The kinetic and isotopic competence of nitric oxide as an intermediate in denitrification

• Published in: The Journal of biological chemistry 1990-01, Vol.265 (2), p.889-895
• Main Authors: GORETSKI, J, HOLLOCHER, T. C
• Format: Article
• Language: English
• Subjects: Analytical, structural and metabolic biochemistry; Bacteria - metabolism; Biological and medical sciences; Chromatography, Gas; Electrochemistry; Fundamental and applied biological sciences. Psychology; Intermediary metabolites. Miscellaneous; Kinetics; Nitrates - metabolism; Nitric Oxide - metabolism; Nitrogen Isotopes; Other biological molecules; Oxidation-Reduction
• ISSN: 0021-9258; 1083-351X
• DOI: 10.1016/S0021-9258(19)40133-6

Rates of NO uptake by five denitrifying bacteria were estimated by NO-electrode and gas chromatography methods under conditions of rather low cell densities and [NOaq]. The rates so measured, VmaxNO, represent lower limits for the true value of that parameter, but nevertheless exceed Vmax for nitrite uptake, VmaxNi, by a factor of two typically. Previous estimates under suboptimal conditions had placed VmaxNO at 0.3-0.5 of VmaxNi (St. John, R. T., and Hollocher, T. C. (1977) J. Biol. Chem. 252, 212-218; Garber, E. A. E., and Hollocher, T.C. (1981) J. Biol. Chem. 256, 5459-5465). The steady-state [NOaq] during denitrification of nitrite by nitrate-grown cells was less than or equal to 1 microM. The above observations, taken with a recent direct estimate for the KmNO for NO uptake of 0.4 microM (Zafiriou, O. C., Hanley, Q. S., and Snyder, G. (1989) J. Biol. Chem. 264, 5694-5699), would allow NO to be a free intermediate between nitrite and N2O with steady-state concentrations of less than or equal to 0.4 microM. As the result of special conditions during cell growth or differential inhibition by azide, it was possible to establish systems that accumulated NO during denitrification of nitrite. In all such cases, VmaxNO less than VmaxNi, and the time required to reach the maximum [NOaq] corresponded closely to the time needed to exhaust the nitrite. A semiquantitative isotope experiment with Paracoccus denitrificans demonstrated the trapping of 15NO from 15NO2- in a pool of NOaq. A quantitative isotope method using low densities of the same bacterium showed that 15N from 15NO2- and 14N from NOg combine randomly to form N2O during the simultaneous denitrification of 15NO2- and NO. The result requires that the pathways from nitrite and NO share a common mononitrogen intermediate. Results to the contrary obtained at high cell densities (first two references cited above) are now believed to have been due to technical artifacts. The present results are consistent with the view that NO is under kinetic control as a free intermediate in denitrification and serve to remove previously imagined constraints on this view.