Properties of the membranes containing the particulate methane monooxygenase from Methylosinus trichosporium OB3b

The particulate methane monooxygenase (pMMO) from Methylosinus trichosporium OB3b was partiallypurified and characterized by measuring the effects of reducing agents and additives, and the stability ofpMMO was studied. Duroquinol was a suitable reducing agent, and pMMO was stabilized by bovine serumalbumin (BSA). Among the additivies, the copper (II) ion stimulated pMMO at low concentration andinhibited at high concentration. The optimum conditions for pMMO activity were as follows: 45 ° C, pH 6.5and 55 mM 3-morpholinopropanesulfonic acid (MOPS) buffer, and the rate of propene epoxide formationwas 13.6 nmol min mg protein. ESR spectra indicate that the copper cluster in the membrane fraction isreduced by duroquinol and oxidized by dioxygen. The result suggests that the copper cluster is containedin the active site of pMMO.     

Redox behavior of copper in particulate methane monooxygenase from Methylosinus trichosporium OB3b

The redox properties of the copper in particulate methane monooxygenase from Methylosinus trichosporium OB3b were investigated. The ESR spectrum of the pMMO-containing membranes from M. trichosporium OB3b indicated a typical type II copper (II) signal (g = 2.24, A = 18.4 mT, g = 2.06, ₂= 0.84). By anaerobic addition of excess amounts of duroquinol, an optimum reductant of pMMO, the ESR spectra indicated that the copper cluster in membranes was reduced and successively oxidized by dioxygen, a substrate of pMMO. The result suggests that the copper is the active site of pMMO or an electron carrier. During the titration, the intensity of the type II copper signal decreased with decreasing potential and the multiple hyperfine structure at g = 2.06 appeared clearly. Although the copper signal did not change by treatment of the EDTA-treated membranes with duroquinol and dioxygen, the copper signal intensity decreased with decreasing potential in the redox titration. These results suggest that some redox mediators play a role as an electron carrier between the active site and a reductant, and the presence of at least two types of copper sites in pMMO- containing membranes. On the basis of the ESR spectra of the EDTA-treated membranes and the as-isolated membranes, it is concluded that one type of the copper sites functions as the active site of pMMO (A-site), and the other type of copper sites plays a role as an electron carrier (E-site)     

Role of iron in particulate methane monooxygenase from Methylosinus trichosporium OB3b

The effect of iron ions on particulate methane monooxygenase was studied by using the EDTA-treated membranes from Methylosinus trichosporium OB3b. When the membrane was treated with EDTA the activity remained 82% of the as-isolated membranes, and the activity of the EDTA-treated membranes was strongly influenced by the addition of metal ions. Among the metal ions, ferric, ferrous and cupric ions stimulated the activity, indicating those ions were needed for the activity. When propargylamine was added, pMMO activity decreased and also the iron ESR signal decreased. As the ESR signal involves the ferrous nitrosyl complex in EDTA-treated membranes, the active site of pMMO may contain a mononuclear non-heme iron.     

Functional expression of the particulate methane mono-oxygenase gene in recombinant Rhodococcus erythropolis

In order to construct an expression system for the particulate methane mono-oxygenase (pMMO) gene (pmo), the structural gene cluster pmoCAB amplified from Methylosinus trichosporium OB3b was inserted into a shuttle vector pBS305 under the control of a dsz promoter and transformed into Rhodococcus erythropolis LSSE8-1. A stable transformant was successfully obtained using ethane as the sole carbon source. Fluorescence in situ hybridization results showed that the dsz promoter allowed the pmo genes to be transcribed in the recombinant strain. The effects of Cu2+ and Zn2+ concentrations on cell growth and pMMO activity in ethane-containing medium were examined. It was discovered that 7.5 microM Cu2+ and 1.8 microM Zn2+ were suitable to achieve high cell concentration and pMMO activity, but the amount of methanol accumulated during methane oxidation by the recombinant strain was still low.     

Mass spectrometric measurements of methane and oxygen utilization by methanotrophic bacteria

Abstract A mass spectrometer with membrane inlet was used to measure methane and oxygen utilization rates at various methane concentrations in Methylosinus trichosporium and a locally isolated strain of a methane-oxidizing coccus (OU-4-1). The apparent K _m for methane was found to be 2 μM for M. trichosporium and 0.8 μM for strain OU-4-1. These K _m-values are 10–30 times lower than most previously reported values. The ratio of oxygen to methane utilization rates was 1.7 for M. trichosporium and 1.5 for strain OU-4-1 corresponding to a growth yield of 0.38 and 0.63 g dry weight/g methane, respectively.     

Spectral and thermodynamic properties of Ag(I), Au(III), Cd(II), Co(II), Fe(III), Hg(II), Mn(II), Ni(II), Pb(II), U(IV), and Zn(II) binding by methanobactin from Methylosinus trichosporium OB3b

Methanobactin (mb) is a novel chromopeptide that appears to function as the extracellular component of a copper acquisition system in methanotrophic bacteria. To examine this potential physiological role, and to distinguish it from iron binding siderophores, the spectral (UV–visible absorption, circular dichroism, fluorescence, and X-ray photoelectron) and thermodynamic properties of metal binding by mb were examined. In the absence of Cu(II) or Cu(I), mb will bind Ag(I), Au(III), Co(II), Cd(II), Fe(III), Hg(II), Mn(II), Ni(II), Pb(II), U(VI), or Zn(II), but not Ba(II), Ca(II), La(II), Mg(II), and Sr(II). The results suggest metals such as Ag(I), Au(III), Hg(II), Pb(II) and possibly U(VI) are bound by a mechanism similar to Cu, whereas the coordination of Co(II), Cd(II), Fe(III), Mn(II), Ni(II) and Zn(II) by mb differs from Cu(II). Consistent with its role as a copper-binding compound or chalkophore, the binding constants of all the metals examined were less than those observed with Cu(II) and copper displaced other metals except Ag(I) and Au(III) bound to mb. However, the binding of different metals by mb suggests that methanotrophic activity also may play a role in either the solubilization or immobilization of many metals in situ.     

Improvement of the purification method for retaining the activity of the particulate methane monooxygenase from Methylosinus trichosporium OB3b

The purification method of particulate methane monooxygenase (pMMO) from Methylosinus trichosporium OB3b was improved, and purified pMMO retained its activity with duroquinol as a reductant. n-Dodecyl-,d-maltoside was used for the solubilization of pMMO and Brij 58 was used for the purification for anion exchange chromatography. Compared to the original pMMO activity in the membrane fraction, 88% of the activity was now retained in the purified material. The purified pMMO monomer (94 kDa) contained only two copper atoms and did not contain iron. Both copper ions showed only a typical type II copper EPR signal with a superhyperfine structure at the g region, indicating that the type II copper ions play an important role as the active site of methane hydroxylation in pMMO.     

Co-metabolic biodegradation of trichloroethylene by Methylosinus trichosporium is stimulated by low concentrations methane or methanol

Co-metabolic biodegradation of trichloroethylene by Methylosinus trichosporium OB3b was stimulated by low concentrations of methane (up to 70 M) or methanol (up to 0.4 mM) but inhibited at higher concentrations of them. A kinetic equation describing the dual effects of methane or methanol is proposed and the relevant kinetic constants have been determined.     

Use of allylthiourea to produce soluble methane monooxygenase in the presence of copper

Methanotrophs expressing soluble methane monooxygenase (sMMO) may find use in a variety of industrial applications. However, sMMO expression is strongly inhibited by copper, and the growth rate may be limited by the aqueous solubility of methane. In this study, addition of allylthiourea decreased intracellular copper in Methylosinus trichosporium OB3b, allowing sMMO production at Cu/biomass ratios normally not permitting sMMO synthesis. The presence of about 1.5 μmoles intracellular Cu g⁻¹ dry biomass resulted in sMMO activity of about 250 μmoles 1-napthol formed per hour gram dry biomass whether this intracellular Cu concentration was achieved by Cu limitation or by allylthiourea addition. No loss of sMMO activity occurred when the growth substrate was switched from methane to methanol when allylthiourea had been added to growth medium containing copper. Addition of copper to medium that was almost copper-free increased the yield of dry biomass from methanol from 0.20 to 0.36 g g⁻¹, demonstrating that some copper was necessary for good growth. This study demonstrated a method by which sMMO can be produced by M. trichosporium OB3b while growing on methanol in copper-containing medium.     

Optimization of methanol biosynthesis from methane using Methylosinus trichosporium OB3b

Methylosinus trichosporium OB3b oxidized methane to methanol in the presence of a high concentration of Cu2+. Further oxidation of methanol to formaldehyde was prevented by adding 200 mM NaCl which acted as a methanol dehydrogenase H inhibitor. The bacterium, 0.6 mg dry cell ml(-1), in methane/air (1:4, v/v) at 25 degrees C in 12.9 mM phosphate buffer (pH 7) containing 20 mM sodium formate and 200 mM NaCl accumulated 7.7 mM methanol over 36 h.     

High-rate conversion of methane to methanol by Methylosinus trichosporium OB3b

Methanol was produced from methane with a high conversion rate using a high cell density process with Methylosinus trichosporium OB3b in the presence of a high concentration of phosphate buffer. More than 1.1 g/L methanol accumulated in the reaction media under optimized reaction conditions (17 g dry cell/L, 400 mmol/L phosphate, and 10 mmol/L MgCl₂) in the presence of 20 mmol/L sodium formate. The conversion rate of methane was over 60%. About 0.95 g/L methanol was produced when the biotransformation was carried out in a membrane aerated reactor into which methane and oxygen were introduced via two separate dense silicone tubing. Our results provide an efficient method and a promising process for high-rate conversion of methane to methanol.     

Evaluation of transformation capacity for degradation of ethylene chlorides by<Emphasis Type="Italic">Methylosinus trichosporium</Emphasis> OB3b

The transformation capacity (T_c) ofMethylosinus trichosporium OB3b in the degradation of ethylene chlorides was determined by measuring the decrease of soluble methane monooxygenase (sMMO) activity of resting cells in batch experiments. All measurements of sMMO activity were taken in the presence of 20 mM formate to avoid the deficiency of reducing power, and within 2 hrs to avoid the effect of natural inactivation from instability of the resting cells. The constant T_c values of 0.58±0.132 and 0.80±0.17 μmol/mg cell were obtained for trichloroethylene (TCE) and 1,2-dichloroethylene (cis andtrans-1,2-DCE), respectively, regardless of their concentrations. The transformation capacity measured by this method can be used to predict the amount of cells that should be stimulated inin-situ bioremediation.     

Optimization of trichloroethylene oxidation by methanotrophs and the use of a colorimetric assay to detect soluble methane monooxygenase activity

Methylosinus trichosporium OB3b biosynthesizes a broad specificity soluble methane monooxygenase that rapidly oxidizes trichloroethylene (TCE). The selective expression of the soluble methane monooxygenase was followed in vivo by a rapid colorimetric assay. Naphthalene was oxidized by purified soluble methane monooxygenase or by cells grown in copper-deficient media to a mixture of 1-naphthol and 2-naphthol. The naphthols were detected by reaction with tetrazotized o-dianisidine to form purple diazo dyes with large molar absorptivities. The rate of color formation with the rapid assay correlated with the velocity of TCE oxidation that was determined by gas chromatography. Both assays were used to optimize conditions for TCE oxidation by M. trichosporium OB3b and to test several methanotrophic bacteria for the ability to oxidize TCE and naphthalene.Abbreviations A₆₀₀ absorbance due to cell density measured at 600 nm - HPLC high pressure liquid chromatography - NADH reduced nicotinamide adenine dinucleotide - SDS-PAGE sodium dodecyl sulfate polyacrylamide gel electrophoresis - sMMO soluble methane monooxygenase - TCE trichloroethylene     

Spectral and thermodynamic properties of Ag(I), Au(III), Cd(II), Co(II), Fe(III), Hg(II), Mn(II), Ni(II), Pb(II), U(IV), and Zn(II) binding by methanobactin from Methylosinus trichosporium OB3b

Methanobactin (mb) is a novel chromopeptide that appears to function as the extracellular component of a copper acquisition system in methanotrophic bacteria. To examine this potential physiological role, and to distinguish it from iron binding siderophores, the spectral (UV–visible absorption, circular dichroism, fluorescence, and X-ray photoelectron) and thermodynamic properties of metal binding by mb were examined. In the absence of Cu(II) or Cu(I), mb will bind Ag(I), Au(III), Co(II), Cd(II), Fe(III), Hg(II), Mn(II), Ni(II), Pb(II), U(VI), or Zn(II), but not Ba(II), Ca(II), La(II), Mg(II), and Sr(II). The results suggest metals such as Ag(I), Au(III), Hg(II), Pb(II) and possibly U(VI) are bound by a mechanism similar to Cu, whereas the coordination of Co(II), Cd(II), Fe(III), Mn(II), Ni(II) and Zn(II) by mb differs from Cu(II). Consistent with its role as a copper-binding compound or chalkophore, the binding constants of all the metals examined were less than those observed with Cu(II) and copper displaced other metals except Ag(I) and Au(III) bound to mb. However, the binding of different metals by mb suggests that methanotrophic activity also may play a role in either the solubilization or immobilization of many metals in situ.     

Quantification of methane oxidation in the rice rhizosphere using 13C-labelled methane

In this paper isotope ratio mass spectrometry is used to determine the methane (CH₄) oxidation fraction in the rhizosphere of intact rice plant-soil systems. Earlier studies on quantification of the methane oxidation were based on inhibition or incubation procedures which strongly interfered with the plant-soil system and resulted in a large variability of the reported fractions, while other studies considered stable isotopes at natural abundance levels to investigate methanotrophy in the rhizosphere of rice. The current work is the first that used ¹³C-labelled CH₄ as additive and calculated the oxidation fraction from the ratio between the added ¹³C-labelled CH₄ and its oxidation product ¹³CO₂. Both labelled gases could be distinguished from the natural abundance percentages. The oxidation fraction for methane was found to be smaller than 7%, suggesting that former approaches overestimate the methane oxidation fraction.     

Effects of oxygen and nitrogen conditions on the transformation kinetics of 1,2-dichloroethenes by Methylosinus trichosporium OB3b and its sMMO C mutant

Transformation kinetics of trans- andcis-dichloroethylenes (DCE) by Methylosinus trichosporium OB3b wild type (WT)and PP319, a mutant that expresses soluble methane monooxygenase at copper levels upto 12 M Cu (sMMO^C), were determined to assess theeffects of O₂level and N₂-fixation on degradationcapabilities. Two issues were examined: (1) the influence of O₂level and nitrogen-limitation on DCE degradationkinetics and toxicity in both organisms, and (2) the relative utility of PP319 forcontaminant degradation in bioreactors. When both organisms were grown underhigh O₂conditions (80% saturation in air), maximum transformation rates(V_max) and apparent first-order rate constants(V_max/K_M) were lower compared with organisms grown under low O₂conditions (10% saturation in air)regardless of nitrogen level. Further, V_max values were near zero innitrogen-limited WT cultures when O₂was high (as expected), whereas PP319 retainedmoderate V_max levels even at high O₂levels. In general, elevatedO₂conditions reduced DCE degradation rates in OB3b, although the negative effectsof O₂were less in PP319 than in the WT. Given that PP319 retained moderate DCEdegradation rates under most O₂and copper conditions, the mutant appears to havesome utility for biodegradation applications.     

Release of fossil methane from mineral soil particles, and its implication for estimation of methane oxidation in a mineral subsoil

In a preliminary experiment we found that methane evolved from a sandy subsoil during aerobic incubation of shaken soil slurries. In the study presented here the methane was found to be released from the sand particles by mechanical weathering, caused by the grinding effect of the shaking. Large amounts of gas (about 0.5 ml gas g^–1 soil) were extracted by intense grinding of the soil in gas tight serum vials. Methane was the main hydrocarbon in the emitted gas, but also a considerable amount of ethane was present, as well as minor amounts of heavier hydrocarbons (up to C₆). The ¹³C-values of the emitted methane and ethane were –33 and –29 , respectively. Together these results demonstrate a thermogenic origin of the gas. This paper also reports the results of an incubation experiment where possible methane oxidation was looked for. If a possible release of methane is not accounted for, methane oxidation may be overlooked, as illustrated in this paper. Methane consumption was detected only in soil from 40 cm, in contrast to soil sampled at 100 cm and deeper where a slight production was measured. When methane oxidation was inhibited by dimethyl-ether, a significant release of methane was seen. The release was probably caused by chemical weathering. When this methane release was taken into account, methane oxidation was found to be present at all measured depths (40 to 200 cm). Fertilization with urea inhibited the methane oxidation at 40 cm but not at deeper layers. It is hypothesized that ammonia oxidizing bacteria were the main methane oxidizers in this mineral subsoil (deeper than 1 m), and that oxidation of methane might be a survival mechanism for ammonia oxidizers in ammonia limited environments.