Detection of Methane Oxidizing Bacteria in Forest Soil by Monooxygenase PCR Amplification.

Atmospheric methane oxidation by a spruce forest soil from Norway at 15 degrees C was found to be maximal at a depth of ca 7 cm. Examination of the kinetics of this methane oxidation revealed an apparent K(m) of 403.1 nM and a V(max) of 2.2 nmol g(-1) dry weight soil h(-1). The low apparent K(m) suggested the presence of active methane oxidizing bacteria with a high affinity for methane. DNA was extracted from the 5-10 cm horizon, purified, and subjected to PCR amplification with primers directed toward the monooxygenase genes pmoA and amoA, which are essential for methane oxidation. Hybridization analysis of the clone library subsequently constructed revealed that 49% of the 76 cloned PCR fragments were putative methanotroph pmoA sequences and 16% were putative ammonium oxidizing nitrifier amoA sequences. Sequencing of 28 clones identified three major groups showing homology to pmoA from Methylococcus capsulatus, beta-subdivision ammonia-oxidizers (amoA), and a new group of monooxygenase pmoA/amoA sequences.

Fluorescent oligonucleotide rDNA probes for specific detection of methane oxidising bacteria.

Oligonucleotide probes targeting the 16S rRNA of distinct phylogenetic groups of methanotrophs were designed for the in situ detection of these organisms. A probe, MG-64, detected specifically type I methanotrophs, while probes MA-221 and MA-621, detected type II methanotrophs in whole cell hybridisations. A probe Mc1029 was also designed which targeted only organisms from the Methylococcus genus after whole cell hybridisations. All probes were labelled with the fluorochrome Cy3 and optimum conditions for hybridisation were determined. Non-specific target sites of the type I (MG-64) and type II (MA-621) probes to non-methanotrophic organisms are highlighted. The probes are however used in studying enrichment cultures and environments where selective pressure favours the growth of methanotrophs over other organisms. The application of these probes was demonstrated in the detection of type I methanotrophs with the MG-64 probe in an enrichment culture from an estuarine sample demonstrating methane oxidation. The detection of type I methanotrophs was confirmed by a 16S rDNA molecular analysis of the estuarine enrichment culture which demonstrated that the most abundant bacterial clone type in the 16S rDNA library was most closely related to Methylobacter sp. strain BB5.1, a type I methanotroph also isolated from an estuarine environment.

Microbial metabolism of methanesulfonic acid

Methanesulfonic acid is a very stable strong acid and a key intermediate in the biogeochemical cycling of sulfur. It is formed in megatonne quantities in the atmosphere from the chemical oxidation of atmospheric dimethyl sulfide (most of which is of biogenic origin) and deposited on the Earth in rain and snow, and by dry deposition. Methanesulfonate is used by diverse aerobic bacteria as a source of sulfur for growth, but is not known to be used by anaerobes either as a sulfur source, a fermentation substrate, an electron acceptor, or as a methanogenic substrate. Some specialized methylotrophs (including Methylosulfonomonas, Marinosulfonomonas, and strains of paragraph signHyphomicrobium and Methylobacterium) can use it as a carbon and energy substrate to support growth. Methanesulfonate oxidation is initiated by cleavage catalysed by methanesulfonate monooxygenase, the properties and molecular biology of which are discussed.

Desulfonation of propanesulfonic acid by comamonas acidovorans strain P53: evidence for an alkanesulfonate sulfonatase and an atypical sulfite dehydrogenase

Evidence is presented for the presence in propanesulfonate-grown Comamonas acidovorans strain P53 of a cytoplasmically located sulfonatase that does not sediment at 100,000 x g. This enzyme catalysed the sulfonate-dependent oxidation of NADH or NADPH, indicating a monooxygenase that effects the addition of molecular oxygen to C(3)-C(6) 1-alkanesulfonates. Enzyme activity was proportional to protein concentration only above approximately 2 mg cytoplasmic fraction protein ml(-1), suggesting that the sulfonatase is a multicomponent enzyme, possibly comparable with methanesulfonate monooxygenase. Enzyme activity was strongly inhibited by divalent metal-chelating agents, but was insensitive to cyanide and azide. Sulfite released from sulfonates by Comamonas acidovorans was oxidized by an unusual sulfite dehydrogenase. This was purified approximately 230-fold and was shown to have a molecular mass of 74.4 kDa, comprising two or more subunits. The enzyme activity was specific in vitro for ferricyanide as an electron acceptor and, unlike other bacterial sulfite dehydrogenases, did not contain native cytochrome c or reduce added cytochrome c. It was a basic protein, insensitive to chloride and sulfate, and exhibited a K(m) for sulfite of approximately 45 &mgr;M.

Molecular Ecological Analysis of Methanogens and Methanotrophs in Blanket Bog Peat.

Abstract Methane production and methane oxidation potential were measured in a 30 cm peat core from the Moorhouse Nature Reserve, UK. The distribution of known groups of methanogens and methane oxidizing bacteria throughout this peat core was assessed. Using 16S rRNA gene retrieval and functional gene probing with genes encoding key proteins in methane oxidation and methanogenesis, several major groups of microorganisms were detected. Methane production and oxidation was detected in all depths of the peat core. PCR amplification and oligonucleotide probing experiments using DNA isolated from all sections of the peat core detected methanotrophs from the groups Methylosinus and Methylococcus and methanogens from the groups Methanosarcinaceae, Methanococcaceae, and Methanobacteriaceae. 16S rDNA sequences amplified with the Methylosinus-specific primer were shown to have a high degree of identity with 16S rDNA sequences previously detected in acidic environments. However, no methanogen sequences were detected by the probes available in this study in the sections of the peat core (above 7 cm) where the majority of methanogenesis occurred, either because of low methanogen numbers or because of the presence of novel methanogen sequences.http://link.springer-ny.com/link/service/journals/00248/bibs/38n3p225.html