Proton translocation during denitrification by a nitrifying--denitrifying Alcaligenes sp

Bioenergetic examination of the heterotrophic nitrifier-denitrifier Thiosphaera pantotropha

The heterotrophic nitrifying-denitrifying bacterium Thiosphaera pantotropha is remarkable as it nitrifies and denitrifies simultaneously. With respect to nitrogenous compounds, whether nitrification or denitrification results in energy conservation is of interest. Proton translocation studies were performed to determine if energy was conserved by the bacterium during heterotrophic nitrification and denitrification. Hydrazine (N2H5+) was employed as the heterotrophic nitrification substrate while nitrate, nitrite and nitrous oxide were used as denitrification substrates. Analysis of the data indicate that the bacterium does not conserve energy when hydrazine was the substrate. Conversely, energy was conserved when either nitrate, nitrite or nitrous oxide functioned as the oxidants during denitrification-dependent proton translocation experiments. Thiosphaera pantotropha thus is similar to other heterotrophic nitrifiers-denitrifiers in that it conserves energy while denitrifying but has not been observed to do so when heterotrophically nitrifying.

Respiration-linked proton translocation coupled to anaerobic reduction of manganese(IV) and iron(III) in Shewanella putrefaciens MR-1

An oxidant pulse technique, with lactate as the electron donor, was used to study respiration-linked proton translocation in the manganese- and iron-reducing bacterium Shewanella putrefaciens MR-1. Cells grown anaerobically with fumarate or nitrate as the electron acceptor translocated protons in response to manganese (IV), fumarate, or oxygen. Cells grown anaerobically with fumarate also translocated protons in response to iron(III) and thiosulfate, whereas those grown with nitrate did not. Aerobically grown cells translocated protons only in response to oxygen. Proton translocation with all electron acceptors was abolished in the presence of the protonophore carbonyl cyanide m-chlorophenylhydrazone (20 microM) and was partially to completely inhibited by the electron transport inhibitor 2-n-heptyl-4-hydroxyquinoline N-oxide (50 microM).

Pathway of oxidation of pyruvic oxime by a heterotrophic nitrifier of the genus Alcaligenes: evidence against nitroethane as an intermediate

The role of nitroethane as an intermediate in the oxidation of pyruvic oxime to nitrate by an Alcaligenes sp. was examined. Unlike pyruvic oxime, which serves as a sole source of C and N for the bacterium, nitroethane was incapable of supporting the growth of the microbe. Nitroethane was metabolized and diauxic growth did occur, however, if the nitroethane medium was amended with yeast extract. Alcaligenes sp. resting cells and cell-free extracts were prepared from nitroethane-yeast extract grown cultures and the maximum rate of nitrite synthesis when nitroethane was the substrate was 6.8 nmol min-1 mg cell protein-1, a 10-fold lower rate than that previously noted for pyruvic oxime oxidation. These cell-free extracts were unable to metabolize pyruvic oxime. Resting cells and cell-free extracts prepared from Alcaligenes sp. cells grown in a pyruvic oxime medium were, conversely, incapable of metabolizing nitroethane. Collectively, these results indicate that nitroethane is not an intermediate in the pathway of pyruvic oxime oxidation and that two separate enzyme systems exist in the Alcaligenes sp. for the metabolism of pyruvic oxime and nitroethane.

Iron respiration-driven proton translocation in aerobic bacteria

Washed cell suspensions of Aquaspirillum magnetotacticum MS-1, A. itersonii E12639, Bacillus subtilis 6633, and Escherichia coli CSH27 translocated protons in response to the added oxidant O2 or NO3-, with triphenylmethylphosphonium bromide as the permeant ion. Iron respiration-driven proton translocation was observed in A. magnetotacticum MS-1, B. subtilis, and E. coli but not in a nonmagnetic strain of A. magnetotacticum (strain NM-1A) or with A. itersonii. Proton translocation to Fe3+ was totally inhibited by 500 microM NaN3 or 0.5 microM carbonyl cyanide m-chlorophenylhydrazone.

Respiration-linked proton flux in Wolinella succinogenes during reduction of N-oxides

Formate uncoupled proton translocation in formate-grown Wolinella succinogenes cells supplied with N-oxides as terminal electron acceptors. In suspensions containing KSCN (but not valinomycin), H2 supported proton translocation when NO3-, NO2-, and NO were provided as oxidants. H+/N-oxide ratios were 4.77 for NO3-, 2.49 for NO2-, and 1.75 for NO. KSCN inhibits N2O reduction thus precluding use of N2O as oxidant. Repeated exposure of cells to NO inhibited their ability to translocated protons with NO as oxidant but only slightly diminished and did not eliminate their capacity for NO3(-)- or NO2(-)-dependent proton flux. Substituting reduced benzyl viologen for H2 and measuring proton uptake provided results consistent with an extramembranal location for the N- oxide reductases. The uncoupler, carbonyl cyanide m-chlorophenylhydrazone, collapsed proton gradients, permitted uptake of 2 mol H+/mol NO3- or NO2-, but unaccountably inhibited NO3- reduction by 50% while leaving H+ uptake stoichiometry of the cells unaffected.

Source of the oxygen atoms of nitrate in the oxidation of nitrite by Nitrobacter agilis and evidence against a P-O-N anhydride mechanism in oxidative phosphorylation

15N, 18O Tracer studies were applied to the aerobic oxidation of nitrite to nitrate by the chemolithotrophic bacterium, Nitrobacter agilis. It was established that, in conversion of nitrite to nitrate, one oxygen atom of nitrate arose from water and none from O2 or inorganic phosphate. This result confirms that of Kumar et al. [(1983) FEBS Lett. 152, 71-74]. Oxygen exchange between water and inorganic phosphate was small and that between water and nitrite or nitrate or any reaction intermediates between these two was not detected. Oxidation of nitrite was, therefore, effectively irreversible under the conditions employed. The uptake of extracellular phosphate was sufficient to allow significant transfer of 18O from phosphate to nitrate if oxidative phosphorylation had occurred by way of a P-O-N anhydride between phosphate (or ADP) and nitrate. The results are, therefore, inconsistent with the occurrence of a reaction of this type during nitrite oxidation.