Aspects of nitrogen fixation and denitrification byAzospirillum

Summary Model experiments were performed to investigate the nitrogen fixation (C₂H₂ reduction) and denitrification (N₂O formation) capabilities ofAzospirillum spp. in association with wheat. Plants and bacteria were grown together for a week and then assayed for activities. This association performed C₂H₂ reduction or N₂O formation, depending on the concentrations of nitrate and oxygen in the vessels. Both activities depended on theAzospirillum strains used. The newly isolatedAzospirillum amazonense strains Y1 and Y6 showed significant C₂H₂ reduction and low N₂O formation in association with wheat under the conditions employed and are possibly useful in practice. A cell-free preparation fromAzospirillum brasilense Sp 7 possessed a cytochrome cd type dissimilatory nitrite reductase.     

Denitrification by Actinomycetes and Purification of Dissimilatory Nitrite Reductase and Azurin from Streptomyces thioluteus

Many actinomycete strains are able to convert nitrate or nitrite to nitrous oxide (N₂O). As a representative of actinomycete denitrification systems, the system of Streptomyces thioluteus was investigated in detail. S. thioluteus attained distinct cell growth upon anaerobic incubation with nitrate or nitrite with concomitant and stoichiometric conversion of nitrate or nitrite to N₂O, suggesting that the denitrification acts as anaerobic respiration. Furthermore, a copper-containing, dissimilatory nitrite reductase (CuNir) and its physiological electron donor, azurin, were isolated. This is the first report to show that denitrification generally occurs among actinomycetes.     

A heme-C-containing enzyme complex that exhibits nitrate and nitrite reductase activity from the dissimilatory iron-reducing bacterium Geobacter metallireducens

Nitrate reduction in the dissimilatory iron-reducing bacterium Geobacter metallireducens was investigated. Nitrate reductase and nitrite reductase activities in nitrate-grown cells were detected only in the membrane fraction. The apparent K _m values for nitrate and nitrite were determined to be 32 and 10 μM, respectively. Growth on nitrate was not inhibited by either tungstate or molybdate at concentrations of 1 mM or less, but was inhibited by both at 10 and 20 mM. Nitrate and nitrite reductase activity in the membrane fraction was not, however, affected by dialysis with 20 mM tungstate. An enzyme complex that exhibited both nitrate and nitrite reductase activity was solubilized from membrane fractions with CHAPS and was partially purified by preparative gel electrophoresis. It was found to be composed of four different polypeptides with molecular masses of 62, 52, 36, and 16 kDa. The 62-kDa polypeptide [a low-midpoint potential (–207 mV), multiheme cytochrome c] exhibited nitrite reductase activity under denaturing conditions. No molybdenum was detected in the complex by plasma-emission mass spectrometry. Received: 26 March 1999 / Accepted: 16 August 1999     

Dissimilatory nitrate reduction by Propionibacterium acnes.

Propionibacterium acnes P13 was isolated from human feces. The bacterium produced a particulate nitrate reductase and a soluble nitrite reductase when grown with nitrate or nitrite. Reduced viologen dyes were the preferred electron donors for both enzymes. Nitrous oxide reductase was never detected. Specific growth rates were increased by nitrate during growth in batch culture. Culture pH strongly influenced the products of dissimilatory nitrate reduction. Nitrate was principally converted to nitrite at alkaline pH, whereas nitrous oxide was the major product of nitrate reduction when the bacteria were grown at pH 6.0. Growth yields were increased by nitrate in electron acceptor-limited chemostats, where nitrate was reduced to nitrite, showing that dissimilatory nitrate reduction was an energetically favorable process in P. acnes. Nitrate had little effect on the amounts of fermentation products formed, but molar ratios of acetate to propionate were higher in the nitrate chemostats. Low concentrations of nitrite (ca. 0.2 mM) inhibited growth of P. acnes in batch culture. The nitrite was slowly reduced to nitrous oxide, enabling growth to occur, suggesting that denitrification functions as a detoxification mechanism.     

Dissimilatory nitrate reduction by Propionibacterium acnes

Propionibacterium acnes P13 was isolated from human feces. The bacterium produced a particulate nitrate reductase and a soluble nitrite reductase when grown with nitrate or nitrite. Reduced viologen dyes were the preferred electron donors for both enzymes. Nitrous oxide reductase was never detected. Specific growth rates were increased by nitrate during growth in batch culture. Culture pH strongly influenced the products of dissimilatory nitrate reduction. Nitrate was principally converted to nitrite at alkaline pH, whereas nitrous oxide was the major product of nitrate reduction when the bacteria were grown at pH 6.0. Growth yields were increased by nitrate in electron acceptor-limited chemostats, where nitrate was reduced to nitrite, showing that dissimilatory nitrate reduction was an energetically favorable process in P. acnes. Nitrate had little effect on the amounts of fermentation products formed, but molar ratios of acetate to propionate were higher in the nitrate chemostats. Low concentrations of nitrite (ca. 0.2 mM) inhibited growth of P. acnes in batch culture. The nitrite was slowly reduced to nitrous oxide, enabling growth to occur, suggesting that denitrification functions as a detoxification mechanism.     

Nitrogenase activity and nitrate respiration inAzospirillum spp.

The interaction between nitrate respiration and nitrogen fixation inAzospirillum lipoferum andA. brasilense was studied. All strains examined were capable of nitrogen fixation (acetylene reduction) under conditions of severe oxygen limitation in the presence of nitrate. A lag phase of about 1 h was observed for both nitrate reduction and nitrogenase activity corresponding to the period of induction of the dissimilatory nitrate reductase. Nitrogenase activity ceased when nitrate was exhausted suggesting that the reduction of nitrate to nitrite, rather than denitrification (the further reduction of nitrite to gas) is coupled to nitrogen fixation. The addition of nitrate to nitrate reductase negative mutants (nr^-) ofAzospirillum did not stimulate nitrogenase activity. Under oxygen-limited conditionsA. brasilense andA. lipoferum were also shown to reduce nitrate to ammonia, which accumulated in the medium. Both species, including strains ofA. brasilense which do not possess a dissimilatory nitrite reductase (nir^-) were also capable of reducing nitrous oxide to N₂.     

Artifacts associated with the use of thiocyanate and valinomycin/K+ as permeant ions in oxidant pulse experiments on denitrifying bacteria

By means of¹⁵N-tracer and oxidant pulse methods and with nitrate-grownParacoccus denitrificans it was found that KSCN completely inhibited reduction of N₂O and nitrate in the 1 to 10 mM range, but had little or no effect on reduction of O₂ or nitrite at 150 mM. These observations confirm a previous report. Potassium thiocyanate was insufficiently permeant across the cytoplasmic membrane ofParacoccus denitrificans andPseudomonas denitrificans even at 150 mM to prevent membrane polarization when oxidant pulses were large. Polarization and inhibition artifacts due to KSCN have created some confusion in the literature. Whereas valinomycin had little direct effect on reduction of nitrite, N₂O, and O₂ individually byPa. denitrificans, it caused a temporary nitrite-dependent inhibition of N₂O reduction. Under nonpolarizing conditions the H⁺/2e^– ratios for O₂, N₂O, and nitrite (8.0, 4.3, and 4.5, respectively) confirmed those reported previously from this laboratory. The present results largely but not entirely agree with data from another laboratory.     

Intermediates of denitrification in the chemoautotroph Thiobacillus denitrificans

Summary Intact cells obtained from Thiobacillus denitrificans grown autotrophically with thiosulfate as the oxidizable substrate and nitrate as the final electron acceptor catalyzed the reduction of nitrate, nitrite and nitric oxide stoichiometrically to nitrogen gas with the concomitant oxidation of thiosulfate. In addition, nitrous oxide was also capable of acting as the terminal oxidant of the respiratory chain with thiosulfate as the reductant. The anaerobic oxidation of thiosulfate by NO₃ ^-, NO, and N₂O was sensitive to the flavoprotein inhibitors, antimycin A or NHQNO, and cyanide or azide thus, implicating the participation of flavins, and cytochromes of b-, c-, and a-types in the denitrification process. The nitrite reductase system, however, was not markedly affected by the electron transport chain inhibitors. The experimental observations suggest that the dissimilatory nitrate reduction in the chemoautotroph T. denitrificans involves nitrite, nitric oxide, and nitrous oxide as theintermediates with nitrogen gas as the final reduction product.Non-Standard Abbreviations TTFA Thenoyltrifluoroacetone - NHQNO 2-n-nonyl-4-hydroxyquinoline N-oxide     

Nitrate and nitrite reductase negative mutants of N2-fixingAzospirillum spp.

Chlorate resistant spontaneous mutants ofAzospirillum spp. (syn.Spirillum lipoferum) were selected in oxygen limited, deep agar tubes with chlorate. Among 20 mutants fromA. brasilense and 13 fromA. lipoferum all retained their functional nitrogenase and 11 from each species were nitrate reductase negative (nr^–). Most of the mutants were also nitrite reductase negative (nir^–), only 3 remaining nir⁺. Two mutants from nr⁺ nir⁺ parent strains lost only nir and became like the nr⁺ nir^– parent strain ofA. brasilense. No parent strain or nr⁺ mutant showed any nitrogenase activity with 10 mM NO ₃ ^– . In all nr^– mutants, nitrogenase was unaffected by 10 mM NO ₃ ^– . Nitrite inhibited nitrogenase activity of all parent strains and mutants including those which were nir^–. It seems therefore, that inhibition of nitrogenase by nitrate is dependent on nitrate reduction. Under aerobic conditions, where nitrogenase activity is inhibited by oxygen, nitrate could be used as sole nitrogen source for growth of the parent strains and one mutant (nr^– nir^–) and nitritite of the parent strains and 10 mutants (all types). This indicates the loss of both assimilatory and dissimilatory nitrate reduction but only dissimilatory nitrite reduction in the mutants selected with chlorate.     

Utilization of nitrate byBeggiatoa alba

Beggiatoa alba B18LD utilizes both nitrate and nitrite as sole nitrogen sources, although nitrite was toxic above 1 mM.B. alba coupledin vivo acetate oxidation, but not sulfide oxidation, with nitrate and nitrite reduction.B. alba could not, however, grow anaerobically with nitrate as the sole electron acceptor. Furthermore, the incorporation of acetate into macromolecules under anaerobic conditions with nitrate as the sole electron acceptor was less 10% of the incorporation with oxygen as the electron acceptor. The product of nitrate reduction byB. alba was ammonia; N₂ or N₂O were not produced. The nitrate reductase activity inB. alba was soluble and it utilized reduced flavins or methyl viologen and dithionite as electron donors. Pyrimidine nucleotides were not used as in vitro electron donors, either alone or with flavins in coupled assays. TheB. alba nitrate reductase activity was competitively inhibited with chlorate and was only mildly inhibited by azide and cyanide. Nitrate was not required for induction of theB. alba nitrate reductase, and neither oxygen nor ammonia repressed its activity. Thus,B. alba nitrate reductase appears to be an assimilatory nitrate reductase with unusual regulatory properties.Non-standard abbreviations MV Methyl viologen - DT dithionite - GS glutamine synthetase - GOGAT glutamine 2-oxoglutarate aminotransferase - PPO 2-diphenyloxazole - POPOP 1,4-(bis)-[2-(5-phenyloxazolyl)] benzene - TCA trichloroacetic acid - CCCP carbonylcyanidem-chlorophenylhydrazone - FCCP carbonylcyanidep-trifluoromethoxyphenylhydrazone - TTFA thenoyltrifluoroacetone - PHEN 1,10-phenanthroline - HOQNO 2-heptyl 4-hydroxyquinoline-n-oxide - 8HQ 8-hydroxyquinoline     

硝态氮异化还原机制及其主导因素研究进展

硝态氮(NO_3~-)异化还原过程通常包含反硝化和异化还原为铵(DNRA)两个方面,是土壤氮素转化的重要途径,其强度大小直接影响着硝态氮的利用和环境效应(如淋溶和氮氧化物气体排放)。反硝化和DNRA过程在反应条件、产物和影响因素等方面常会呈现出协同与竞争的交互作用机制。综述了反硝化和DNRA过程的研究进展及其二者协同竞争的作用机理,并阐述了在NO_3~-、pH、有效C、氧化还原电位(Eh)等环境条件和土壤微生物对其发生强度和产物的影响,提出了今后应在产生机理、土壤环境因素、微生物学过程以及与其他氮素转化过程耦联作用等方面亟需深入研究,以期增进对氮素循环过程的认识以及为加强氮素管理利用提供依据。     

Nitrous Oxide Formation in the Colne Estuary, England: the Central Role of Nitrite

Nitrate and nitrite concentrations in the water and nitrous oxide and nitrite fluxes across the sediment-water interface were measured monthly in the River Colne estuary, England, from December 1996 to March 1998. Water column concentrations of N₂O in the Colne were supersaturated with respect to air, indicating that the estuary was a source of N₂O for the atmosphere. At the freshwater end of the estuary, nitrous oxide effluxes from the sediment were closely correlated with the nitrite concentrations in the overlying water and with the nitrite influx into the sediment. Increases in N₂O production from sediments were about 10 times greater with the addition of nitrite than with the addition of nitrate. Rates of denitrification were stimulated to a larger extent by enhanced nitrite than by nitrate concentrations. At 550 μM nitrite or nitrate (the highest concentration used), the rates of denitrification were 600 μmol N · m⁻² · h⁻¹ with nitrite but only 180 μmol N · m⁻² · h⁻¹ with nitrate. The ratios of rates of nitrous oxide production and denitrification (N₂O/N₂ × 100) were significantly higher with the addition of nitrite (7 to 13% of denitrification) than with nitrate (2 to 4% of denitrification). The results suggested that in addition to anaerobic bacteria, which possess the complete denitrification pathway for N₂ formation in the estuarine sediments, there may be two other groups of bacteria: nitrite denitrifiers, which reduce nitrite to N₂ via N₂O, and obligate nitrite-denitrifying bacteria, which reduce nitrite to N₂O as the end product. Consideration of free-energy changes during N₂O formation led to the conclusion that N₂O formation using nitrite as the electron acceptor is favored in the Colne estuary and may be a critical factor regulating the formation of N₂O in high-nutrient-load estuaries.     

The Earthworm Gut: an Ideal Habitat for Ingested N2O-Producing Microorganisms

The in vivo production of nitrous oxide (N₂O) by earthworms is due to their gut microbiota, and it is hypothesized that the microenvironment of the gut activates ingested N₂O-producing soil bacteria. In situ measurement of N₂O and O₂ with microsensors demonstrated that the earthworm gut is anoxic and the site of N₂O production. The gut had a pH of 6.9 and an average water content of approximately 50%. The water content within the gut decreased from the anterior end to the posterior end. In contrast, the concentration of N₂O increased from the anterior end to the mid-gut region and then decreased along the posterior part of the gut. Compared to the soil in which worms lived and fed, the gut of the earthworm was highly enriched in total carbon, organic carbon, and total nitrogen and had a C/N ratio of 7 (compared to a C/N ratio of 12 in soil). The aqueous phase of gut contents contained up to 80 mM glucose and numerous compounds that were indicative of anaerobic metabolism, including up to 9 mM formate, 8 mM acetate, 3 mM lactate, and 2 mM succinate. Compared to the soil contents, nitrite and ammonium were enriched in the gut up to 10- and 100-fold, respectively. The production of N₂O by soil was induced when the gut environment was simulated in anoxic microcosms for 24 h (the approximate time for passage of soil through the earthworm). Anoxia, high osmolarity, nitrite, and nitrate were the dominant factors that stimulated the production of N₂O. Supplemental organic carbon had a very minimal stimulatory effect on the production of N₂O, and addition of buffer or ammonium had essentially no effect on the initial N₂O production rates. However, a combination of supplements yielded rates greater than that obtained mathematically for single supplements, suggesting that the maximum rates observed were due to synergistic effects of supplements. Collectively, these results indicate that the special microenvironment of the earthworm gut is ideally suited for N₂O-producing bacteria and support the hypothesis that the in situ conditions of the earthworm gut activate ingested N₂O-producing soil bacteria during gut passage.     

Production of nitric oxide in Nitrosomonas europaea by reduction of nitrite

Nitrosomonas europaea and Nitrosovibrio sp. produced NO and N₂O during nitrification of ammonium. Less then 15% of the produced NO was due to chemical decomposition of nitrite. Production of NO and especially of N₂O increased when the bacteria were incubated under anaerobic conditions at decreasing flow rates of air, or at increasing cell densities. Low concentrations of chlorite (10 M) inhibited the production of NO and N₂, but not of nitrite indicating that NO and N₂O were not produced during the oxidative conversion of ammonium to nitrite. NO and N₂O were produced during reduction of nitrite with hydrazine as electron donor in almost stoichiometric quantities indicating that reduction of nitrite was the main source of NO and N₂O.     

The reduction of nitrous oxide to dinitrogen by Escherichia coli

Escherichia coli K12 reduces nitrous oxide stoichiometrically to molecular nitrogen with rates of 1.9 mol/h x mg protein. The activity is induced by anaerobiosis and nitrate. N₂+formation from N₂O is inhibited by C₂H₂ (K _i 0.03 mM in the medium) and nitrite (K _i=0.3 mM) but not by azide. A mutant defective in FNR synthesis is unable to reduce N₂O to N₂. The reaction in the wild type could routinely be followed by gas chromatography and alternatively by mass spectrometry measuring the formation of ¹⁵N₂ from ¹⁵N₂O. The enzyme catalyzing N₂O-reduction in E. coli could not be identified; it is probably neither nitrate reductase nor nitrogenase. E. coli does not grow with N₂O as sole respiratory electron acceptor. N₂O-reduction might not have a physiological role in E. coli, and the enzyme involved might catalyze something else in nature, as it has a low affinity for the substrate N₂O (apparent K _m3.0 mM). The capability for N₂O-reduction to N₂ is not restricted to E. coli but is also demonstrable in Yersinia kristensenii and Buttiauxella agrestis of the Enterobacteriaceae. E. coli is able to produce NO and N₂O from nitrite by nitrate reductase, depending on the assay conditions. In such experiments NO _inf2 ^sup- is not reduced to N₂ because of the high demand for N₂O of N₂O-reduction and the inhibitory effect of NO _inf2 ^sup- on this reaction.Dedicated to Professor L. Jaenicke, Köln, on the occassion of his 70th birthday     

Anaerobic nitrate reduction to ammonium in two strains isolated from coastal marine sediment: A dissimilatory pathway

Abstract: A total of 28 nitrate-reducing bacteria were isolated from marine sediment (Mediterranean coast of France) in which dissimilatory reduction of nitrate to ammonium (DRNA) was estimated as 80% of the overall nitrate consumption. Thirteen isolates were considered as denitrifiers and ten as dissimilatory ammonium producers. ¹⁵N ammonium production from ¹⁵N nitrate by an Enterobacter sp. and a Vibrio sp., the predominant bacteria involved in nitrate ammonification in marine sediment, was characterized in pure culture studies. For both strains studied, nitrate-limited culture (1 mM) produced ammonium as the main product of nitrate reduction (> 90%) while in the presence of 10 mM nitrate, nitrite was accumulated in the spent media and ammonia production was less efficient. Concomitantly with the dissimilation of nitrate to nitrite and ammonium the molar yield of growth on glucose increased. Metabolic products of glucose were investigated under different growth conditions. Under anaerobic conditions without nitrate, ethanol was formed as the main product; in the presence of nitrate, ethanol disappeared and acetate increased concomitantly with an increased amount of ammonium. These results indicate that nitrite reduction to ammonium allows NAD regeneration and ATP synthesis through acetate formation, instead of ethanol formation which was favoured in the absence of nitrate.     

Aerobic and anaerobic nitrate and nitrite reduction in free-living cells of Bradyrhizobium sp. (Lupinus)

Induction, energy gain, effect on growth, and interaction of nitrate and nitrite reduction of Bradyrhizobium sp. (Lupinus) USDA 3045 were characterized. Both nitrate and nitrite were reduced in air, although nitrite reduction was insensitive to ammonium inhibition. Anaerobic reduction of both ions was shown to be linked with energy conservation. A dissimilatory ammonification process was detected, which has not been reported in rhizobia so far. Nevertheless, anaerobic conversion of nitrate to ammonium was lower than 40%, which suggests the presence of an additional, nitrite reductase of denitrifying type. Nitrite toxicity caused a non-linear relationship between biomass produced and >2 mM concentrations of each N oxyanion consumed. At > or =5 mM initial concentrations of nitrate, a stoichiometric nitrite accumulation occurred and nitrite remained in the medium. This suggests an inhibition of nitrite reductase activity by nitrate, presumably due to competition with nitrate reductase for electron donors. Lowering of growth temperature almost completely diminished nitrite accumulation and enabled consumption as high as 10 mM nitrate, which confirms such a conclusion.     

Mass Spectrometric Studies of the Effect of pH on the Accumulation of Intermediates in Denitrification by Paracoccus denitrificans

We have used a quadrupole mass spectrometer with a gas-permeable membrane inlet for continuous measurements of the production of N₂O and N₂ from nitrate or nitrite by cell suspensions of Paracoccus denitrificans. The use of nitrate and nitrite labeled with ¹⁵N was shown to simplify the interpretation of the results when these gases were measured. This approach was used to study the effect of pH on the production of denitrification intermediates from nitrate and nitrite under anoxic conditions. The kinetic patterns observed were quite different at acidic and alkaline pH values. At pH 5.5, first nitrate was converted to nitrite, then nitrite was converted to N₂O, and finally N₂O was converted to N₂. At pH 8.5, nitrate was converted directly to N₂, and the intermediates accumulated to only low steady-state concentrations. The sequential usage of nitrate, nitrite, and nitrous oxide observed at pH 5.5 was simulated by using a kinetic model of a branched electron transport chain in which alternative terminal reductases compete for a common reductant.     

Nitric oxide reduction, the last step in denitrification by Fusarium oxysporum, is obligatorily mediated by cytochrome P450nor

The involvement of cytochrome P450nor (P450nor) is the most striking feature of the fungal denitrifying system, and has never been shown in bacterial systems. To establish the physiological significance of the P450nor, we constructed and investigated mutants of Fusarium oxysporum that lacked the gene for P450nor. We mutated the gene by targeted integration of a disrupted gene into the chromosome of F. oxysporum. The mutants were shown to contain neither P450nor protein nor nitric oxide (NO) reductase (Nor) activity, implying that they are indeed deficient in P450nor. These mutants had apparently lost the denitrifying activity and failed to evolve nitrous oxide (N₂O) upon incubation under oxygen-limiting conditions in the presence of nitrate. Their mycelia exhibited normal levels of dissimilatory nitrite reductase (Nir) activity and were able to evolve NO under these conditions. The promoter region of the P450nor gene was fused to lacZ and introduced into the wild-type strain of F. oxysporum. The transformed strain produced β-galactosidase under denitrifying conditions as efficiently as the wild type does P450nor. These results represent unequivocal genetic evidence that P450nor is essential for the reduction of NO to N₂O, the last step in denitrification by F. oxysporum. Received: 28 June 1999 / Accepted: 22 December 1999