V. F. Gal'chenko

A Study of Nucleotide Sequences of nifH Genes of Some Methanotrophic Bacteria

Using a previously developed primer system, nifH gene fragments 450 nucleotides long were amplified, cloned, and sequenced for representatives of nitrogen-fixing methanotrophic bacteria of the genera Methylococcus, Methylocystis, and Methylosinus. Fragments of nifH genes were also detected and sequenced in representatives of the genera Methylomonas and Methylobacter, which were not considered diazotrophs until recently. Phylogenetic analysis revealed the remoteness of nifH gene sequences of methanotroph types I and II. At the same time, a close relationship was found between nifH of type I methanotrophs and representatives of γ-proteobacteria and between nifH genes of type II methanotrophs and representatives of α-proteobacteria. The results obtained in this study are in good accordance with the data of phylogenetic analysis based on 16S rRNA sequence comparison with the only exception being Methylococcus capsulatus strains, whose nifH genes proved to be closely related to nifH genes of Methylocystis and Methylosinus representatives. Our findings extend the database of primary sequences of nifH genes and allow the contribution of methanotrophs to the process of nitrogen fixation to be estimated.

A system of oligonucleotide primers for the amplification of nifH genes of different taxonomic groups of prokaryotes

Based on the analysis of the nifH gene nucleotide sequences from GenBank, a system of primers was developed that makes it possible to obtain 370- and 470-bp PCR fragments of the nifH gene of nitrogen-fixing bacteria and archaea. The effectiveness of the proposed system for revealing the presence of nifH genes was demonstrated by PCR on the DNA isolated from nitrogen-fixing prokaryotes for which the primary structure of these genes is known and which belong to different taxonomic groups. nifH sequences of nitrogen-fixing prokaryotes of the genera Xanthobacter, Beijerinckia, and Methanosarcina, for which the capacity for nitrogen fixation was demonstrated earlier, but no data existed on the nucleotide composition of these genes, were determined and deposited in GenBank.

[Biogeochemical processes of methane cycle in the soils, swamps and lakes of Western Siberia].

The biogeochemical processes of methane production and oxidation were studied in the upper horizons of tundra and taiga soils and raised bogs and lake bottom sediments near the Tarko-Sale gas field in western Siberia. Both in dry and water-logged soils, the total methane concentration (in soil particles and gaseous phase) was an order of magnitude higher than in the soil gaseous phase alone (22 and 1.1 nl/cm3, respectively). In bogs and lake bottom sediments methane concentration was as high as 11 μl/cm3. Acetate was the major precursor of the newly formed methane. The rate of aceticlastic methanogenesis reached 55 ng C/(cm3day), whereas that of autotrophic methanogenesis was an order of magnitude lower. The most active methane production and oxidation were observed in bogs and lake sediments, where the δ13C values of CO2were inversely related to the intensity of bacterial methane oxidation. Methane diffusing from bogs and lake bottom sediments showed δ13C values ranging from –78 to –47‰, whereas the δ13C value of carbon dioxide ranged from –18 to –1‰. In these ecosystems, methane emission comprised from 3 to 206 mg CH4/(m2day). Conversely, the dry and water-logged soils of the tundra and taiga took up atmospheric methane at a rate varying from 0.3 to 5.3 mg CH4/(m2day). Methane consumption in soils was of biological nature. This was confirmed by the radioisotopic method and chamber experiments, in which weighting of methane carbon was observed (the δ13C value changed from –51 to –41‰).

Dormant forms of Micrococcus luteus and Arthrobacter globiformis not platable on standard media

The colony-forming ability of long (3–9 months) incubated cystlike resting cells (CRC) of the nonspore-forming gram-positive bacteria Micrococcus luteus and Arthrobacter globiformis was studied in this work. The preservation of the CRC proliferative potential as assayed by plating on standard LB agar was shown to depend on the conditions of the formation of the dormant cells. In aged post-stationary cultures of micrococci and arthrobacters grown under carbon and phosphorus limitation the number of colony-forming units (CFU/ml) of CRC decreased in the course of 3–9 month incubation to the level of 106–107 CFU/ml. However, M. luteus CRC obtained under carbon and nitrogen limitation and A. globiformis CRC obtained under nitrogen limitation and starvation completely lost their ability to form colonies on standard solid medium after 4–6 months of incubation and turned into a ‘non-culturable’ (non-platable) state. In this case, the ratio of live cells in the population of M. luteus and A. globiformis ‘non-culturable’ CRCs (determined by the Live/Dead staining test) was 10–44% of the total cell number. To study the possible preservation of proliferative potential in non-platable CRCs, various methods of their reactivation were applied. Although preincubation of CRC suspensions in a buffer solution of 0.1 M K2HPO4 (pH 7.4) or in the presence of lysozyme (1 or 10 μg/ml) resulted in increased numbers of live cells (determined by the Live/Dead test) or in disruption of the cell conglomerates, it did not increase considerably the CFU titer on LB medium. Variations in the medium composition, such as addition of sodium pyruvate as an antioxidant or dilution of the medium, promoted the formation of macrocolonies by a small portion of nonplateable CRC of M. luteus (50−80 CFU/ml), whereas the number of the cells capable of microcolony formation (mCFU) was 1.8–6.8 × 105 mCFU/ml, exceeding the CFU titers by four orders of magnitude. The application of semisolid agar and the most probable number (MPN) method was the most efficient for determination of the mCFU titer, and an almost complete reversion of ‘non-culturable’ micrococcal CRCs to microcolony formation was observed (up to 2.3 × 107 mCFU/ml). The usefulness of diluted complete media for the restoration of the colony-forming ability of the dormant forms was confirmed in experiments with ‘nonculturable’ CRCs of A. globiformis. The development of special procedures and methods for determining actively proliferating cells not detected by ordinary methods is of great importance for advanced monitoring studies.

Seasonal dynamics of atmospheric methane oxidation in gray forest soils

Seasonal fluctuations in the methane fluxes in the soil–atmosphere system were determined for gray forest soils of Central Russia. Consumption of atmospheric methane was found to exceed methane emission in gray forest soils under forest and in the agrocenosis. The average annual rates of atmospheric methane consumption by the soil under forest and in the agrocenosis were 0.026 and 0.008 mg C-CH4/(m2 h), respectively. The annual rate of atmospheric methane oxidation in the gray forest soils of Moscow oblast was estimated to be 0.68 kton. Seasonal fluctuations in the methane oxidation activity were due to changes in the hydrothermal conditions and in the reserves of readily decomposable organic matter and mineral nitrogen, as well as to changes in the activity of methane oxidizers.

Growth of Mesophilic Methanotrophs at Low Temperatures

The optimal growth of mesophilic methanotrophic bacteria (collection strains of the genera Methylocystis, Methylomonas, Methylosinus, and Methylobacter) occurred within temperature ranges of 31–34°C and 23–25°C. None of the 12 strains studied were able to grow at 1.5 or 4°C. Representatives of six methanotrophic species (strains Mcs. echinoides2, Mm. methanica12, Mb. bovis89, Mcs. pyriformis14, Mb. chroococcum90, and Mb. vinelandii87) could grow at 10°C (with a low specific growth rate). The results obtained suggest that some mesophilic methane-oxidizing bacteria display psychrotolerant (psychrotrophic) but not psychrophilic properties. In general, the Rosso model, which describes bacterial growth rate as a function of temperature, fits the experimental data well, although, for most methanotrophs, with symmetrical approximations for the optimal temperature.

Methane Content in the Bottom Sediments and Water Column of the Black Sea

The methane content in the bottom sediments and water column of the Black Sea was determined using various methods of desorption and analysis of gases and various methods of calculating their concentrations. The head-space method with the use of salting out and calculation by an internal standard proved to be the most accurate procedure for the analysis of methane concentration in bottom sediments. The methane content in bottom sediments increased downward along the sediment thickness. In the upper 50–70 cm of shelf sediments, two minimums of methane concentration were revealed; in deep-sea sediments, only one minimum was recorded (in the 20–50 cm horizons). In the water column, methane concentrations slowly grew from the surface to a depth of 150–200 m and abruptly increased to a depth of 700–1200 m, remaining virtually constant in underlying layers. In certain deep-sea regions, peaks of methane content in the 1000–1200 m horizons of the water column were revealed, which were most probably due to local influx of abyssal waters enriched with this gas.

Phenotypic variability in Azospirillum brasilense strains Sp7 and Sp245: Association with dormancy and characteristics of the variants

The state of metabolic dormancy in diazotrophic bacteria Azospirillum brasilense Sp7 (non-endophytic strain) and Sp245 (endophytic strain) was found to be associated with phenotypic variability. The latter manifested itself in the extension of the spectrum of A. brasilense phenotypic variants resulting from plating of cyst-like resting cells (CRC) on solid media and was more pronounced in strain Sp7. The major colony’s morphological variants of strain Sp7 were (1) the dominant S type; (2) the highly pigmented Pg type; (3) the R type; (4) the Sm type, forming small colonies; and (5) the Sg type, forming segmented colonies. In addition to their colony morphology, the variants differed in the phenotype stability during transfers on the standard solid medium and in their motility in semisolid agar. The occurrence frequency of the phenotypic variants depended on the conditions and duration of incubation (storage) of the CRC of strain Sp7, as well as on heat treatment (at 55 and 60°C for 10 min) of the cells prior to inoculation. The maximum frequency of S → Pg transitions (up to 74%) was observed during the germination of CRC stored in a spent culture medium at −20°C for 4 months; the maximum frequency (up to 100%) of S → Sm transitions was observed after inoculation of the CRC subjected to heat treatment. The Pg variants were the most stable, whereas other types reverted rapidly to the S or Pg variant. The S variant grown in semisolid agar exhibited the mixed type of motility (Swa+Gri+, swarming and migration in the form of microcolonies); the Pg and Sg variants showed the Swa+Gri− (swarming) phenotype and the Sm variant was nonmotile (Swa−Gri− phenotype). The spectrum of phenotypic variants of the endophytic strain Sp245 was narrower than that of strain Sp7 and was represented by S, Sm, and M (mucoid) variants that differed in the patterns of cell motility: the dominant S type displayed the swarming pattern (Swa+Gri−), the mucoid M type showed the mixed type (Swa+Gri+) of motility, and the Sm variant was nonmotile. The differences between the nonendophytic strain Sp7 and the endophytic strain Sp245 in their capacity for phenotypic dissociation and cell motility in semisolid media may reflect their ability to adapt to changing ambient conditions and specificity of plant-microbial interactions.

Rates of Microbial Production and Oxidation of Methane in the Bottom Sediments and Water Column of the Black Sea

Rates of biogeochemical (microbial) processes of methane production and methane oxidation were determined in the bottom sediments and water column of the Black Sea. Aerobic bacterial oxidation of methane was confined to the upper 20–30 cm of Holocene bottom sediments of the shelf (0.7–259 ng C/(dm3 day)) and to oxygenated waters (0.2–45 ng C/(dm3 day)). In reduced sediments of the deep-sea zone and in the hydrogen sulfide–containing water column, considerable rates of anaerobic methane oxidation were recorded, comparable to or exceeding the rates of methane oxidation in oxygenated layers. From one-fourth to one-half of the methane formed in bottom sediments was oxidized immediately therein. The major part of the remaining methane was oxidized in the water column, and a smaller portion arrived in the atmosphere.

[Detection of microorganisms in the environment and the preliminary appraisal of their physiological state by X-ray microanalysis].

The paper deals with the X-ray microanalysis of the elemental composition of bacteriomorphic particles in 170 000-year-old Antarctic permafrost sediments and in indoor dust. A comparative analysis of the phosphorus, sulfur, calcium, and potassium contents and the Ca/K and P/S ratios in these particles and in reference microbial cells occurring in different physiological states showed that the absence of P and/or S peaks in the X-ray spectrum of an object may indicate that it is abiotic. Resting microbial forms can be revealed on the basis of the following characteristic features: an increased content of Ca, a high Ca/K ratio, and a low P/S ratio. Model experiments with nonviable bacterial and yeast micromummies with alterations in the structural and barrier functions of the cytoplasmic membrane showed that micromummies can be recognized by a superhigh content of a marker element (e.g., P, K, or Si), accumulated due to facilitated diffusion along a deliberately created concentration gradient. Such an analysis of the permafrost sediment and dust made it possible to suggest the presence of mummified cells in these objects. The possibility of using X-ray microanalysis for the detection of microbial cells in natural habitats in order to enhance the efficiency of ecological monitoring of the environment is discussed.