Demethylation and degradation of phenylmethylethers by the sulfide-methylating homoacetogenic bacterium strain TMBS 4

Biochemical studies on anaerobic phenylme-thylether cleavage by homoacetogenic bacteria have been hampered so far by the complexity of the reaction chain involving methyl transfer to acetyl-CoA synthase and subsequent methyl group carbonylation to acetyl-CoA. Strain TMBS 4 differs from other demethylating homoacetogenic bacteria in using sulfide as a methyl acceptor, thereby forming methanethiol and dimethylsulfide. Growing and resting cells of strain TMBS 4 used alternatitively CO₂ as a precursor of the methyl acceptor CO for homoacetogenic acetate formation. Demethylation was inhibited by propyl iodide and reactivated by light, indicating involvement of a corrinoid-dependent methyltransferase. Strain TMBS 4 contained ca. 750 nmol g dry mass^-1 of a corrinoid tentatively identified as 5-hydroxybenzimidazolyl cobamide. A photometric assay for measuring the demethylation activity in cell extracts was developed based on the formation of a yellow complex of Ti³⁺ with 5-hydroxyvanillate produced from syringate by demethylation. In cell extracts, the methyltransfer reaction from methoxylated aromatic compounds to sulfide or methanethiol depended on reductive activation by Ti³⁺. ATP and Mg²⁺ together greatly stimulated this reductive activation without being necessary for the demethylation reaction itself. The specific activity of the transmethylating enzyme system increased proportionally with protein concentration up to 3 mg ml^-1 reaching a constant level of 20 nmol min^-1 mg^-1 at protein concentrations 10 mg ml^-1. The specific rate of activation increased in a non-linear manner with protein concentration. Strain TMBS 4 degraded gallate, the product of sequential demethylations, to 3 acetate through the phloroglucinol pathway as found earlier with Pelobacter acidigallici.Abbreviations BV benzyl viologen - CTAB cetyltrimethylammonium bromide - H₄folate tetrahydrofolate - MOPS 3-[N-morpholino]propanesulfonic acid - MV methyl viologen - NTA nitrilotriacetate - t_d doubling time - TMB 3,4,5-trimethoxybenzoate     

Holophaga foetida gen. nov., sp. nov., a new,homoacetogenic bacterium degrading methoxylated aromatic compounds

A polyphasic approach was used in which genotypic and phenotypic properties of a gram-negative, obligately anaerobic, rod-shaped bacterium isolated from a black anoxic freshwater mud sample were determined. Based on these results, the name Holophaga foetida gen. nov., sp. nov. is proposed. This microorganism produced dimethylsulfide and methanethiol during growth on trimethoxybenzoate or syringate. The only other compounds utilized were pyruvate and trihydroxybenzenes such as gallate, phloroglucinol, or pyrogallol. The aromatic compounds were degraded to acetate. Although comparison of the signature nucleotide pattern of the five established subclasses of Proteobacteria with the 16S rDNA sequence of Holophaga foetida revealed a relationship to members of the -subclass, the phylogenetic position within the radiation of this class is so deep and dependent upon the number and selection of reference sequences that its affiliation to the Proteobacteria must be considered tentative. The type strain is H. foetida strain TMBS4 (DSM 6591).F. Bak died on 27 December 1992. A very promising and productive career thus ended much too early     

Formation of methylmercaptan and dimethylsulfide from methoxylated aromatic compounds in anoxic marine and fresh water sediments

Abstract Anaerobic formation of dimethylsulfide (DMS) and methylmercaptan (MSH) in anoxic sulfide-containing slurries from marine and fresh water sediments was stimulated by addition of syringate (4-hydroxy,3,5,-dimethoxybenzoate) and 3,4,5,-trimethoxybenzoate. The release of DMS and MSH occurred during the consumption of the aromatic monomers and ceased after their depletion. DMS was the dominant methylated sulfur compound in fresh water sediments, in contrast to marine sediments where MSH was predominant. No production of volatile organic sulfur compounds was observed in slurries containing gallate (3,4,5,-trihydroxybenzoate) or in autoclaved controled. About 50–65% of the methoxy carbon could be accounted for by peak accumulation of DMS and MSH. In the saline sediments, large amounts of CH₄ were formed during the period when DMS and MSH disappeared. About 65–70% of the methylcarbon of the volatile methylated sulfur compounds (VMSC) could be accounted for in the produced CH₄. This study demonstrates a previously unknown microbial process by which DMS and MSH are formed during anaerobic decomposition of methoxylated aromatic compounds in marine and freshwater sediments.     

Methyl chloride metabolism of the strictly anaerobic,methyl chloride-utilizing homoacetogen strain MC

The methyl chloride metabolism of the homoacetogenic, methyl chloride-utilizing strain MC was investigated with cell extracts and cell suspensions of the organism. Cell extracts were found to contain all enzyme activities required for the conversion of methyl chloride or of H₂ plus CO₂ to acetate. They catalyzed the dechlorination of methyl chloride with tetrahydrofolate as the methyl acceptor at a rate of 20 nmol/min × mg of cell protein. Also, the O-demethylation of vanillate with tetrahydrofolate could be measured at a rate of 40 nmol/min × mg. Different enzyme systems appeared to be responsible for the dehalogenation of CH₃Cl and for the O-demethylation of methoxylated aromatic compounds, since cells grown with methoxylated aromatic compounds exhibited a significantly lower activity of CH₃Cl conversion than methyl chloride grown cells and vice versa. In addition, ammonium thiocyanate (5 mM) completely inhibited CH₃Cl dechlorination, whereas the consumption of vanillate was not affected significantly. The data were taken to indicate, that the methyl chloride dehalogenation is catalyzed by a specific, inducible enzyme present in strain MC, and that tetrahydrofolate rather than the corrinoid-protein involved in acetate formation is the primary acceptor of the methyl group in the dechlorination reaction.     

Isolation of a dimethylsulfide-utilizingHyphomicrobium species and its application in biofiltration of polluted air

The methylotrophic bacteriumHyphomicrobium VS was enriched and isolated, using activated sewage sludge as inoculum in mineral medium containing dimethylsulfide (DMS) at a low concentration to prevent toxicity. DMS concentrations above 1 mM proved to be growth inhibiting.Hyphomicrobium VS could use DMS, dimethylsulfoxide (DMSO), methanol, formaldehyde, formate, and methylated amines as carbon and energy source. Carbon was assimilated via the serine pathway. DMS-grown cells respired sulfide, thiosulfate, methanethiol, dimethyldisulfide and dimethyltrisulfide.To testHyphomicrobium VS for application in biofiltration of air polluted with volatile sulfur compounds two laboratory scale trickling biofilters with polyurethane and lava stone as carrier material were started up by inoculation with this bacterium. Both methanol- and DMS-grown cells could be used. Only a short adaptation period was needed. Short term experiments showed that high concentrations of DMS (1–2 µmol 1^–1) were removed very efficiently by the biofilters at space velocities up to 100 h^–1.Abbreviations VSC volatile sulfur compounds - DMS dimethylsulfide - DMDS dimethyldisulfide - DMTS dimethyltrisulfide - MT methanethiol - DMSO dimethylsulfoxide     

Microbial transformations of methylated sulfur compounds in anoxic salt marsh sediments

Anoxic salt marsh sediments were amended with several methylated sulfur compounds. Sediment microbes transformed the added compounds into other volatile methylated sulfur compounds and eventually mineralized the compounds to CH₄ and presumably to CO₂ and H₂S. The principal methyl-sulfur product of dimethylsulfoniopropionate (DMSP) was found to be dimethylsulfide (DMS), with only small amounts of methane thiol (MSH) produced. By contrast, methionine and S-methyl cysteine were degraded mostly to MSH and to lesser amounts of DMS. Dimethylsulfoxide (DMSO) was biologically converted to DMS. Dimethyldisulfide (DMDS) was rapidly reduced to MSH by the sediment microflora, and some DMS was also produced. DMS, whether added directly or when derived from other precursors, was metabolized with the production of MSH. Methane thiol was also metabolized, and evidence suggests that MSH may be biologically methylated to form DMS. Experiments with selective microbial inhibitors were used to ascertain which microbial groups were responsible for the observed transformations. Based on these experiments, it appears that both sulfate-reducing and methane-producing bacteria may be involved in transforming and mineralizing methylated sulfur compounds. A simple scheme of how methylated sulfur compounds may be transformed in the environment is presented.     

Photocatabolism of Aromatic Compounds by the Phototrophic Purple Bacterium Rhodomicrobium vannielii

The phototrophic purple non-sulfur bacterium Rhodomicrobium vannielii grew phototrophically (illuminated anaerobic conditions) on a variety of aromatic compounds (in the presence of CO₂). Benzoate was universally photocatabolized by all five strains of R. vannielii examined, and benzyl alcohol was photocatabolized by four of the five strains. Catabolism of benzyl alcohol by phototrophic bacteria has not been previously reported. Other aromatic substrates supporting reasonably good growth of R. vannielii strains were the methoxylated benzoate derivatives vanillate (4-hydroxy-3-methoxybenzoate) and syringate (4-hydroxy-3,5-dimethoxybenzoate). However, catabolism of vanillate and syringate led to significant inhibition of bacteriochlorophyll synthesis in R. vannielii cells, eventually causing cultures to cease growing. No such effect on photopigment synthesis in cells grown on benzoate or benzyl alcohol was observed. Along with a handful of other species of anoxygenic phototrophic bacteria, the ability of the species R. vannielii to photocatabolize aromatic compounds indicates that this organism may also be ecologically significant as a consumer of aromatic derivatives in illuminated anaerobic habitats in nature.     

Isolation and characterization of a methyl chloride utilizing,strictly anaerobic bacterium

From sludge obtained from the sewage digester plant in Stuttgart-Möhringen a strictly anaerobic bacterium was enriched and isolated with methyl chloride as the energy source. The isolate, which was tentatively called strain MC, was nonmotile, gram-positive, and occurred as elongated cocci arranged in chains. Cells of strain MC formed about 3 mol of acetate per 4 mol of CH₃Cl consumed, indicating that the organism was a homoacetogenic bacterium fermenting methyl chloride plus CO₂ according to: The organism grew with 2–3% methyl chloride in the gas phase at a doubling time of near 30 h. Dichloromethane was not utilized. The bacterium also grew on carbon monoxide, H₂ plus CO₂, and methoxylated aromatic compounds. Optimal growth with methyl chloride was observed at 25°C and pH 7.3–7.7. The G+C-content of the DNA was 47.5±1.5%. The methyl chloride conversion appeared to be inducible, since H₂ plus CO₂-grown cells lacked this ability. From the morphological and physiological characteristics, the isolate could not be affiliated to a known species.     

Organic sulfur metabolisms in hydrothermal environments

Sulfur is central to the metabolisms of many organisms that inhabit extreme environments. While biotic and abiotic cycling of organic sulfur compounds has been well documented in low‐temperature anaerobic environments, cycling of organic sulfur in hydrothermal environments has received less attention. Recently published thermodynamic data have been used to estimate aqueous alkyl thiol and sulfide activities in deep‐sea hydrothermal systems. Here we use geochemical mixing models to predict fluid compositions that result from mixing end‐member hydrothermal fluid from the East Pacific Rise with bottom seawater. These fluid compositions are combined with estimates of methanethiol and dimethylsulfide activities to evaluate energy yields for potential organic sulfur‐based metabolisms under hydrothermal conditions. Aerobic respiration has the highest energy yields (over ?240 kJ/mol e^?) at lower temperature; however, oxygen is unlikely to persist at high temperatures, restricting aerobic respiration to mesophilic communities. Nitrite reduction to N₂ has the highest energy yields at higher temperatures (greater than ～40 °C). Nitrate and nitrite reduction to ammonium also yield significant energy (up to ?70 kJ/mol e^?). Much lower, but still feasible energy yields are calculated for sulfate reduction, disproportionation, and reduction with H₂. Organic compound family and the activity of methanethiol and dimethylsulfide were less important than metabolic strategy in determining overall energy yields. All metabolic strategies considered were exergonic within some portion of the mixing regime suggesting that organic sulfur‐based metabolisms may be prevalent within deep‐sea hydrothermal vent microbial communities.     

C1-cycle of sulfur compounds

C₁ organic sulfides are part of many ecosystems and play an important role in the global sulfur budget and climate regulation. At this point, fluxes and conversions of these compounds are only superficially understood. Understanding of the regulating mechanisms will be necessary to quantify the role of these compounds in the global sulfur budget at their climatic role. In this review, the current knowledge of fluxes and conversions of C₁ organic sulfides in different ecosystems is presented.Abbreviations CCN cloud condensation nuclei - COS carbonylsulfide - DMS dimethylsulfide - DMDS dimethyldisulfide - DMSO dimethylsulfoxide - DMSO₂ dimethylsulfurdioxide - DMSP dimethylsulfoniopropionate - MA methylamine - 3-MPA 3-mercaptopropionate - MPPA 3-methiolpropionate - MT methanethiol     

Eubacterium aggreganssp. nov., a New Homoacetogenic Bacterium from Olive Mill Wastewater Treatment Digestor

A strictly anaerobic, homoacetogenic, Gram-positive, non spore-forming bacterium, designated strain SR12^T(T=type strain), was isolated from an anaerobic methanogenic digestor fed with olive mill wastewater. Yeast extract was required for growth but could also be used as sole carbon and energy source. Strain SR12^Tutilized a few carbohydrates (glucose, fructose and sucrose), organic compounds (lactate, crotonate, formate and betaine), alcohols (methanol), the methoxyl group of some methoxylated aromatic compounds, and H₂+CO₂. The end-products of carbohydrate fermentation were acetate, formate, butyrate, H₂and CO₂. End-products from lactate and methoxylated aromatic compounds were acetate and butyrate. Strain SR12^Twas non-motile, formed aggregates, had a G+C content of 55 mol % and grew optimally at 35°C and pH 7.2 on a medium containing glucose. Phylogenetically, strain SR12^Twas related toEubacterium barkeri, E. callanderi, andE. limosumwithE. barkerias the closest relative (similarity of 98%) with which it bears little phenotypic similarity or DNA homology (60%). On the basis of its phenotypic, genotypic, and phylogenetic characteristics, we propose to designate strain SR12^TasEubacterium aggreganssp. nov. The type strain is SR12^T(=DSM 12183).     

Obligate Sulfide-Dependent Degradation of Methoxylated Aromatic Compounds and Formation of Methanethiol and Dimethyl Sulfide by a Freshwater Sediment Isolate, Parasporobacterium paucivorans gen. nov., sp. nov.

Methanethiol (MT) and dimethyl sulfide (DMS) have been shown to be the dominant volatile organic sulfur compounds in freshwater sediments. Previous research demonstrated that in these habitats MT and DMS are derived mainly from the methylation of sulfide. In order to identify the microorganisms that are responsible for this type of MT and DMS formation, several sulfide-rich freshwater sediments were amended with two potential methyl group-donating compounds, syringate and 3,4,5-trimethoxybenzoate (0.5 mM). The addition of these methoxylated aromatic compounds resulted in excess accumulation of MT and DMS in all sediment slurries even though methanogenic consumption of MT and DMS occurred. From one of the sediment slurries tested, a novel anaerobic bacterium was isolated with syringate as the sole carbon source. The strain, designated Parasporobacterium paucivorans, produced MT and DMS from the methoxy groups of syringate. The hydroxylated aromatic residue (gallate) was converted to acetate and butyrate. Like Sporobacterium olearium, another methoxylated aromatic compound-degrading bacterium, the isolate is a member of the XIVa cluster of the low-GC-content Clostridiales group. However, the new isolate differs from all other known methoxylated aromatic compound-degrading bacteria because it was able to degrade syringate in significant amounts only in the presence of sulfide.     

Selective isolation of Acetobacterium woodii on methoxylated aromatic acids and determination of growth yields

Anaerobic enrichments with methoxylated aromatic compounds as substrates (vanillate, syringate, trimethoxycinnamate) were inoculated from freshwater mud and sewage sludge samples. In 12 out of 16 cultures the same type of rod-shaped, motile bacteria was selectively enriched. Two strains, NZva16 and NZva24, were isolated in pure culture and recognized as Acetobacterium woodii by comparison with the type strain (DSM 1030).All three Acetobacterium strains were able to grow with all 10 of the tested aromatic compounds containing methoxyl groups. In the presence of bicarbonate, these substrates were used as sole organic electron donors and carbon sources. UV-absorption spectra revealed that the aromatic rings were not degraded, and that the corresponding hydroxy derivatives of the methoxylated compounds were formed. The only further fermentation product formed was acetate. When equimolar concentrations of the methoxylated benzoic acid derivatives were applied, the growth yields were proportional to the number of methoxyl groups per molecule. Methoxyl groups or methanol were metabolized by homoacetate fermentation: in the presence of bicarbonate 4 mol of acetate. In case of the methoxylated cinnamic acid derivatives less acetate was formed and the corresponding hydroxy derivatives of phenylpropionic acid appeared as a result of the double bond reduction in the acrylate side chain. In comparison to the benzoate derivatives with the same number of methoxyl groups, higher growth yields were obtained with the cinnamate derivatives.     

Anaerobic degradation of phenylacetate and 4-hydroxyphenylacetate by denitrifying bacteria

From various oxic or anoxic habitats anaerobic enrichment cultures were set up which completely oxidized aromatic amino acids to CO₂ with nitrate as electron acceptor. Tyrosine and tryptophan at first were degraded to phenol and indole, respectively, prior to utilization of the aromatic ring; with phenylalanine no intermediates were detected. Attempts to isolate denitrifying bacteria able to completely degrade aromatic amino acids were unsuccessful. Starting with these enrichments several strains of denitrifying bacteria were anaerobically enriched and isolated with known fermentation products of amino acids (phenylacetate, 4-OH-phenylacetate, 2-OH-benzoate) plus nitrate as sole sources of carbon and energy.Three strains were characterized further. They grew well in defined mineral salts medium, were gram-negative and facultatively anaerobic with strictly oxidative metabolism; molecular oxygen, nitrate or nitrite served as electron acceptors. The isolates were tentatively identified as pseudomonads, but could not be aligned to known species. They oxidized a variety of aromatic compounds completely to CO₂ anaerobically and, with some exceptions, also aerobically. The substrates included among others: (4-OH)-phenylacetate, (4-OH)-phenylglyoxylate, benzoate, 2-aminobenzoate, phenol, OH-benzoates, indole and notably toluene. Reduced alicyclic compounds were not utilized. During anaerobic degradation of (4-OH)-phenylacetate transient accumulation of (4-OH)-phenylglyoxylate was observed.It is proposed that anaerobic -oxidation of the-CH₂–COOH side chain to -CO–COOH initiates anaerobic degradation of (4-OH)-phenylacetate. This implies a novel type of anaerobic -hydroxylation with water as the oxygen donor. Abbreviation. Hydroxyl groups were abbreviated as OH     

Anaerobic and aerobic metabolism of diverse aromatic compounds by the photosynthetic bacterium Rhodopseudomonas palustris.

The purple nonsulfur photosynthetic bacterium Rhodopseudomonas palustris used diverse aromatic compounds for growth under anaerobic and aerobic conditions. Many phenolic, dihydroxylated, and methoxylated aromatic acids, as well as aromatic aldehydes and hydroaromatic acids, supported growth of strain CGA001 in both the presence and absence of oxygen. Some compounds were metabolized under only aerobic or under only anaerobic conditions. Two other strains, CGC023 and CGD052, had similar anaerobic substrate utilization patterns, but CGD052 was able to use a slightly larger number of compounds for growth. These results show that R. palustris is far more versatile in terms of aromatic degradation than had been previously demonstrated. A mutant (CGA033) blocked in aerobic aromatic metabolism remained wild type with respect to anaerobic degradative abilities, indicating that separate metabolic pathways mediate aerobic and anaerobic breakdown of diverse aromatics. Another mutant (CGA047) was unable to grow anaerobically on either benzoate or 4-hydroxybenzoate, and these compounds accumulated in growth media when cells were grown on more complex aromatic compounds. This indicates that R. palustris has two major anaerobic routes for aromatic ring fission, one that passes through benzoate and one that passes through 4-hydroxybenzoate.     

Isolation from a methanogenic ferulate degrading consortium of an anaerobe that converts methoxyl groups of aromatic acids to volatile fatty acids

An anaerobic, non-motile, rod shaped bacterium is described which cleaves the phenylether bonds of methoxylated aromatic substrates to give the corresponding hydroxy aromatic derivatives and mixed volatile fatty acids, chain length, C₁, C₂ and C₄. The bacterium was isolated from an anaerobic digestor fed with contents from a wood fiber to alcohol fermentation plant, using anaerobic rolltube medium with ferulate as the carbon and energy source. Moles fatty acid produced per 100 mole of methoxyl group of aromatic substrate fermented were approximately: acetate, 14; butyrate, 18; and formate, 15. For the fermentation of equimolar amounts of methoxylated aromatic compounds, growth yields were proportional to the number of methoxylated groups per molecule, and the amount of cells per methoxyl group did not alter when phenylacrylate derivatives were used as substrates. The organism was unable to reduce the side-chain double bond of phenylacrylate derivatives. Coculture of the bacterium on ferulate with Methanospirillum hungatei, or Desulfovibrio in the presence of SO ₄ ⁼ resulted in no nett production of formate, and small quantities of methane and sulfide were produced respectively. The isolate utilized glucose, fructose, and lactate, but not methanol or H₂–CO₂ as growth substrates. Lactate, butyrate, acetate, formate and small quantities of H₂ were produced from glucose fermentation. No reduction of SO ₄ ⁼ or NO ₃ ^- occurred during fermentation of glucose or methoxylated aromatics and no growth occurred in the presence of oxygen.     

Methanethiol utilization and sulfur reduction by anaerobic halophilic saccharolytic bacteria

A number of sulfur compounds were tested as sulfur sources for the growth of three strains of anaerobic halophilic saccharolytic bacteria isolated from hypersaline water bodies of the eastern Crimea (USSR). Dithionite and sulfite at 1 mM concentration completely inhibited the growth of all strains. Methanethiol turned out to be the sole sulfur source for growth ofHalobacteroides strains in the defined medium with glucose and leucine. Methanethiol also stimulated growth of cultures in the complex medium with yeast extract. TheHaloincola saccharolytica Z-7787 appeared to be capable of methanethiol formation from methionine. All organisms studied were capable of heterotrophic sulfur reduction, producing up to 13 mM H₂S, but no evidence that they gain energy from the process has been obtained. The extremely halophilicHalobacteroides lacumaris may participate in sulfidogenesis at the high salinity (20–30% NaCl). The ecological position of haloanaerobes in halophilic community is discussed.     

Purification and characterization of dimethylsulfide monooxygenase from Hyphomicrobium sulfonivorans

Dimethylsulfide (DMS) is a volatile organosulfur compound which has been implicated in the biogeochemical cycling of sulfur and in climate control. Microbial degradation is a major sink for DMS. DMS metabolism in some bacteria involves its oxidation by a DMS monooxygenase in the first step of the degradation pathway; however, this enzyme has remained uncharacterized until now. We have purified a DMS monooxygenase from Hyphomicrobium sulfonivorans, which was previously isolated from garden soil. The enzyme is a member of the flavin-linked monooxygenases of the luciferase family and is most closely related to nitrilotriacetate monooxygenases. It consists of two subunits: DmoA, a 53-kDa FMNH₂-dependent monooxygenase, and DmoB, a 19-kDa NAD(P)H-dependent flavin oxidoreductase. Enzyme kinetics were investigated with a range of substrates and inhibitors. The enzyme had a K_m of 17.2 (± 0.48) μM for DMS (k_cat = 5.45 s⁻¹) and a V_max of 1.25 (± 0.01) μmol NADH oxidized min⁻¹ (mg protein⁻¹). It was inhibited by umbelliferone, 8-anilinonaphthalenesulfonate, a range of metal-chelating agents, and Hg²⁺, Cd²⁺, and Pb²⁺ ions. The purified enzyme had no activity with the substrates of related enzymes, including alkanesulfonates, aldehydes, nitrilotriacetate, or dibenzothiophenesulfone. The gene encoding the 53-kDa enzyme subunit has been cloned and matched to the enzyme subunit by mass spectrometry. DMS monooxygenase represents a new class of FMNH₂-dependent monooxygenases, based on its specificity for dimethylsulfide and the molecular phylogeny of its predicted amino acid sequence. The gene encoding the large subunit of DMS monooxygenase is colocated with genes encoding putative flavin reductases, homologues of enzymes of inorganic and organic sulfur compound metabolism, and enzymes involved in riboflavin synthesis.Dimethylsulfide (DMS) is a volatile organosulfur compound, important in the biogeochemical cycling of sulfur and global climate regulation (4, 9). Bacterial metabolism of DMS is an important sink of the compound in nature and is thought to account for degradation of over 80% of the DMS produced in the marine environment. Although bacterial pathways of DMS degradation have been studied previously in Hyphomicrobium spp. and in Thiobacillus spp. (12, 36), they remain poorly characterized, and few enzymes of DMS metabolism have been purified (see reference 32). DMS monooxygenase was first reported from an assay of NADH-dependent oxygen uptake in the presence of DMS by cell extracts of Hyphomicrobium S (12), an activity also demonstrated in cell extracts of other Hyphomicrobium, Thiobacillus, and Arthrobacter isolates (6, 7, 34), with specific activities around 30 nmol NADH oxidized min⁻¹ mg protein⁻¹. The enzyme has not previously been purified or characterized.The aims of this study were to purify and characterize the DMS monooxygenase enzyme from a member of the genus Hyphomicrobium. Since Hyphomicrobium S is no longer available, studies were undertaken using the type strain of H. sulfonivorans. The strain was originally isolated from garden soil and grows on DMS, as well as the related compounds dimethyl sulfoxide (DMSO) and dimethylsulfone (DMSO₂). During growth on DMSO₂, H. sulfonivorans first reduces DMSO₂ to DMSO by a dimethylsulfone reductase, and subsequently a DMSO reductase converts DMSO to DMS, which is further oxidized to methanethiol and formaldehyde by a DMS monooxygenase. Oxidation of methanethiol to formaldehyde by methanethiol oxidase yields another mole of formaldehyde, which is either assimilated into biomass or oxidized to carbon dioxide to provide reducing equivalents (Fig. ​(Fig.1).1). DMS monooxygenase activity is present in the soluble protein fraction during growth on these compounds (6, 7). A 53-kDa polypeptide was previously observed in organisms grown on DMS, DMSO, and DMSO₂ (6, 7), but its significance in the metabolism of these compounds was unknown.Open in a separate windowFIG. 1.Pathway and enzymes of dimethylsulfone degradation in Hyphomicrobium sulfonivorans S1. Reduction of dimethylsulfone [DMSO₂; (CH₃)₂SO₂] to dimethyl sulfoxide [DMSO; (CH₃)₂SO] and further reduction of DMSO to dimethylsulfide provides the substrate for DMS monooxygenase. Formaldehyde is either assimilated (via the serine cycle) or oxidized to CO₂ providing reducing equivalents. Sulfide is oxidized to sulfate; see reference 7 for further details.     

Demethylation of aromatic compounds by strain B10 and complete degradation of 3-methoxybenzoate in co-culture with Desulfosarcina strains

Summary A pure culture presumably of an Acetobacterium sp. from a waste water pond, strain B10, was able to grow with several methoxylated aromatic compounds by demethylation (or demethoxylation) to the corresponding hydroxilated substances. Acetate was formed from the eliminated methyl or methoxy groups and from CO₂. Demethylation of 3-methoxybenzoate occurred simultaneously with glucose or lactate fermentation if induced, methanol-grown cells of strain B10 were used as an inoculum. If 2-vanillin or 2,3-dimethoxybenzaldehyde were supplied as the only carbon sources, these substances were first oxidized to the corresponding benzoic acid derivatives and subsequently demethylated. In mixed cultures of strain B10 and Desulfosarcina variabilis or Desulfosarcina strain DSU3 the 3-hydroxybenzoate formed by strain B10 from 3-methoxybenzoate was completely degraded to acetate and presumably CO₂ by the sulphate reducers. Acetate could be oxidized to CO₂ upon extended incubation. The complete degradation of 3-methoxybenzoate to CO₂ by co-cultures of strain B10 and Desulfosarcina strains seemed to proceed via a commensalistic, rather than via a syntrophic interaction of the participating organisms. Offprint requests to: J. Winter     

Investigation of mercaptans,organic sulfides,and inorganic sulfur compounds as sulfur sources for the growth of methanogenic bacteria

A variety of compounds were investigated for use as sulfur sources for the growth of methanogenic bacteria.Methanococcus (Mc.) deltae, Mc. maripaludis, Methanobacterium (Mb.) speciesGC-2B, GC-3B, andMMY, Methanobrevibacter (Mbr.) ruminantium, andMethanosarcina (Ms.) barkeri strain 227 grew well with sulfide, S^o, thiosulfate, or cysteine as sole sulfur source.Mbr. ruminatium was able to grow on SO ₄ ⁼ or SO ₃ ⁼ , andMs. barkeri strain 227 was able to grow on SO ₃ ⁼ , but not on SO ₄ ⁼ as a sole sulfur source.Mc. jannaschii grew with sulfide, S^o, thiosulfate or SO ₃ ⁼ , but not on cysteine or SO ₄ ⁼ as sole surface source.Mc. thermolithotrophicus, Mc. jannaschii, Mc. deltae, andMb. thermoautotrophicum strains Marburg and H were able to grow with methanethiol, ethanethiol,n-propanethiol,n-butanethiol, methyl sulfide, dimethyl sulfoxide, ethyl sulfide, or CS₂ as a sulfur source, when very low levels (20–30 M) of sulfide were present; no growth occurred on 5–100 M sulfide alone. Methanethiol, ethanethiol, and methyl sulfide-using cultures produced sulfide during growth.