Regular proteinaceous layers ofThermococcus stetteri cell envelope

Proteinaceous layers of theThermococcus stetteri cell envelope were investigated and found to consist of regularly arrayed subunits 18 nm in diameter. According to the results of sodium dodecyl sulfate-polyacrylamide gel electrophoresis, two major proteins were present. They were glycosylated and had molecular weights of 80,000 and 210,000. In addition to two external regular proteinaceous layers, cells ofT. stetteri were found to have internal regular layers tightly attached to the cytoplasmic membrane. In the region of flagella attachment to the cell, polar membrane-like structures were found in the cytoplasm.     

Pseudodesulfovibrio alkaliphilus,sp. nov., an alkaliphilic sulfate-reducing bacterium isolated from a terrestrial mud volcano

Antonie van Leeuwenhoek - The diversity of anaerobic microorganisms in terrestrial mud volcanoes is largely unexplored. Here we report the isolation of a novel sulfate-reducing alkaliphilic...     

Tepidibacillus fermentans gen. nov., sp. nov.: a moderately thermophilic anaerobic and microaerophilic bacterium from an underground gas storage

A novel moderately thermophilic bacterium, strain STGH^T, was isolated from Severo-Stavropolskoye underground gas storage (Russia). Cells of strain STGH^T were spore-forming motile straight rods 0.3 μm in diameter and 2.0–4.0 μm in length having a Gram-positive cell wall structure. The temperature range for growth was 36–65 °C, with an optimum at 50–52 °C. The pH range for growth was 5.5–8.0, with an optimum at pH 7.0–7.5. Growth of strain STGH^T was observed at NaCl concentrations ranging from 0 to 4.0 % (w/v) with an optimum at 1.0 % (w/v). Strain STGH^T grew anaerobically by reduction of nitrate, thiosulfate, S⁰ and AQDS using a number of complex proteinaceous compounds, organic acids and carbohydrates as electron donors. Nitrate was reduced to nitrite; thiosulfate and sulfur were reduced to sulfide. It also was able to ferment pyruvate, glucose, fructose, and maltose. The strain STGH^T did not grow under aerobic conditions during incubation with atmospheric concentration of oxygen but was able to microaerobic growth (up to 10 % of oxygen in gas phase). The G+C content of DNA of strain STGH^T was 34.8 mol%. 16S rRNA gene sequence analysis revealed that the isolated organism belongs to the class Bacilli. We propose to assign strain STGH^T to a new species of a novel genus Tepidibacillus fermentans gen. nov., sp.nov. The type strain is STGH^T (=DSM 23802^T, =VKM B-2671^T).     

Sulfate reduction and inorganic carbon assimilation in acidic thermal springs of the Kamchatka peninsula

Thermoacidophilic sulfate reduction, which remains a poorly studied process, was investigated in the present work. Radioisotope analysis with ³⁵S-labeled sulfate was used to determine the rates of dissimilatory sulfate reduction in acidic thermal springs of Kamchatka, Russia. Sulfate reduction rates were found to vary from 0.054 to 12.9 nmol SO₄/(cm³ day). The Oil Site spring (Uzon caldera, 60°C, pH 4.2) and Oreshek spring (Mutnovskii volcano, 91°C, pH 3.5) exhibited the highest activity of sulfate-reducing prokaryotes. Stable enrichment cultures reducing sulfate at pH and temperature values close to the environmental ones were obtained from these springs. Analysis of the 16S rRNA gene sequences revealed that a chemolithoautotrophic bacterium Thermodesulfobium sp. 3127-1 was responsible for sulfate reduction in the enrichment from the Oil Site spring. A chemoorganoheterotrophic archaeon Vulcanisaeta sp. 3102-1 (phylum Crenarchaeota) was identified in the enrichment from Oreshek spring. Thus, dissimilatory sulfate reduction under thermoacidophilic conditions was demonstrated and the agents responsible for this process were revealed.     

Diversity and abundance of Crenarchaeota in terrestrial habitats studied by 16S RNA surveys and real time PCR

Novel phylogenetic lineages of as yet uncultivated crenarchaeota have been frequently detected in low to moderate-temperature, marine and terrestrial environments. In order to gain a more comprehensive view on the distribution and diversity of Crenarchaeota in moderate habitats, we have studied 18 different terrestrial and freshwater samples by 16S rDNA-based phylogenetic surveys. In seven different soil samples of diverse geographic areas in Europe (forest, grassland, ruderal) and Asia (permafrost, ruderal) as well as in two microbial mats, we have consistently found one particular lineage of crenarchaeota. The diversity of Crenarchaeota in freshwater sediments was considerably higher with respresentative 16S rDNA sequences distributed over four different groups within the moderate crenarchaeota. Systematic analysis of a 16S rDNA universal library from a sandy ecosystem containing 800 clones exclusively revealed the presence of the soil-specific crenarchaeotal cluster. With primers specific for non-thermophilic crenarchaeota we established a rapid method to quantify archaeal 16S rDNA in real time PCR. The relative abundance of crenarchaeotal rDNA was 0.5-3% in the bulk soil sample and only 0.16% in the rhizosphere of the sandy ecosystem. A nearby agricultural setting yielded a relative abundance of 0.17% crenarchaeotal rDNA. In total our data suggest that soil crenarchaeota represent a stable and specific component of the microbiota in terrestrial habitats.     

The Genome Sequence of the Crenarchaeon Acidilobus saccharovorans Supports a New Order,Acidilobales, and Suggests an Important Ecological Role in Terrestrial Acidic Hot Springs

Acidilobus saccharovorans is an anaerobic, organotrophic, thermoacidophilic crenarchaeon isolated from a terrestrial hot spring. We report the complete genome sequence of A. saccharovorans, which has permitted the prediction of genes for Embden-Meyerhof and Entner-Doudoroff pathways and genes associated with the oxidative tricarboxylic acid cycle. The electron transfer chain is branched with two sites of proton translocation and is linked to the reduction of elemental sulfur and thiosulfate. The genomic data suggest an important role of the order Acidilobales in thermoacidophilic ecosystems whereby its members can perform a complete oxidation of organic substrates, closing the anaerobic carbon cycle.Acidophilic microorganisms are widely dispersed in natural acidic environments, including volcanic hot springs, and are, in the majority, aerobes (14). However, such anoxic, high-temperature, acidic environments are inhabited by metabolically versatile anaerobic thermoacidophiles of the archaeal phylum Crenarchaeota. Lithoautotrophic thermoacidophiles oxidize molecular hydrogen in the course of elemental sulfur (S⁰) respiration. Organotrophs couple the oxidation of organic substrates to the reduction of S⁰ or thiosulfate. They all belong to the genus Acidilobus in the family Acidilobaceae and to the genus Caldisphaera in the family Caldisphaeraceae (4, 13, 22, 24). Acidilobaceae and Caldisphaeraceae form the crenarchaeal order Acidilobales (24). Acidilobus saccharovorans was isolated from an acidic hot spring of Uzon Caldera, Kamchatka, Russia (24). It is an obligately anaerobic acidophile with a range of growth from pH 2.5 to 5.8 (optimum at pH 3.5 to 4) and a temperature range from 60 to 90°C (optimum at 80 to 85°C). It utilizes a wide range of proteinaceous and carbohydrate substrates and cannot grow lithoautotrophically on H₂ and CO₂ (24). S⁰ and thiosulfate stimulate growth and are reduced to H₂S. Protons cannot serve as electron acceptors, since no H₂ is produced during growth in the absence of S⁰ (24). Genomic sequences of aerobic, thermoacidophilic euryarchaea Thermoplasma acidophilum (26) and Picrophilus torridus (8) give an insight into the thermoacidophilic survival strategy. However, no genomes of obligately anaerobic, thermoacidophilic archaea were available until now. Here we present the genome of A. saccharovorans and show that it encodes numerous hydrolytic enzymes and metabolic pathways necessary for the utilization and complete mineralization of organic substrates in its natural habitat, acidic hot springs.     

The Geoglobus acetivorans Genome: Fe(III) Reduction,Acetate Utilization,Autotrophic Growth,and Degradation of Aromatic Compounds in a Hyperthermophilic Archaeon

Geoglobus acetivorans is a hyperthermophilic anaerobic euryarchaeon of the order Archaeoglobales isolated from deep-sea hydrothermal vents. A unique physiological feature of the members of the genus Geoglobus is their obligate dependence on Fe(III) reduction, which plays an important role in the geochemistry of hydrothermal systems. The features of this organism and its complete 1,860,815-bp genome sequence are described in this report. Genome analysis revealed pathways enabling oxidation of molecular hydrogen, proteinaceous substrates, fatty acids, aromatic compounds, n-alkanes, and organic acids, including acetate, through anaerobic respiration linked to Fe(III) reduction. Consistent with the inability of G. acetivorans to grow on carbohydrates, the modified Embden-Meyerhof pathway encoded by the genome is incomplete. Autotrophic CO₂ fixation is enabled by the Wood-Ljungdahl pathway. Reduction of insoluble poorly crystalline Fe(III) oxide depends on the transfer of electrons from the quinone pool to multiheme c-type cytochromes exposed on the cell surface. Direct contact of the cells and Fe(III) oxide particles could be facilitated by pilus-like appendages. Genome analysis indicated the presence of metabolic pathways for anaerobic degradation of aromatic compounds and n-alkanes, although an ability of G. acetivorans to grow on these substrates was not observed in laboratory experiments. Overall, our results suggest that Geoglobus species could play an important role in microbial communities of deep-sea hydrothermal vents as lithoautotrophic producers. An additional role as decomposers would close the biogeochemical cycle of carbon through complete mineralization of various organic compounds via Fe(III) respiration.     

<Emphasis Type="Italic">Thermosulfurimonas marina</Emphasis> sp. nov., an Autotrophic Sulfur-Disproportionating and Nitrate-Reducing Bacterium Isolated from a Shallow-Sea Hydrothermal Vent

A thermophilic, anaerobic, chemolithoautotrophic bacterium (strain SU872^T) was isolated from a shallow-sea hydrothermal vent at Kunashir Island. The cells were motile, gram-negative, oval or rodshaped 0.5?0.6 μm thick and 1.5?2.0 μm long, occurring singly or in pairs. Strain SU872^T grew at 50 to 79°C (optimum at 74°C), pH from 5.0 to 8.0 (optimum at 6.7?7.0), and NaCl concentration of 1.5–4.5%. Strain SU872^T was able to grow by disproportionation of elemental sulfur, thiosulfate, or sulfite, with CO₂/HCO₃^? as the sole carbon source. Growth was enhanced in the presence of ferrihydrite (poorly crystalline Fe(III) oxide) as as a sulfide-scavenging agent. Sulfate was not used as an electron acceptor. Growth also occurred with elemental sulfur, thiosulfate, or sulfite (but not sulfide) as electron donors and nitrate as an electron acceptor, with production of sulfate and ammonium. Analysis of the 16S rRNA gene sequence revealed 97.8% similarity between strain SU872^T and the type strain Thermosulfurimonas dismutans S95^T (phylum Thermodesulfobacteria). According to the results of DNA–DNA hybridization, the similarity of genomic DNA of the strains SU872^T and T. dismutans S95^T was 48%. Based on its phenotypic characteristics and the results of phylogenetic analysis, it is proposed to assign the isolate to a new species of the genus Thermosulfurimonas,—Thermosulfurimonas marina sp. nov., with the type strain SU872^T (=DSM 104922^T, =VKM B-3177^T, =UNIQEM SU872^T).