Microbial characterization of thermophilicArchaea isolated from the Guaymas Basin hydrothermal vent

The temperature gradient-forming device, an accessory unit for normal light microscopes to study the biology of hyperthermophilic microorganisms

To date, the behavior of hyperthermophilic microorganisms in their biotope has been studied only to a limited degree; this is especially true for motility. One reason for this lack of knowledge is the requirement for high-temperature microscopy-combined, in most cases, with the need for observations under strictly anaerobic conditions-for such studies. We have developed a custom-made, low-budget device that, for the first time, allows analyses in temperature gradients up to 40°C over a distance of just 2 cm (a biotope-relevant distance) with heating rates up to ∼5°C/s. Our temperature gradient-forming device can convert any upright light microscope into one that works at temperatures as high as 110°C. Data obtained by use of this apparatus show how very well hyperthermophiles are adapted to their biotope: they can react within seconds to elevated temperatures by starting motility-even after 9 months of storage in the cold. Using the temperature gradient-forming device, we determined the temperature ranges for swimming, and the swimming speeds, of 15 selected species of the genus Thermococcus within a few months, related these findings to the presence of cell surface appendages, and obtained the first evidence for thermotaxis in Archaea.

Thermococcus celericrescens sp. nov., a fast-growing and cell-fusing hyperthermophilic archaeon from a deep-sea hydrothermal vent

A fast-growing and cell-fusing hyperthermophilic archaeon was isolated from a hydrothermal vent at Suiyo Seamount, Izu-Bonin Arc, Western Pacific Ocean. Strain TS2T is an irregular, motile coccus that is generally 0.7–1.5 μm in diameter and possesses a polar tuft of flagella. In the mid-exponential phase of growth, cells that appeared black under phase-contrast microscopy fused at room temperature in the presence of a DNA-intercalating dye, as previously observed in Thermococcus coalescens. Cell fusion was not observed in later growth phases. Transmission electron microscopy revealed that the cells in the mid-exponential phase had a 5 nm-thick, electron-dense cell envelope that appeared to associate loosely with the cytoplasmic membrane. As the growth stage progressed, a surface layer developed on the membrane under the envelope and the envelope eventually peeled off. These observations suggest that the surface layer prevents the fusion of cells. Cells of strain TS2T grew at 50–85 °C, pH 5.6–8.3 and at NaCl concentrations of 1.0 to 4.5 %, with optimal growth occurring at 80 °C, pH 7.0 and 3.0 % NaCl. Under optimal growth conditions, strain TS2T grew very fast with an apparent doubling time of 20 min. It is suggested that the biosynthesis of the surface layer cannot catch up with cell multiplication in the mid-exponential phase and thus cells without the surface layer are generated. Strain TS2T was an anaerobic chemo-organotroph that grew on either yeast extract or tryptone as the sole growth substrate. The genomic DNA G+C content was 54.6 mol%. Phylogenetic analysis based on 16S rRNA gene sequencing indicated that the isolate belongs to the genus Thermococcus. However, no significant DNA–DNA hybridization was observed between the genomic DNA of strain TS2T and phylogenetically related Thermococcus species. On the basis of this evidence, strain TS2T is proposed to represent a novel species, Thermococcus celericrescens sp. nov., a name chosen to reflect the fast growth of the strain. The type strain is TS2T (=NBRC 101555T=JCM 13640T=DSM 17994T).

Genomic markers of ancient anaerobic microbial pathways: sulfate reduction, methanogenesis, and methane oxidation

Genomic markers for anaerobic microbial processes in marine sediments-sulfate reduction, methanogenesis, and anaerobic methane oxidation-reveal the structure of sulfate-reducing, methanogenic, and methane-oxidizing microbial communities (including uncultured members); they allow inferences about the evolution of these ancient microbial pathways; and they open genomic windows into extreme microbial habitats, such as deep subsurface sediments and hydrothermal vents, that are analogs for the early Earth and for extraterrestrial microbiota.

Effects of micronutrients on growth and starch hydrolysis of Thermococcus guaymasensis and Thermococcus aggregans

The effects of micronutrients on growth of Thermococcus guaymasensis and Thenrmococcus aggregans in a starch-containing medium were investigated. A trace minerals solution, a vitamins solution and calcium chloride were omitted from the medium or added in different amounts. The growth rates of both species were not affected over a significant range of concentrations of these compounds, but appreciable inhibition of growth was observed after the addition of elemental sulfur to the medium. T. guaymasensis exhibited a significant tolerance to high amounts of trace element and vitamin solutions but growth was inhibited by the omission of these compounds from the medium. Moreover, both amylolytic and pullulytic activities increased in the presence of 6-fold higher amounts of trace element and vitamin solutions, compared to the concentrations used in the usual medium. In T. aggregans, both enzymatic activities were enhanced in the presence of either increased (4-fold) amounts of trace element and vitamin solutions, or after the addition of elemental sulfur to the medium. Furthermore, larger activities of starch-hydrolysing enzymes were detected with a 10-fold higher concentration of calcium chloride, compared to the usual medium, in the absence of trace element and vitamin solutions. When both Thermococcus species were tested for the tolerance to specific cations and oxyanions, T. guaymasensis exhibited higher tolerance compared to T. aggregans, the former strain being capable to grow in the presence of 6 mM Ni2+, 4mM Cu2+, 1.5 mM SeO4(2-), and 1.5 mM MoO4(2-). The content of total cell proteins followed the pattern of starch-hydrolysing enzymes and an over-expression of proteins in the range of 35, 50 and 70 kDa was observed.

Effects of hydrostatic pressure and temperature on physiological traits of Thermococcus guaymasensis and Thermococcus aggregans growing on starch

The effects of temperature and hydrostatic pressure on growth of two novel Thermococcus species, T. guaymasensis and T. aggregans, were investigated. These archaea, isolated from the Guaymas Basin hydrothermal vent site at 2000 meters depth, are able to grow on starch in sulfur-depleted medium producing significant amounts of amylases and pullulanases. At 85 degrees C, T. guaymasensis exhibited a barophilic response at 20 and 35 MPa but inhibition of growth occurred at 50 MPa; at 50 MPa, cell replication was repressed, the mean cell size increased, and production of starch-hydrolysing enzymes was significantly stimulated. Barophily was also expressed by T. guaymasensis under 20 MPa at sub-optimal temperature (70 C) but morphological alterations of cells were observed earlier (35 MPa). No barophily was exhibited by T. aggregans at 85 degrees C. In this case, cell replication was repressed at 20 MPa and remarkable inhibition of growth occurred at 50 MPa. Only when T. aggregans was cultivated at 75 degrees C, a significant barophilic response was exhibited at 20 MPa, as shown by the rate of replication and metabolism. These results show that Thermococcus species, although isolated from the same ecosystem, differ with regard to the effects of pressure and temperature on cell physiology. The metabolic responses and their significance for potential biotechnological applications are also discussed.