The role of glycerol in the nutrition of halophilic archaeal communities: a study of respiratory electron transport

Abstract Respiratory electron transport activity in the Dead Sea and saltern crystallizer ponds, hypersaline environments inhabited by dense communities of halophilic archaea and unicellular green algae of the genus Dunaliella , was assayed by measuring reduction of 2-( p -iodophenyl)-3( p -nitrophenyl)-5-phenyl tetrazolium chloride (INT) to INT-formazan. Typical rates obtained were in the order of 5.5–17.7 nmol INT reduced h ⁻¹ per 10⁶ cells at 35 ° C. In Dead Sea water samples, respiratory activity was stimulated more than two-fold by addition of glycerol, but not by any of the other carbon compounds tested, including sugars, organic acids, and amino acids, or by addition of inorganic nutrients. Stimulation by glycerol had a half-saturation constant of 0.75 μM. A similar respiratory activity was also found when Dead Sea water samples were diluted with distilled water and incubated in the light. As Dunaliella cells did not reduce INT, it is suggested that photosynthetically produced glycerol leaking from the algae is the preferred carbon and energy source for the development of halophilic archaea in hypersaline environments. In samples from saltern crystallizer pond stimulation of INT reduction by glycerol was much less pronounced, probably because the community was less severely carbon-limited.     

Uptake and turnover of acetate in hypersaline environments

Abstract: Acetate uptake and turnover rates were determined for the heterotrophic community in hypersaline environments (saltern crystallizer ponds, the Dead Sea) dominated by halpphilic Archaea. Acetate was formed from glycerol, which is potentially the major available carbon source for natural communities of halophilic Archaea. Values of [ K _t+ S _n] (the sum of the substrate affinity and the substrate concentration present in situ) for acetate measured in saltern crystallizer ponds were around 4.5–11.5 μM, while in the Dead Sea during a Dunaliella bloom values up to 12.8 μM were found. Maximal theoretical rates ( V _max) of acetate uptake in saltern crystallizer ponds were 12–56 nmol l⁻¹ h⁻¹, with estimated turnover times for acetate ( T _t) between 127–730 h at 35°C. V _max values measured in the Dead Sea were between 0.8 and 12.8 nmol l⁻¹ h⁻¹, with turnover times in the range of 320–2190 h. V _max values for acetate were much lower than those for glycerol. Comparisons with pure cultures of halophilic Archaea grown under different conditions showed that the natural communities were not adapted for preferential use of acetate. Both in natural brines and in pure cultures of halophilic Archaea, acetate incorporation rates rapidly decreased above the optimum pH value, probably since acetate enters the cell only in its unionized form. The low affinity for acetate, together with low potential utilization rates result in the long acetate turnover times, which explains the accumulation of acetate observed when low concentrations of glycerol are supplied as a nutrient to natural communities of halophilic Archaea.     

Characterization of the dominant halophilic archaea in a bacterial bloom in the dead sea

Abstract A mass bloom of halophilic archaea developed in the Dead Sea in the summer of 1992, with peak densities of more than 3 × 10⁷ cells/ml, imparting a red coloration to the water. Microscopical examination showed a numerical dominance of pleomorphic, flat cells. Attempts to identify the dominant type of halophilic archaea by means of growth experiments, both on agar plates and by dilution in liquid media, were unsuccessful, as viable counts obtained were two or more orders of magnitude lower than the total microscopic counts. Analysis of the polar lipids in the Dead Sea biomass during the bloom showed one major glycolipid to be present in the extracts, corresponding with the sulfated diglycosyl diether lipid (S-DGD-1) characteristic of the genus Haloferax . No indications were found for the presence of significant amounts of other glycolipids that indicate the presence of large numbers of Dead Sea archaea such as Halobacterium sodomense or Haloarcula marismortui , or Halobacterium species such as H. halobium, H. salinarium and H. saccharovorum . Thus, the numerically dominant organisms in the bloom is probably a difficult to culture, not yet isolated, representative of the genus Haloferax .     

Phylogenetic analyses of some extremely halophilic archaea isolated from Dead Sea water, determined on the basis of their 16S rRNA sequences.

Twenty-two extremely halophilic aerobic archaeal strains were isolated from enrichments prepared from Dead Sea water samples collected 57 years ago. The isolates were phenotypically clustered into five different groups, and a representative from each group was chosen for further study. Almost the entire sequences of the 16S rRNA genes of these representatives, and of Haloarcula hispanica ATCC 33960, were determined to establish their phylogenetic positions. The sequences of these strains were compared to previously published sequences of 27 reference halophilic archaea (members of the family Halobacteriaceae) and two other archaea, Methanobacterium formicicum DSM 1312 and Methanospirillum hungatei DSM 864. Phylogenetic analysis using approximately 1,400 base comparisons of 16S rRNA-encoding gene sequences demonstrated that the five isolates clustered closely to species belonging to three different genera--Haloferax, Halobacterium, and Haloarcula. Strains E1 and E8 were closely related and identified as members of the species Haloferax volcanii, and strain E12 was closely related and identified as a member of the species Halobacterium salinarum. However, strains E2 and E11 clustered in the Haloarcula branch with Haloarcula hispanica as the closest relative at 98.9 and 98.8% similarity, respectively. Strains E2 and E11 could represent two new species of the genus Haloarcula. However, because strains of these two new species were isolated from a single source, they will not be named until additional strains are isolated from other sources and fully characterized.     

Distribution of glycerol dehydrogenase and glycerol kinase activity in halophilic archaea

Abstract A constitutive NAD⁺-dependent glycerol dehydrogenase activity was detected in Halobacterium salinarium and Halobacterium cutirubrum . Optimal activity was found at 3 M KCl and pH 8–10. No glycerol dehydrogenase activity could be demonstrated in representatives of the genera Haloferax and Haloarcula , even when grown in the presence of glycerol, or in Halobacterium saccharovorum and Halobacterium sodomense . Glycerol kinase activity was shown to be present constitutively in all halophilic archaea examined. The finding that glycerol dehydrogenase is found only in part of the halophilic arachaea makes dihydroxyacetone an improbable candidate as the precursor for the glycerol moiety of halobacterial lipids.     

Taxonomic analysis of extremely halophilic archaea isolated from 56-years-old dead sea brine samples

A taxonomic study comprising both phenotypic and genotypic characterization, has been carried out on a total of 158 extremely halophilic aerobic archaeal strains. These strains were isolated from enrichments prepared from Dead Sea water samples dating from 1936 that were collected by B. E. Volcani for the demonstration of microbial life in the Dead Sea. The isolates were examined for 126 morphological, physiological, biochemical and nutritional tests. Numerical analysis of the data, by using the S(J) coefficient and UPGMA clustering method, showed that the isolates clustered into six phenons. Twenty-two out of the 158 strains used in this study were characterized previously (ARAHAL et al., 1996) and were placed into five phenotypic groups. The genotypic study included both the determination of the guanineplus-cytosine content of the DNA and DNA-DNA hybridization studies. For this purpose, representative strains from the six phenons were chosen. These groups were found to represent some members of three different genera - Haloarcula (phenons A, B, and C), Haloferax (phenons D and E) and Halobacterium (phenon F) - of the family Halobacteriaceae, some of them never reported to occur in the Dead Sea, such as Haloarcula hispanica, while Haloferax volcanii (phenons D and E) was described in the Dead Sea by studies carried out several decades later than Volcani's work.     

PCR and blot hybridization for rapid identification of Haloferax species

Based on the amplification of a 16S rDNA, a PCR assay for the identification of species of Haloferax to genus level was performed. Two variable regions of the 16S rDNA in Haloferax spp. were selected as genus-specific primers for the PCR assay and hybridization probe. Five genera of halophilic Archaea and Escherichia coli were examined as outside groups. Using this approach, all strains of Haloferax spp. were positive. In contrast, all species belonging to the most closely related genera, including Natrinema, Halorubrum, Halobacterium, and Haloarcula, were negative. In addition, the mass bloom of halophilic Archaea that develops in the El-Mallahet saltern of Alexandria City was positive using the same approach. This assay, which does not require pure cultures of microorganisms, is a specific and rapid method for identifying Haloferax spp. in hypersaline environments.     

N-linked glycosylation in Archaea: two paths to the same glycan

N‐linked protein glycosylation occurs in all three branches of life, eukaryotes, bacteria and archaea. The simplest system is that of the bacterium, Campylobacter jejuni, in which a heptasaccharide glycan is added to multiple proteins from a single lipid carrier molecule. In the eukaryotic system a conserved tetradecasaccharide modification is first added to target proteins, but is then modified by trimming and addition of other glycans from additional carrier molecules resulting in a diverse array of glycans of distinct functionality. In the halophilic Archaea from the Dead Sea, Haloferax volcanii, the surface array or S‐layer protein is glycosylated with a pentasaccharide. This glycan is synthesized from two separate carrier molecules, one that carries a tetrasaccharide and another that carries the terminal mannose, in a process that is analogous to that of eukaryotes. In this issue of Molecular Microbiology the glycosylation of the S‐layer of another halophilic Archaea from the Dead Sea, Haloarcula marismortui is characterized ( Calo et al., 2011 ). This S‐layer is glycosylated with the same pentasaccharide as that of Hfx. volcanii, but the intact pentasaccharide is synthesized on a single carrier molecule in Har. marismortui in a process that more closely resembles that of the bacterial N‐linked system.     

岱山盐场可培养嗜盐菌的多样性及其产酶活性筛选

从岱山盐场采集样品,利用选择性培养基分离培养嗜盐菌,对盐田环境中可培养嗜盐菌的多样性及产酶活性进行研究.共分离得到181株嗜盐菌菌株,通过真细菌和古生菌两对通用引物扩增其16S rRNA 基因,并采用限制性内切酶Hinf I进行ARDRA(amplified rDNA restriction analysis)多态性分析,共分为21个不同的操作分类单元(operation taxonomy units, OTUs),其中嗜盐细菌有12个OTUs,嗜盐古菌有9个OTUs.选取具有不同酶切图谱的代表菌株进行克隆测序,BLAST 比对及系统发育分析将嗜盐细菌归于7个属,其中嗜盐单胞菌属(Halomonas)的菌株数占优势,是嗜盐细菌总数的46.8%;嗜盐古菌归于4个属,盐盒菌属(Haloarcula)的菌株数占优势,是嗜盐古菌总数的49.1%.对分离菌株的产酶活性进行检测表明,岱山盐田环境蕴含丰富的产淀粉酶、蛋白酶和脂肪酶等生物活性酶的嗜盐菌, 其中盐盒菌属产酶菌株数最丰富.研究结果表明,岱山盐田环境中具有较为丰富的嗜盐菌多样性,是筛选产酶菌株的重要资源库.     

First evidence for the salt-dependent folding and activity of an esterase from the halophilic archaea Haloarcula marismortui

A gene encoding an esterase from Haloarcula marismortui, a halophilic archaea from the Dead Sea, was cloned, expressed in Escherichia coli, and the recombinant protein (Hm EST) was biochemically characterized. The enzymatic activity of Hm EST was shown to exhibit salt dependence through salt-dependent folding. Hm EST exhibits a preference for short chain fatty acids and monoesters. It is inhibited by phenylmethylsulfonyl fluoride, diethyl-p-nitrophenyl phosphate, and 5-methoxy-3-(4-phenoxyphenyl)-3H-[1,3,4]oxadiazol-2-one, confirming the conclusion from sequence alignments that Hm EST is a serine carboxylesterase belonging to the hormone-sensitive lipase family. The activity of Hm EST is optimum in the presence of 3 M KCl and no activity was detected in the absence of salts. Far–UV circular dichroism showed that Hm EST is totally unfolded in salt-free medium and secondary structure appears in the presence of 0.25–0.5 M KCl. After salt depletion, the protein was able to recover 60% of its initial activity when 2 M KCl was added. A 3D model of Hm EST was built and its surface properties were analyzed, pointing to an enrichment in acidic residues paralleled by a depletion in basic residues. This peculiar charge repartition at the protein surface supports a better stability of the protein in a high salt environment.     

Diversity of Archaea in hypersaline environments characterized by molecular-phylogenetic and cultivation studies

The diversity of Archaea from three different hypersaline environments was analyzed and compared by polymerase chain reaction (PCR)-based molecular phylogenetic techniques and cultivation approaches. The samples originated from a crystallization pond of a solar saltern in Spain (FC); an alkaline lake in Nevada, USA, (EMF); and a small pond from a slag heap of a potassium mine in Germany (DIE). Except for two 16S rDNA sequences that were related to crenarchaeota from soil and did not apparently belong to the indigenous halophilic community, all sequences recovered from environmental DNA or cultivated strains grouped within the Halobacteriaceae. Mostly 16S rDNA sequences related to the genera Halorubrum and Haloarcula were detected in sample FC, and organisms belonging to these genera were also recovered by cultivation. In contrast, sequences related to five different groups of halophilic archaea were amplified from sample DIE (including novel lineages with only uncultivated phylotypes), but the organisms that were cultivated from this sample fell into different groups (i.e., Natronococcus, Halorubrum, or unaffiliated) and did not overlap with those predicted using the culture-independent approach. With respect to the highly alkaline sample, EMF, four groups were predicted from the environmental 16S rDNA sequences, two of which ( Natronomonas and Haloarcula) were also recovered through cultivation together with Natronococcus isolates. In summary, we found that halophilic archaea dominate the archaeal populations in these three hypersaline environments and show that culturability of the organisms predicted by molecular surveys might strongly depend on the habitat chosen. While a number of novel halophilic archaea have been isolated, we have not been able to cultivate representatives of the new lineages that were detected in this and several other environmental studies.     

DNA-rRNA hybridization studies on Halococcus saccharolyticus and other halobacteria

Abstract Several representative extremely halophilic archaea (formerly archaebacteria) were studied with respect to their genetic relatedness by using a DNA-rRNA hybridization approach. Our results confirm the phylogenetic relatedness of Halococcus morrhuae and Halococcus saccharolyticus but support their separation as two different taxa, at least at species level. In addition, this phylogenetic relatedness was significantly lower than that between species belonging to the genera Haloferax and Haloarcula .     

Sugar-glycerol cofermentations in lactobacilli: the fate of lactate.

The simultaneous fermentation of glycerol and sugar by lactobacillus brevis B22 and Lactobacillus buchneri B190 increases both the growth rate and total growth. The reduction of glycerol to 1,3-propanediol by the lactobacilli was found to influence the metabolism of the sugar cofermented by channelling some of the intermediate metabolites (e.g., pyruvate) towards NADH-producing (rather than NADH-consuming) reactions. Ultimately, the absolute requirement for NADH to prevent the accumulation of 3-hydroxypropionaldehyde leads to a novel lactate-glycerol cofermentation. As a result, additional ATP can be made not only by (i) converting pyruvate to acetate via acetyl phosphate rather than to the ethanol usually found and (ii) oxidizing part of the intermediate pyruvate to acetate instead of the usual reduction to lactate but also by (iii) reoxidation of accumulated lactate to acetate via pyruvate. The conversion of lactate to pyruvate is probably catalyzed by NAD-independent lactate dehydrogenases that are found only in the cultures oxidizing lactate and producing 1,3-propanediol, suggesting a correlation between the expression of these enzymes and a raised intracellular NAD/NADH ratio. The enzymes metabolizing glycerol (glycerol dehydratase and 1,3-propanediol dehydrogenase) were expressed in concert without necessary induction by added glycerol, although their expression may also be influenced by the intracellular NAD/NADH ratio set by the different carbohydrates fermented.     

内蒙古锡林浩特地区嗜盐古菌多样性的研究

从内蒙古锡林浩特地区3个不同的盐湖中共分离到165株古菌,通过ARDRA分析后得到不同的类群,从各个类群中随机选取1~2个代表菌株进行16S rDNA序列测定和系统发育的分析。结果表明分离的菌株分布在Halorubrum,Natronococcus,Natronorubrum,Haloterrigena,Halorhabdus,Halobiforma,Haloarcula,Haloferax8个属和另外两个分支中,表现了锡林浩特地区嗜盐古菌的多样性。部分菌株的16S rDNA序列同源性低于97%,可能是潜在的新属或新种,代表了该地区嗜盐古菌的独特类型。     

Cloning and sequencing of ftsZ homolog from extremely halophilic archaeon Haloarcula japonica strain TR-1.

The gene encoding FtZ was cloned from triangular disc-shaped extremely halophilic archaeon Haloarcula japonica strain TR-1. Nucleotide sequencing analysis of the possible ftsZ gene revealed that the structural gene consisted of an open reading frame of 1,182 nucleotides encoding 394 amino acids. The deduced amino acid sequence of the Ha. japonica FtsZ showed high identities with those Halobacterium salinarom, Haloferax volcanii and Haloferax mediterranei FtsZs.     

Amino Acid Biosynthesis in the Halophilic Archaeon Haloarcula hispanica

Biosynthesis of proteinogenic amino acids in the extremely halophilic archaeon Haloarcula hispanica was explored by using biosynthetically directed fractional 13C labeling with a mixture of 90% unlabeled and 10% uniformly 13C-labeled glycerol. The resulting 13C-labeling patterns in the amino acids were analyzed by two-dimensional 13C,1H correlation spectroscopy. The experimental data provided evidence for a split pathway for isoleucine biosynthesis, with 56% of the total Ile originating from threonine and pyruvate via the threonine pathway and 44% originating from pyruvate and acetyl coenzyme A via the pyruvate pathway. In addition, the diaminopimelate pathway involving diaminopimelate dehydrogenase was shown to lead to lysine biosynthesis and an analysis of the 13C-labeling pattern in tyrosine indicated novel biosynthetic pathways that have so far not been further characterized. For the 17 other proteinogenic amino acids, the data were consistent with data for commonly found biosynthetic pathways. A comparison of our data with the amino acid metabolisms of eucarya and bacteria supports the theory that pathways for synthesis of proteinogenic amino acids were established before ancient cells diverged into archaea, bacteria, and eucarya.     

Mechanisms of acetate formation and acetate activation in halophilic archaea

The halophilic archaea Halococcus (Hc.) saccharolyticus, Haloferax (Hf.) volcanii, and Halorubrum (Hr.) saccharovorum were found to generate acetate during growth on glucose and to utilize acetate as a growth substrate. The mechanisms of acetate formation from acetyl-CoA and of acetate activation to acetyl-CoA were studied. Hc. saccharolyticus, exponentially growing on complex medium with glucose, formed acetate and contained ADP-forming acetyl-CoA synthetase (ADP-ACS) rather than acetate kinase and phosphate acetyltransferase or AMP-forming acetyl-CoA synthetase. In the stationary phase, the excreted acetate was completely consumed, and cells contained AMP-forming acetyl-CoA synthetase (AMP-ACS) and a significantly reduced ADP-ACS activity. Hc. saccharolyticus, grown on acetate as carbon and energy source, contained only AMP-ACS rather than ADP-ACS or acetate kinase. Cell suspensions of Hc. saccharolyticus metabolized acetate only when they contained AMP-ACS activity, i.e., when they were obtained after growth on acetate or from the stationary phase after growth on glucose. Suspensions of exponential glucose-grown cells, containing only ADP-ACS but not AMP-ACS, did not consume acetate. Similar results were obtained for the phylogenetic distantly related halophilic archaea Hf. volcanii and Hf. saccharovorum. We conclude that, in halophilic archaea, the formation of acetate from acetyl-CoA is catalyzed by ADP-ACS, whereas the activation of acetate to acetyl-CoA is mediated by an inducible AMP-ACS.Abbreviations. Hc. Halococcus - Hf. Haloferax - Hr. Halorubrum - Hb. Halobacterium An erratum to this article can be found at     

Transformation of members of the genus Haloarcula with shuttle vectors based on Halobacterium halobium and Haloferax volcanii plasmid replicons.

We have stably transformed both Haloarcula vallismortis and Haloarcula hispanica with the halobacterium-Escherichia coli shuttle vectors pWL102 (based on the Haloferax volcanii pHV2 replicon) and pUBP2 (based on the Halobacterium halobium pHH1 replicon). Haloferax volcanii, Halobacterium halobium, and Haloarcula vailismortis are equally distant from one another and span the phylogenetic depth of the halophilic Archaea; thus, these vectors may be generally useful for the halophiles. Both Haloarcula vallismortis and Haloarcula hispanica exhibit previously unreported complex life cycles and are therefore significant as genetically approachable models of cellular differentiation within the Archaea.     

Availability, uptake and turnover of glycerol in hypersaline environments

Abstract A sensitive assay for glycerol and other polyols was developed, based on periodate oxidation to formaldehyde, followed by a colorimetric assay with 3-methyl-2-benzothiazolone hydrazone. Apparent glycerol concentrations thus measured in saltern crystallizer ponds were around 20–36 μM, while in the Dead Sea, during a Dunaliella bloom, values were up to 27 μM. However, these values probably overestimate the glycerol concentrations present, as shown by labeled glycerol uptake experiments. Values of [K + S_n] (natural concentration + affinity constant) in saltern ponds were as low as 0.76–1.4 μM, with V_max values of 193–303 nmol 1⁻¹h⁻¹, and turnover times between 2.6–7.2 h at 35°C. Similar measurements in the Dead Sea were: [K + S_n] 0.07–1.41 μM, V_max values 160–426 nmol 1⁻¹h⁻¹, and turnover times in the range of 0.45–3.3 h.