Degradation of hydroquinone,gentisate, and benzoate by a fermenting bacterium in pure or defined mixed culture

From a methanogenic fixed-bed reactor fed with hydroquinone as sole energy and carbon source, a rodshaped bacterium was isolated in pure culture which could degrade hydroquinone and gentisate (2,5-dihydroxybenzoate). In syntrophic coculture with either Desulfovibrio vulgaris or Methanospirillum hungatei, also benzoate could be degraded. Other substrates such as sugars, fatty acids, alcohols, and cyclohexane derivatives were not degraded. Sulfate, sulfite, or nitrate were not used as external electron acceptor. The isolate was a Gram-negative, non-motile, nonsporeforming strict anaerobe; the guanine-plus-cytosine content of the DNA was 53.2±1.0 mol%. In pure culture, hydroquinone was degraded to acetate and benzoate, probably via an intermediate carboxylation. In syntrophic mixed cultures, all three substrates were converted completely to acetate. Phenol was never detected as a fermentation product.     

Effects of soil and water content on methyl bromide oxidation by the ammonia-oxidizing bacterium Nitrosomonas europaea

Little information exists on the potential of NH(3)-oxidizing bacteria to cooxidize halogenated hydrocarbons in soil. A study was conducted to examine the cooxidation of methyl bromide (MeBr) by an NH(3)-oxidizing bacterium, Nitrosomonas europaea, under soil conditions. Soil and its water content modified the availability of NH(4)(+) and MeBr and influenced the relative rates of substrate (NH(3)) and cosubstrate (MeBr) oxidations. These observations highlight the complexity associated with characterizing soil cooxidative activities when soil and water interact to differentially affect substrate and cosubstrate availabilities.     

Anaerobic degradation of naphthalene by a pure culture of a novel type of marine sulphate-reducing bacterium

Incubation of marine sediment in anoxic, sulphate-rich medium in the presence of naphthalene resulted in the enrichment of sulphate-reducing bacteria. Pure cultures with short, oval cells (1.3 by 1.3–1.9 μm) were isolated that grew with naphthalene as the only organic carbon source and electron donor for sulphate reduction to sulphide. One strain, NaphS2, was characterized. It affiliated with completely oxidizing sulphate-reducing bacteria of the δ-subclass of the Proteobacteria, as revealed by 16S rRNA sequence analysis. 2-Naphthoate, benzoate, pyruvate and acetate were used in addition to naphthalene. Quantification of substrate consumption, sulphide formation and formed cell mass revealed that naphthalene was completely oxidized with sulphate as the electron acceptor.     

Effect of shale kerogen oxidation products on biodegradation of petroleum and petroleum products in soil and water

Effect of oxidation products of shale kerogen (high-molecular-weight acids with 6-22 carbon atoms) on biodegradation of oil and oil products in soil and water was studied. High-molecular-weight acids (HMWA) not only affected the layer of oil and/or oil products and dispersed it into small particles, but also stimulated growth of Rhodococcus erythropolis VKM AS-1339D, degraders of oil and oil products. Addition of 0.001-0.003% HMWA to a medium to be purified from oil products increased the extent of bacterial biodegradation by a factor of 1.1-5.0.     

Consumption of NO by methanotrophic bacteria in pure culture and in soil

Abstract The methanotrophs Methylomonas angile (type I) and Methylosinus trichosporium (type II) produced nitrite, nitrate and N₂O during growth on methane, apparently by heterotrophic nitrification of ammonium. The methanotrophs were also able to consume NO but did not produce it. After incubation of soil from a drained paddy field in the presence of CH₄ the numbers of methanotrophs increased from 10⁵ to 10⁷ per gram dry weigth. The thus enriched soil showed increased rates of NO consumption while rates of NO production did not change.     

Biodegradation of 2,4,5-trichlorophenoxyacetic acid in soil by a pure culture of Pseudomonas cepacia.

A pure culture of Pseudomonas cepacia AC1100 was able to degrade and grow in presence of 2,4,5-trichlorophenoxyacetic acid in soil. At optimum temperature (30 degrees C) and moisture content (15 to 50% [wt/vol]) strain AC1100 could degrade as much as 95% of 2,4,5-trichlorophenoxyacetic acid at high concentration (1 mg/g of soil) within 1 week.     

Growth of a facultative anaerobe under oxygen-limiting conditions in pure culture and in co-culture with a sulfate-reducing bacterium

Abstract The occurrence and properties were studied of glucose-metabolizing bacteria present in the anaerobic sediment 5–10 cm below the surface of an estuarine tidal mud-flat. Of all these bacteria (10⁴– 10⁵ per g wet sediment) 80–90% were facultatively anaerobic species. Chemostat enrichments on glucose under aerobic, oxygen-limited and alternately aerobic-anaerobic conditions also yielded cultures dominated by facultative anaerobes. One of the dominant species, tentatively identified as a Vibrio sp., was studied in more detail under oxygen-limiting conditions. Fermentative and respiratory metabolisms were found to operate simultaneously, and the ratio between the two was regulated by the extent of oxygen limitation. A small fraction of the acetate formed under such growth conditions was shown to be subsequently respired. A co-culture was established of the Vibrio sp. and a sulfate-reducing bacterium ( Desulfovibrio HL21 ) in an aerated chemostat. The importance of these observations is discussed in relation to the role of facultative anaerobes in anaerobic habitats.     

High-affinity methane oxidation by a soil enrichment culture containing a type II methanotroph

Methanotrophic bacteria in an organic soil were enriched on gaseous mixing ratios of <275 parts per million of volume (ppmv) of methane (CH4). After 4 years of growth and periodic dilution (>10(20) times the initial soil inoculum), a mixed culture was obtained which displayed an apparent half-saturation constant [Km(app)] for CH4 of 56 to 186 nM (40 to 132 ppmv). This value was the same as that measured in the soil itself and about 1 order of magnitude lower than reported values for pure cultures of methane oxidizers. However, the Km(app) increased when the culture was transferred to higher mixing ratios of CH4 (1,000 ppmv, or 1%). Denaturing gradient gel electrophoresis of the enrichment grown on <275 ppmv of CH4 revealed a single gene product of pmoA, which codes for a subunit of particulate methane monooxygenase. This suggested that only one methanotroph species was present. This organism was isolated from a sample of the enrichment culture grown on 1% CH4 and phylogenetically positioned based on its 16S rRNA, pmoA, and mxaF gene sequences as a type II strain of the Methylocystis/Methylosinus group. A coculture of this strain with a Variovorax sp., when grown on <275 ppmv of CH4, had a Km(app) (129 to 188 nM) similar to that of the initial enrichment culture. The data suggest that the affinity of methanotrophic bacteria for CH4 varies with growth conditions and that the oxidation of atmospheric CH4 observed in this soil is carried out by type II methanotrophic bacteria which are similar to characterized species.     

Metabolism of diethylphthalate by a soil bacterium

A microorganism capable of degrading diethylphthalate as a sole carbon source was isolated from garden soil and tentatively identified asMicrococcus sp. Monoethylphthalate and phthalic acid were shown to be the intermediates by thin-layer chromatography and spectrophotometric and mass spectral analysis. The strain degraded diethylphthalate mainly through monoethylphthalate and phthalic acid as was evidenced by oxygen uptake and enzymatic studies. Ethanol also supported the growth of this organism. It appeared that the entire molecule was metabolized byMicrococcus sp.     

Anaerobic oxidation of p-cresol by a denitrifying bacterium

Metabolism of p-cresol (pCr) under nitrate-reducing conditions is mediated by the denitrifying bacterial isolate PC-07. The methyl substituent of the substrate is oxidized anaerobically by whole-cell suspensions of PC-07 through a series of dehydrogenation and hydration reactions to yield p-hydroxybenzoate (pOHB) in stoichiometric proportions. The partially oxidized intermediates in the pathway p-hydroxybenzyl alcohol and p-hydroxybenzaldehyde can also serve as substrates for pOHB formation. Nitrate is required as the external electron acceptor and is reduced to molecular N2. Reduction of the nitrate is stoichiometric, with pCr serving as the electron donor. In addition, the molar relationship between the electron acceptor (NO3-) reduced to the electron donor oxidized decreased to approximately 2:3 and then to 1:3 when p-hydroxybenzyl alcohol or p-hydroxybenzaldehyde, respectively, served as substrates. The decreased ratios were to be expected when the partially oxidized intermediates served as substrates, because they provided correspondingly less reducing power for pOHB formation. The anaerobic oxidation of pCr by PC-07 demonstrates a mechanism whereby aromatic compounds can be transformed in anoxic environments.     

Frankia strains of soil underBetula pendula: Behaviour in soil and in pure culture

A K/Rb isotope dilution method was used to determine the uptake of K from undisturbed subsoils. Rb was applied to the topsoil (0–30 cm) to trace the K taken up from the topsoil by crops. The K/Rb ratio in the crops increases when roots contact the Rb-free subsoil. This change in the K/Rb ratio enables the calculation of the uptake of K from the subsoil. Results of 34 field experiments on loess-parabrown soils in N. Germany showed that the subsoil (>30 cm) supplied, on average, 34% of the total K uptake by spring wheat (range 9–70%). The range between the experimental sites is considered in relation to the contents of K in the top and subsoils (as extracted by 0.025 N CaCl₂ solution), the proportion of the total root length in the subsoils, and competition for K between roots in the top and subsoil. In subsoils with similar K contents, uptake from the subsoil decreased significantly from 65 to 21% of total K uptake, as K contents in the topsoils increased from 4 to 8 mg K/100 g. On sites with the same K contents in topsoils (9 mg K/100 g), the subsoil supplied 12 to 61% of total K uptake as the K contents of the subsoil increased from 2 to 27 mg K/100 g. The contribution of uptake of K from the subsoil increased with the development of the crop, from 8% at first node stage to 35% at ear emergence, as the proportion of total root length in the subsoil increased. High root length densities in the topsoil (9 cm/cm³) resulted in competition for K between roots and increased uptake of K from the subsoil.     

Catabolism of homophthalic acid by a soil bacterium

A microorganism capable of degrading homophthalic acid as a sole source of carbon was isolated from soil. The strain was tentatively identified as Pseudomonas sp. Oxygen uptake studies were carried out with possible intermediates. Assays for several different enzymes were performed. Homophthalic acid may be metabolized by this bacterium via p-hydroxyphenyl acetic acid and homogentisic acid intermediates.     

Anaerobic oxidation of p-cresol by a denitrifying bacterium.

Metabolism of p-cresol (pCr) under nitrate-reducing conditions is mediated by the denitrifying bacterial isolate PC-07. The methyl substituent of the substrate is oxidized anaerobically by whole-cell suspensions of PC-07 through a series of dehydrogenation and hydration reactions to yield p-hydroxybenzoate (pOHB) in stoichiometric proportions. The partially oxidized intermediates in the pathway p-hydroxybenzyl alcohol and p-hydroxybenzaldehyde can also serve as substrates for pOHB formation. Nitrate is required as the external electron acceptor and is reduced to molecular N2. Reduction of the nitrate is stoichiometric, with pCr serving as the electron donor. In addition, the molar relationship between the electron acceptor (NO3-) reduced to the electron donor oxidized decreased to approximately 2:3 and then to 1:3 when p-hydroxybenzyl alcohol or p-hydroxybenzaldehyde, respectively, served as substrates. The decreased ratios were to be expected when the partially oxidized intermediates served as substrates, because they provided correspondingly less reducing power for pOHB formation. The anaerobic oxidation of pCr by PC-07 demonstrates a mechanism whereby aromatic compounds can be transformed in anoxic environments.