Changes in the microbial community in Japan Trench sediment from a depth of 6292 m during cultivation without decompression.

A sample of deep-sea sediment was obtained from the Japan Trench at a depth of 6292 m using a pressure-retaining sediment sampler. Microorganisms in the sediment sample were cultivated in marine broth 2216 at ambient pressure (65 MPa) without decompression, and at atmospheric pressure (0.1 MPa) as a control experiment. 16S ribosomal RNA genes (rDNA) were amplified by PCR from DNA extracted from the original sediment sample and the mixed cultures, and the nucleotide sequences were determined. The results of phylogenetic analysis based on 16S rDNA sequences indicated that microbial diversity in the original sediment samples showed a wide distribution of types in the domain Bacteria. Furthermore, in the mixed cultures incubated at 65 MPa without decompression, bacterial strains belonging to the Shewanella barophiles branch and the genus Moritella existed together at the beginning of cultivation, and Moritella strains became dominant towards the end of the cultivation period. Finally, in the mixed cultures incubated at atmospheric pressure, strains belonging to the genus Pseudomonas were dominant at all times. Analysis of fatty acids extracted from the cultures supported the phylogenetic results.

Pressure and temperature effects on growth and viability of the hyperthermophilic archaeon Thermococcus peptonophilus.

We studied the effects of high temperatures and elevated hydrostatic pressures on the physiological behavior and viability of the extremely thermophilic deep-sea archaeon Thermococcus peptonophilus. Maximal growth rates were observed at 30 and 45 MPa although no significant increases in cell yields were detected. Growth at 60 MPa was slower. The optimal growth temperature shifted from 85 degrees C at 30 MPa to 90-95 degrees C at 45 MPa. Cell viability during the stationary phase was also enhanced under high pressure. A trend towards barophily at pressures greater than those encountered in situ at the sea floor was demonstrated at increasing growth temperatures. The viability of cells during starvation, at high temperature (90, 95 degrees C), and at low temperature (10 degrees C) was enhanced at 30 and 45 MPa as compared to atmospheric pressure. These results show that the extremely thermophilic archaeon T. peptonophilus is a barophile.

Pyrococcus horikoshii sp. nov., a hyperthermophilic archaeon isolated from a hydrothermal vent at the Okinawa Trough.

A hyperthermophilic, anaerobic archaeon was isolated from hydrothermal fluid samples obtained at the Okinawa Trough vents in the NE Pacific Ocean, at a depth of 1395m. The strain is obligately heterotrophic, and utilizes complex proteinaceous media (peptone, tryptone, or yeast extract), or a 21-amino-acid mixture supplemented with vitamins, as growth substrates. Sulfur greatly enhances growth. The cells are irregular cocci with a tuft of flagella, growing optimally at 98 degrees C (maximum growth temperature 102 degrees C), but capable of prolonged survival at 105 degrees C. Optimum growth was at pH 7 (range 5-8) and NaCl concentration 2.4% (range 1%-5%). Tryptophan was required for growth, in contrast to the closely related strains Pyrococcus furiosus and P. abyssi. Thin sections of the cell, viewed by transmission electron microscopy, revealed a periplasmic space similar in appearance to the envelope of P. furiosus. The predominant cell membrane component was tetraether lipid, with minor amounts of diether lipids. Treatment of the cells by mild osmotic shock released an extract that contained a Zn(2+)-dependent alkaline phosphatase. Phylogenetic analysis of the sequences encoding 16S rRNA and glutamate dehydrogenase places the isolate with certainty within the genus Pyrococcus although there is relatively low DNA-DNA hybridization (< 63%) with described species of this genus. Based on the reported results, we propose a new species, to be named Pyrococcus horikoshii sp.nov.