The amino acid composition of proteins from anaerobic halophilic bacteria of the order Halanaerobiales

We performed a comparative analysis of the genome sequences of three anaerobic halophilic fermentative bacteria belonging to the order Halanaerobiales: Halanaerobium praevalens, the alkaliphilic "Halanaerobium hydrogeniformans", and the thermophilic Halothermothrix orenii to assess the amino acid composition of their proteins. Members of the Halanaerobiales were earlier shown to accumulate KCl rather than organic compatible solutes for osmotic balance, and therefore the presence of a dominantly acidic proteome was predicted. Past reports indeed showed a large excess of acidic over basic amino acids in whole-cell hydrolysates of selected members of the order. However, the genomic analysis did not show unusually high contents of acidic amino acids or low contents of basic amino acids. The apparent excess of acidic amino acids in these anaerobic halophiles reported earlier is due to the high content in their proteins of glutamine and asparagine, which yield glutamate and aspartate upon acid hydrolysis. It is thus suggested that the proteins of the Halanaerobiales, which are active in the presence of high intracellular KCl concentrations, do not possess the typical acidic signature of the 'halophilic' proteins of the Archaea of the order Halobacteriales or of the extremely halophilic bacterium Salinibacter.     

The effect of salts on the activity and stability of Escherichia coli and Haloferax volcanii dihydrofolate reductases

The extremely halophilic Archae require near-saturating concentrations of salt in the external environment and in their cytoplasm, potassium being the predominant intracellular cation. The proteins of these organisms have evolved to function in concentrations of salt that inactivate or precipitate homologous proteins from non-halophilic species. It has been proposed that haloadaptation is primarily due to clustering of acidic residues on the surface of the protein, and that these clusters bind networks of hydrated ions. The dihydrofolate reductases from Escherichia coli (ecDHFR) and two DHFR isozymes from Haloferax volcanii (hvDHFR1 and hvDHFR2) have been used as a model system to compare the effect of salts on a mesophilic and halophilic enzyme. The KCl-dependence of the activity and substrate affinity was investigated. ecDHFR is largely inactivated above 1M KCl, with no major effect on substrate affinity. hvDHFR1 and hvDHFR2 unfold at KCl concentrations below approximately 0.5M. Above approximately 1M, the KCl dependence of the hvDHFR activities can be attributed to the effect of salt on substrate affinity. The abilities of NaCl, KCl, and CsCl to enhance the stability to urea denaturation were determined, and similar efficacies of stabilization were observed for all three DHFR variants. The DeltaG degrees (H(2)O) values increased linearly with increasing KCl and CsCl concentrations. The increase of DeltaG degrees (H(2)O) as a function of the smallest cation, NaCl, is slightly curved, suggesting a minor stabilization from cation binding or screening of electrostatic repulsion. At their respective physiological ionic strengths, the DHFR variants exhibit similar stabilities. Salts stabilize ecDHFR and the hvDHFRs by a common mechanism, not a halophile-specific mechanism, such as the binding of hydrated salt networks. The primary mode of salt stabilization of the mesophilic and halophilic DHFRs appears to be through preferential hydration and the Hofmeister effect of salt on the activity and entropy of the aqueous solvent. In support of this conclusion, all three DHFRs are similarly stabilized by the non-ionic cosolute, sucrose.     

Neutron structure factors of in-vivo deuterated amorphous protein C-phycocyanin

Neutron powder diffraction measurements of fully deuterated protein C-phycocyanin have been made at three temperatures, 295, 200, and 77 K, using dry and partially hydrated samples. The average coherent structure factors and the corresponding radial distribution functions d(r) are determined. The changes in d(r) functions observed in hydrated samples depend strongly on the level of hydration and most of these changes are due to water-protein interactions. At 0.365 gram D₂O per gram of protein, the water crystallized into hexagonal ice at 200 K and below, but at 0.175 gram D₂O per gram of protein, no crystallization of water was observed. At the higher hydration a peak appears in the radial distribution function which indicates that the average distance of the water molecule in the first hydration shell from the amino acid residues is 3.5 Å.     

Influence of hydration on the conformational stability and formation of bends in terminally blocked dipeptides

The conformations of 23 terminally blocked dipeptide sequences were examined by conformational energy calculations that included the effects of the aqueous solvent. Starting structures were derived from combinations of minimum-energy conformations of hydrated single residues. Their conformational energies were then minimized using the ECEPP potential (Empirical Conformational Energy Program for Peptides) with hydration included. Short-range interactions dominate in stabilizing the conformations of the hydrated dipeptides. Differences between conformational stabilities of hydrated and unhydrated dipeptides in many cases are due to the competition of solute–water and intramolecular hydrogen bonds. In other cases, perturbation of the hydration shell of the solute by close approach of solute atoms alters conformational preferences. Probabilities of formation of bends were calculated and compared to the corresponding quantities for unhydrated dipeptides and to those calculated from x-ray structures. For bends in dipeptides containing two nonpolar amino acids, computations omitting hydration yield better results. However, better agreement with experimental (x-ray) bend probabilities for dipeptides containing glycine or polar amino acids is obtained only in some sequences when hydration is included. The results are rationalized by the observation that, in proteins, bends containing nonpolar sequences occur on the inside, shielded from the solvent. Bends containing glycine or polar amino acids occur frequently on the surface of the protein, but they are not completely hydrated.     

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.     

Structural Basis for the Aminoacid Composition of Proteins from Halophilic Archea

Proteins from halophilic organisms, which live in extreme saline conditions, have evolved to remain folded at very high ionic strengths. The surfaces of halophilic proteins show a biased amino acid composition with a high prevalence of aspartic and glutamic acids, a low frequency of lysine, and a high occurrence of amino acids with a low hydrophobic character. Using extensive mutational studies on the protein surfaces, we show that it is possible to decrease the salt dependence of a typical halophilic protein to the level of a mesophilic form and engineer a protein from a mesophilic organism into an obligate halophilic form. NMR studies demonstrate complete preservation of the three-dimensional structure of extreme mutants and confirm that salt dependency is conferred exclusively by surface residues. In spite of the statistically established fact that most halophilic proteins are strongly acidic, analysis of a very large number of mutants showed that the effect of salt on protein stability is largely independent of the total protein charge. Conversely, we quantitatively demonstrate that halophilicity is directly related to a decrease in the accessible surface area.     

Structural stability of halophilic proteins

An examination of halobacterial amino acids exchanges as they appear in the known Spirulina platensis [2Fe-2S] ferredoxin tertiary structure indicated that most of the additional acidic residues of the halophiles occurred on the external surface of the alga structure; however, further negative changes were not placed in the ferredoxin active site region. A statistical investigation of the amino acid compositions of seven halophile and nonhalophile protein counterparts indicated that the bulkiness of amino acids used by halophiles is considerably reduced and that the overall hydrophobicity of halophilic and non halophilic molecules was essentially the same. It is suggested that the principal mode of structural stabilization for halophilic proteins is effective competition with the cytoplasmic salt for water through utilization of many external carboxyl groups of glutamic and aspartic acids. A reduction is residue bulkiness would prevent inactivation in the presence of the high molarity, antichaotropic KCl. Halophilic functionality is preserved through avoidance of additional negative charge at the active site surface.     

Differences in the interaction of inorganic and organic (hydrophobic) cations with phosphatidylserine membranes

The interaction of phosphatidylserine dispersions with “hydrophobic”, organic cations (acetylcholine, tetraethylammonium ion) is compared with that of simple inorganic cations (Na⁺, Ca²⁺); differences in the hydration properties of the two classes of ions exist in the bulk phase as evident from spin-lattice relaxation time T₁, measurements. It is shown that the reaction products (cation-phospholipid) differ markedly in their physicochemical behaviour. With increasing concentration both classes of ions reduce the ζ-potential of phosphatidylserine surfaces, the monovalent inorganic cations being only slightly more effective than the hydrophobic cations. Inorganic cations cause precipitation of the lipid once the surface charge of the bilayer is reduced to a certain threshold value. This is not the case with the organic cations. The difference is probably associated with the different hydration properties of the resulting complexes. Thus binding of Ca²⁺ causes displacement of water of hydration and formation of an anhydrous, hydrophobic calcium-phosphatidylserine complex which is insoluble in water, whereas the product of binding of the organic cations is hydrated, hydrophilic and water soluble. The above findings are consistent with NMR results which show that the phosphodiester group is involved in the binding of both classes of cations as well as being the site of the primary hydration shell. Besides affecting interbilayer membrane interactions such as those involved in cell adhesion and membrane fusion, the binding of both classes of cation can affect the molecular packing within a bilayer.     

Impact of ligand and protein desolvation on ligand binding to the S1 pocket of thrombin

In the present study, we investigate the impact of a tightly bound water molecule on ligand binding in the S1 pocket of thrombin. The S1 pocket contains a deeply buried deprotonated aspartate residue (Asp189) that is, due to its charged state, well hydrated in the uncomplexed state. We systematically studied the importance of this water molecule by evaluating a series of ligands that contains pyridine-type P1 side chains that could potentially alter the binding properties of this water molecule. All of the pyridine derivatives retain the original hydration state albeit sometimes with a slight perturbance. In order to prevent a direct H-bond formation with Asp189, and to create a permanent positive charge on the P1 side chain that is positioned adjacent to the Asp189 carboxylate anion, we methylated the pyridine nitrogen. This methylation resulted in displacement of water but was accompanied by a loss in binding affinity. Quantum chemical calculations of the ligand solvation free energy showed that the positively charged methylpyridinium derivatives suffer a large penalty of desolvation upon binding. Consequently, they have a substantially less favorable enthalpy of binding. In addition to the ligand desolvation penalty, the hydration shell around Asp189 has to be overcome, which is achieved in nearly all pyridinium derivatives. Only for the ortho derivative is a partial population of a water next to Asp189 found. Possibly, the gain of electrostatic interactions between the charged P1 side chain and Asp189 helps to compensate for the desolvation penalty. In all uncharged pyridine derivatives, the solvation shell remains next to Asp189, partly mediating interactions between ligand and protein. In the case of the para-pyridine derivative, a strongly disordered cluster of water sites is observed between ligand and Asp189.     

Ion-mediated water flow

Summary The electroosmotic flows of solution produced by the chloride salts of H, Na, K, tetramethylammonium (TMA) and tetraethylammonium (TEA) through three membranes of net negative charge and high water content (40 to 60%) have been obtained. The amount of solution transported, (EO _s), increased in the order: HCl, KCl, NaCl, TMACl and TEACl in a membrane of 43% hydration. In membranes 60% hydrated the order became HCl, KCl, NaCl, TEACl and TMACl. (EO _s) for a salt increased as membrane hydration became larger. The permselectivity of the three membranes for cations declined in the order: HCl, KCl=NaCl, TMACl and TEACl. Cation permselectivity also declined with increases in membrane hydration. The (EO _s) is a net solution flow and is the difference between the cation-induced water flow and the chloride-induced water flow in the opposite direction. In membranes of moderate to high H₂O content, co-ion transport is significant and the water-flow associated with co-ion movement must be determined if the contribution of the counter-ion ([EO]_cation) to the (EO _s) is to be found. Cl-ion induced water flow was determined by assuming an identity of K and Cl ions. [EO]_cation increased as the hydrated radii of the cations increased and for any particular cation [EO]_cation was at least 100% greater in the 60% hydrated membrane than in the 43% hydrated membrane. The current-induced water flow was found to be composed of both an electroosmotic and an osmotic component. The latter represented between 10 and 40% of the total water flow.Presented in part before the American Physiological Society at the 54^th meeting of the F.A.S.E.B., Atlantic City, N.J., April, 1970.     

An Extremely Halophilic Proteobacterium Combines a Highly Acidic Proteome with a Low Cytoplasmic Potassium Content

Halophilic archaea accumulate molar concentrations of KCl in their cytoplasm as an osmoprotectant and have evolved highly acidic proteomes that function only at high salinity. We examined osmoprotection in the photosynthetic Proteobacteria Halorhodospira halophila and Halorhodospira halochloris. Genome sequencing and isoelectric focusing gel electrophoresis showed that the proteome of H. halophila is acidic. In line with this finding, H. halophila accumulated molar concentrations of KCl when grown in high salt medium as detected by x-ray microanalysis and plasma emission spectrometry. This result extends the taxonomic range of organisms using KCl as a main osmoprotectant to the Proteobacteria. The closely related organism H. halochloris does not exhibit an acidic proteome, matching its inability to accumulate K⁺. This observation indicates recent evolutionary changes in the osmoprotection strategy of these organisms. Upon growth of H. halophila in low salt medium, its cytoplasmic K⁺ content matches that of Escherichia coli, revealing an acidic proteome that can function in the absence of high cytoplasmic salt concentrations. These findings necessitate a reassessment of two central aspects of theories for understanding extreme halophiles. First, we conclude that proteome acidity is not driven by stabilizing interactions between K⁺ ions and acidic side chains but by the need for maintaining sufficient solvation and hydration of the protein surface at high salinity through strongly hydrated carboxylates. Second, we propose that obligate protein halophilicity is a non-adaptive property resulting from genetic drift in which constructive neutral evolution progressively incorporates weakly stabilizing K⁺-binding sites on an increasingly acidic protein surface.     

Amino-acid solvation structure in transmembrane helices from molecular dynamics simulations

Understanding the solvation of amino acids in biomembranes is an important step to better explain membrane protein folding. Several experimental studies have shown that polar residues are both common and important in transmembrane segments, which means they have to be solvated in the hydrophobic membrane, at least until helices have aggregated to form integral proteins. In this work, we have used computer simulations to unravel these interactions on the atomic level, and classify intramembrane solvation properties of amino acids. Simulations have been performed for systematic mutations in poly-Leu helices, including not only each amino acid type, but also every z-position in a model helix. Interestingly, many polar or charged residues do not desolvate completely, but rather retain hydration by snorkeling or pulling in water/headgroups--even to the extent where many of them exist in a microscopic polar environment, with hydration levels corresponding well to experimental hydrophobicity scales. This suggests that even for polar/charged residues a large part of solvation cost is due to entropy, not enthalpy loss. Both hydration level and hydrogen bonding exhibit clear position-dependence. Basic side chains cause much less membrane distortion than acidic, since they are able to form hydrogen bonds with carbonyl groups instead of water or headgroups. This preference is supported by sequence statistics, where basic residues have increased relative occurrence at carbonyl z-coordinates. Snorkeling effects and N-/C-terminal orientation bias are directly observed, which significantly reduces the effective thickness of the hydrophobic core. Aromatic side chains intercalate efficiently with lipid chains (improving Trp/Tyr anchoring to the interface) and Ser/Thr residues are stabilized by hydroxyl groups sharing hydrogen bonds to backbone oxygens.     

Microsolvation and hydration enthalpies of CaC2O4(H2O) n (n = 0-16) and C2O4 2-(H2O) n (n = 0-14): an ab initio study

We studied hydrated calcium oxalate and its ions at the restricted Hartree–Fock RHF/6-31G* level of theory. Performing a configurational search seems to improve the fit of the HF/6-31G* level to experimental data. The first solvation shell of calcium oxalate contains 13 water molecules, while the first solvation shell of oxalate ion is formed by 14 water molecules. The first solvation shell of Ca(II) is formed by six water molecules, while the second shell contains five. At 298.15 K, we estimate the asymptotic limits (infinite dilution) of the total standard enthalpies of hydration for Ca(II), oxalate ion and calcium oxalate as ?480.78, –302.78 and –312.73 kcal mol^?1, resp. The dissociation of hydrated calcium oxalate is an endothermic process with an asymptotic limit of +470.84 kcal mol^?1.

Effect of Hofmeister ions on protein thermal stability: roles of ion hydration and peptide groups?

We have systematically explored the Hofmeister effects of cations and anions (0.3-1.75 M range) for acidic Desulfovibrio desulfuricans apoflavodoxin (net charge −19, pH 7) and basic horse heart cytochrome c (net charge +17, pH 4.5). The Hofmeister effect of the ions on protein thermal stability was assessed by the parameter dT_trs/d[ion] (T_trs; thermal midpoint). We show that dT_trs/d[ion] correlates with ion partition coefficients between surface and bulk water and ion surface tension effects: this suggests direct interactions between ions and proteins. Surprisingly, the stability effects of the different ions on the two model proteins are similar, implying a major role of the peptide backbone, instead of charged groups, in mediation of the interactions. Upon assessing chemical/physical properties of the ions responsible for the Hofmeister effects on protein stability, ion charge density was identified as most important. Taken together, our study suggests key roles for ion hydration and the peptide group in facilitating interactions between Hofmeister ions and proteins.     

Cation-pi and amino-acceptor interactions between hydrated metal cations and DNA bases. A quantum-chemical view

Cation-pi interactions between cytosine and hexahydrated cations have been characterized using ab initio method with inclusion of electron correlation effects, assuming idealized and crystal geometries of the interacting species. Hydrated metal cations can interact with nucleobases in a cation-pi manner. The stabilization energy of such complexes would be large and comparable to the one for cation-pi complex with benzene. Further, polarized water molecules belonging to the hydration shell of the cation are capable to form a strong hydrogen bond interaction with the nitrogen lone electron pair of the amino groups of bases and enforce a pronounced sp3 pyramidalization of the nucleobase amino groups. However, in contrast to the benzene-cation complexes, the cation-pi configurations are highly unstable for a nucleobase since the conventional in plane binding of hydrated cations to the acceptor sites on the nucleobase is strongly preferred. Thus, a cation-pi interaction with a nucleobase can occur only if the position of the cation is locked above the nucleobase plane by another strong interaction. This indeed can occur in biopolymers and may have an effect on the local DNA architecture. Nevertheless, nucleobases have no intrinsic propensity to form cation-pi interactions.     

Dynamics of lysozyme and its hydration water under an electric field

The effects of a static electric field on the dynamics of lysozyme and its hydration water are investigated by means of incoherent quasi-elastic neutron scattering (QENS). Measurements were performed on lysozyme samples, hydrated respectively with heavy water (D ₂O) to capture the protein dynamics and with light water (H ₂O), to probe the dynamics of the hydration shell, in the temperature range from 210 < T < 260 K. The hydration fraction in both cases was about ～ 0.38 gram of water per gram of dry protein. The field strengths investigated were respectively 0 kV/mm and 2 kV/mm ( ～2 × 10 ⁶ V/m) for the protein hydrated with D ₂O and 0 kV and 1 kV/mm for the H ₂O-hydrated counterpart. While the overall internal protons dynamics of the protein appears to be unaffected by the application of an electric field up to 2 kV/mm, likely due to the stronger intra-molecular interactions, there is also no appreciable quantitative enhancement of the diffusive dynamics of the hydration water, as would be anticipated based on our recent observations in water confined in silica pores under field values of 2.5 kV/mm. This may be due to the difference in surface interactions between water and the two adsorption hosts (silica and protein), or to the existence of a critical threshold field value E _c ～2–3 kV/mm for increased molecular diffusion, for which electrical breakdown is a limitation for our sample.     

Cation—π and Amino-Acceptor Interactions Between Hydrated Metal Cations and DNA Bases. A Quantum-Chemical View

Abstract

Cation—π interactions between cytosine and hexahydrated cations have been characterized using ab initio method with inclusion of electron correlation effects, assuming idealized and crystal geometries of the interacting species. Hydrated metal cations can interact with nucleobases in a cation—π manner. The stabilization energy of such complexes would be large and comparable to the one for cation—π complex with benzene. Further, polarized water molecules belonging to the hydration shell of the cation are capable to form a strong hydrogen bond interaction with the nitrogen lone electron pair of the amino groups of bases and enforce a pronounced sp³ pyramidalization of the nucleobase amino groups. However, in contrast to the benzene—cation complexes, the cation—π configurations are highly unstable for a nucleobase since the conventional in plane binding of hydrated cations to the acceptor sites on the nucleobase is strongly preferred. Thus, a cation—π interaction with a nucle-obase can occur only if the position of the cation is locked above the nucleobase plane by another strong interaction. This indeed can occur in biopolymers and may have an effect on the local DNA architecture. Nevertheless, nucleobases have no intrinsic propensity to form cation—π interactions.     

Interrelationships between water and cellular metabolism in Artemia cysts. VI. RNA and protein synthesis

Using ¹⁴CO₂ as a labelled precursor the relationship between the initiation of protein and RNA synthesis, and water concentration, has been examined in cysts (encysted embryos) of the brine shrimp, Artemia salina. Although incorporation of radioactivity into amino acids and nucleotides occurred in cysts at hydrations as low as 0.3 g H₂O/g dried cysts, incorporation into proteins and RNA was not measurable until the cysts had achieved a hydration in the range of 0.6–0.6 g/g. In no case was radioactivity detected in DNA of unemerged cysts. Fully hydrated cysts (about 1.3 g/g) that were actively synthesizing proteins and RNA, stopped doing so when dehydrated to levels below the same hydration range: thus, the hydration dependence does not involve appreciable hysteresis. The hydration range required to initiate synthesis of these macromolecules is essentially the same as that previously shown to initiate embryonic development.