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The abundance and phylogenetic diversity of the microbial community in the hydrogenetic ferromanganese crust, sandy sediment and overlying seawater were investigated using a culture-independent molecular analysis based on the 16S rRNA gene. These samples were carefully collected from the Takuyo-Daigo Seamount, located in the northwest Pacific Ocean, by a remotely operated vehicle. Based on quantitative PCR analysis, Archaea occupy a significant portion of the prokaryotic communities in the ferromanganese crust and the sediment samples, while Bacteria dominated in the seawater samples. Phylotypes belonging to Gammaproteobacteria and to Marine group I (MGI) Crenarchaeota were abundant in clone libraries constructed from the ferromanganese crust and sediment samples, while those belonging to Alphaproteobacteria were abundant in that from the seawater sample. Comparative analysis indicates that over 80% of the total phylotype richness estimates for the crust community were unique as compared with the sediment and seawater communities. Phylotypes related to Nitrosospira belonging to the Betaproteobacteria and those related to Nitrosopumilus belonging to MGI Crenarchaeota were detected in the ferromanganese crust, suggesting that these ammonia-oxidizing chemolithoautotrophs play a role as primary producers in the microbial ecosystem of hydrogenetic ferromanganese crusts that was formed as precipitates from seawater. [ABSTRACT FROM AUTHOR]

The phylogenetic diversity of archaeal 16S rRNA genes in a thermoacidic spring field of Ohwakudani, Hakone, Japan, was investigated by PCR-based analysis using a novel Archaea-specific primer designed in the present study. Clone libraries of archaeal 16S rRNA genes were constructed from hot water (78 °C) and mud (28 °C) samples by PCR using a newly designed forward primer and a previously reported forward primer with reverse primers. Most phylotypes found in the libraries from the hot water sample were related to cultured (hyper)thermophiles. The phylotypes and their detection frequencies from the hot water sample were similar for the libraries amplified with the two different primer sets. In contrast, phylotypes having a low similarity (<95%) to cultured Archaea were found in the libraries from the mud sample. Some of the phylotypes were relatively close to members of Thermoplasmata (80-93% similarity) and the others were not clearly affiliated with Crenarchaeota and Euryarchaeota, but related to Thaumarchaeota and Korarchaeota. The phylotypes and their detection frequencies were significantly different between the two libraries of the mud sample. Our results from the PCR-based analysis using the redesigned primer suggest that more diverse, uncultured Archaea are present in acidic environments at a low temperature than previously recognized. [ABSTRACT FROM AUTHOR]

The ability of Eukarya, Bacteria and Archaea to perform N-glycosylation underlies the importance and possible antiquity of this post-translational protein modification. However, in contrast to the relatively well-studied eukaryal and bacterial pathways, the archaeal N-glycosylation process is less understood. To remedy this disparity, the following study has examined 56 available archaeal genomes with the aim of identifying glycosyltransferases and oligosaccharyltransferases, including those putatively catalyzing this post-translational processing event. This analysis reveals that while oligosaccharyltransferases, central components of the N-glycosylation pathway, are found across the range of archaeal phenotypes, the N-glycosylation machinery of hyperthermophilic Archaea may well rely on fewer components than do the parallel systems of nonhyperthermophilic Archaea. Moreover, genes encoding predicted glycosyltransferases of hyperthermophilic Archaea tend to be far more scattered within the genome than is the case with nonhyperthermophilic species, where putative glycosyltransferase genes are often clustered around identified oligosaccharyltransferase-encoding sequences. [ABSTRACT FROM AUTHOR]

There is controversy regarding the existence of archaeal pathogens. Periodontitis is one of the human diseases in which Archaea have been suggested to have roles as pathogens. This study was performed to investigate the distribution of Archaea in Japanese patients with periodontitis and to examine the serum IgG responses to archaeal components. Subgingival plaque samples were collected from 111 periodontal pockets of 49 patients (17 with aggressive periodontitis and 32 with chronic periodontitis), and 30 subgingival plaque samples were collected from 17 healthy subjects. By PCR targeting the 16S rRNA gene, Archaea were detected in 15 plaque samples (13.5% of total samples) from 11 patients (29.4% of patients with aggressive periodontitis and 18.8% of patients with chronic periodontitis). Archaea were detected mostly (14/15) in severe diseased sites (pocket depth ≥6 mm), while no amplicons were observed in any samples from healthy controls. Sequence analysis of the PCR products revealed that the majority of Archaea in periodontal pockets were a Methanobrevibacter oralis-like phylotype. Western immunoblotting detected IgG antibodies against M. oralis in eight of the 11 sera from patients. These results suggest the potential of Archaea ( M. oralis) as an antigenic pathogen of periodontitis. [ABSTRACT FROM AUTHOR]

The glutamine synthetase (EC 6.3.1.2) from the haloarchaeon Haloferax mediterranei has been purified and characterized in order to understand the ammonium assimilation in haloarchaea. Based on sodium dodecyl sulfate polyacrylamide gel electrophoresis and gel-filtration chromatography, the enzyme consists of eight subunits of 51.7 kDa, suggesting that this enzyme belongs to the glutamine synthetase type II. The purified enzyme has been characterized with respect to its optimum temperature (45°C) and pH value (8.0). The optimal NaCl or KCl concentrations for the reaction were 0.5 and 0.25 M, respectively. The effect ofl-methionine-d,l-sulphoximine and different divalent metal ions has also been tested. The glutamine synthetase presented here is unusual; it shows the typical characteristic of eukaryotic and soil bacteria glutamine synthetases. [ABSTRACT FROM AUTHOR]