Publications by authors named "Evgenii N Frolov"

A novel Gram-negative, motile, rod-shaped bacterium, designated 4137-cl, was isolated from a thermal spring of North Ossetia (Russian Federation). Strain 4137-cl grew at 30-50 °C (optimum 42 °C) with 0-3.5% NaCl (optimum 0-0.

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An aerobic, obligately chemolithoautotrophic, sulfur-oxidizing bacterium, strain AK1, was isolated from a terrestrial hot spring of the Uzon Caldera, Kamchatka, Russia. The cells of the new isolate were Gram-negative motile rods with a single polar flagellum. Strain AK1 grew at 37-55 °C (optimum 50 °C) with 0-1.

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Article Synopsis
  • Thermodesulfovibrio is a genus of thermophilic sulfate-reducing bacteria, currently recognized to have five species.
  • Two new strains, 3907-1M and 3462-1, were isolated from hot springs, demonstrating the ability to use hydrogen and acetate for growth, with strain 3907-1M also showing autotrophic growth potential, a first for this genus.
  • Genomic and phylogenomic analyses led to the classification of these strains as new species, indicating that the Thermodesulfovibrio genus has previously underestimated ecological flexibility and metabolic capabilities.
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The anaerobic oxidation of fatty acids and alcohols occurs near the thermodynamic limit of life. This process is driven by syntrophic bacteria that oxidize fatty acids and/or alcohols, their syntrophic partners that consume the products of this oxidation, and the pathways for interspecies electron exchange via these products or direct interspecies electron transfer (DIET). Due to the interdependence of syntrophic microorganisms on each other's metabolic activity, their isolation in pure cultures is almost impossible.

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One of the important current issues of bioenergetics is the establishment of the thermodynamic limits of life. There is still no final understanding of what is the minimum value of the energy yield of a reaction that is sufficient to be used by an organism (the so-called "biological quantum of energy"). A reasonable model for determination of the minimal energy yield would be microorganisms capable of living on low-energy substrates, such as acetogenic prokaryotes.

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The genome of sp. strain 3827-6, a facultative autotrophic hyperthermophilic archaeon isolated from a Kamchatka hot spring, was sequenced and analyzed. Genome analysis predicted the dicarboxylate/4-hydroxybutyrate cycle and a [NiFe]-hydrogenase, as well as the tricarboxylic acid cycle, altogether determining the possibility of both autotrophic and heterotrophic growth of this strain.

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The family Thermodesulfobiaceae, comprising one genus Thermodesulfobium with two validly published species, is currently assigned to order Thermoanaerobacterales within the class Clostridia of the phylum Bacillota. At the same time, the very first 16S rRNA gene sequence-based phylogenetic studies of representatives of the genus pointed out great differences between Thermodesulfobium and other members of the phylum Bacillota. Subsequent studies of new Thermodesulfobium representatives supported deep phylogenetic branching of this lineage within bacterial tree, implying that it represents a novel phylum.

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Microbial communities of the Kamchatka Peninsula terrestrial hot springs were studied using radioisotopic and cultural approaches, as well as by the amplification and sequencing of and 16S rRNA genes fragments. Radioisotopic experiments with S-labeled sulfate showed that microbial communities of the Kamchatka hot springs are actively reducing sulfate. Both the cultivation experiments and the results of and 16S rRNA genes fragments analyses indicated the presence of microorganisms participating in the reductive part of the sulfur cycle.

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Dissimilatory sulfate reduction (DSR)-an important reaction in the biogeochemical sulfur cycle-has been dated to the Palaeoarchaean using geological evidence, but its evolutionary history is poorly understood. Several lineages of bacteria carry out DSR, but in archaea only Archaeoglobus, which acquired DSR genes from bacteria, has been proven to catalyse this reaction. We investigated substantial rates of sulfate reduction in acidic hyperthermal terrestrial springs of the Kamchatka Peninsula and attributed DSR in this environment to Crenarchaeota in the Vulcanisaeta genus.

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The Calvin-Benson-Bassham (CBB) cycle assimilates CO for the primary production of organic matter in all plants and algae, as well as in some autotrophic bacteria. The key enzyme of the CBB cycle, ribulose-bisphosphate carboxylase/oxygenase (RubisCO), is a main determinant of de novo organic matter production on Earth. Of the three carboxylating forms of RubisCO, forms I and II participate in autotrophy, and form III so far has been associated only with nucleotide and nucleoside metabolism.

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An obligately anaerobic, sulfate-reducing micro-organism, strain 3127-1T, was isolated from geothermally heated soil (Oil Site, Uzon Caldera, Kamchatka, Russia). The new isolate was a moderately thermoacidophilic anaerobe able to grow with H2 or formate by respiration of sulfate or thiosulfate. The pH range for growth was 3.

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