Anaerobic degradation of 3-hydroxybenzoate by a newly isolated nitrate-reducing bacterium

A Gram-negative nitrate-reducing bacterium, strain Asl-3, was isolated from activated sludge with nitrate and 3-hydroxybenzoate as sole source of carbon and energy. The new isolate was facultatively anaerobic, catalase- and oxidase-positive and polarly monotrichously flagellated. In addition to nitrate, nitrite, N2O, and O2 served as electron acceptors. Growth with 3-hydroxybenzoate and nitrate was biphasic: nitrate was completely reduced to nitrite before nitrite reduction to N2 started. Benzoate, 3-hydroxybenzoate, 4-hydroxybenzoate, protocatechuate or phenyl-acetate served as electron and carbon source under aerobic and anaerobic conditions. During growth with excess carbon source, poly-beta-hydroxybutyrate was formed. These characteristics allow the affiliation of strain Asl-3 with the family Pseudomonadaceae. Analogous to the pathway of 4-hydroxybenzoate degradation in other bacteria, the initial step in anaerobic 3-hydroxybenzoate degradation by this organism was activation to 3-hydroxy-benzoyl-CoA in an ATP-consuming reaction. Cell extracts of 3-hydroxybenzoate-grown cells exhibited 3-hydroxybenzoyl-CoA synthetase activity of 190 nmol min-1 mg protein-1 as well as benzoyl-CoA synthetase activity of 86 nmol min-1 mg protein-1. A reductive dehydroxylation of 3-hydroxybenzoyl-CoA could not be demonstrated due to rapid hydrolysis of chemically synthesized 3-hydroxybenzoyl-CoA by cell extracts.     

Anaerobic degradation of long-chain dicarboxylic acids by methanogenic enrichment cultures

Abstract Methanogenic enrichment cultures fermented the long-chain dicarboxylates adipate, pimelate, suberate, azelate, and sebacate (C₆-C₁₀) stoichiometrically to acetate and methane. After several transfers, the cultures contained cells of only a few morphologically distinguishable types. During anaerobic degradation of dicarboxylic acids with even-numbered carbon atoms, propionate accumulated intermediately, and butyrate was the intermediate product of degradation of those with an odd number of carbon atoms. Degradation of the long-chain dicarboxylates depended strictly on the presence of hydrogenotrophic methanogens. The primary attack in these processes was β-oxidation rather than decarboxylation. A general scheme of anaerobic degradation of long-chain dicarboxylic acids has been deduced from these results.     

Acidophilic degradation of methanol by a methanogenic enrichment culture

Abstract An acidophilic methanogenic enrichment culture was obtained in a continuous up-flow anaerobic sludge blanket reactor operated at pH 4.2 with methanol as the sole carbon source. The specific methylotrophic methanogenic activity of the enriched reactor sludge at pH 5 was 3.57 g COD g⁻¹ volatile suspended solids day⁻¹ and the apparent doubling time of the biomass was 15.8 h. Acidic conditions were obligatory, since the enrichment culture was not able to produce methane or to grow at pH 7. Based on morphological characteristics, the dominant methanogenic species in the enrichment culture was a Methanosarcina .     

Anaerobic degradation of isobutyrate by methanogenic enrichment cultures and by a Desulfococcus multivorans strain

Methanogenic enrichment cultures with isobutyrate as sole source of carbon and energy were inoculated with sediment and sludge samples from freshwater and marine origin. Over more than 20 transfers, these cultures fermented 2 mol isobutyrate with 1 mol CO₂ via an intermediate formation of n-butyrate to 4 mol acetate and 1 mol CH₄. The primary isobutyrate-fermenting bacteria could not be purified. From one of the marine enrichment cultures, a sulfate-reducing bacterium was isolated which oxidized isobutyrate with sulfate completely to CO₂. Based on its physiological and morphological properties, this strain was assigned to the known species Desulfococcus multivorans. It also oxidized many other fatty acids without significant release of short-chain intermedeates. The enzymes involved in isobutyrate degradation by this bacterium were assayed in cell-free extracts. The results indicate that isobutyrate is activated to its CoA derivative and oxidized via methylmalonate semialdehyde to propionyl-CoA. Propionyl-CoA is further converted via the methylmalonyl-CoA pathway to acetyl-CoA which is finally cleaved by the CO-dehydrogenase system. It is evident that this is not the pathway used by the fermenting bacteria prevailing in the methanogenic enrichment cultures. There results are discussed on the basis of energetical considerations.     

Fermentation of methanethiol and dimethylsulfide by a newly isolated methanogenic bacterium

From dilution series in defined mineral medium, a marine iregular coccoid methanogenic bacterium (strain MTP4) was isolated that was able to grow on methanethiol as sole source of energy. The strain also grew on dimethylsulfide, mono-, di-, and trimethylamine, methanol and acetate. On formate the organism produced methane without significant growth. Optimal growth on MT, with doubling times of about 20 h, occurred at 30°C in marine medium. The isolate required p-aminobenzoate and a further not identified vitamin. Strain MTP4 had a high tolerance to hydrogen sulfide but was very sensitive to mechanical forces or addition of detergents such as Triton X-100 or sodium dodecylsulfate. Methanethiol was fermented by strain MTP4 according to the following equation:

Anaerobic degradation of citrate under sulfate reducing and methanogenic conditions

Citrate is an important component of metal processing effluents such as chemical mechanical planarization wastewaters of the semiconductor industry. Citrate can serve as an electron donor for sulfate reduction applied to promote the removal of metals, and it can also potentially be used by methanogens that coexist in anaerobic biofilms. The objective of this study was to evaluate the degradation of citrate with sulfate-reducing and methanogenic biofilms. During batch bioassays, the citrate, acetate, methane and sulfide concentrations were monitored. The results indicate that independent of the biofilm or incubation conditions used, citrate was rapidly fermented with specific rates ranging from 566 to 720 mg chemical oxygen demand (COD) consumed per gram volatile suspended solids per day. Acetate was found to be the main fermentation product of citrate degradation, which was later degraded completely under either methanogenic or sulfate reducing conditions. However, if either sulfate reduction or methanogenesis was infeasible due to specific inhibitors (2-bromoethane sulfonate), absence of sulfate or lack of adequate microorganisms in the biofilm, acetate accumulated to levels accounting for 90–100% of the citrate-COD consumed. Based on carbon balances measured in phosphate buffered bioassays, acetate, CO₂ and hydrogen are the main products of citrate fermentation, with a molar ratio of 2:2:1 per mol of citrate, respectively. In bicarbonate buffered bioassays, acetogenesis of H₂ and CO₂ increased the yield of acetate. The results taken as a whole suggest that in anaerobic biofilm systems, citrate is metabolized via the formation of acetate as the main metabolic intermediate prior to methanogenesis or sulfate reduction. Sulfate reducing consortia must be enriched to utilize acetate as an electron donor in order to utilize the majority of the electron-equivalents in citrate.     

Anaerobic degradation of hydroaromatic compounds by newly isolated fermenting bacteria

Aerobic organisms degrade hydroaromatic compounds via the hydroaromatic pathway yielding protocatechuic acid which is further metabolized by oxygenase-mediated ring fission in the 3-oxoadipate pathway. No information exists on anaerobic degradation of hydroaromatics so far. We enriched and isolated from various sources of anoxic sediments several strains of rapidly growing gram-negative bacteria fermenting quinic (1,3,4,5-tetrahydroxy-cyclohexane-1-carboxylic acid) and shikimic acid (3,4,5-trihydroxy-1-cyclohexene-1-carboxylic acid) in the absence of external electron acceptors. Quinic and shikimic acid were the only ones utilized of more than 30 substrates tested. The marine isolates formed acetate, butyrate, and H₂, whereas all freshwater strains formed acetate and propionate as typical fermentation products. Aromatic intermediates were not involved in this degradation. Characterization of the isolates, fermentation balances for both hydroaromatic compounds, and enzyme activities involved in one degradation pathway are presented.Abbreviations BV benzyl viologen (1,1-dibenzyl-4,4-bipyridinium dichloride) - CoA coenzyme A - CTAB cetyltrimethylammonium bronide - DCPIP 2,4-dichlorophenolindophenol - DTT 1,4-dithiotheriol - MV methyl viologen (1,1-dimethyl-4,4-bipyridinium dichloride) - Tricine N-[tris-(hydroxymethyl)-methyl]-glycine - Tris tris-(hydroxymethyl)-aminomethane     

Monochloro- and dichloroacetic acids as carbon and energy sources for a stable,methanogenic mixed culture

A stable methanogenic mixed culture was enriched from an industrial environment to utilize chloroacetate as sole carbon and energy source for growth. It immobilized spontaneously on activated charcoal and grew reproducibly on this carrier in a fluidized bed reactor when supplied with an anaerobic mineral salts medium. Substrate disappearance was complete. Methane, CO₂ and chloride ions were conclusively identified as the metabolic products and quantified. The growth yield from chloroacetate was about 1 g of protein/mol of carbon. The calculated degradation rate in the fluidized bed reactor was 0.2 to 0.8 mmol/l·h. The first metabolic intermediate from [2–¹³C]monochloroacetate in portions of biofilm-coated carrier was shown by ¹³C-NMR to be glycolate, from which ¹³CO₂ and ¹³CH₄ were formed. Glycolate was formed in an oxygen-insensitive hydrolysis, but its conversion to CO₂ and CH₄ was strictly anaerobic and sensitive to inhibition by bromoethanesulfonate. Degradation of [1-¹⁴C]-and [2-¹⁴C]-chloroacetate each yielded the same amount of [¹⁴C]-methane. We thus presume glycolate to be cleaved to CO₂ and H₂, which were the substrates for methanogenesis. Dehalogenation was limited to chlorobromo-, iodo- and dichloroacetate. These four compounds and glycolate were utilized as the sole carbon and energy sources by the methanogenic mixed culture.     

Activation of aromatic acids and aerobic 2-aminobenzoate metabolism in a denitrifying Pseudomonas strain

The initial reactions possibly involved in the acrobic and anaerobic metabolism of aromatic acids by a denitrifying Pseudomonas strain were studied. Several acyl CoA synthetases were found supporting the view that activation of several aromatic acids preceeds degradation. A benzoyl CoA synthetase activity (AMP forming) (apparent K _m values of the enzyme from nitrate grown cells: 0.01 mM benzoate, 0.2 mM ATP, 0.2 mM coenzyme A) was present in aerobically grown and anaerobically, nitrate grown cells when benzoate or other aromatic acids were present. In addition to benzoate and fluorobenzoates, also 2-amino-benzoate was activated, albeit with unfavorable K _m (0.5 mM 2-aminobenzoate). A 2-aminobenzoyl CoA synthetase (AMP forming) was induced both aerobically and anaerobically with 2-aminobenzoate as growth substrate which had a similar substrate spectrum but a low K _m for 2-aminobenzoate (<0.02 mM). Anaerobic growth on 4-hydroxybenzoate induced a 4-hydroxybenzoyl CoA synthetase, and cyclohexanecarboxylate induced another synthetase. In contrast, 3-hydroxybenzoate and phenyl-acetate grown anaerobic cells appeared not to activate the respective substrates at sufficient rates. Contrary to an earlier report extracts from aerobic and anaerobic 2-aminobenzoate grown cells catalysed a 2-aminobenzoyl CoA-dependent NADH oxidation. This activity was 10–20 times higher in aerobic cells and appeared to be induced by 2-aminobenzoate and oxygen. In vitro, 2-aminobenzoyl CoA reduction was dependent on 2-aminobenzoyl CoA NAD(P)H, and oxygen. A novel mechanism of aerobic 2-aminobenzoate degradation is suggested, which proceeds via 2-aminobenzoyl CoA.     

Fermentative degradation of glutarate via decarboxylation by newly isolated strictly anaerobic bacteria

Two strains of new strictly anaerobic, gramnegative bacteria were enriched and isolated from a freshwater (strain WoG13) and a saltwater (strain CuG11) anoxic sediment with glutarate as sole energy source. Strain WoG13 formed spores whereas strain CuG11 did not. Both strains were rod-shaped, motile bacteria growing in carbonate-buffered, sulfide-reduced mineral medium supplemented with 2% of rumen fluid. Both strains fermented glutarate to butyrate, isobutyrate, CO₂, and small amounts of acetate. With methylsuccinate, the same products were formed, and succinate was fermented to propionate and CO₂. No sugars, amino acids or other organic acids were used as substrates. Molar growth yields (Ys) were very small (0.5–0.9 g cell dry mass/mol dicarboxylate). Cells of strain WoG13 contained no cytochromes, and the DNA base ratio was 49.0±1.4 mol% guanine-plus-cytosine. Enzyme activities involved in glutarate degradation could bedemonstrated in cell-free extracts of strain WoG13. A pathway of glutarate fermentation via decarboxylation of glutaconyl-CoA to crotonyl-CoA is suggested which forms butyrate and partly isobutyrate by subsequent isomerization.     

Anaerobic degradation of p-xylene in sediment-free sulfate-reducing enrichment culture

Anaerobic degradation of p-xylene was studied with sulfate-reducing enrichment culture. The enrichment culture was established with sediment-free sulfate-reducing consortium on crude oil. The crude oil-degrading consortium prepared with marine sediment revealed that toluene, and xylenes among the fraction of alkylbenzene in the crude oil were consumed during the incubation. The PCR-denaturing gradient gel electrophoresis (DGGE) analysis of 16S rRNA gene for the p-xylene degrading sulfate-reducing enrichment culture showed the presence of the single dominant DGGE band pXy-K-13 coupled with p-xylene consumption and sulfide production. Sequence analysis of the DGGE band revealed a close relationship between DGGE band pXy-K-13 and the previously described marine sulfate-reducing strain oXyS1 (similarity value, 99%), which grow anaerobically with o-xylene. These results suggest that microorganism corresponding to pXy-K-13 is an important sulfate-reducing bacterium to degrade p-xylene in the enrichment culture.     

Anaerobic degradation of m-cresol by Desulfobacterium cetonicum is initiated by formation of 3-hydroxybenzylsuccinate

The anaerobic bacterium Desulfobacterium cetonicum oxidized m-cresol completely with sulfate as electron acceptor. During growth, 3-hydroxybenzylsuccinate (identified by gas chromatography/mass spectroscopy and by comparison of high-performance liquid chromatography retention time and UV spectrum with a chemically synthesized reference compound) accumulated in the medium. This finding indicates that the methyl group of m-cresol is activated by addition to fumarate as in the case of anaerobic toluene metabolism. In cell-free extracts of D. cetonicum, the formation of 3-hydroxybenzylsuccinate from m-cresol and fumarate was detected at an activity of 0.5 nmol min^–1 (mg protein)^–1. This reaction depended strictly on anoxic assay conditions. Treatment with air resulted in a complete loss of activity; however, some activity could be recovered after restoring anoxic conditions. The activity was slightly membrane-associated. 3-Hydroxybenzylsuccinate was degraded via CoA thioesterification and further oxidation to 3-hydroxybenzoyl-CoA as subsequent steps in the degradation pathway. Received: 20 May 1999 / Accepted: 19 July 1999     

Anaerobic degradation of benzene in BTX mixtures dependent on sulfate reduction

Abstract Enrichment cultures from marine sediments mineralized benzene while using sulfate as the terminal electron acceptor. Parallel cultures using river marsh sediment displayed no activity. Mineralization was confirmed by release of ¹⁴CO₂ from radiolabeled benzene. The dependence on sulfate reduction was demonstrated by stoichiometric balances and the use of specific inhibitors. This work supports recent observations that anaerobic benzene degradation takes place coupled to sulfate reduction.     

Anaerobic degradation of dimethylsulfoniopropionate to 3-S-methylmercaptopropionate by a marine Desulfobacterium strain

Dimethylsulfoniopropionate, an osmolyte of marine algae, is thought to be the major precursor of dimethyl sulfide, which plays a dominant role in biogenic sulfur emission. The marine sulfate-reducing bacterium Desulfobacterium strain PM4 was found to degrade dimethylsulfoniopropionate to 3-S-methylmercaptopropionate. The oxidation of one of the methyl groups of dimethylsulfoniopropionate was coupled to the reduction of sulfate; this process is similar to the degradation betaine to dimethylglycine which was described earlier for the same strain. Desulfobacterium PM4 is the first example of an anaerobic marine bacterium that is able to demethylate dimethylsulfoniopropionate.Abbreviations DMSP dimethylsulfoniopropionate - DMS dimethyl sulfide - MMPA 3-S-methylmercaptopropionate     

Anaerobic degradation of 3-halobenzoates by a denitrifying bacterium

A denitrifying bacterium was isolated from a river sediment after enrichment on 3-chlorobenzoate under anoxic, denitrifying conditions. The bacterium, designated strain 3CB-1, degraded 3-chlorobenzoate, 3-bromobenzoate, and 3-iodobenzoate with stoichiometric release of halide under conditions supporting anaerobic growth by denitrification. The 3-halobenzoates and 3-hydroxybenzoate were used as growth substrates with nitrate as the terminal electron acceptor. The doubling time when growing on 3-halobenzoates ranged from 18 to 25 h. On agar plates with 1 mM 3-chlorobenzoate as the sole carbon source and 30 mM nitrate as the electron acceptor, strain 3CB-1 formed small colonies (1–2 mm in diameter) in 2 to 3 weeks. Anaerobic degradation of both 3-chlorobenzoate and 3-hydroxybenzoate was dependent on nitrate as an electron acceptor and resulted in nitrate reduction corresponding to the stoichiometric values for complete oxidation of the substrate to CO₂. 3-Chlorobenzoate was not degraded in the presence of oxygen. 3-Bromobenzoate and 3-iodobenzoate were also degraded under denitrifying conditions with stoichiometric release of halide, but 3-fluorobenzoate was not utilized by the bacterium. Utilization of 3-chlorobenzoate was inducible, while synthesis of enzymes for 3-hydroxybenzoate degradation was constitutively low, but inducible. Degradation was specific to the position of the halogen substituent, and strain 3CB-1 did not utilize 2- or 4-chlorobenzoate. Received: 6 November 1998 / Accepted: 19 January 1999     

Propionate metabolism in a methanogenic enrichment culture. Direct reductive carboxylation and acetogenesis pathways

Abstract Serial dilutions of methanogenic sludges in propionate medium gave a methanogenic non-acetoclastic enrichment degrading 1 mol of propionate to 1.6 mol of acetate and 0.17 mol of methane, with a transient accumulation of butyrate. NMR recordings showed the conversion of [2-¹³C]- and [3-¹³C]-propionate to [3-¹³C]- and [4-¹³C]-butyrate, respectively, thus demonstrating a reductive carboxylation of propionate to butyrate. The labelling found in the accumulated acetate and fermentation balances also suggested that reductive carboxylation was the major pathway involved in propionate conversion to acetate.     

Anaerobic degradation of phenol by pure cultures of newly isolated denitrifying pseudomonads

From various oxic or anoxic habitats several strains of bacteria were isolated which in the absence of molecular oxygen oxidized phenol to CO₂ with nitrate as the terminal electron acceptor. All strains grew in defined mineral salts medium; two of them were further characterized. The bacteria were facultatively anaerobic Gramnegative rods; metabolism was strictly oxidative with molecular oxygen, nitrate, or nitrite as electron acceptor. The isolates were tentatively identified as pseudomonads. Besides phenol many other benzene derivatives like cresols or aromatic acids were anaerobically oxidized in the presence of nitrate. While benzoate or 4-hydroxybenzoate was degraded both anaerobically and aerobically, phenol was oxidized under anaerobic conditions only. Reduced alicyclic compounds were not degraded. Preliminary evidence is presented that the first reaction in anaerobic phenol oxidation is phenol carboxylation to 4-hydroxybenzoate.     

Anaerobic degradation ofm-cresol via methyl oxidation to 3-hydroxybenzoate by a denitrifying bacterium

The anaerobic degradation of m-cresol was studied in a denitrifying bacterium. In the initial studies, hypothetical intermediates of m-cresol degradation were tested in growth experiments and in adaptation studies with dense cell suspensions. Results suggested a degradation of m-cresol via 3-hydroxybenzoate. To verify this, the degradation of m-cresol was followed in concentrated cell suspensions in the presence of metabolic inhibitors. Fluoroacetate treatment resulted in the transient accumulation of substantial amounts of 3-hydroxybenzoate. In the presence of iodoacetamide, not only was 3-hydroxybenzoate transiently formed, but benzoate was also accumulated. These findings support a degradation of m-cresol via initial anaerobic methyl oxidation to 3-hydroxybenzoate, followed by reductive dehydroxylation to benzoate or benzoyl-CoA. Studies with extracts of m-cresol-grown cells showed the presence of several enzyme activities to be postulated for this pathway. No evidence was found for a carboxylation, hydroxylation of the aromatic ring, or direct ring reduction as the initial step in m-cresol metabolism. Received: 29 November 1994 / Accepted: 7 March 1995     

Anaerobic degradation of 3-hydroxypropanoate by a newly isolated Clostridium sp.

A strain (ToHP1) of anaerobic bacteria which degrades 3-hydroxypropanoate was isolated in pure culture from the sludge of an anaerobic digestor at a Tokyo sewage treatment facility. The strain grew by degrading 3-hydroxypropanoate, lactate, and pyruvate to propionate and acetate. It also grew auxotrophically by degrading 2-hydroxybutanoate to butyrate and propionate in the presence of acetate. Cells were lemon-shaped rods; 1.4 to 3.6 μm in length and 0.5 to 1.1 μm in width. Spores with a diameter of 0.8 to 1.1 μm were formed subterminally. The strain occurred singly or in pairs. It stained gram-positive. The strain grew optimally at 30 to 35°C and ca. pH 7.2. It required yeast extract for growth. The strain did not utilize nitrate, sulfate, sulfite, thiosulfate, or elemental sulfur as an electron acceptor. The guanine plus cytosine content of the DNA was 43 mol%. Strain ToHP1 was identified as a member of the genus Clostridium.     

Anaerobic mineralization of cholesterol by a novel type of denitrifying bacterium

A novel denitrifying bacterium, strain 72Chol, was enriched and isolated under strictly anoxic conditions on cholesterol as sole electron donor and carbon source. Strain 72Chol grew on cholesterol with oxygen or nitrate as electron acceptor. Strictly anaerobic growth in the absence of oxygen was demonstrated using chemically reduced culture media. During anaerobic growth, nitrate was initially reduced to nitrite. At low nitrate concentrations, nitrite was further reduced to nitrogen gas. Ammonia was assimilated. The degradation balance measured in cholesterol-limited cultures and the amounts of carbon dioxide, nitrite, and nitrogen gas formed during the microbial process indicated a complete oxidation of cholesterol to carbon dioxide. A phylogenetic comparison based on total 16S rDNA sequence analysis indicated that the isolated micro-organism, strain 72Chol, belongs to the β2-subgroup in the Proteobacteria and is related to Rhodocyclus, Thauera, and Azoarcus species. Received: 16 July 1996 / Accepted: 5 December 1996