Halobacterium Species Research Articles

Halobacterium yunchengense sp. nov., Natronomonas amylolytica sp. nov., Halorientalis halophila sp. nov., Halobellus salinisoli sp. nov., halophilic archaea isolated from a saline lake and inland saline soil.

Four halophilic archaeal strains YCN1T, YCN58T, LT38T, and LT62T were isolated from Yuncheng Salt Lake (Shanxi, China) and Tarim Basin (Xinjiang, China), respectively. Phylogenetic and phylogenomic analyses showed that these four strains tightly cluster with related species of Halobacterium, Natronomonas, Halorientalis, and Halobellus, respectively. The AAI, ANI, and dDDH values between these four strains and their related species of respective genera were lower than the proposed threshold values for species delineation. Strains YCN1T, YCN58T, LT38T, and LT62T could be differentiated from the current species of Halobacterium, Natronomonas, Halorientalis, and Halobellus, respectively, based on the comparison of diverse phenotypic characteristics. The polar lipid profiles of these four strains were closely similar to those of respective relatives within the genera Halobacterium, Natronomonas, Halorientalis, and Halobellus, respectively. The phenotypic, phylogenetic, and genome-based analyses indicated that strains YCN1T, YCN58T, LT38T, and LT62T represent respective novel species within the genera Halobacterium, Natronomonas, Halorentalis, and Halobellus, for which the names Halobacterium yunchengense sp. nov., Natronomonas amylolytica sp. nov., Halorientalis halophila sp. nov., and Halobellus salinisoli sp. nov. are proposed, respectively.

Halobacterium hubeiense sp. nov., a haloarchaeal species isolated from a bore core drilled in Hubei Province, PR China.

Eight colonies of live microbes were isolated from an extensively surface-sterilized halite sample which had been retrieved from a depth of 2000 m from a salt mine in the Qianjiang Depression, Hubei Province, PR China. The eight colonies, obtained after 4 weeks of incubation, were named JI20-1T-JI20-8 and JI20-1T was selected as the type strain. The strains have been previously described, including a genomic analysis based on the complete genome for strain JI20-1T and draft genomes for the other strains. In that study, the name Halobacterium hubeiense was suggested, based on the location of the drilling site. Previous phylogenomic analysis showed that strain JI20-1T is most closely related to the Permian isolate Halobacterium noricense from Alpine rock salt. The orthologous average nucleotide identity (orthoANI) and digital DNA-DNA hybridization (dDDH) percentages between the eight strains are 100-99.6 % and 99.8-96.4 %, respectively. The orthoANI and dDDH values of these strains with respect to the type strains of species of the genus Halobacterium are 89.9-78.2 % and 37.3-21.6 %, respectively, supporting their placement in a novel extremely halophilic archaeal species. The phylogenomic tree based on the comparison of sequences of 632 core-orthologous proteins confirmed the novel species status for these haloarchaea. The polar lipid profile includes phosphatidylglycerol, phosphatidylglycerol phosphate methyl ester, phosphatidylglycerol sulfate, and sulfated galactosyl mannosyl galactosyl glucosyl diether, a profile compatible with that of Halobacterium noricense. Based on genomic, phenotypic, and chemotaxonomic characterization, we propose strain JI20-1T (=DSM 114402T = HAMBI 3616T) as the type strain of a novel species in the genus Halobacterium, with the name Halobacterium hubeiense sp. nov.

TbsP and TrmB jointly regulate gapII to influence cell development phenotypes in the archaeon Haloferax volcanii.

Microbial cells must continually adapt their physiology in the face of changing environmental conditions. Archaea living in extreme conditions, such as saturated salinity, represent important examples of such resilience. The model salt-loving organism Haloferax volcanii exhibits remarkable plasticity in its morphology, biofilm formation, and motility in response to variations in nutrients and cell density. However, the mechanisms regulating these lifestyle transitions remain unclear. In prior research, we showed that the transcriptional regulator, TrmB, maintains the rod shape in the related species Halobacterium salinarum by activating the expression of enzyme-coding genes in the gluconeogenesis metabolic pathway. In Hbt. salinarum, TrmB-dependent production of glucose moieties is required for cell surface glycoprotein biogenesis. Here, we use a combination of genetics and quantitative phenotyping assays to demonstrate that TrmB is essential for growth under gluconeogenic conditions in Hfx. volcanii. The ∆trmB strain rapidly accumulated suppressor mutations in a gene encoding a novel transcriptional regulator, which we name trmB suppressor, or TbsP (a.k.a. "tablespoon"). TbsP is required for adhesion to abiotic surfaces (i.e., biofilm formation) and maintains wild-type cell morphology and motility. We use functional genomics and promoter fusion assays to characterize the regulons controlled by each of TrmB and TbsP, including joint regulation of the glucose-dependent transcription of gapII, which encodes an important gluconeogenic enzyme. We conclude that TrmB and TbsP coregulate gluconeogenesis, with downstream impacts on lifestyle transitions in response to nutrients in Hfx. volcanii.

Halobacterium wangiae sp. nov. and Halobacterium zhouii sp. nov., two extremely halophilic archaea isolated from sediment of a salt lake and saline soil of an inland saltern.

Two novel halophilic archaeal strains, Gai3-17T and XZYJT26T, were isolated from the sediment of Gaize salt lake and the saline soil of Mangkang ancient solar saltern in Tibet, PR China, respectively. Strains Gai3-17T and XZYJT26T were related to each other (96.5 and 89.7% similarity, respectively) and showed 97.5-95.4 and 91.5-87.7% similarities to the current members of Halobacterium based on 16S rRNA and rpoB' genes. The phylogenomic analysis indicated that strains Gai3-17T and XZYJT26T formed two distinct clades and clustered with the Halobacterium species. The two strains can be differentiated from the type strains of the six species with validly published names based on several phenotypic characteristics. The phospholipids of the two strains were phosphatidic acid, phosphatidylglycerol and phosphatidylglycerol phosphate methyl ester. One major glycolipid, sulphated galactosyl mannosyl glucosyl diether, was detected in strain Gai3-17T, while four glycolipids, mannosyl glucosyl diether, sulphated mannosyl glucosyl diether, disulphated mannosyl glucosyl diether and sulphated galactosyl mannosyl glucosyl diether were observed in strain XZYJT26T. The average nucleotide identity, digital DNA-DNA hybridization and amino acid identity values among the two strains and the members of Halobacterium were no more than 81, 25 and 77 %, respectively. These overall genome-related indices were below the threshold values for species boundary, indicating that strains Gai3-17T and XZYJT26T represent two novel species of Halobacterium. Thus, two novel species, Halobacterium wangiae sp. nov. and Halobacterium zhouii sp. nov., are proposed to accommodate strains Gai3-17T (=CGMCC 1.16101T=JCM 33551T) and XZYJT26T (=CGMCC 1.16682T=JCM 33556T), respectively.

Thermal Equilibrium and Energy Conversion of a New Photoreceptor with Two Chromophores as Studied by In Situ Spectroscopy

Archaerhodopsin-4 (aR4), an unknown structured membrane protein from Halobacterium species XZ515 found in a salt lake in China, functions as a proton pump similar to that of bacteriorhodopsin (bR). It has a seven-transmembrane topology and a protonated Schiff base formed by the retinal chromophore with the lysine 217 on the helix G through a covalent bond linkage. Absorption of a photon causes photoisomerization of the retinal chromophore from the all-trans to the 13-cis, 15-anti configuration and triggers a series of structural rearrangements of the protein that initiates a vectorial translocation of a proton out of the cell. aR4 has not only a retinal as the premier chromophore, but also a bacterioruberin as the second chromophore. Furthermore, aR4 has an opposite temporal order of proton uptake and release at neutral pH as compared with bR. In order to elucidate how the retinal cis-trans thermal equilibrium is maintained and modulated by the second chromophore, and further affect the proton uptake and release order, the photocycle kinetics, and the energy conversion efficiency in the claret membrane, in situ 2D solid-state NMR of the specifically labelled receptors in the claret membranes, reinforced with many single point mutation analyses and function assays were carried out. Hydrogen bonding and hydrophobic interactions were identified as the mechanistic origin of multiple outcomes, including direct electromechanical coupling to the dynamics of conformational changes within the receptor, direct monomer interactions, and energy conversion efficiency in native membranes. These new insights may be generalized to other receptors and proteins in which metastable thermal equilibria have been identified and perturbed by ligand binding and downstream signaling.

Halobacterium litoreum sp. nov., isolated from a marine solar saltern.

Halophilic archaeal strain ZS-54-S2T was isolated from Zhoushan marine solar saltern, China. Cells were rod-shaped, Gram-stain-negative and formed red-pigmented colonies on an agar plate. Strain ZS-54-S2T was able to grow at 20-50 °C (optimum 35 °C), at 1.7-4.8 M NaCl (optimum 3.9 M), at 0.005-1.0 M MgCl2 (optimum 0.05 M) and at pH 5.0-9.5 (optimum pH 7.0). The cells lysed in distilled water and the minimal NaCl concentration to prevent cell lysis was found to be 5 % (w/v). The major polar lipids of the strain were phosphatidic acid, phosphatidylglycerol, phosphatidylglycerol phosphate methyl ester, two glycolipids, which were chromatographically identical to sulfated galactosyl mannosyl galactofuranosyl glucosyl diether and galactosyl mannosyl glucosyl diether, and an unidentified glycolipid, which was chromatographically identical to one detected in Halobacterium salinarum ATCC 33171T. The 16S rRNA gene and rpoB' gene of strain ZS-54-S2T were phylogenetically related to the corresponding genes of Halobacterium noricense JCM 15102T (97.5 % and 90.6 % relatedness, respectively), Halobacterium jilantaiense CGMCC 1.5337T (96.9 and 91.2 %), Halobacterium rubrum CGMCC 1.12575T (96.8 and 90.3 %) and Halobacterium salinarum CGMCC 1.1958T (96.5 and 88.4 %). The DNA G+C content of strain ZS-54-S2T was 66.7 mol%. The phenotypic, chemotaxonomic and phylogenetic properties suggested that strain ZS-54-S2T (=CGMCC 1.12562T=JCM 30038T) represents a new species of Halobacterium, for which the name Halobacteriumlitoreum sp. nov. is proposed.

A transcription network of interlocking positive feedback loops maintains intracellular iron balance in archaea.

Iron is required for key metabolic processes but is toxic in excess. This circumstance forces organisms across the tree of life to tightly regulate iron homeostasis. In hypersaline lakes dominated by archaeal species, iron levels are extremely low and subject to environmental change; however, mechanisms regulating iron homeostasis in archaea remain unclear. In previous work, we demonstrated that two transcription factors (TFs), Idr1 and Idr2, collaboratively regulate aspects of iron homeostasis in the model species Halobacterium salinarum. Here we show that Idr1 and Idr2 are part of an extended regulatory network of four TFs of the bacterial DtxR family that maintains intracellular iron balance. We demonstrate that each TF directly regulates at least one of the other DtxR TFs at the level of transcription. Dynamical modeling revealed interlocking positive feedback loop architecture, which exhibits bistable or oscillatory network dynamics depending on iron availability. TF knockout mutant phenotypes are consistent with model predictions. Together, our results support that this network regulates iron homeostasis despite variation in extracellular iron levels, consistent with dynamical properties of interlocking feedback architecture in eukaryotes. These results suggest that archaea use bacterial-type TFs in a eukaryotic regulatory network topology to adapt to harsh environments.

Identification of extremely halophilic archaea associated with adult Artemia urmiana

The brine shrimp, Artemia is the dominant macrozooplankton present in many hypersaline environments. Artemia urmiana is the only macroscopic organism in Urmia Salt Lake (Iran), and the high salinity of the lake makes it a suitable environment for halophilic archaea too. Because of common environment for Artemia and extreme halophiles; this investigation is concentrated on studying the relationship between Artemia and halophilic archaea in Urmia Lake. In this study first the procedure of arhaea isolation was done. Then, isolated strains were sub-cultured and DNA was extracted and amplified by PCR using specific primers for amplifying archaeal 16S rRNA. The amplified archeal DNA fragments were purified, and sequenced. 16S rRNA sequences were compared to known sequences using the NCBI BLAST program. Sequences relating to Halorubrum, Haloarcula and Halobacterium species were identified in Urmia Salt Lake water and Artemia adults and the phylogenetic tree of different species was constructed. Only Halorubrum species were present in association with Artemia. They belong to Halobacteriaceae family of archeae which are isolated from different salt lakes in different parts of world and we could show their existence in adult Artemia, another organism living in hypersaline enviroments.

Halanaeroarchaeum sulfurireducens gen. nov., sp. nov., the first obligately anaerobic sulfur-respiring haloarchaeon, isolated from a hypersaline lake

Anaerobic enrichments with acetate as electron donor and carbon source, and elemental sulfur as electron acceptor at 4 M NaCl using anaerobic sediments and brines from several hypersaline lakes in Kulunda Steppe (Altai, Russia) resulted in isolation in pure culture of four strains of obligately anaerobic haloarchae growing exclusively by sulfur respiration. Such metabolism has not yet been demonstrated in any known species of Halobacteria, and in the whole archaeal kingdom, acetate oxidation with sulfur as acceptor was not previously demonstrated. The four isolates had nearly identical 16S rRNA gene sequences and formed a novel genus-level branch within the family Halobacteriaceae. The strains had a restricted substrate range limited to acetate and pyruvate as electron donors and elemental sulfur as electron acceptor. In contrast to aerobic haloarchaea, the biomass of anaerobic isolates completely lacked the typical red pigments. Growth with acetate+sulfur was observed between 3-5 M NaCl and at a pH range from 6.7 to 8.0. The membrane core lipids were dominated by archaeols. On the basis of distinct physiological and phylogenetic data, the sulfur-respiring isolates represent a novel species of a new genus in the family Halobacteriaceae, for which the name Halanaeroarchaeaum sulfurireducens gen. nov., sp. nov. is proposed. The type strain of the type species is HSR2T (=JCM 30661T=UNIQEM U935T).

The complete genome of a viable archaeum isolated from 123‐million‐year‐old rock salt

Live microbes have been isolated from rock salt up to Permian age. Only obligatory cellular functions can be performed in halite-buried cells. Consequently, their genomic sequences are likely to remain virtually unchanged. However, the available sequence information from these organisms is scarce and consists of mainly ribosomal 16S sequences. Here, live archaea were isolated from early Cretaceous (∼ 123 million years old) halite from the depth of 2000 m in Qianjiang Depression, Hubei Province, China. The sample was radiologically dated and subjected to rigorous surface sterilization before microbe isolation. The isolates represented a single novel species of Halobacterium, for which we suggest the name Halobacterium hubeiense, type strain Hbt. hubeiense JI20-1. The species was closely related to a Permian (225-280 million years old) isolate, Halobacterium noricense, originating from Alpine rock salt. This study is the first one to publish the complete genome of an organism originating from surface-sterilized ancient halite. In the future, genomic data from halite-buried microbes can become a key factor in understanding the mechanisms by which these organisms are able to survive in harsh conditions deep underground or possibly on other celestial bodies.

Flagellar filament bio-templated inorganic oxide materials - towards an efficient lithium battery anode.

Designing a new generation of energy-intensive and sustainable electrode materials for batteries to power a variety of applications is an imperative task. The use of biomaterials as a nanosized structural template for these materials has the potential to produce hitherto unachievable structures. In this report, we have used genetically modified flagellar filaments of the extremely halophilic archaea species Halobacterium salinarum to synthesize nanostructured iron oxide composites for use as a lithium-ion battery anode. The electrode demonstrated a superior electrochemical performance compared to existing literature results, with good capacity retention of 1032 mAh g−1 after 50 cycles and with high rate capability, delivering 770 mAh g−1 at 5 A g−1 (~5 C) discharge rate. This unique flagellar filament based template has the potential to provide access to other highly structured advanced energy materials in the future.

Novel expression and characterization of a light driven proton pump archaerhodopsin 4 in a Halobacterium salinarum strain

Archaerhodopsin 4 (AR4), a new member of the microbial rhodopsin family, is isolated from Halobacterium species xz515 in a Tibetan salt lake. AR4 functions as a proton pump similar to bacteriorhodopsin (BR) but with an opposite temporal order of proton uptake and release at neutral pH. However, further studies to elucidate the mechanism of the proton pump and photocycle of AR4 have been inhibited due to the difficulty of establishing a suitable system in which to express recombinant AR4 mutants. In this paper, we report a reliable method for expressing recombinant AR4 in Halobacterium salinarum L33 with a high yield of up to 20mg/l. Experimental results show that the recombinant AR4 retains the light-driven proton pump characteristics and photo-cycling kinetics, similar to that in the native membrane. The functional role of bacterioruberin in AR4 and the trimeric packing of AR4 in its native and recombinant forms are investigated through light-induced kinetic measurements, two-dimensional solid-state NMR experiments, dynamic light scattering (DLS) and Fourier transform infrared spectroscopy (FTIR). Such approaches provide new insights into structure–function relationships of AR4, and form a basis for other archaeal rhodopsins.

Inference of expanded Lrp-like feast/famine transcription factor targets in a non-model organism using protein structure-based prediction.

Widespread microbial genome sequencing presents an opportunity to understand the gene regulatory networks of non-model organisms. This requires knowledge of the binding sites for transcription factors whose DNA-binding properties are unknown or difficult to infer. We adapted a protein structure-based method to predict the specificities and putative regulons of homologous transcription factors across diverse species. As a proof-of-concept we predicted the specificities and transcriptional target genes of divergent archaeal feast/famine regulatory proteins, several of which are encoded in the genome of Halobacterium salinarum. This was validated by comparison to experimentally determined specificities for transcription factors in distantly related extremophiles, chromatin immunoprecipitation experiments, and cis-regulatory sequence conservation across eighteen related species of halobacteria. Through this analysis we were able to infer that Halobacterium salinarum employs a divergent local trans-regulatory strategy to regulate genes (carA and carB) involved in arginine and pyrimidine metabolism, whereas Escherichia coli employs an operon. The prediction of gene regulatory binding sites using structure-based methods is useful for the inference of gene regulatory relationships in new species that are otherwise difficult to infer.

Halobacterium rubrum sp. nov., isolated from a marine solar saltern.

Halophilic archaeal strain TGN-42-S1(T) was isolated from the Tanggu marine solar saltern, China. Cells from strain TGN-42-S1(T) were observed to be pleomorphic rods, stained Gram-negative, and formed red-pigmented colonies on solid media. Strain TGN-42-S1(T) was found to be able to grow at 20-50°C (optimum 35-37°C), at 1.7-4.8M NaCl (optimum 3.1M), at 0-1.0M MgCl2 (optimum 0.1M), and at pH 5.0-9.0 (optimum pH 7.0-7.5). The cells lysed in distilled water, and the minimal NaCl concentration to prevent cell-lysis was found to be 10% (w/v). The major polar lipids of the strain were phosphatidic acid, phosphatidylglycerol, phosphatidylglycerol phosphate methyl ester, phosphatidylglycerol sulfate, galactosyl mannosyl glucosyl diether (TGD-1), sulfated galactosyl mannosyl glucosyl diether (S-TGD-1), sulfated galactosyl mannosyl galactofuranosyl glucosyl diether (S-TeGD), and three unidentified glycolipids which were chromatographically identical to those of the Halobacterium species. The 16S rRNA gene and rpoB' gene of strain TGN-42-S1(T) were phylogenetically related to the corresponding genes of Halobacterium jilantaiense CGMCC 1.5337(T) (98.8 and 93.5% nucleotide identity, respectively), Halobacterium salinarum CGMCC 1.1958(T) (98.4 and 91.9%), and Halobacterium noricense JCM 15102(T) (96.9 and 91.1%). The DNA G+C content of strain TGN-42-S1(T) was determined to be 69.2mol%. Strain TGN-42-S1(T) showed low DNA-DNA relatedness with Hbt. jilantaiense CGMCC 1.5337(T) and Hbt. salinarum CGMCC 1.1958(T), the most closely related members of the genus Halobacterium. The phenotypic, chemotaxonomic, and phylogenetic properties suggested that strain TGN-42-S1(T) (=CGMCC 1.12575(T) =JCM 19908(T)) represents a new species of Halobacterium, for which the name Halobacterium rubrum sp. nov. is proposed.

Biofilm formation by haloarchaea

A fluorescence-based live-cell adhesion assay was used to examine biofilm formation by 20 different haloarchaea, including species of Halobacterium, Haloferax and Halorubrum, as well as novel natural isolates from an Antarctic salt lake. Thirteen of the 20 tested strains significantly adhered (P-value < 0.05) to a plastic surface. Examination of adherent cell layers on glass surfaces by differential interference contrast, fluorescence and confocal microscopy showed two types of biofilm structures. Carpet-like, multi-layered biofilms containing micro- and macrocolonies (up to 50 μm in height) were formed by strains of Halobacterium salinarum and the Antarctic isolate t-ADL strain DL24. The second type of biofilm, characterized by large aggregates of cells adhering to surfaces, was formed by Haloferax volcanii DSM 3757T and Halorubrum lacusprofundi DL28. Staining of the biofilms formed by the strongly adhesive haloarchaeal strains revealed the presence of extracellular polymers, such as eDNA and glycoconjugates, substances previously shown to stabilize bacterial biofilms. For Hbt. salinarum DSM 3754T and Hfx. volcanii DSM 3757T , cells adhered within 1 day of culture and remained viable for at least 2 months in mature biofilms. Adherent cells of Hbt. salinarum DSM 3754T showed several types of cellular appendages that could be involved in the initial attachment. Our results show that biofilm formation occurs in a surprisingly wide variety of haloarchaeal species.

Spherical particles of halophilic archaea correlate with exposure to low water activity--implications for microbial survival in fluid inclusions of ancient halite.

Viable extremely halophilic archaea (haloarchaea) have been isolated from million-year-old salt deposits around the world; however, an explanation of their supposed longevity remains a fundamental challenge. Recently small roundish particles in fluid inclusions of 22 000- to 34 000-year-old halite were identified as haloarchaea capable of proliferation (Schubert BA, Lowenstein TK, Timofeeff MN, Parker MA, 2010, Environmental Microbiology, 12, 440–454). Searching for a method to produce such particles in the laboratory, we exposed rod-shaped cells of Halobacterium species to reduced external water activity (aw). Gradual formation of spheres of about 0.4 μm diameter occurred in 4 m NaCl buffer of aw ≤ 0.75, but exposure to buffered 4 m LiCl (aw ≤ 0.73) split cells into spheres within seconds, with concomitant release of several proteins. From one rod, three or four spheres emerged, which re-grew to normal rods in nutrient media. Biochemical properties of rods and spheres were similar, except for a markedly reduced ATP content (about 50-fold) and an increased lag phase of spheres, as is known from dormant bacteria. The presence of viable particles of similar sizes in ancient fluid inclusions suggested that spheres might represent dormant states of haloarchaea. The easy production of spheres by lowering aw should facilitate their investigation and could help to understand the mechanisms for microbial survival over geological times.

Brazilian solar saltworks - ancient uses and future possibilities

Coastal solar saltworks of Brazil are exploited for sea salt, which becomes progressively concentrated by evaporation. This study aimed to review the current and new potential uses of these systems, in order to provide more dynamic for this activity. The first evaporation ponds are also used for artisanal fisheries, ensuring the livelihood of many families. All the brine rich in secondary salts (bittern) can be widely used by the chemical industry, while the Brazil shows an incipient production of "flower of salt", a salt with distinct characteristics with higher market value than sodium chloride. On the other hand, the saltponds have a high potential for management and obtaining of large populations of Artemia spp., purifying the brine through the action as biological filter. This microcrustacean occurs naturally in intermediate salinity ponds, being commonly used in aquaculture. Species of microalgae and halobacteria found in the saltworks are employed for extraction of beta-carotene and glycerol, used in an extensive list of products with high commercial value. These ecosystems represent refuge zones for many species of migratory birds, becoming imperative to promote the conservation of these hypersaline wetlands.

Archaeal diversity along a subterranean salt core from the Salar Grande (Chile)

The Salar Grande in the Coastal Range of Northern Chile is a fossil evaporitic basin filled with almost pure halite (95% NaCl average). It is assumed that the basin has not received input of brines since the Pliocene (5.3 to 1.8 million years). Below 1 m the halite has remained undissolved since this time, whereas the upper layer has been dissolved and recrystallized by dripping fogs and occasional rainfall. We compared the archaeal community at different depths using both nested PCR and cultivation. The upper 10 cm of halite crust contained diverse haloarchaeal species, including several from new genera, but their provenance is unknown. For samples deeper in the core, a new and rigorous procedure for chemically sterilizing the surface of single halite crystals was developed. These halite crystals contained only species of the genus Halobacterium (Hbt.). Halobacterium salinarum-like sequences were detected by PCR, and evidence that they were from ancient DNA include: comparison with numerous negative controls; detection of 16S rRNA sequence differences in non-conserved regions, indicating genuine evolutionary mutations rather than PCR-cloning artefacts; independent isolation of Hbt. salinarum from ancient halite; and diverse mechanisms possessed by this species for minimizing radiation damage and thus enhancing its potential for long-term survival. Haloarchaea related to Hbt. noricense were obtained from enrichment cultures from ≈ 0.4 and 15.4 m depth. We investigated Hbt. noricense strain A1 and found that when trapped inside halite crystals its recovery was as rapid after 27 months of entombment as at day 0, faring much better than other extreme halophiles. A biogeographical investigation showed that Hbt. noricense-like organisms were: commonly found in surface-sterilized ancient halite, associated with salt mines, in halite crusts, and, despite a much more intense search, only rarely detected in surface environments. We conclude that some Halobacterium species are specialists at long-term survival in halite.

Translationally optimal codons associate with aggregation‐prone sites in proteins

We analyze the relationship between codon usage bias and residue aggregation propensity in the genomes of four model organisms, Escherichia coli, yeast, fly, and mouse, as well as the archaeon Halobacterium species NRC-1. Using the Mantel-Haenszel procedure, we find that translationally optimal codons associate with aggregation-prone residues. Our results are qualitatively and quantitatively similar to those of an earlier study where we found an association between translationally optimal codons and buried residues. We also combine the aggregation-propensity data with solvent-accessibility data. Although the resulting data set is small, and hence statistical power low, results indicate that the association between optimal codons and aggregation-prone residues exists both at buried and at exposed sites. By comparing codon usage at different combinations of sites (exposed, aggregation-prone sites versus buried, non-aggregation-prone sites; buried, aggregation-prone sites versus exposed, non-aggregation-prone sites), we find that aggregation propensity and solvent accessibility seem to have independent effects of (on average) comparable magnitude on codon usage. Finally, in fly, we assess whether optimal codons associate with sites at which amino acid substitutions lead to an increase in aggregation propensity, and find only a very weak effect. These results suggest that optimal codons may be required to reduce the frequency of translation errors at aggregation-prone sites that coincide with certain functional sites, such as protein-protein interfaces. Alternatively, optimal codons may be required for rapid translation of aggregation-prone regions.

Halobacterium sp. SP1(1) as a starter culture for accelerating fish sauce fermentation

Application of Halobacterium sp. SP1(1) for the acceleration of fish sauce fermentation. Traditional fish sauce fermentation was mimicked using Halobacterium sp. SP1(1) as starter culture. Protease activity, peptide release and α-amino content (parameters used to monitor the progress of the fermentation) were high at day 10 in tests and day 20 in un-inoculated controls. The total protein and nitrogen contents were also high in tests compared with controls. The amino acid profile observed at the end of fermentation in experimental samples, when compared with the commercial sauce preparation, was found to be better with respect to flavour and aroma contributing amino acids as well as essential amino acid lysine. Microflora analysis of the final fish sauce revealed the absence of any nonhalophilic or halotolerant micro-organisms. The protease-producing halophilic isolates obtained from the fish sauce of eviscerated and uneviscerated controls were identified as Halobacterium sp. F1 and F2, respectively, by 16S rDNA sequence analysis. Exogenous augmentation of Halobacterium sp. SP1(1) accelerated the fish sauce fermentation process with an additive effect on the existing natural microflora present in the fish during fermentation. Halobacterium sp SP1(1), therefore, can be used as an important starter culture for accelerating the fish fermentation process, which is attributed to its extracellular protease. The present study is the first report on use of Halobacterium species as a starter culture for accelerating fish sauce fermentation. Use of halobacterial starter cultures may revolutionize the process in fish sauce industries by reducing the fermentation time and making the process more economical with improved nutritive value of product.