Unexpected dependence on pH of NO release from Paracoccus pantotrophus cytochrome cd1.

A previous study of nitrite reduction by Paracoccus pantotrophus cytochrome cd(1) at pH 7.0 identified early reaction intermediates. The c-heme rapidly oxidised and nitrite was reduced to NO at the d(1)-heme. A slower equilibration of electrons followed, forming a stable complex assigned as 55% cFe(III)d(1)Fe(II)-NO and 45% cFe(II)d(1)Fe(II)-NO(+). No catalytically competent NO release was observed. Here we show that at pH 6.0, a significant proportion of the enzyme undergoes turnover and releases NO. An early intermediate, which was previously overlooked, is also identified; enzyme immediately following product release is a candidate. However, even at pH 6.0 a considerable fraction of the enzyme remains bound to NO so another component is required for full product release. The kinetically stable product formed at the end of the reaction differs significantly at pH 6.0 and 7.0, as does its rate of formation; thus the reaction is critically dependent on pH.

Stopped-flow Fourier transform infrared spectroscopy allows continuous monitoring of azide reduction, carbon monoxide inhibition, and ATP hydrolysis by nitrogenase.

Stopped-flow FTIR spectroscopy was used to monitor continuously the pre-steady- and steady-state phases of azide reduction by nitrogenase and the accompanying hydrolysis of ATP. This was characterized by a ca. 1.3 s lag phase that is explained by the number of Fe protein cycles required to effect the reductions of azide to N(2) + NH(3), N(2)H(4) + NH(3), or 3NH(3). Extrapolation of the steady-state time course for azide reduction to zero time showed that one azide binds within 200 ms to each FeMo cofactor. Inhibition of azide reduction by CO was established at times <400 ms, which was faster than the appearance of the first observable IR band assigned to CO (1904 cm(-)(1) detectable at ca. 1 s with maximum amplitude at ca. 7 s). IR bands associated with the rapidly formed (<400 ms) CO species that inhibits azide reduction were not observed over the range 1700-2100 cm(-)(1). This suggests either that the CO is initially bridging two or more Fe atoms or that a rapid reduction of CO to a formyl state occurs by insertion into a metal-hydride bond. The frequencies and time courses for the appearance and loss of the CO bands under hi- and lo-CO conditions were essentially unaffected by the presence of 20 mM azide, consistent with CO being a noncompetitive inhibitor of azide reduction and with azide and CO binding to different sites on the FeMo cofactor.