Cowpox in a human, Russia, 2015.

We investigated the first laboratory-confirmed human case of cowpox virus infection in Russia since 1991. Phylogenetic studies of haemagglutinin, TNF-α receptor-like protein and thymidine kinase regions showed significant differences with known orthopoxviruses, including unique amino-acid substitutions and deletions. The described cowpox virus strain, taking into account differences, is genetically closely related to strains isolated years ago in the same geographical region (European part of Russia and Finland), which suggests circulation of viral strains with common origin in wild rodents without spread over long distances and appearance in other parts of the world.

[Microbial potential for cleaning the oiled iron scale].

The possibility of using microorganisms to clean oiled iron scale of metallurgical production was investigated with the goal of recuperation. A stable microbial association growing on mineral oil as the sole carbon source was isolated from a sample from oiled iron scale taken directly from a metallurgical plant. For microbial cultures isolated from this association, the taxonomic position, as well as their morphological and cultural characteristics, were determined. The microorganisms belonged to the genera Luteimonas, Alcanivorax, Flavobacterium, and Pseudomonas. Microbial associations oxidizing mineral oil were found to contain some microorganisms incapable of its utilization, which stimulated the hydrocarbon-oxidizing microflora. Application of the isolates, as well as of the strains from microbial collections, resulted in a 58% decrease in residual oil content in treated samples of the oiled iron scale.

[Antimicrobic features of phenolic lipids].

The connection between the efficiency of phenolic lipids (PL) and their hydrophobic property (solubility) and hydrophobic property of microorganisms' cell structure is shown. The mixture of amphiphilic di(oxiphenil)-phenil-methanes, which act bacteriostatically under 15 mg/l, possesses maximal efficiency against Staphylococcus aureus. Against Mycobacterium smegmatis with hydrophobic cell wall, hydrophobic 2,4-dialkylocibenzol 70 mg/l was the most effective. Hexylresorcin (HR) stops the development of gram-positive bacteria in concentrations 20-50 mg/l, that of gram-negative bacteria in concentration 65 mg/l, that of M. smegmatis at 70 mg/l, and that of yeast and fungi at 300 mg/l. HR prevails bacteria spores germination in the concentration 25-100 mg/l. The dependence of antibacterial action of isomers and homologues of alkylresorcins on their structure--number, position, and length of alkyl substituents--is studied.

[Desulfovibrio hontreensis sp. nov., a Sulfate-Reducing Bacterium Isolated from Marine Biofoulings at the South Vietnam Coastal Area].

A Desulfovibrio strain physiologically similar to and phylogeneticall related to "D. caledoniensis" SEBR 7250, D. portus MSL79, and D. dechloracetivorans ATCC 700912 (96.9, 95.9, and 95.8% similarity of the 16S rRNA gen sequences, respectively) was isolated from marine biofouling in the coastal zone of the South China Sae (Nha Trang, South Vietnam). The cells of strain ME were gram-negative motile vibrios (0.4-0.6 x 1.3-2 µm) with a single flagellum. The strain grew at 20 to 39 degrees C (growth optimum at 34-37 degrees C), pH 5.8 to 8.5 (pH optimum at 6.8-7.5), and salinity from 0.08 to 1.1 M Na+ (optimum at 0.2-0.3 M Na+). In the presence of sulfate, the strain grew autotrophically with hydrogen or on lactate, formate, pyruvate, fumarate, and malate. Weak growth occurred on succinate, glycerol, and fructose. In the absence of sulfate, the strain was able to ferment pyruvate, malate (weakly), but not lactate. Sulfate, sulfite, thiosulfate, elemental sulfur, and dimethyl sulfoxide were used as electron acceptors. Vitamins and yeast extract were not required for growth. The G+C content was 52.4 mol %. Predominant fatty acids were C18:0 (13.9%), C16:0 (9.6%), iso-C16:0 (9.5%), C18: 1w7 (8.8%), anteiso-C15:0 (8.1%), and iso-C 17:1 (7.2%). The fatty acid composition was close to that of D. dechloracetivorans BO and has some similarity to that of D. portus. Based on its genotypic and phenotypic characteristics, strain ME maybe considered as a new species, for which the name Desulfovibrio hontrensis sp. nov. is proposed.

[A microbiological study of an underground gas storage in the process of gas extraction].

The numbers of microorganisms belonging to ecologically significant groups and the rates of terminal microbial processes of sulfate reduction and methanogenesis were determined in the liquid phase of an underground gas storage (UGS) in the period of gas extraction. The total number of microorganisms in water samples from the operation and injection wells reached 2.1 x 10(6) cells/ml. Aerobic organotrophs (including hydrocarbon- and oil-oxidizing ones) and various anaerobic microorganisms (fermenting bacteria, methanogens, acetogens, sulfate-, nitrate-, and iron-reducing bacteria) were constituent parts of the community. The radioisotopic method showed that, in all the UGS units, the terminal stages of organic matter decomposition included sulfate reduction and methanogenesis, with the maximal rate of these processes recorded in the aqueous phase of above-ground technological equipment which the gas enters from the operation wells. A comparative analysis by these parameters of different anaerobic ecotopes, including natural hydrocarbon fields, allows us to assess the rate of these processes in the UGS as high throughout the annual cycle of its operation. The data obtained indicate the existence in the UGS of a bacterial community that is unique in its diversity and metabolic capacities and able to make a certain contribution to the geochemistry of organic and inorganic compounds in the natural and technogenic ecosystem of the UGS and thus influence the industrial gas composition.

[A microbiological study of an underground gas storage in the process of gas injection].

The liquid phase of different units of an underground gas storage (UGS) in the period of gas injection was studied with respect to its hydrochemical composition and characterized microbiologically. The presence of viable aerobic and anaerobic bacteria was revealed in the UGS stratal and associated waters. An important source of microorganisms and biogenic elements in the ecosystem studied is water and various technogenic admixtures contained in trace amounts in the gas entering from the gas main in the period of gas injection into the storage. Owing to this fact, the bacterial functional diversity, number, and activity are maximal in the system of gas treatment and purification and considerably lower in the observation well zone. At the terminal stages, the anaerobic transformation of organic matter in the UGS aqueous media occurs via sulfate reduction and methanogenesis; exceptionally high rates of these processes (up to 4.9 x 10(5) ng S(2-)l(-1) day(-1) and 2.8 x 10(6) nl CH4 l(-1) day(-1), respectively) were recorded for above-ground technological equipment.

[Nucleotide composition and homologies in the DNA of new extreme halophilic soil archaebacteria]. / Nukleotidnyi sostav i gomologii v DNK novykh pochvennykh ékstremal'no galofil'nykh arkhebakterii.

DNA nucleotide composition was studied in extreme halophilic bacteria belonging to the genera Halobacterium, Halococcus, Natronobacterium and Natronococcus. The cultures were shown to be a monolithic group of microorganisms with the content of GC pairs typical of extreme halophilic archebacteria. The difference between the content of DNA major and minor components was twice as high in Halobacterium distributus strains isolated from sulfate saline soils as compared to cultures of this species isolated from natural waters with a high salinity. DNA minor components were not found in haloalkalophilic microorganisms from soda saline soils in contrast to those from soda lakes. The results of DNA-DNA hybridization indicate that the Halobacterium genus is highly heterogeneous. The newly isolated strains of extremely halophilic H. distributus are characterized by the low homology of their DNAs both among themselves and with other species of the genus. However, the hybridization data for the collection strains H. vallismortis 1398 and H. halobium 996 from the National Collection of Microorganisms are indicative of a high homology (80-100%) which is not characteristic of cultures belonging to different species. These results as well as some phenotypical properties of H. vallismortis 1398 different from those of this species type strain support the data reported in the literature about the genetic instability of extreme halophilic archebacteria. The analysis of homologies in DNA nucleotide sequences may be used to study the taxonomy of extreme halophilic archebacteria.

[Absorption of 14C-dicarboxylic acids by bacteria of the family Halobacteriaceae]. / Pogloshchenie 14C-dikarbonovykh kislot bakteriiami iz semeistva Halobacteriaceae.

Cultures of the family Halobacteriaceae belonging to the species Halobacterium halobium, H. cutirubrum, H. vallismortis and Halococcus morrhuae were shown to be capable of assimilating 14C-succinate. Halobacterium salinarium lacked this ability. The transport systems of C4-dicarboxylates differed in Halobacterium halobium 996 and H. vallismortis 1398, on the one hand, and Halococcus morrhuae 1235, on the other. The differences involve the kinetic parameters and stereospecificity of transport systems, the ability to take up different labelled C4-dicarboxylates, the pH-dependence of transport, and the action of CCCP, a protonophorous uncoupling agent. Halobacteria are capable of labelled succinate uptake at a lower NaCl content in the incubation medium than it is necessary for their growth. The optimal temperature for 14C-succinate uptake by halobacteria is higher than the optimal temperature of their growth. For all of the studied cultures, the transport system of dicarboxylate was shown to differ from that of E. coli common for C4-dicarboxylates and aspartate.

[Comparative characteristics of the transport systems of C4-dicarboxylic acids in cultures of the genera Halobacterium and Halococcus]. / Sravnitel'naia kharakteristika transportnykh sistem C4-dikarbonovykh kislot u kul'tur rodov Halbacterium i Halococcus.

The transport systems of the extreme halophilic organisms, Halobacterium and Halococcus, differ to a considerable degree in the kinetic parameters of succinate and fumarate transport, the exchange between exocellular and endocellular labeled dicarboxylates, and the rate at which labeled compounds in the cell are incorporated into cellular metabolism.

[Utilization of H2O2 as the oxygen source by bacteria of the genera Pseudomonas and Rhodococcus]. / Ispol'zovanie H2O2 v kachestve istochnika kisloroda bakteriiami rodov Pseudomonas i Rhodococcus.

The growth of bacteria of the genera Pseudomonas and Rhodococcus in the presence of hydrogen peroxide as the sole source of oxygen was studied. The toxic effect of H2O2 in the concentration range of 100-200 microg/ml was shown to extend the lag phase by 2 to 3 days. Apart from the peroxide toxicity, the bacterial growth was inhibited by the toxic effect of dissolved oxygen in concentrations over 100 microg O2/ml; in the presence of a liquid hydrocarbon phase, this effect was alleviated. Under decreased partial pressure of oxygen in the presence of hydrocarbons (12-15 vol %), the culture growth was initiated at high initial concentrations of H2O2 (300 microg/ml). When hydrogen peroxide concentrations exceeded 320 microg/ml, no growth occurred, no matter how much hydrocarbon was added.

[Dynamics of microbial processes in the stratal waters of the Romashkinskoe oil field]. / Dinamika mikrobnykh protsessov v plastovykh vodakh Romashkinskogo neftianogo mestorozhdeniia.

Dynamics of the microbial processes developing in parallel with the exploitation of the Romashkinskoe oil field (Tatarstan) was studied in two areas differing in the degree of stratal water freshening. Flooding the strata in conjunction with purposeful measures on stratal microflora activation was shown to increase the microbial population density and activate both methanogenesis and sulfate-reduction; the latter process was limited by the low sulfate concentration. Development of anaerobic processes correlated with changes in acetate concentration in the stratal water. High mineralization (over 200 g/l) inhibited the stratal water microflora even if other conditions were favorable. Isotopic analysis of the carbonate carbon showed that the bicarbonate concentration increased in the stratal water due to microbial degradation of oil hydrocarbons and further participation of the biogenic carbon dioxide in dissolution of the carbonate cement of the oil-bearing strata. In strongly desalinated stratal water, the proportion of the newly formed bicarbonate was as high as 80%.

[Microbiological processes in a high-temperature oil field]. / Mikrobiologicheskie protsessy v vysokotemperaturnom neftianom mestorozhdenii.

Thermophilic sulfate-reducing bacteria (SRB) oxidizing lactate, butyrate, and C12-C16 n-alkanes of oil at a temperature of 90 degrees C were isolated from samples of water and oil originating from oil reservoirs of the White Tiger high-temperature oil field (Vietnam). At the same time, no thermophiles were detected in the injected seawater, which contained mesophilic microorganisms and was the site of low-temperature processes of sulfate reduction and methanogenesis. Thermophilic SRB were also found in samples of liquid taken from various engineering reservoirs used for oil storage, treatment, and transportation. These samples also contained mesophilic SRB, methanogens, aerobic oil-oxidizing bacteria, and heterotrophs. Rates of bacterial production of hydrogen sulfide varied from 0.11-2069.63 at 30 degrees C and from 1.18-173.86 at 70 degrees C micrograms S/(1 day); and those of methane production, varied from 58.4-100 629.8 nl CH4/(1 day) (at 30 degrees C). The sulfur isotopic compositions of sulfates contained in reservoir waters and of hydrogen sulfide of the accompanying gas indicate that bacterial sulfate reduction might be effective in the depth of the oil field.