The protonmotive force in Pseudomonas aeruginosa and its relationship to exoprotease production

In Pseudomonas aeruginosa ATCC 10145 a negative correlation was observed between the protonmotive force (delta P) and the amount of exoprotease produced, with a decrease in delta P resulting in an increase in exoprotease. The two components of delta P, the transmembrane pH gradient (delta pH) and the membrane potential (delta psi) were examined independently and it was observed that delta psi varied very little under the conditions which influenced the activities of exoprotease. However, a positive correlation existed between pH and exoprotease production although the intracellular pH varied very little with either changes in growth rate or changes in extracellular pH. It was observed that with a decrease in growth rate, delta pH became more alkaline and increased exoprotease activities were recorded. Furthermore, an increase in extracellular pH to give an artificial alteration in delta pH, and, consequently, a decrease in delta P, increased exoprotease production, thus confirming the importance of delta pH in exoprotease production.     

Effect of substrate on the regulation of exoprotease production by Pseudomonas aeruginosa ATCC 10145

Exoprotease production by Pseudomonas aeruginosa ATCC 10145 was growth-associated when cultures were grown on complex substrates such as proteins but it occurred during the decelerating growth phase when the organism was grown on amino acids, mixtures of amino acids or simple carbon sources. NH4Cl and simple carbon sources caused repression. Exoprotease was produced in chemostat cultures in response to growth under any of the nutrient limitations studied (carbon, nitrogen or phosphate). Furthermore, by growing at rates less than approximately 0.1 h-1, the repression of enzyme production could be overcome to a large degree. At low growth rates there was an inverse relationship between growth rate and exoprotease production. Thus, exoprotease production was depressed by available energy sources and was increased in response to any nutrient limitation.     

Differential Inhibition by Allylsulfide of Nitrification and Methane Oxidation in Freshwater Sediment

Addition of nitrapyrin, allylthiourea, C(inf2)H(inf2), and CH(inf3)F to freshwater sediment slurries inhibited CH(inf4) oxidation and nitrification to similar extents. Dicyandiamide and allylsulfide were less inhibitory for CH(inf4) oxidation than for nitrification. Allylsulfide was the most potent inhibitor of nitrification, and the estimated 50% inhibitory concentrations for this process and CH(inf4) oxidation were 0.2 and 121 (mu)M, respectively. At a concentration of 2 (mu)M allylsulfide, growth and CH(inf4) oxidation activity of Methylosinus trichosporium OB3b were not inhibited. Allylsulfide at 200 (mu)M inhibited the growth of M. trichosporium by approximately 50% but did not inhibit CH(inf4) oxidation activity. Nitrite production by cells of M. trichosporium was not significantly affected by allylsulfide, except at a concentration of 2 mM, when growth and CH(inf4) oxidation were also inhibited by about 50%. Methane monooxygenase activity present in soluble fractions of M. trichosporium was not inhibited significantly by allylsulfide at either 200 (mu)M or 2 mM. These results suggest that the partial inhibition of CH(inf4) oxidation in sediment slurries by high allylsulfide concentrations may be caused by an inhibition of the growth of methanotrophs rather than an inhibition of methane monooxygenase activity specifically. We conclude that allylsulfide is a promising tool for the study of interactions of methanotrophs and nitrifiers in N cycling and CH(inf4) turnover in natural systems.     

Photodissimilation of Fructose to H(inf2) and CO(inf2) by a Dinitrogen-Fixing Cyanobacterium, Anabaena variabilis

The ability of cyanobacteria to serve as biocatalysts in the production of H(inf2) as a fuel and chemical feedstock was investigated with Anabaena variabilis. The results show that A. variabilis, when incubated under argon, dissimilated fructose to H(inf2) and CO(inf2) in a light-dependent reaction. The H(inf2) production had an obligate requirement for fructose and was heterocyst dependent, since NH(inf4)(sup+)-grown cultures lacking heterocysts failed to produce H(inf2). Differential inhibition studies with CO showed that nitrogenase is the main enzyme catalyzing the H(inf2) production. Net H(inf2) yield increased with increasing concentrations of fructose up to 10 mM in the medium. The average apparent conversion efficiency of fructose to H(inf2) (net H(inf2) produced/fructose removed from the medium) was about 10, although higher conversion efficiencies of 15 to 17 could be obtained during shorter periods and at optimum fructose concentrations. Under the same conditions, the ratio of CO(inf2) released to fructose removed from the medium was about 3.5, suggesting that only a fraction of the fructose carbon was completely oxidized to CO(inf2). Under conditions of carbon excess, which prevents H(inf2) uptake, the maximum ratio of H(inf2) to CO(inf2) was found to be 3.0. This is higher than the expected value of 2.0, indicating that water was also a source of reductant in this fructose-mediated H(inf2) production. Inhibition of H(inf2) evolution by 3-(3,4-dichlorophenyl)-1,1-dimethylurea confirmed a role for photosystem II in this process. The rate of H(inf2) production by A. variabilis SA1 was 46 ml h(sup-1) g (dry weight)(sup-1). This high rate was maintained for over 15 days. About 30% of this H(inf2) was derived from water (10 ml of H(inf2) h(sup-1) g [dry weight](sup-1)). These results show that filamentous, heterocystous cyanobacteria can serve as biocatalysts in the high-efficiency conversion of biomass-derived sugars to H(inf2) as a fuel source while simultaneously dissimilating water to H(inf2).     

Degradation of Trimethylbenzene Isomers by an Enrichment Culture under N(inf2)O-Reducing Conditions

A microbial culture enriched from a diesel fuel-contaminated aquifer was able to grow on 1,3,5-trimethylbenzene (1,3,5-TMB) and 1,2,4-TMB under N(inf2)O-reducing conditions, but it did not degrade 1,2,3-TMB. The oxidation of 1,3,5-TMB to CO(inf2) was coupled to the production of biomass and the reduction of N(inf2)O. N(inf2)O was used to avoid toxic effects caused by NO(inf2)(sup-) accumulation during growth with NO(inf3)(sup-) as the electron acceptor. In addition to 1,3,5-TMB and 1,2,4-TMB, the culture degraded toluene, m-xylene, p-xylene, 3-ethyltoluene, and 4-ethyltoluene.     

Methylmercury Oxidative Degradation Potentials in Contaminated and Pristine Sediments of the Carson River, Nevada

Sediments from mercury-contaminated and uncontaminated reaches of the Carson River, Nevada, were assayed for sulfate reduction, methanogenesis, denitrification, and monomethylmercury (MeHg) degradation. Demethylation of [(sup14)C]MeHg was detected at all sites as indicated by the formation of (sup14)CO(inf2) and (sup14)CH(inf4). Oxidative demethylation was indicated by the formation of (sup14)CO(inf2) and was present at significant levels in all samples. Oxidized/reduced demethylation product ratios (i.e., (sup14)CO(inf2)/(sup14)CH(inf4) ratios) generally ranged from 4.0 in surface layers to as low as 0.5 at depth. Production of (sup14)CO(inf2) was most pronounced at sediment surfaces which were zones of active denitrification and sulfate reduction but was also significant within zones of methanogenesis. In a core taken from an uncontaminated site having a high proportion of oxidized, coarse-grain sediments, sulfate reduction and methanogenic activity levels were very low and (sup14)CO(inf2) accounted for 98% of the product formed from [(sup14)C]MeHg. There was no apparent relationship between the degree of mercury contamination of the sediments and the occurrence of oxidative demethylation. However, sediments from Fort Churchill, the most contaminated site, were most active in terms of demethylation potentials. Inhibition of sulfate reduction with molybdate resulted in significantly depressed oxidized/reduced demethylation product ratios, but overall demethylation rates of inhibited and uninhibited samples were comparable. Addition of sulfate to sediment slurries stimulated production of (sup14)CO(inf2) from [(sup14)C]MeHg, while 2-bromoethanesulfonic acid blocked production of (sup14)CH(inf4). These results reveal the importance of sulfate-reducing and methanogenic bacteria in oxidative demethylation of MeHg in anoxic environments.     

Effect of gramicidin D on the exoprotease activity of Bacillus thuringiensis

A treatment of Bacillus thuringiensis cells with gramicidine D in the medium containing the yeast and polysaccharides increases the lag-phase up to 12 h without a change of the rate during the logarithmic phase of the culture growth. The exoprotease activity of cells treated with gramicidine reaches a maximum value 4 h earlier in comparison with the control culture, and the activity level is increased 2-fold. At a concentration increasing the exoprotease activity, gramicidine was found to induce the permeability of Bac. thuringiensis membranes for potassium ions. An additional introduction of 250 mM KCl or NaCl into the medium inhibits only the exoprotease activity of cells treated with gramicidine. It is assumed that the ability of gramicidine to increase the exoprotease activity of Bac. thuringiensis may be due to a change in the intrabacterial ionic composition.     

Comparison of the Efficacies of Chloromethane, Methionine, and S-Adenosylmethionine as Methyl Precursors in the Biosynthesis of Veratryl Alcohol and Related Compounds in Phanerochaete chrysosporium

The effect on veratryl alcohol production of supplementing cultures of the lignin-degrading fungus Phanerochaete chrysosporium with different methyl-(sup2)H(inf3)-labelled methyl precursors has been investigated. Both chloromethane (CH(inf3)Cl) and l-methionine caused earlier initiation of veratryl alcohol biosynthesis, but S-adenosyl-l-methionine (SAM) retarded the formation of the compound. A high level of C(sup2)H(inf3) incorporation into both the 3- and 4-O-methyl groups of veratryl alcohol occurred when either l-[methyl-(sup2)H(inf3)]methionine or C(sup2)H(inf3)Cl was present, but no significant labelling was detected when S-adenosyl-l-[methyl-(sup2)H(inf3)]methionine was added. Incorporation of C(sup2)H(inf3) from C(sup2)H(inf3)Cl was strongly antagonized by the presence of unlabelled l-methionine; conversely, incorporation of C(sup2)H(inf3) from l-[methyl-(sup2)H(inf3)]methionine was reduced by CH(inf3)Cl. These results suggest that l-methionine is converted either directly or via an intermediate to CH(inf3)Cl, which is utilized as a methyl donor in veratryl alcohol biosynthesis. SAM is not an intermediate in the conversion of l-methionine to CH(inf3)Cl. In an attempt to identify the substrates for O methylation in the metabolic transformation of benzoic acid to veratryl alcohol, the relative activities of the SAM- and CH(inf3)Cl-dependent methylating systems on several possible intermediates were compared in whole mycelia by using isotopic techniques. 4-Hydroxybenzoic acid was a much better substrate for the CH(inf3)Cl-dependent methylation system than for the SAM-dependent system. The CH(inf3)Cl-dependent system also had significantly increased activities toward both isovanillic acid and vanillyl alcohol compared with the SAM-dependent system. On the basis of these results, it is proposed that the conversion of benzoic acid to veratryl alcohol involves para hydroxylation, methylation of 4-hydroxybenzoic acid, meta hydroxylation of 4-methoxybenzoic acid to form isovanillic acid, and methylation of isovanillic acid to yield veratric acid.     

Inhibition of Methanogenesis by Methyl Fluoride: Studies of Pure and Defined Mixed Cultures of Anaerobic Bacteria and Archaea

Methyl fluoride (fluoromethane [CH(inf3)F]) has been used as a selective inhibitor of CH(inf4) oxidation by aerobic methanotrophic bacteria in studies of CH(inf4) emission from natural systems. In such studies, CH(inf3)F also diffuses into the anaerobic zones where CH(inf4) is produced. The effects of CH(inf3)F on pure and defined mixed cultures of anaerobic microorganisms were investigated. About 1 kPa of CH(inf3)F, similar to the amounts used in inhibition experiments, inhibited growth of and CH(inf4) production by pure cultures of aceticlastic methanogens (Methanosaeta spp. and Methanosarcina spp.) and by a methanogenic mixed culture of anaerobic microorganisms in which acetate was produced as an intermediate. With greater quantities of CH(inf3)F, hydrogenotrophic methanogens were also inhibited. At a partial pressure of CH(inf3)F of 1 kPa, homoacetogenic, sulfate-reducing, and fermentative bacteria and a methanogenic mixed culture of anaerobic microorganisms based on hydrogen syntrophy were not inhibited. The inhibition by CH(inf3)F of the growth and CH(inf4) production of Methanosarcina mazei growing on acetate was reversible. CH(inf3)F inhibited only acetate utilization by Methanosarcina barkeri, which is able to use acetate and hydrogen simultaneously, when both acetate and hydrogen were present. These findings suggest that the use of CH(inf3)F as a selective inhibitor of aerobic CH(inf4) oxidation in undefined systems must be interpreted with great care. However, by a careful choice of concentrations, CH(inf3)F may be useful for the rapid determination of the role of acetate as a CH(inf4) precursor.     

Hydrogen Concentration Profiles at the Oxic-Anoxic Interface: a Microsensor Study of the Hindgut of the Wood-Feeding Lower Termite Reticulitermes flavipes (Kollar)

Molecular hydrogen is a key intermediate in lignocellulose degradation by the microbial community of termite hindguts. With polarographic, Clark-type H(inf2) microelectrodes, we determined H(inf2) concentrations at microscale resolution in the gut of the wood-feeding lower termite Reticulitermes flavipes (Kollar). Axial H(inf2) concentration profiles obtained from isolated intestinal tracts embedded in agarose Ringer solution clearly identified the voluminous hindgut paunch as the site of H(inf2) production. The latter was strictly coupled with both a low redox potential (E(infh) = -200 mV) and the absence of oxygen, in agreement with the growth requirements of the cellulolytic, H(inf2)-producing flagellates located in the hindgut paunch. Luminal H(inf2) partial pressures were much higher than expected (ca. 5 kPa) and increased more than threefold when the guts were incubated under a N(inf2) headspace. Radial H(inf2) concentration gradients showed a steep decrease from the gut center towards the periphery, indicating the presence of H(inf2)-consuming activities both within the lumen and at the gut epithelium. Measurements under controlled gas headspace showed that the gut wall was also a sink for externally supplied H(inf2), both under oxic and anoxic conditions. With O(inf2) microelectrodes, we confirmed that the H(inf2) sink below the gut epithelium is located within the microoxic gut periphery, but the H(inf2)-consuming activity itself, at least a substantial part of it, was clearly due to an anaerobic process. These results are in accordance with the recently reported presence of methanogens attached in large numbers to the luminal side of the hindgut epithelium of R. flavipes. If the oxygen partial pressure was increased, O(inf2) penetrated deeper and H(inf2) production was suppressed; it ceased completely as soon as the gut was fully oxic. In experiments with living termites, externally supplied H(inf2) (20 kPa) stimulated methane formation five- to sixfold to 0.93 (mu)mol (g of termite)(sup-1) h(sup-1), indicating that the methanogenic activity in R. flavipes hindguts is not saturated for hydrogen under in situ conditions. This rate was in good agreement with the H(inf2) uptake rates exhibited by isolated hindguts, which would account for more than half of the CH(inf4) formed by living termites under comparable conditions.     

Capacity for Methane Oxidation in Landfill Cover Soils Measured in Laboratory-Scale Soil Microcosms

Laboratory-scale soil microcosms containing different soils were permeated with CH(inf4) for up to 6 months to investigate their capacity to develop a methanotrophic community. Methane emissions were monitored continuously until steady states were established. The porous, coarse sand soil developed the greatest methanotrophic capacity (10.4 mol of CH(inf4) (middot) m(sup-2) (middot) day(sup-1)), the greatest yet reported in the literature. Vertical profiles of O(inf2), CH(inf4), and methanotrophic potential in the soils were determined at steady state. Methane oxidation potentials were greatest where the vertical profiles of O(inf2) and CH(inf4) overlapped. A significant increase in the organic matter content of the soil, presumably derived from methanotroph biomass, occurred where CH(inf4) oxidation was greatest. Methane oxidation kinetics showed that a soil community with a low methanotrophic capacity (V(infmax) of 258 nmol (middot) g of soil(sup-1) (middot) h(sup-1)) but relatively high affinity (k(infapp) of 1.6 (mu)M) remained in N(inf2)-purged control microcosms, even after 6 months without CH(inf4). We attribute this to a facultative, possibly mixotrophic, methanotrophic microbial community. When purged with CH(inf4), a different methanotrophic community developed which had a lower affinity (k(infapp) of 31.7 (mu)M) for CH(inf4) but a greater capacity (V(infmax) of 998 nmol (middot) g of soil(sup-1) (middot) h(sup-1)) for CH(inf4) oxidation, reflecting the enrichment of an active high-capacity methanotrophic community. Compared with the unamended control soil, amendment of the coarse sand with sewage sludge enhanced CH(inf4) oxidation capacity by 26%; K(inf2)HPO(inf4) amendment had no significant effect, while amendment with NH(inf4)NO(inf3) reduced the CH(inf4) oxidation capacity by 64%. In vitro experiments suggested that NH(inf4)NO(inf3) additions (10 and 71 (mu)mol (middot) g of soil(sup-1)) inhibited CH(inf4) oxidation by a nonspecific ionic effect rather than by specific inhibition by NH(inf4)(sup+).     

Inhibition of the Plaquing Efficiency of T4r+ Bacteriophage by Subtilisin

The mechanism by which the replicative cycle of T4r(+) phage is inhibited by certain nonhost bacterial systems was investigated. Some Bacillaceae, especially Bacillus subtilis, decreased the plaquing efficiency of this virus more than 95% within 24 hr of exposure. Sarcina lutea and Micrococcus sp. both failed to cause any significant change in the infectivity of T4r(+) phage. Preliminary investigations into the nature of the inhibitory substance(s) suggested that an extracellularly elicited protein was at least partially responsible for this effect. Further analysis has implicated subtilisin, an exoprotease from B. subtilis, as the cause of some, if not all, of the observed decrease in plaquing efficiency. Gel-filtration chromatography of control and treated (14)C-labeled T4r(+) phage showed a wide dispersal of phage-specific material of these particles after 24 hr of exposure to pure subtilisin or to expended medium exoprotease from B. subtilis. It was concluded that B. subtilis exoprotease is capable of chemically altering the structure of the phage capsid, thus causing a decrease in its plaquing efficiency.     

Kinetics of Inhibition of Methane Oxidation by Nitrate, Nitrite, and Ammonium in a Humisol

The kinetics of inhibition of CH(inf4) oxidation by NH(inf4)(sup+), NO(inf2)(sup-), and NO(inf3)(sup-) in a humisol was investigated. Soil slurries exhibited nearly standard Michaelis-Menten kinetics, with half-saturation constant [K(infm(app))] values for CH(inf4) of 50 to 200 parts per million of volume (ppmv) and V(infmax) values of 1.1 to 2.5 nmol of CH(inf4) g of dry soil(sup-1) h(sup-1). With one soil sample, NH(inf4)(sup+) acted as a simple competitive inhibitor, with an estimated K(infi) of 8 (mu)M NH(inf4)(sup+) (18 nM NH(inf3)). With another soil sample, the response to NH(inf4)(sup+) addition was more complex and the inhibitory effect of NH(inf4)(sup+) was greater than predicted by a simple competitive model at low CH(inf4) concentrations (<50 ppmv). This was probably due to NO(inf2)(sup-) produced through NH(inf4)(sup+) oxidation. Added NO(inf2)(sup-) was inherently more inhibitory of CH(inf4) oxidation at low CH(inf4) concentrations, and more NO(inf2)(sup-) was produced as the CH(inf4)-to-NH(inf4)(sup+) ratio decreased and the competitive balance shifted. NaNO(inf3) was a noncompetitive inhibitor of CH(inf4) oxidation, but inhibition was evident only at >10 mM concentrations, which also altered soil pHs. Similar concentrations of NaCl were also inhibitory of CH(inf4) oxidation, so there may be no special inhibitory mechanism of nitrate per se.     

The Importance of Hydrogen in Landfill Fermentations

Forty-two samples taken from two landfills were monitored for CH(inf4) production and apparent steady-state H(inf2) concentration. The rates of methanogenesis in these samples ranged from below the detection limit to 1,900 (mu)mol kg (dry weight)(sup-1) day(sup-1), and the median steady-state hydrogen concentration was 1.4 (mu)M in one landfill and 5.2 (mu)M in the other. To further investigate the relationship between hydrogen concentration and methanogenesis, a subset of seven landfill samples was selected on basis of their rates of CH(inf4) production, H(inf2) concentrations, sample pHs, and moisture contents. Samples with H(inf2) concentrations of <20 nM had relatively small amounts of volatile fatty acids (VFAs) (undetectable to 18.6 mmol of VFA kg [dry weight](sup-1)), while samples with H(inf2) concentrations of >100 nM had relatively high VFA levels (133 to 389 mmol of VFA kg [dry weight](sup-1)). Samples with high H(inf2) and VFA contents had relatively low pH values (<=6.3). However, methanogenic and syntrophic bacteria were present in all samples, so the lack of methanogenesis in some samples was not due to a lack of suitable inocula. The low rates of methanogenesis in these samples were probably due to inhibitory effects of low pH and VFA accumulation, resulting from a thermodynamic uncoupling of fatty acid oxidation. As in other anaerobic ecosystems, H(inf2) is a critical intermediate that may be used to monitor the status of landfill fermentations.     

Biosynthesis of Poly(3-Hydroxyalkanoic Acid) Copolymer from CO(inf2) in Pseudomonas acidophila through Introduction of the DNA Fragment Responsible for Chemolithoautotrophic Growth of Alcaligenes hydrogenophilus

Pseudomonas acidophila is a bacterial strain producing a poly(3-hydroxyalkanoic acid) (PHA) copolymer from low-molecular-weight organic compounds such as formate and acetate. The genes responsible for PHA production were cloned in cosmid pIK7 containing a 14.8-kb HindIII fragment of P. acidophila DNA. With the aim of developing a means of producing a PHA copolymer from CO(inf2), cosmid pIK7 was introduced into a polymer-negative mutant of the chemolithoautotrophic bacterium Alcaligenes eutrophus PHB(sup-)4. However, the recombinant strain produced a homopolymer of 3-hydroxybutyric acid (polyhydroxybutyric acid) from CO(inf2). Since it was thought that the composition of the accumulated polymer might depend not on the PHA biosynthetic genes but on the metabolism of the host strain, a recombinant plasmid, pFUS, containing the genes for chemolithoautotrophic growth of the hydrogen-oxidizing bacterium A. hydrogenophilus was introduced into P. acidophila by conjugation. The recombinant plasmid pFUS was stably maintained in P. acidophila in the absence of chemolithoautotrophic or antibiotic selection. This pFUS-harboring strain possessed the ability to grow under a gas mixture of H(inf2), O(inf2), and CO(inf2) in a mineral salts medium, and PHA copolymer accumulation was confirmed by nuclear magnetic resonance spectral analysis. A gas chromatogram obtained by gas chromatography-mass spectrometry showed the composition of the polymer to be 52.8% 3-hydroxybutyrate, 41.1% 3-hydroxyoctanoate, and 6.1% 3-hydroxydecanoate. This is the first report of the production of a PHA copolymer from CO(inf2) as sole carbon source.     

Exoprotease Activity of Two Marine Bacteria during Starvation

Exoprotease activity during 120 h of total energy and nutrient starvation was examined in two marine bacteria, Vibrio sp. strain S14 and Pseudomonas sp. strain S9. The activity was determined by spectrophotometric measurement of the rate of release of soluble color from an insoluble azure dye derivative of hide powder (hide powder azure). Starved cells of both strains (5 h for S14, and 4 or 24 h for S9) showed greater extracellular proteolytic activity than at the onset of starvation. The exoprotease activity of cells starved for longer periods of time then decreased, but was found to be present at significant levels throughout the starvation period studied (120 h). The accumulation of exoprotease activity in the bulk phase during starvation indicated that both strains constitutively excreted extracellular proteases. As deduced from experiments with chloramphenicol, de novo protein synthesis during starvation was required for the production and/or release of the exoproteases into the surrounding environment. The degradation of hide powder azure allowed an immediate increase in respiration rate, also by long-term-starved cells. This suggests that metabolic systems are primed to respond to the availability of substrates, allowing the cells to recover rapidly. The regulation of exoprotease activity was also studied and found to be different in the two strains. Casamino Acids repressed exoprotease activity in Pseudomonas sp. strain S9, whereas a mechanism similar to catabolite repression was found for Vibrio sp. strain S14 in that glucose repressed activity and cyclic AMP reversed this effect. The exoproteases appeared to be metalloproteinases because the addition of EDTA to cell-free starvation supernatants from both strains significantly inhibited the activity of the proteases.     

Criteria and Methodology for Identifying Respiratory Denitrifiers

Respiratory denitrification is not always adequately established when bacteria are characterized. We have tested a simple method that allows one to evaluate whether the two necessary criteria to claim denitrification have been met, namely, that N(inf2) or N(inf2)O is produced from nitrate or nitrite and that this reduction is coupled to a growth yield increase. Microorganisms were cultured in sealed tubes under a helium headspace and in the presence of 0, 2, 4, 7, and 10 mM nitrate or nitrite. After growth had ceased, N(inf2) and N(inf2)O were quantified by gas chromatography and the final protein concentration was measured. Net protein production was linearly related to nitrate concentration for all denitrifiers tested and ranged from 2 to 6 g of protein per mol of electron equivalent reduced. Nitrogen recovery as N(inf2) plus N(inf2)O from nitrate and nitrite transformed exceeded 80% for all denitrifiers. We also suggest that a rate of N gas production of >10 (mu)mol/min/g of protein can be used as an additional characteristic definitive of denitrification since this process produces gas more rapidly than other processes. These characteristics were established after evaluation of a variety of well-characterized respiratory denitrifiers and other N(inf2)O-producing nitrate reducers. Several poorly characterized denitrifiers were also tested and confirmed as respiratory denitrifiers, including Aquaspirillum itersonii, Aquaspirillum fasciculus, Bacillus azotoformans, and Corynebacterium nephridii. These criteria distinguished respiratory denitrifiers from other groups that reduce nitrate or produce N(inf2)O. Furthermore, they correctly identified respiratory denitrification in weak denitrifiers, a group in which the existence of this process may be overlooked.     

Iron limitation by transferrin promotes simultaneous cheating of pyoverdine and exoprotease in Pseudomonas aeruginosa

Pseudomonas aeruginosa is a primary bacterial model to study cooperative behaviors because it yields exoproducts such as siderophores and exoproteases that act as public goods and can be exploited by selfish nonproducers behaving as social cheaters. Iron-limited growth medium, mainly casamino acids medium supplemented with transferrin, is typically used to isolate and study nonproducer mutants of the siderophore pyoverdine. However, using a protein as the iron chelator could inadvertently select mutants unable to produce exoproteases, since these enzymes can degrade the transferrin to facilitate iron release. Here we investigated the evolutionary dynamics of pyoverdine and exoprotease production in media in which iron was limited by using either transferrin or a cation chelating resin. We show that concomitant loss of pyoverdine and exoprotease production readily develops in media containing transferrin, whereas only pyoverdine loss emerges in medium treated with the resin. Characterization of exoprotease- and pyoverdine-less mutants revealed loss in motility, different mutations, and large genome deletions (13–33 kb) including Quorum Sensing (lasR, rsal, and lasI) and flagellar genes. Our work shows that using transferrin as an iron chelator imposes simultaneous selective pressure for the loss of pyoverdine and exoprotease production. The unintended effect of transferrin uncovered by our experiments can help to inform the design of similar studies.Subject terms: Bacteriology, Microbial ecology     

Production of Galacto-Oligosaccharide from Lactose by Sterigmatomyces elviae CBS8119

Volume 61, no. 11, p. 4022, column 2, line 10: "K(inf2)HSO(inf4)" and "KH(inf2)SO(inf4)" should read "K(inf2)HPO(inf4)" and "KH(inf2)PO(inf4)," respectively. Line 13: "K(inf2)HSO(inf4)" should read "K(inf2)HPO(inf4)." Line 14: "KH(inf2)SO(inf4)" and "0.2 g of CaCO(inf3)" should read "KH(inf2)PO(inf4)" and "1 g of CaCO(inf3)," respectively. [This corrects the article on p. 4022 in vol. 61.].     

Kinetic Analyses of Desulfurization of Dibenzothiophene by Rhodococcus erythropolis in Batch and Fed-Batch Cultures

The DbtS(sup+) phenotype (which confers the ability to oxidize selectively the sulfur atom of dibenzothiophene [DBT] or dibenzothiophene sulfone [DBTO(inf2)]) of Rhodococcus erythropolis N1-36 was quantitatively characterized in batch and fed-batch cultures. In flask cultures, production of the desulfurization product, monohydroxybiphenyl (OH-BP), was maximal at pH 6.0, while specific productivity (OH-BP cell(sup-1)) was maximal at pH 5.5. Quantitative measurements in fermentors (in both batch and fed-batch modes) demonstrated that DBTO(inf2) as the sole sulfur source yielded a greater amount of product than did DBT. Specifically, 100 (mu)M DBT maximally yielded (apprx=)40 (mu)M OH-BP, while 100 (mu)M DBTO(inf2) yielded (apprx=)60 (mu)M OH-BP. Neither maintaining the pH at 6.0 nor adding an additional carbon source increased the yield of OH-BP. The presence of SO(inf4)(sup2-) in growth media repressed expression of desulfurization activity, but SO(inf4)(sup2-) added to suspensions of cells grown in DBT or DBTO(inf2) did not inhibit desulfurization activity.