Search PubMed⌕ Search

SEARCH · Search PubMed

Results for “Halobacteriales”

Search indexed PubMed citations on genomics, clinical trials, systematic reviews and public health. Explore titles, authors and supplied subject terms, then open the PubMed record.

Quote a phrase for an exact phrase match. Source license links do not imply unrestricted reuse.

At least 37 records · Page 2Linked to original sources

Community composition of a hypersaline endoevaporitic microbial mat.

A hypersaline, endoevaporitic microbial community in Eilat, Israel, was studied by microscopy and by PCR amplification of genes for 16S rRNA from different layers. In terms of biomass, the oxygenic layers of the community were dominated by Cyanobacteria of the Halothece, Spirulina, and Phormidium types, but cell counts (based on 4',6'-diamidino-2-phenylindole staining) and molecular surveys (clone libraries of PCR-amplified genes for 16S rRNA) showed that oxygenic phototrophs were outnumbered by the other constituents of the community, including chemotrophs and anoxygenic phototrophs. Bacterial clone libraries were dominated by phylotypes affiliated with the Bacteroidetes group and both photo- and chemotrophic groups of alpha-proteobacteria. Green filaments related to the Chloroflexi were less abundant than reported from hypersaline microbial mats growing at lower salinities and were only detected in the deepest part of the anoxygenic phototrophic zone. Also detected were nonphototrophic gamma- and delta-proteobacteria, Planctomycetes, the TM6 group, Firmicutes, and Spirochetes. Several of the phylotypes showed a distinct vertical distribution in the crust, suggesting specific adaptations to the presence or absence of oxygen and light. Archaea were less abundant than Bacteria, their diversity was lower, and the community was less stratified. Detected archaeal groups included organisms affiliated with the Methanosarcinales, the Halobacteriales, and uncultured groups of Euryarchaeota.

Archaea↗

Intragenomic heterogeneity and intergenomic recombination among haloarchaeal rRNA genes.

More than one copy of rRNA operons, which code for both the small-subunit (SSU) and large-subunit (LSU) rRNA, are often found in prokaryotes. It is generally assumed that all rRNA operons within a single cell are almost identical. A notable exception is the extremely halophilic archaeal genus Haloarcula, most species of which are known to harbor highly divergent rRNA operons that differ at approximately 5% of the nucleotide positions in the SSU gene and at 1 to 2% of the nucleotide positions in the LSU gene. We report that such intragenomic heterogeneity is not unique to Haloarcula, as high levels of intragenomic sequence variation have been observed for the SSU genes of two other genera of extreme halophiles, Halosimplex and Natrinema. To investigate this in detail, the two rRNA operons of Halosimplex carlsbadense and the four operons of Natrinema sp. strain XA3-1 were cloned and completely sequenced. The SSU and LSU genes of H. carlsbadense show the highest levels of intragenomic heterogeneity observed so far in archaea (6.7 and 2.6%). The operons of Natrinema sp. strain XA3-1 have additional unusual characteristics, such as identical internal transcribed spacers, while one of four SSU genes is 5% divergent and all LSU genes differ from each other by 0.9 to 1.9%. The heterogeneity among the Natrinema sp. strain XA3-1 LSU genes is localized in hot spots, and one of these regions is shown to be the result of a recombination event with a distantly related halophile. This is the first example of interspecies recombination between rRNA genes in archaea, and the recombination occurred over one of the largest phylogenetic distances ever reported for such an event. We suggest that intragenomic heterogeneity of rRNA operons is an ancient and stable trait in several lineages of the Halobacteriales. The impact of this phenomenon on the taxonomy of extremely halophilic archaea is discussed.

Base Sequence↗

Higher-level classification of the Archaea: evolution of methanogenesis and methanogens.

We used a phylogenetic approach to analyze the evolution of methanogenesis and methanogens. We show that 23 vertically transmitted ribosomal proteins do not support the monophyly of methanogens, and propose instead that there are two distantly related groups of extant archaea that produce methane, which we have named Class I and Class II. Based on this finding, we subsequently investigated the uniqueness of the origin of methanogenesis by studying both the enzymes of methanogenesis and the proteins that synthesize its specific coenzymes. We conclude that hydrogenotrophic methanogenesis appeared only once during evolution. Genes involved in the seven central steps of the methanogenic reduction of carbon dioxide (CO(2)) are ubiquitous in methanogens and share a common history. This suggests that, although extant methanogens produce methane from various substrates (CO(2), formate, acetate, methylated C-1 compounds), these archaea have a core of conserved enzymes that have undergone little evolutionary change. Furthermore, this core of methanogenesis enzymes seems to originate (as a whole) from the last ancestor of all methanogens and does not appear to have been horizontally transmitted to other organisms or between members of Class I and Class II. The observation of a unique and ancestral form of methanogenesis suggests that it was preserved in two independent lineages, with some instances of specialization or added metabolic flexibility. It was likely lost in the Halobacteriales, Thermoplasmatales and Archaeoglobales. Given that fossil evidence for methanogenesis dates back 2.8 billion years, a unique origin of this process makes the methanogenic archaea a very ancient taxon.

Archaea↗

Archaeal phylogeny based on proteins of the transcription and translation machineries: tackling the Methanopyrus kandleri paradox.

BACKGROUND: Phylogenetic analysis of the Archaea has been mainly established by 16S rRNA sequence comparison. With the accumulation of completely sequenced genomes, it is now possible to test alternative approaches by using large sequence datasets. We analyzed archaeal phylogeny using two concatenated datasets consisting of 14 proteins involved in transcription and 53 ribosomal proteins (3,275 and 6,377 positions, respectively). RESULTS: Important relationships were confirmed, notably the dichotomy of the archaeal domain as represented by the Crenarchaeota and Euryarchaeota, the sister grouping of Sulfolobales and Aeropyrum pernix, and the monophyly of a large group comprising Thermoplasmatales, Archaeoglobus fulgidus, Methanosarcinales and Halobacteriales, with the latter two orders forming a robust cluster. The main difference concerned the position of Methanopyrus kandleri, which grouped with Methanococcales and Methanobacteriales in the translation tree, whereas it emerged at the base of the euryarchaeotes in the transcription tree. The incongruent placement of M. kandleri is likely to be the result of a reconstruction artifact due to the high evolutionary rates displayed by the components of its transcription apparatus. CONCLUSIONS: We show that two informational systems, transcription and translation, provide a largely congruent signal for archaeal phylogeny. In particular, our analyses support the appearance of methanogenesis after the divergence of the Thermococcales and a late emergence of aerobic respiration from within methanogenic ancestors. We discuss the possible link between the evolutionary acceleration of the transcription machinery in M. kandleri and several unique features of this archaeon, in particular the absence of the elongation transcription factor TFS.

Archaea↗

Crowding in extremophiles: linkage between solvation and weak protein-protein interactions, stability and dynamics, provides insight into molecular adaptation.

The study of the molecular adaptation of microorganisms to extreme environments (solvent, temperature, etc.) has provided tools to investigate the complex relationships between protein-solvent and protein-protein interactions, protein stability and protein dynamics, and how they are modulated by the crowded environment of the cell. We have evaluated protein-solvent and protein-protein interactions by solution experiments (analytical ultracentrifugation, small angle neutron and X-ray scattering, density) and crystallography, and protein dynamics by energy resolved neutron scattering. This review concerns work from our laboratory on (i) proteins from extreme halophilic Archaea, and (ii) psychrophile, mesophile, thermophile and hyperthermophile bacterial cells.

Adaptation, Biological↗

Life in unusual environments: progress in understanding the structure and function of enzymes from extreme halophilic bacteria.

Extreme halophilic archaea are saturated with salt and the intracellular electrolyte concentration exceeds that of the extracellular environment. Enzymes and other proteins from extreme halophilic archaea have been purified for many years and studied by biochemical and biophysical solution methodologies. They are active and stable at multimolar salt concentrations and denature below 2 to 3 M NaCl or KCl. Adaptation to these high concentrations of salt, genetic and evolutionary aspects, and the possibility of biotechnological applications are problems of considerable interest. Since the status of this fascinating field of research was reviewed in 1992, malate dehydrogenase from Haloarcula marismortui, now known to be a tetramer, was sequenced, its gene was cloned and expressed in active form, and its physical properties were redefined. A single mutation of Arg100 (in the enzyme active site) to Gln switched the enzyme specificity from malate to lactate dehydrogenase. Recent determination of its molecular structure by X-ray crystallography (O. Dym et al., in press) provides an exciting basis for the understanding of the structure and function of extreme halophilic enzymes. A major problem which so far has not been tackled in the study of extreme halophilic archaea is the understanding of protein nucleic acid interactions which are essential for the performance of biological function. Whereas the stability and activity of enzymes and other proteins can be modified to perform at high salt concentrations by use of currently known structural concepts, the existence of meaningful protein nucleic acid interactions in physiological concentrations of 4 to 5 M KCl constitutes an unsolved enigma worth intensive investigation.

Environment↗

A protein-serine phosphatase from the halophilic archaeon Haloferax volcanii.

We have detected a protein phosphatase activity in soluble extracts from the halophilic archaeon Haloferax volcanii. This activity was markedly stimulated by the divalent metal ions Mn2+ and Cd2+. It dephosphorylated phosphoseryl residues in casein, mixed histones, and phosphorylase a, but not phosphotyrosyl residues in reduced, carboxyamidomethylated and maleylated lysozyme. This protein phosphatase activity was inhibited by NaF, Zn2+, vanadate, molybdate, inorganic phosphate, inorganic pyrophosphate, or p-nitrophenyl phosphate, or by treatment with diethylpyrocarbonate. Activity was unaffected by other potential inhibitors or activators such as polyamines, heparin, cyclic nucleotides, Ca2+/calmodulin, tartrate, tetramisole, okadaic acid, microcystin LR, or sulfhydryl-modifying agents. The functional similarities between this protein-serine phosphatase and that previously identified in another archaeon, the extreme acidothermophile Sulfolobus solfataricus, suggest the existence of a family of divalent metal ion-stimulated protein-serine phosphatases of extremely ancient origin in the Archaea.

Cadmium↗

Localization of proteins HL29 and HL31 from Haloarcula marismortui within the 50 S ribosomal subunit by chemical crosslinking.

Isolated 50 S ribosomal subunits from the halophilic archaebacterium Haloarcula marismortui were treated in situ with the homobifunctional and cleavable crosslinking reagent dithiobis(succinimidyl propionate) (12 A). Several crosslinked complexes were obtained. Among these were the protein pairs HmaL4-HL29 and HmaL18-HL31; HL29 and HL31 are ribosomal proteins without any equivalent in eubacterial ribosomes. The crosslinked protein pairs were isolated on a preparative scale by combining conventional ion-exchange chromatography and reverse phase high-pressure liquid chromatography. The monomeric proteins involved in crosslink formation were unambiguously identified by two-dimensional gel electrophoresis and N-terminal or internal protein sequencing. Due to the homology between HmaL4 and HmaL18 and their Escherichia coli counterparts, and the roughly known location of these proteins within the 50 S subunit, our results demonstrate that HL29 is probably located in the centre of the large subunit in the vicinity of the peptidyltransferase domain, whereas HL31 must be situated within the central protuberance close to the region of the 5 S RNA.

Amino Acid Sequence↗

Novel plasmids from alkaliphilic halomonads.

Seventeen alkaliphilic halomonads were examined for the presence of plasmids. Of these, eight strains harbored one or more from 5.3 to 33 kb in size, the first plasmids to be identified from an alkaliphilic halomonad source. Restriction and hybridization analysis revealed three strains that maintained an identical 5.9-kb plasmid which we named pAH1, two that had an identical 33-kb plasmid, and three others, of which one carried two plasmids of 5.3 and 15 kb, the former being designated pAH2. The two final strains maintained plasmids of 15 and 20.5 kb. Restriction mapping of both pAH1 and pAH2 indicated that they have a number of unique restriction sites and are of a small enough size to make them suitable for vector construction.

DNA, Archaeal↗

HF1 and HF2: novel bacteriophages of halophilic archaea.

Two novel halophilic archaebacterial bacteriophages, HF1 and HF2, were isolated from an Australian solar saltern. They were morphologically identical with icosahedral-shaped heads (diameter 58 nm) and contractile tails (length 94 nm). Other similarities included sensitivity to reduced ionic conditions, similar protein profiles by SDS-PAGE, and dsDNA genomes of identical size (73.5 kbp) with analogous restriction patterns. DNA-DNA hybridization data showed the two phages to be closely related. HF1 has a broad host-range, infecting members of three halobacterial genera including Halobacterium salinarium and the genetically well-characterized strain Haloferax volcanii WFD11. Mutants showing increased plating efficiency on alternative hosts were readily selectable. By contrast, HF2 showed a limited host range, confined to the closely related dam-methylated strains Ch2 and H. saccharovorum.

Bacteriophages↗

Gas vesicle formation in halophilic Archaea.

Gas vesicles are intracellular, microbial flotation devices that consist of mainly one protein, GvpA. The formation of halobacterial gas vesicles occurs along a complex pathway involving 14 different gvp genes that are clustered in a genomic region termed the "vac region". Various vac regions found in Halobacterium salinarum (p-vac and c-vac), Haloferax mediterranei (mc-vac), and Natronobacterium vacuolatum (nv-vac) have been investigated. Except for the latter vac region, the arrangement of the gvp genes is identical. Single gvp genes have been mutated to study the effect on gas vesicle synthesis in transformants and to determine their possible function. Each vac region exhibits a characteristic transcription pattern, and regulatory steps have been observed at the DNA, RNA, and protein level, indicating a complex regulatory network acting during gas vesicle gene expression.

Archaeal Proteins↗

Presence of two novel cardiolipins in the halophilic archaeal community in the crystallizer brines from the salterns of Margherita di Savoia (Italy) and Eilat (Israel).

Two novel cardiolipin derivatives were recently detected in Halobacterium salinarum, namely an archaeal analog of bisphosphatidylglycerol (BPG) and a glycocardiolipin (GlyC). GlyC was found to be tightly bound to bacteriorhodopsin. To obtain information on the presence and distribution of these archaeal cardiolipins, we have analyzed the lipids extracted from the crystallizer ponds of the salterns of Margherita di Savoia (Italy) and Eilat (Israel) and from cultures of representative species of the Halobacteriaceae by electrospray ionization mass spectrometry. BPG was present as a minor lipid component in the lipids extracted from the biomass of the Margherita di Savoia and the Eilat salterns, while GlyC was detected only in the extract of the biomass of Margherita di Savoia. Both compounds were enriched in the membrane fraction obtained by dialysis of the cells against distilled water. We detected BPG in all members of the Halobacteriaceae tested, but GlyC has so far been found only in the genera Halobacterium and Haloarcula. A sulfated diglycosyl diether was the major glycolipid detected in the biomass of both salterns.

Biomass↗

The lysogenic region of virus phiCh1: identification of a repressor-operator system and determination of its activity in halophilic Archaea.

phiCh1 is a temperate virus infecting the haloalkaliphilic archaeon Natrialba magadii. As for all temperate viruses, a control of the lysogenic state versus the lytic life cycle is essential. Two open reading frames (ORFs) have been identified as putative repressor encoding genes: ORF48 and ORF49. The protein of ORF48 showed sequence similarities to putative repressor molecules. ORF49 was identified by the analysis of a mutant of phiCh1: the lysogenic strain carrying mutant phiCh1-1 showed a different lysis behavior than wild type virus phiCh1, indicating a dysfunction in the regulation of gene expression. Here, we show that the intergenic region between ORF48 and ORF49 comprises a promoter/operator sequence that is a transcriptionally active region in the model system Haloferax volcanii. Transcription from this region can be repressed by the activity of the ORF48 gene product. Gp43/gp44 has an enhancing effect on this regulatory sequence. Evidence is given for a possible binding site of Rep and gp43/gp44 within the coding region of the rep gene.

Archaeal Viruses↗

Evidence of interspecies hydrogen transfer from glycerol in saline environments.

Two halanaerobic bacteria--Halanaerobium saccharolytica subsp. senegalense and Halanaerobium sp. strain FR1H--produced acetate, H2, and CO2 from glycerol fermentation, but the glycerol consumption rate was low. In contrast, in the presence of the moderately halophilic hydrogenotrophic sulfate-reducing bacterium, Desulfohalobium retbaense, used as H2 scavenger in the coculture, glycerol oxidation by both halanaerobes significantly increased. Cocultures of both halanaerobes with D. retbaense on glycerol led to acetate, hydrogen sulfide, and CO2 production, whereas glycerol fermentation by the two strains led to the production of acetate, hydrogen, and CO2. The increased glycerol oxidation by H. saccharolytica and strain FRI H in coculture with D. retbaense resulted from low H2 partial pressure caused by the hydrogen-oxidizing activity of D. retbaense. These results provide the first evidence of interspecies hydrogen transfer in saline environments and indicate that this mechanism may play an important role in organic matter mineralization in hypersaline ecosystems.

Bacteria, Anaerobic↗

Comparative evaluation of Raman spectroscopy at different wavelengths for extremophile exemplars.

Raman spectra have been obtained for extremophiles from several geological environments; selected examples have been taken from hot and cold deserts comprising psychrophiles, thermophiles and halophiles. The purpose of this study is the assessment of the effect of the wavelength of the laser excitation on the ability to determine unique information from the Raman spectra about the specificity of detection of biomolecules produced as a result of the survival strategies adopted by organisms in extreme terrestrial environments. It was concluded that whereas FT-Raman spectroscopy at 1064 nm gave good quality results the time required to record the data was relatively large compared with other wavelengths of excitation but that better access to the CH stretching region for organic molecules was given. Shorter wavelength excitation of biomolecules in the blue-green regions of the visible spectrum using a conventional dispersive spectrometer was more rapid but very dependent upon the type of chemical compound being studied; most relevant biomolecules fluoresced at these wavelengths but carotenoids exhibited a resonance effect which resulted in an improved detection capability. Minerals and geological materials, in contrast, were best studied at these visible wavelengths. In general, the best compromise system for the excitation of the Raman spectra of both geological and biological materials was provided using a 785 nm laser coupled with a dispersive spectrometer, especially for accessing the 1800-200 cm(-1) wavenumber shift region where much of the definitive analytical information resides. This work will have conclusions relevant to the use of miniaturised Raman spectrometers for the detection of biomolecules in extraterrestrial planetary exploration.

Antarctic Regions↗

Glucose transport of Haloferax volcanii requires the Na(+)-electrochemical potential gradient and inhibitors for the mammalian glucose transporter inhibit the transport.

The uptake of glucose and its non-metabolizing analogues by Haloferax volcanii, one of the glucose-utilizing Halobacteria, was examined using intact cells and envelope vesicles. Results obtained were: (1) The transport system is inducible. (2) The uptake requires the gradient of Na(+)-electrochemical potential. (3) Inhibitors for mammalian glucose transport also have an effect on this system, implying that the transporters resemble each other. (4) It is suggested that the mobility of the transporter is regulated by the membrane energization.

Biological Transport, Active↗

Reason for the lack of light-dark adaptation in pharaonis phoborhodopsin: reconstitution with 13-cis-retinal.

The reconstitution of pharaonis phoborhodopsin was performed by incubation of its opsin with 13-cis-retinal. Spectrum change was very slow, and two phases of the change were observed: the first and second phases are due to the transient formation of 13-cis pigment and spontaneous isomerization to all-trans-retinal, respectively. Slow binding supports an idea that the retinal binding pocket of ppR is highly restricted. Being bent in the configuration, 13-cis-retinal cannot be accommodated in the pocket due to the steric hindrance. This is a possible reason for the lack of light-dark adaptation.

Archaeal Proteins↗

Evidence for farnesol-mediated isoprenoid synthesis regulation in a halophilic archaeon, Haloferax volcanii.

Farnesol strongly inhibited growth of a halophilic archaeon, Haloferax volcanii, with an IC50 value of only 2 microM (0.4 microgram/ml) in rich medium and 50 nM (0.01 microgram/ml) in minimal medium without lysis. Other isoprenoid alcohols such as isopentenol, dimethylallyl alcohol, geraniol, and geranylgeraniol at 500 microM did not affect its growth. Mevalonate, which is the precursor of all isoprenoid membrane lipids in archaea, led to recovery of the growth inhibition of H. volcanii, but acetate had no such effect. Farnesol inhibited incorporation of acetate, but not mevalonate, into the lipid fraction. These results suggest that farnesol inhibited the biosynthetic pathway from acetate (acetyl-CoA) to mevalonate. Farnesol is known to be derived from the important intermediate of isoprenoids, farnesyl diphosphate (FPP), and found in neutral lipid fraction from this archaeon. Moreover, the cell-free extracts from H. volcanii could phosphorylate farnesol with ATP to generate farnesyl monophosphate and FPP. We conclude that farnesol-mediated isoprenoid synthesis regulation system by controlling farnesol concentration is present in H. volcanii.

Acetates↗