Positive Pressure Effect on Manganese Binding by Bacteria in Deep-Sea Hydrothermal Plumes

Pressure as an environmental parameter for microbial life--a review

Microbial life has been prevailing in the biosphere for the last 3.8 Ga at least. Throughout most of the Earth's history it has experienced a range of pressures; both dynamic pressure when the young Earth was heavily bombarded, and static pressure in subsurface environments that could have served as a refuge and where microbial life nowadays flourishes. In this review, we discuss the extent of high-pressure habitats in early and modern times and provide a short overview of microbial survival under dynamic pressures. We summarize the current knowledge about the impact of microbial activity on biogeochemical cycles under pressures characteristic of the deep subsurface. We evaluate the possibility that pressure can be a limiting parameter for life at depth. Finally, we discuss the open questions and knowledge gaps that exist in the field of high-pressure geomicrobiology.

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.

Microbial metal-binding mechanisms and their relation to nuclear waste disposal

The cell surface polymers of microorganisms readily bind a variety of metal ions, which enables the organisms to immobilize potentially toxic metal ions before they encounter the plasma membrane. Under appropriate chemical conditions, bound metal ions can form a variety of minerals that may be of major geological importance. Many studies have shown the occurrence of metal binding and biomineralization in nature, but detailed knowledge of the underlying mechanisms is lacking. The microbial influence of this binding may be indirect, such as physicochemical influences on the solution chemistry, Eh, and pH; or direct, when it is determined by the type of organisms present, their energy metabolism, and the structural and chemical characteristics of the cell surface and extracellular polymers. Metal binding by bacterial cell surfaces has several implications in nuclear waste disposal including adsorption of soluble radionuclides. A detailed knowledge of the chemical mechanisms of metal interactions with the microbial cell surface will enhance our understanding of the geochemical environment within a nuclear waste disposal vault.Key words: biomineralization, radionuclide immobilization, biofilm, bacterial cell surface.

Preliminary description and nutritional characterization of a chemoorganotrophic archaeobacterium growing at temperatures of up to 110 ° isolated from a submarine hydrothermal vent environment

Summary: An extremely thermophilic coccoid bacterium, designated strain ES4, was isolated from a flange (a newly described geological structure associated with massive sulphide mounds) at the Juan de Fuca Ridge hydrothermal vent system. The organism is a salt-requiring obligately anaerobic chemoorganotroph which reduces elemental sulphur but can grow very poorly in the absence of sulphur. Organic substrates utilized include yeast extract, peptone and amino acid hydrolysate as well as individual amino acids, the peptide Leu-Ser and starch. When growing on a defined medium, ES4 requires a supplement of vitamins and 20 amino acids at trace concentrations. Growth is most rapid in the temperature range 90-99 °C, with a maximum growth temperature of about 110 °C. In the optimal temperature range for growth, ES4 has a doubling time of about 1 h and can reach densities of 109 cells ml-1. Insensitivity to the antibiotics vancomycin, streptomycin and chloramphenicol, and the presence of di- and tetra-ether phytanyl lipids, indicate that ES4 is an archaeobacterium.