characteristics in optical and EPR spectroscopy. Electrochemistry-induced FTIR spectroscopy indicated an aspartic acid ligating a OH-/H2O at the heme {gamma}I axial site as a possible candidate for involvement in this mixed spin characteristic. Furthermore, EPR spectroscopy confirmed the ability of heme {gamma}I to bind NO in the reduced state. Heme I exhibited a rhombic high spin signal, in line with its ligation by a proximal tyrosine observed in the crystal structure. Redox titrations down to -610 mV nor addition of dithionite resulted in the reduction of heme I, indicating a very low midpoint potential for this heme. In vivo chemistry at this heme I, the candidate for the comproportionation of hydroxylamine and ammonium, is thus likely to be initiated solely on the oxidized heme, in contrast to previously reported DFT calculations. The reduction potentials of the {gamma}-subunit hemes were in line with the proposed electron transfer of heme {gamma}II to heme {gamma}I for the reduction of NO to hydroxylamine (E0 = - 30 mV).

biochemistry↗

Methanotrophs are vigorous H2S oxidizers using a sulfide:quinone oxidoreductase and a ba3-type terminal oxidase

Hydrogen sulfide (H2S) is produced in a wide range of anoxic environments where sulfate (SO42-) reduction is coupled to decomposition of organic matter. In the same environments, methane (CH4) is the end product of an anaerobic food chain and both H2S and CH4 diffuse upwards into oxic zones where aerobic microorganisms can utilize these gases. Methane-oxidizing bacteria are known to oxidize a major part of the produced CH4 in these ecosystems, mitigating the emissions of this potent greenhouse gas to the atmosphere. However, how methanotrophy is affected by toxic H2S is largely unexplored. Here, we show that a single microorganism can oxidize CH4 and H2S simultaneously. By oxidizing H2S, the thermoacidophilic methanotroph Methylacidiphilum fumariolicum SolV can alleviate the inhibitory effects on CH4 oxidation. In response to H2S, strain SolV upregulated a type III sulfide:quinone oxidoreductase (SQR) and a sulfide-insensitive ba3-type terminal oxidase to dissipate the reducing equivalents derived from H2S oxidation. Through extensive chemostat cultivation of M. fumariolicum SolV we demonstrate that it converts high loads of H2S to elemental sulfur (S0). Moreover, we show chemolithoautotrophy by tracing 13CO2 fixation into new biomass by using H2S as sole energy source. Molecular surveys revealed several putative SQR sequences in a range of proteobacterial methanotrophs from various environments, suggesting that H2S detoxification is much more widespread in methanotrophs than previously assumed, enabling them to connect carbon and sulfur cycles in new ways.

microbiology↗