Physiological,biochemical, and cytological characteristics of a halotolerant and alkalitolerant methanotroph grown on methanol

The halotolerant alkaliphilic methanotroph Methylomicrobium buryatense 5B is capable of growth at high methanol concentrations (up to 1.75 M). At optimal values of pH and salinity (pH 9.5 and 0.75% NaCl), the maximum growth rate on 0.25 M methanol (0.2 h-1) was twice as high as on methane (0.1 h-1). The maximum growth rate increased with increasing medium salinity and was lower at neutral than at alkaline pH. The growth of the bacterium on methanol was accompanied by a reduction in the degree of development of intracytoplasmic membranes, the appearance of glycogen granules in cells, and the accumulation of formaldehyde, formate, and an extracellular glycoprotein at concentrations of 1.2 mM, 8 mM, and 2.63 g/l, respectively. The glycoprotein was found to contain 23% protein and 77% carbohydrates, the latter being dominated by glucose, mannose, and aminosugars. The major amino acids were glutamate, aspartate, glycine, valine, and isoleucine. The glycoprotein content rose to 5 g/l when the concentration of potassium nitrate in the medium was augmented tenfold. The activities of sucrose-6-phosphate synthase, glycogen synthase, and NADH dehydrogenase in methanol-grown cells were higher than in methane-grown cells. The data obtained suggest that the high methanol tolerance of M. buryatense 5B is due to the utilization of formaldehyde for the synthesis of sucrose, glycogen, and the glycoprotein and to the oxidation of excess reducing equivalents through the respiratory chain.     

New thermophilic methanotrophs of the genus Methylocaldum

Two pure cultures of obligate methanotrophs, strains H-11 and 0-12, growing in the temperature range from 30 to 61 degrees C with an optimum at 55 degrees C were isolated from samples of silage and manure. Based on the results of analysis of the 16S rRNA genes, membrane-bound methane monooxygenase, and phenotypic properties, the isolates were assigned to the genus Methylocaldum. Significant temperature-dependent variations in morphology and phospholipid and fatty acid composition were revealed. Both strains assimilated methane carbon via the ribulose monophosphate, serine, and ribulose bisphosphate pathways. The activity of hexulose phosphate synthase was independent of the cultivation temperature; however, the activities of hydroxypyruvate reductase and ribulose bisphosphate carboxylase were higher in cells grown at 55 degrees C that in cells grown at 37 degrees C, indicating the important roles of the serine and ribulose bisphosphate pathways in the thermoadaptation of the strains under study. NH4+ assimilation occurred through reductive amination of alpha-ketoglutarate and via the glutamate cycle. The relationship between the physiological-biochemical peculiarities of the isolates and their thermophilic nature is discussed.     

Taxonomic characterization of new alkaliphilic and alkalitolerant methanotrophs from soda lakes of the Southeastern Transbaikal region and description of Methylomicrobium buryatense sp.nov

Five strains of obligate methanotrophic bacteria (4G, 5G, 6G, 7G and 5B) isolated from bottom sediments of Southeastern Transbaikal soda lakes (pH 9.5-10.5) are taxonomically described. These bacteria are aerobic, Gram-negative monotrichous rods having tightly packed cup-shaped structures on the outer cell wall surface (S-layers) and Type I intracytoplasmic membranes. All the isolates possess particulate methane monooxygenase (pMMO) and one strain (5G) also contains soluble methane monooxygenase (sMMO). They assimilate methane and methanol via the ribulose monophosphate pathway (RuMP). The isolates are alkalitolerant or facultatively alkaliphilic, able to grow at pH 10.5-11.0 and optimally at pH 8.5-9.5. These organisms are obligately dependent on the presence of sodium ions in the growth medium and tolerate up to 0.9-1.4 M NaCl or 1 M NaHCO3. Although being mesophilic, all the isolates are resistant to heating (80 degrees C, 20 min), freezing and drying. Their cellular fatty acids profiles primarily consist of C(16:1). The major phospholipids are phosphatidylethanolamine and phosphatidylglycerol. The main quinone is Q-8. The DNA G+C content ranges from 49.2-51.5 mol %. Comparative 16S rDNA sequencing showed that the newly isolated methanotrophs are related to membres of the Methylomicrobium genus. However, they differ from the known members of this genus by DNA-DNA relatedness. Based on pheno- and genotypic characteristics, we propose a new species of the genus Methylomicrobium Methylomicrobium buryatense sp. nov.     

Aerobic methanotrophic communities in the bottom sediments of Lake Baikal

The results of the first methodical investigation into the aerobic methanotrophic communities inhabiting the bottom sediments of Lake Baikal are reported. Use of the radioisotopic method revealed methane consumption in 12 10- to 50-cm-long sediment cores. The maximum methane consumption rates (495-737 microl/(dm3 day) were recorded in sediments in the regions of hydrothermal vents and oil and gas occurrence. Methane consumption was most active in the surface layers of the sediments (0-4 cm); it decreased with the sediment depth and became negligible or absent at depths below 20 cm. The number of methanotrophic bacteria usually ranged from 100 to 1000 cells/cm3 of sediment and reached 1 million cells/cm3 in the regions of oil and gas occurrence. The 17 enrichment cultures obtained were represented mainly by morphotype II methanotrophs. Phylogenetic analysis of the enrichment cultures in terms of the amino acid sequence of the alpha subunit of the membrane-bound methane monooxygenase revealed the predominance of methanotrophs of the genus Methylocystis. The results obtained suggest the presence of an active aerobic methanotrophic community in Lake Baikal.     

Molecular diversity of methanotrophs in Transbaikal soda lake sediments and identification of potentially active populations by stable isotope probing

Soda lakes are an environment with an unusually high pH and often high salinity. To identify the active methanotrophs in the Soda lake sediments, sediment slurries were incubated with a 10% (v/v) (13)CH(4) headspace and the (13)C-labelled DNA was subsequently extracted from these sediments following CsCl density gradient centrifugation. This DNA was then used as a template for PCR amplification of 16S rRNA genes and genes encoding PmoA and MmoX of methane monooxygenase, key enzymes in the methane oxidation pathway. Phylogenetic analysis of 16S rRNA genes, PmoA and MmoX identified that strains of Methylomicrobium, Methylobacter, Methylomonas and 'Methylothermus' had assimilated the (13)CH(4). Phylogenetic analysis of PmoA sequences amplified from DNA extracted from Soda lake sediments before Stable Isotope Probing (SIP) treatment showed that a much wider diversity of both type I and type II methanotroph sequences are present in this alkaline environment. The majority of methanotroph sequences detected in the (13)C-DNA studies were from type I methanotrophs, with 50% of 16S rRNA clones and 100% of pmoA clones from both Lake Suduntuiskii Torom and Lake Gorbunka suggesting that the type I methanotrophs are probably responsible for the majority of methane oxidation in this environment.     

Structural and functional features of methanotrophs from hypersaline and alkaline lakes

Ten strains of aerobic methanotrophic bacteria represented by halophilic neutrophiles or halotolerant alkaliphiles were isolated from saline and alkaline lakes of southeast Siberia, Mongolia, Africa, and North America. Based on analysis of the nucleotide sequences of 16S rRNA gene and the pmoA gene encoding particulate methane monooxygenase, the isolates were classified as Methylomicrobium alcaliphilum, Methylomicrobium buryatense, and Methylobacter marinus. All strains of the genus Methylomicrobium were shown to synthesize glycoprotein S-layers located on the cell surface with hexagonal symmetry (p6) as a monolayer of cup-shaped structures or fine “inverted” conical structures and as plates consisting of protein subunits with inclined (p2) symmetry. During adaptation to the high salinity of the medium, isolated methanotrophs synthesize osmoprotectants: ectoine, sucrose, and glutamate. The ectC gene encoding ectoine synthase (EctC) was identified in six methanotrophic strains. Phylogenetic analysis of translated amino acid sequence of the ectC gene fragment suggests lateral transfer of the genes of ectoine synthesis as the most probable way for methanotrophs to acquire resistance to high external salinity.     

Potential activity of methane and ammonia oxidation by methanotropic communities from soda lakes of the southern Transbaikal

Radioisotopic measurements of the methane consumption by mud samples taken from nine Southern Transbaikal soda lakes (pH 9.5-10.6) showed an intense oxidation of methane in the muds of lakes Khuzhirta, Bumalai Nur, Gorbunka, and Suduntuiskii Torom, with the maximum oxidation rate in the mud of lakes Khuzhirta (33.2 nmol/(ml day)). The incorporation rate of the radioactive label from 14CH4 into 14CO2 was higher than into acid-stable metabolites. Optimum pH values for methane oxidation in water samples were 7-8, whereas mud samples exhibited two peaks of methane oxidation activity (at pH 8.15-9.4 and 5.8-7.0). The majority of samples could oxidize ammonium to nitrites; the oxidation was inhibited by methane. The PCR amplification analysis of samples revealed the presence of genes encoding soluble and particulate methane monooxygenase and methanol dehydrogenase. Three alkaliphilic methanotrophic bacteria of morphotype I were isolated from mud samples in pure cultures, one of which, B5, was able to oxidize ammonium to nitrites at pH 7-11. The data obtained suggest that methanotrophs are widely spread in the soda lakes of Southern Transbaikal, where they actively oxidize methane and ammonium.