Crystallization of halophilic malate dehydrogenase from Halobacterium marismortui

Malate dehydrogenase from the extreme halophile Halobacterium marismortui crystallizes in highly concentrated phosphate solution in space group 12 with cell dimensions a = 113.8 A, b = 122.8 A, c = 126.7 A, beta = 98.1 degrees. The halophilic enzyme was found to be unstable at lower concentrations of phosphate. It associates with unusually large amounts of water and salt, and the combined particle volume shows a tight fit in the unit cell.     

Lactate dehydrogenase from the extreme halophilic archaebacterium Halobacterium marismortui

D-Lactate dehydrogenase from the extreme halophilic archaebacterium Halobacterium marismortui has been partially purified by ammonium-sulfate fractionation, hydrophobic and ion exchange chromatography. Catalytic activity of the enzyme requires salt concentrations beyond 1M NaCl: optimum conditions are 4M NaCl or KCl, pH 6-8, 50 degrees C. Michaelis constants for NADH and pyruvate under optimum conditions of enzymatic activity are 0.070 and 4.5mM, respectively. As for other bacterial D-specific lactate dehydrogenases, fructose 1,6-bisphosphate and divalent cations (Mg2+, Mn2+) do not affect the catalytic activity of the enzyme. As shown by gel-filtration and ultracentrifugal analysis, the enzyme under the conditions of the enzyme assay is a dimer with a subunit molecular mass close to 36 kDa. At low salt concentrations (less than 1M), as well as high concentrations of chaotropic solvent components and low pH, the enzyme undergoes reversible deactivation, dissociation and denaturation. The temperature dependence of the enzymatic activity shows non-linear Arrhenius behavior with activation energies of the order of 90 and 25 kJ/mol at temperatures below and beyond ca. 30 degrees C. In the presence of high salt, the enzyme exhibits exceptional thermal stability; denaturation only occurs at temperatures beyond 55 degrees C. The half-time of deactivation at 70 and 75 degrees C is 300 and 15 min, respectively. Maximum stability is observed at pH 7.5-9.0.     

Preliminary X-ray diffraction studies on 2 Fe-ferredoxin from Halobacterium of the Dead Sea

The 2 Fe-ferredoxin from the Halobacterium of the Dead Sea has been crystallized. The space group is P6₃22 with one protein molecule per asymmetric unit. The cell parameters are $\text{a = b = 60.6}\text{A}\text{?}\text{, c = 127.8}\text{A}\text{?}$. The crystals are stable under radiation and diffract to high resolution.     

Characterization and crystallization of ribosomal particles from Halobacterium marismortui

Ribosomes and their subunits have been isolated from Halobacterium marismortui, an extremely halophilic bacterium from the Dead Sea. The stability and functional activity of the subunits were tested under a wide range of salt conditions. Three-dimensional microcrystals of the large ribosomal subunits have been obtained. Electron microscopy of positively stained thin sections of these crystals showed that the particles are closely packed with approximate cell constants of 310 × 350 Å.     

Halobacterium volcanii spec. nov., a Dead Sea halobacterium with a moderate salt requirement

A halophilic bacterium was isolated from bottom sediment from the Dead Sea. The organism possessed the properties of the halobacteria, but differed from the known species in two important respects, 1) the cells were disc-shaped and often cupped when grown under optimum conditions, 2) the optimum requirements for sodium chloride was in the range 1.7–2.5 molar which is about half of that generally reported for the halobacteria. The organism was assigned to the genus Halobacterium and described as Halobacterium volcanii spec.nov. The optimum sodium chloride concentration for growth was close to that found in the Dead Sea. The tolerance for magnesium chloride was very high; the organism grew well in media containing magnesium chloride in the concentrations found in the Dead Sea. Halobacterium volcanii is therefore remarkably well fitted for life in the Dead Sea.     

Three-dimensional structure of the regular surface glycoprotein layer of Halobacterium volcanii from the Dead Sea

A three-dimensional reconstruction from electron micrographs of negatively stained cell envelopes of Halobacterium volcanii has revealed the structure of the surface glycoprotein to a resolution of 2 nm. The glycoprotein is arranged on a p6 lattice with a lattice constant of 16.8 nm. It forms 4.5 nm high, dome-shaped, morphological complexes with a narrow pore at the apex opening into a `funnel' towards the cell membrane. The polarity of the structure was derived from freeze-etching experiments and `edge' views. Six radial protrusions emanate from each morphological complex and join around the 3-fold axis to provide lateral connectivity. Using the primary structure of the surface glycoprotein of the closely related species Halobacterium halobium (Lechner and Sumper, 1987) and the cell envelope profile from a previous X-ray analysis of the same species (Blaurock et al., 1976) we have integrated our reconstruction into a model of halobacterial cell envelope.     

Halobacterium volcanii spec. nov., a Dead Sea halobacterium with a moderate salt requirement.

A halophilic bacterium was isolated from bottom sediment from the Dead Sea. The organism possessed the properties of the halobacteria, but differed from the known species in two important respects, 1) the cells were disc shaped and often cupped when grown under optimum conditions, 2) the optimum requirements for sodium chloride was in the range 1.7--2.5 molar which is about half of that generally reported for the halobacteria. The organism was assigned to the genus Halobacterium and described as Halobacterium volcanni spec. rov. The optimum sodium chloride concentration for growth was close to that found in the Dead Sea. The tolerance for magnesium chloride was very high; the organism grew well in media containing magnesium chloride in the concentrations found in the Dead Sea. Halobacterium volcanii is therefore remarkably well fitted for life in the Dead Sea.     

Characterization of alcohol dehydrogenase (ADH12) from Haloarcula marismortui, an extreme halophile from the Dead Sea

Haloarchaeal alcohol dehydrogenases are of increasing interest as biocatalysts in the field of white biotechnology. In this study, the gene adh12 from the extreme halophile Haloarcula marismortui (HmADH12), encoding a 384 residue protein, was cloned into two vectors: pRV1 and pTA963. The resulting constructs were used to transform host strains Haloferax volcanii (DS70) and (H1209), respectively. Overexpressed His-tagged recombinant HmADH12 was purified by immobilized metal-affinity chromatography (IMAC). The His-tagged protein was visualized by SDS-PAGE, with a subunit molecular mass of 41.6 kDa, and its identity was confirmed by mass spectrometry. Purified HmADH12 catalyzed the interconversion between alcohols and aldehydes and ketones, being optimally active in the presence of 2 M KCl. It was thermoactive, with maximum activity registered at 60°C. The NADP(H) dependent enzyme was haloalkaliphilic for the oxidative reaction with optimum activity at pH 10.0. It favored a slightly acidic pH of 6.0 for catalysis of the reductive reaction. HmADH12 was significantly more tolerant than mesophilic ADHs to selected organic solvents, making it a much more suitable biocatalyst for industrial application.     

Solution studies of elongation factor Tu from the extreme halophile Halobacterium marismortui.

The activity, stability and structure in solution of polypeptide elongation factor hEF-Tu from Halobacterium marismortui have been investigated. The protein is stable in aqueous solutions only at high concentrations of NaCl, KCl or ammonium sulphate, whereas it is more active in exchanging GDP at lower salt concentrations. It is more active and stable at lower pH values than is non-halophilic EF-Tu. The structure in solution of the protein was determined by complementary density, ultracentrifugation, dynamic light-scattering and neutron-scattering measurements. The protein has large hydration interactions, similar to those of other halophilic proteins: 0.4 (+/- 0.1) g of water and 0.20 (+/- 0.05) g of KCl associated with 1 g of protein, with a water/KCl mass ratio always remaining close to 2. The kinetics of inactivation at low salt concentrations showed a stabilizing effect of NaCl when compared to KCl. At low salt concentration, inactivation, protein unfolding and aggregation were strongly correlated. The results suggest that the stabilization model proposed for halophilic malate dehydrogenase by Zaccai et al., involving extensive protein interactions with hydrated salt ions, is also valid for hEF-Tu.     

Molecular basis for the special properties of proteins and enzymes from Halobacterium marismortui

Abstract Three proteins from Halobacterium marismortui , malate dehydrogenase (hMDH), glutamate dehydrogenase (hGDH) and ferredoxin (hFD) were purified and characterized with respect to their molecular masses, amino acid composition and, for hFD only, primary structure. Striking features of halophilic proteins are: the high excess of acidic over basic residues; acidic clusters in the sequence. Low-salt concentration causes inactivation and changes in structural parameters of hMDH and hGDH. Reactivation of hMDH involves long-lived stable intermediates. The salt concentration optimum of enzymic activity is independent of salt nature. The high capacity of halophilic proteins to retain water and salt is due to unique molecular properties, studied by physico-chemical techniques.     

35Cl nuclear magnetic resonance studies of anion binding to halophilic proteins: Ferredoxin from Halobacterium of the Dead Sea

The anion-binding characteristics of ferredoxin from Halobacterium of the Dead Sea have been studied by ³⁵Cl^? NMR. It is found that the binding constant of Cl^? to halophilic ferredoxin is ca. 0.09 at 28 °C and that the binding enthalpy is positive. It is also found that the correlation time for chloride ions bound to halophilic ferredoxin is about 10 ns. The effect on the ³⁵Cl^?1 NMR signal of adding competing anions is also studied. Halophilic proteins like ferredoxin which have a high negative charge bind anions with low affinity but the ³⁵Cl^? quadrupole relaxation technique can conveniently monitor such weak binding.     

Single crystals of large ribosomal particles from Halobacterium marismortui diffract to 6 A

Large, well-ordered three-dimensional crystals of 50 S ribosomal subunits from Halobacterium marismortui have been obtained by seeding. The crystals have been characterized with synchrotron X-ray radiation as monoclinic, space group P2(1), with unit cell dimensions of a = 182(+/- 5) A, b = 584(+/- 10) A, c = 186(+/- 5) A, beta = 109 degrees. At 4 degrees C, the crystals (0.6 mm X 0.6 mm X 0.1 mm) diffract to 6 A resolution and are stable in the synchrotron beam for several hours. Compact packing is reflected from the crystallographic unit cell parameters and from electron micrographs of positively stained thin sections of embedded crystals.     

Different routes to the same ending: comparing the N-glycosylation processes of Haloferax volcanii and Haloarcula marismortui, two halophilic archaea from the Dead Sea

Recent insight into the N-glycosylation pathway of the haloarchaeon, Haloferax volcanii, is helping to bridge the gap between our limited understanding of the archaeal version of this universal post-translational modification and the better-described eukaryal and bacterial processes. To delineate as yet undefined steps of the Hfx. volcanii N-glycosylation pathway, a comparative approach was taken with the initial characterization of N-glycosylation in Haloarcula marismortui, a second haloarchaeon also originating from the Dead Sea. While both species decorate the reporter glycoprotein, the S-layer glycoprotein, with the same N-linked pentasaccharide and employ dolichol phosphate as lipid glycan carrier, species-specific differences in the two N-glycosylation pathways exist. Specifically, Har. marismortui first assembles the complete pentasaccharide on dolichol phosphate and only then transfers the glycan to the target protein, as in the bacterial N-glycosylation pathway. In contrast, Hfx. volcanii initially transfers the first four pentasaccharide subunits from a common dolichol phosphate carrier to the target protein and only then delivers the final pentasaccharide subunit from a distinct dolichol phosphate to the N-linked tetrasaccharide, reminiscent of what occurs in eukaryal N-glycosylation. This study further indicates the extraordinary diversity of N-glycosylation pathways in Archaea, as compared with the relatively conserved parallel processes in Eukarya and Bacteria.     

Primary structures of ribosomal proteins from the archaebacterium Halobacterium marismortui and the eubacterium Bacillus stearothermophilus.

Approximately 40 ribosomal proteins from each Halobacterium marismortui and Bacillus stearothermophilus have been sequenced either by direct protein sequence analysis or by DNA sequence analysis of the appropriate genes. The comparison of the amino acid sequences from the archaebacterium H marismortui with the available ribosomal proteins from the eubacterial and eukaryotic kingdoms revealed four different groups of proteins: 24 proteins are related to both eubacterial as well as eukaryotic proteins. Eleven proteins are exclusively related to eukaryotic counterparts. For three proteins only eubacterial relatives-and for another three proteins no counterpart-could be found. The similarities of the halobacterial ribosomal proteins are in general somewhat higher to their eukaryotic than to their eubacterial counterparts. The comparison of B stearothermophilus proteins with their E coli homologues showed that the proteins evolved at different rates. Some proteins are highly conserved with 64-76% identity, others are poorly conserved with only 25-34% identical amino acid residues.     

Functional implications related to the gene structure of the elongation factor EF-Tu from Halobacterium marismortui.

The primary structure of the gene for the elongation factor EF-Tu from the halophilic archaebacterium Halobacterium marismortui (hEF-Tu) is described. It is the first gene of a halophilic elongation factor EF-Tu to be sequenced. When the sequence of hEF-Tu is compared to that of homologous proteins from other organisms, the highest identity (61%) is found with EF-Tu from Methanococcus vannielii, a non-halophilic archaebacterium. In the search for halophilic characteristics therefore the most appropriate comparison is with the M. vannielii sequence. The excess of acidic amino acid residues in the hEF-Tu sequence (already observed in the composition of other halophilic proteins) results to a large extent from changes of Lys, Asn or Gln to Asp or Glu. A structural analysis algorithm applied to the halophilic sequence places these acidic residues on the surface of the protein. The corresponding residues in the crystal structure of the first domain of EF-Tu from E. coli (the only EF-Tu structure available) are grouped in patches on the protein surface, in each of which several residues that may be far apart in the sequence come quite close to each other in the tertiary structure.     

Haloarcula marismortui (Volcani) sp. nov., nom. rev., an extremely halophilic bacterium from the Dead Sea

An extremely halophilic red archaebacterium isolated from the Dead Sea (Ginzburg et al., J. Gen. Physiol. 55: 187-207, 1970) belongs to the genus Haloarcula and differs sufficiently from the previously described species of the genus to be designated a new species; we propose the name Haloarcula marismortui (Volcani) sp. nov., nom. rev. because of the close resemblance of this organism to "Halobacterium marismortui," which was first described by Volcani in 1940. The type strain is strain ATCC 43049.