Transcription of the his3 gene region in Saccharomyces cerevisiae

The dodecamer d(CpGpCpGpApApTpTpCpGpCpG) or C-G-C-G-A-A-T-T-C-G-C-G crystallizes as slightly more than one full turn of right-handed B-DNA. It is surrounded in the crystal by one bound spermine molecule and 72 ordered water molecules, most of which associate with polar N and O atoms at the exposed edges of base-pairs. Hydration within the major groove is principally confined to a monolayer of water molecules associated with exposed N and O groups on the bases, with most association being monodentate. Waters hydrating backbone phosphate oxygens tend not to be ordered, except where they are immobilized by 5-methyl groups from nearby thymines. In contrast, the minor groove is hydrated in an extensive and regular manner, with a zigzag “spine” of first- and second-shell hydration along the floor of the groove serving as a foundation for less-regular outer shells extending beyond the radius of the phosphate backbone. This spine network bridges purine N-3 and pyrimidine O-2 atoms in adjacent base-pairs. It is particularly regular in the A-A-T-T center, and is disrupted at the C-G-C-G ends, in part by the presence of the N-2 amino groups on guanine residues. The minor groove hydration spine may be responsible for the stability of the B form of polymers containing only A · T and I · C base-pairs, and its disruption may explain the ease of transition to the A form of polymers with G · C pairs.     

Monte-Carlo Simulation of DNA Duplex Hydration. B and B′ Conformations of Poly(dA) · Poly(dT) Have Different Hydration Shells

Abstract

Monte-Carlo simulation of poly(dA) · poly(dT) hydration by 30 water molecules per nucleotide pair has been performed. Two B-family conformations, both with a 36° helical twist but with different minor groove widths, were considered. One conformation is Arnott's standard B form, the other one is specific for poly(dA) · poly(dT) B′ form with a narrowed minor groove. The mean energies and the mean numbers of water-water and water-DNA hydrogen bonds are close for the two conformations. Nevertheless, the hydration shell of the B' form differs drastically from that of the standard B form. The water arrangement in the minor groove of the B′ form resembles the spine of hydration in the central part of Dickerson's dodecamer d(CGCGAATTCGCG). No such spine is formed in the hydration shell of the usual B form with a wider minor groove. In this conformation water bridges between adenine N3 or thymine O2 and oxygen of the sugar ring of the neighbouring nucleotide along the chain can be formed (“strings” in Dickerson's decamer d(CCAAGATTGG)).     

Solvation of the left-handed hexamer d(5BrC-G-5BrC-G-5 BrC-G) in crystals grown at two temperatures

Crystals of the hexadeoxyoligomer d(5BrC-G-5BrC-G-5BrC-G) were grown at different temperatures (5 degrees C, 18 degrees C and 37 degrees C) in the absence of divalent cations. The crystals grown at 5 degrees C did not diffract X-rays, while those grown at 18 degrees C and 37 degrees C did. The oligomer adopts the left-handed ZI conformation in both crystals. The main difference resides in a more extensive hydration shell in the crystal grown at high temperature than in the crystal grown at low temperature. The high-temperature crystal displays a spine of hydration running deep in the minor groove and linking exocyclic O-2 atoms of the pyrimidine rings. In both crystalline forms, a hydrated sodium ion bound to the N-7 of a guanine ring was found. Strings of water molecules bridging phosphate anionic oxygen atoms are found along the backbone. The absolute values of the propeller-twist are also different in both structures although the values of the twist are very similar. The results point to the importance of the crystallization conditions when analysing fine structural details like solvation properties of oligomers.     

Life: Self-Directing with Unlimited Variability on Self-Speeding

Abstract

The crystal structure of the deoxyoctamer d(G-G-^Br U-A-^BrU-A-C-C) was refined to a resolution of 1.7Å using combined diffractometer and synchrotron data. The analysis was carried out independently in two laboratories using different procedures. Although the final results are identical the comparison of the two approaches highlights potential problems in the refinement of oligonucleotides when only limited data are available.

As part of the analysis the positions of 84 solvent molecules in the asymmetric unit were established. The DNA molecule is highly solvated, particularly the phosphate-sugar backbone and the functional groups of the bases. The major groove contains, in the central ^BrU-A-^BrU-A region, a ribbon of water molecules forming closed pentagons with shared edges. These water molecules are linked to the base O and N atoms and to the solvent chains connecting the O-1 phosphate oxygen atoms on each strand. The minor groove is also extensively hydrated with a continuous network in the central region and other networks at each end. The pattern of hydration is briefly compared with that observed in the crystal structure of a B-dodecamer.     

Water spines and networks in G-quadruplex structures

Quadruplex DNAs can fold into a variety of distinct topologies, depending in part on loop types and orientations of individual strands, as shown by high-resolution crystal and NMR structures. Crystal structures also show associated water molecules. We report here on an analysis of the hydration arrangements around selected folded quadruplex DNAs, which has revealed several prominent features that re-occur in related structures. Many of the primary-sphere water molecules are found in the grooves and loop regions of these structures. At least one groove in anti-parallel and hybrid quadruplex structures is long and narrow and contains an extensive spine of linked primary-sphere water molecules. This spine is analogous to but fundamentally distinct from the well-characterized spine observed in the minor groove of A/T-rich duplex DNA, in that every water molecule in the continuous quadruplex spines makes a direct hydrogen bond contact with groove atoms, principally phosphate oxygen atoms lining groove walls and guanine base nitrogen atoms on the groove floor. By contrast, parallel quadruplexes do not have extended grooves, but primary-sphere water molecules still cluster in them and are especially associated with the loops, helping to stabilize loop conformations.     

Ordered water structure in an A-DNA octamer at 1.7 A resolution

The crystal structure of the deoxyoctamer d(G-G-Br U-A-BrU-A-C-C) was refined to a resolution of 1.7 A using combined diffractometer and synchrotron data. The analysis was carried out independently in two laboratories using different procedures. Although the final results are identical the comparison of the two approaches highlights potential problems in the refinement of oligonucleotides when only limited data are available. As part of the analysis the positions of 84 solvent molecules in the asymmetric unit were established. The DNA molecule is highly solvated, particularly the phosphate-sugar back-bone and the functional groups of the bases. The major groove contains, in the central BrU-A-BrU-A region, a ribbon of water molecules forming closed pentagons with shared edges. These water molecules are linked to the base O and N atoms and to the solvent chains connecting the O-1 phosphate oxygen atoms on each strand. The minor groove is also extensively hydrated with a continuous network in the central region and other networks at each end. The pattern of hydration is briefly compared with that observed in the structure of a B-dodecamer.     

Solvent-accessible surfaces of nucleic acids

Static solvent-accessible surface areas were calculated for DNA and RNA double helices of varied conformation, composition and sequence, for the single helix of poly(rC), and for a transfer RNA. The results show that for DNA and RNA double helices, two thirds of the water-accessible surface area become buried on double helix formation; phosphate oxygens retain near maximal exposure while the bases are 80% buried. Transfer RNA exposes slightly less surface per residue than does double-helical RNA, despite the presence of several additional “modified” groups, all of which are exposed significantly.When a probe corresponding to a single water molecule is used, both the total and atom type exposures are very similar for A-DNA and B-DNA, although marked differences appear in the major and minor groove exposures between the two conformations. For a given base-pair, the accessible surface area buried upon double-helical stacking is nearly constant (within 5%) for different sequences of neighboring base-pairs.For probes larger than single water molecules, there exist considerable differences in the total and atom type exposures of A-DNA and B-DNA. Conformational transitions between the A-DNA and B-DNA helical forms can thus be related to differences in the accessible areas for “structured” water, or a secondary hydration shell, rather than to interactions with individual water molecules of the primary hydration shell. The base-composition dependence of DNA helical conformation can be explained in terms of the opposing effects of thymine methyl groups of A · T base-pairs and the amino groups of G · C base-pairs upon the solvent within the grooves.The area calculations show that primarily the major groove of B-DNA and the minor groove of A-DNA have sufficient accessible surface area to be recognized by a probe size corresponding to the side-chains of amino acids.     

Structural insights into the effect of hydration and ions on A-tract DNA: a molecular dynamics study

DNA structure is known to be sensitive to hydration and ionic environment. To explore the dynamics, hydration, and ion binding features of A-tract sequences, a 7-ns Molecular dynamics (MD) study has been performed on the dodecamer d(CGCAAATTTGCG)(2). The results suggest that the intrusion of Na(+) ion into the minor groove is a rare event and the structure of this dodecamer is not very sensitive to the location of the sodium ions. The prolonged MD simulation successfully leads to the formation of sequence dependent hydration patterns in the minor groove, often called spine of hydration near the A-rich region and ribbon of hydration near the GC regions. Such sequence dependent differences in the hydration patterns have been seen earlier in the high resolution crystal structure of the Drew-Dickerson sequence, but not reported for the medium resolution structures (2.0 approximately 3.0 A). Several water molecules are also seen in the major groove of the MD simulated structure, though they are not highly ordered over the extended MD. The characteristic narrowing of the minor groove in the A-tract region is seen to precede the formation of the spine of hydration. Finally, the occurrence of cross-strand C2-H2.O2 hydrogen bonds in the minor groove of A-tract sequences is confirmed. These are found to occur even before the narrowing of the minor groove, indicating that such interactions are an intrinsic feature of A-tract sequences.     

Structure of the B-DNA decamer C-C-A-A-C-G-T-T-G-G and comparison with isomorphous decamers C-C-A-A-G-A-T-T-G-G and C-C-A-G-G-C-C-T-G-G

The crystal structure of the DNA decamer C-C-A-A-C-G-T-T-G-G has been solved to a resolution of 1.4 A, and is compared with the 1.3 A structure of C-C-A-A-G-A-T-T-G-G and the 1.6 A structure of C-C-A-G-G-C-C-T-G-G. All three decamers crystallize isomorphously in space group C2 with five base-pairs per asymmetric unit, and with decamer double helices stacked atop one another along the c axis in a manner that closely approximates a continuous B helix. This efficient stacking probably accounts for the high resolution of the crystal data. Comparison of the three decamers reveals the following. (1) Minor groove width is more variable than heretofore realized. Regions of A.T base-pairs tend to be narrower than average, although two successive A.T base-pairs alone may not be sufficient to produce narrowing. The minor groove is wider in regions where BII phosphate conformations are opposed diagonally across the groove. (2) Narrow regions of minor groove exhibit a zig-zag spine of hydration, as was first seen in C-G-C-G-A-A-T-T-C-G-C-G, whereas wide regions show two ribbons of water molecules down the walls, connecting base edge N or O with sugar O-4' atoms. Regions of intermediate groove width may accommodate neither pattern of hydration well, and may exhibit a less regular pattern of hydration. (3) Base-pair stacking is virtually identical at equivalent positions in the three decamers. The unconnected step from the top of one decamer helix to the bottom of the next helix is a normal helix step in all respects, except for the absence of connecting phosphate groups. (4) BII phosphate conformation require the unstacking of the two bases linked by the phosphate, but do not necessarily follow as an inevitable consequence of unstacking. They have an influence on minor groove width as noted in point (1) above. (5) Sugar ring pseudorotation P and main-chain torsion angle delta show an excellent correlation as given by the equation: delta = 40 degrees cos (P + 144 degrees) + 120 degrees. Although centered around C-2'-endo, the conformations in these B-DNA helices are distributed broadly from C-3'-exo to O-4'-endo, unlike the tighter clustering around C-3'-endo observed in A-DNA oligomer structures.     

Structure and hydration of BamHI DNA recognition site: a molecular dynamics investigation

The results of a 3-ns molecular dynamics simulation of the dodecamer duplex d(TATGGATCCATA)(2) recognized by the BamHI endonuclease are presented here. The DNA has been simulated as a flexible molecule using an AMBER force field and the Ewald summation method, which eliminates the undesired effects of truncation and permits evaluation of the full effects of electrostatic forces. The starting B conformation evolves toward a configuration quite close to that observed through x-ray diffraction in its complex with BamHI. This configuration is fairly stable and the Watson-Crick hydrogen bonds are well maintained over the simulation trajectory. Hydration analysis indicates a preferential hydration for the phosphate rather than for the ester oxygens. Hydration shells in both the major and minor groove were observed. In both grooves the C-G pairs were found to be more hydrated than A-T pairs. The "spine of hydration" in the minor groove was clear. Water residence times are longer in the minor groove than in the major groove, although relatively short in both cases. No special long values are observed for sites where water molecules were observed by x-ray diffraction, indicating that water molecules having a high probability of being located in a specific site are also fast-exchanging.     

Structural principles of B-DNA grooves hydration in fibers as revealed by Monte Carlo simulations and X-ray diffraction

Being interested in possible effects of sequence-dependent hydration of B-DNA with mixed sequence in fibers, we performed a series of Monte Carlo calculations of hydration of polydeoxyribonucleotides in B form, considering all sequences with dinucleotide repeat. The computational results allow the ten base-stacking types to be classified in accordance with their primary hydration in the minor groove. As a rule, the minor groove is occupied by two water molecules per base pair in the depth of the groove, which are located nearly midway between the planes of successive base pairs and symmetrically according to the dyad there. The primary hydration of the major groove depends on the type of the given base pair. The coordinates of 3 water molecules per base pair in the depth of the major groove are determined by the type of this pair together with its position and orientation in the helix, and are practically independent on the adjacent base pairs. A/T-homopolymer tracts do not fit into this hydration pattern; the base pair edges are hydrated autonomously in both grooves. Analysis of the Li-B-DNA x-ray diffraction intensities reveals those two water positions in the minor groove. In the major groove, no electronic density peaks in sufficient distance from the base edges were found, thus confirming the absence of any helical invariance of primary hydration in this region. With the help of the rules proposed in this paper it is possible to position the water molecules of the first hydration shell in the grooves of canonical B-DNA for any given sequence.     

DNA minor groove electrostatic potential: influence of sequence-specific transitions of the torsion angle gamma and deoxyribose conformations

The structural adjustments of the sugar-phosphate DNA backbone (switching of the γ angle (O5′–C5′–C4′–C3′) from canonical to alternative conformations and/or C2′-endo → C3′-endo transition of deoxyribose) lead to the sequence-specific changes in accessible surface area of both polar and non-polar atoms of the grooves and the polar/hydrophobic profile of the latter ones. The distribution of the minor groove electrostatic potential is likely to be changing as a result of such conformational rearrangements in sugar-phosphate DNA backbone. Our analysis of the crystal structures of the short free DNA fragments and calculation of their electrostatic potentials allowed us to determine: (1) the number of classical and alternative γ angle conformations in the free B-DNA; (2) changes in the minor groove electrostatic potential, depending on the conformation of the sugar-phosphate DNA backbone; (3) the effect of the DNA sequence on the minor groove electrostatic potential. We have demonstrated that the structural adjustments of the DNA double helix (the conformations of the sugar-phosphate backbone and the minor groove dimensions) induce changes in the distribution of the minor groove electrostatic potential and are sequence-specific. Therefore, these features of the minor groove sizes and distribution of minor groove electrostatic potential can be used as a signal for recognition of the target DNA sequence by protein in the implementation of the indirect readout mechanism.     

Visualisation of extensive water ribbons and networks in a DNA minor-groove drug complex.

The crystal structure is reported of a complex between an ethyl derivative of the minor-groove drug furamidine and the dodecanucleotide duplex d(CGCGAATTCGCG)2, which has been refined to 1.85 A resolution and an R factor of 16.6% for data collected at -173 degreesC. An exceptionally large number (220) of water molecules have been located. The majority of these occur in the first coordination shell of solvation. There are extensive networks of connected waters, both in the major and minor grooves. In particular, there are 21 water molecules associated with the minor-groove drug, via hydrogen bonds from the four charged nitrogen atoms. One cluster of four waters is situated in the groove itself; the majority are on the outer edge of the groove, and serve to bridge between the outward-directed drug nitrogen atoms and backbone phosphate oxygen atoms. These bridges are both intra- and inter-strand, with the net effect that the outer edge of the drug molecule is covered by ribbons of water molecules.     

Water and ion binding around RNA and DNA (C,G) oligomers

The dynamics, hydration, and ion-binding features of two duplexes, the A(r(CG)(12)) and the B(d(CG)(12)), in a neutralizing aqueous environment with 0.25 M added KCl have been investigated by molecular dynamics (MD) simulations. The regular repeats of the same C=G base-pair motif have been exploited as a statistical alternative to long MD simulations in order to extend the sampling of the conformational space. The trajectories demonstrate the larger flexibility of DNA compared to RNA helices. This flexibility results in less well defined hydration patterns around the DNA than around the RNA backbone atoms. Yet, 22 hydration sites are clearly characterized around both nucleic acid structures. With additional results from MD simulations, the following hydration scale for C=G pairs can be deduced: A-DNA相似文献   

Hydration of the RNA duplex r(CGCAAAUUUGCG)2 determined by NMR.

The so-called spine of hydration in the minor groove of AnTn tracts in DNA is thought to stabilise the structure, and kinetically bound water detected in the minor groove of such DNA species by NMR has been attributed to a narrow minor groove [Liepinsh, E., Leupin, W. and Otting, G. (1994) Nucleic Acids Res. 22, 2249-2254]. We report here an NMR study of hydration of an RNA dodecamer which has a wide, shallow minor groove. Complete assignments of exchangeable protons, and a large number of non-exchangeable protons in r(CGCAAAUUUGCG)2 have been obtained. In addition, ribose C2'-OH resonances have been detected, which are probably involved in hydrogen bonds. Hydration at different sites in the dodecamer has been measured using ROESY and NOESY experiments at 11.75 and 14.1 T. Base protons in both the major and minor grooves are in contact with water, with effective correlation times for the interaction of approximately 0.5 ns, indicating weak hydration, in contrast to the hydration of adenine C2H in the homologous DNA sequence. NOEs to H1' in the minor groove are consistent with hydration water present that is not observed in the analogous DNA sequence. Hydration kinetics in nucleic acids may be determined by chemical factors such as hydrogen-bonding more than by simple conformational factors such as groove width.     

NMR observation of individual molecules of hydration water bound to DNA duplexes: direct evidence for a spine of hydration water present in aqueous solution.

The residence times of individual hydration water molecules in the major and minor grooves of DNA were measured by nuclear magnetic resonance (NMR) spectroscopy in aqueous solutions of d-(CGCGAATTCGCG)2 and d-(AAAAATTTTT)2. The experimental observations were nuclear Overhauser effects (NOE) between water protons and the protons of the DNA. The positive sign of NOEs with the thymine methyl groups shows that the residence times of the hydration water molecules near these protons in the major groove of the DNA must be shorter than about 500 ps, which coincides with the behavior of surface hydration water in peptides and proteins. Negative NOEs were observed with the hydrogen atoms in position 2 of adenine in both duplexes studied. This indicates that a 'spine of hydration' in the minor groove, as observed by X-ray diffraction in DNA crystals, is present also in solution, with residence times significantly longer than 1 ns. Such residence times are reminiscent of 'interior' hydration water molecules in globular proteins, which are an integral part of the molecular architecture both in solution and in crystals.     

1 A crystal structures of B-DNA reveal sequence-specific binding and groove-specific bending of DNA by magnesium and calcium

The 1 A resolution X-ray crystal structures of Mg(2+) and Ca(2+) salts of the B-DNA decamers CCAACGTTGG and CCAGCGCTGG reveal sequence-specific binding of Mg(2+) and Ca(2+) to the major and minor grooves of DNA, as well as non-specific binding to backbone phosphate oxygen atoms. Minor groove binding involves H-bond interactions between cross-strand DNA base atoms of adjacent base-pairs and the cations' water ligands. In the major groove the cations' water ligands can interact through H-bonds with O and N atoms from either one base or adjacent bases, and in addition the softer Ca(2+) can form polar covalent bonds bridging adjacent N7 and O6 atoms at GG bases. For reasons outlined earlier, localized monovalent cations are neither expected nor found.Ultra-high atomic resolution gives an unprecedented view of hydration in both grooves of DNA, permits an analysis of individual anisotropic displacement parameters, and reveals up to 22 divalent cations per DNA duplex. Each DNA helix is quite anisotropic, and alternate conformations, with motion in the direction of opening and closing the minor groove, are observed for the sugar-phosphate backbone. Taking into consideration the variability of experimental parameters and crystal packing environments among these four helices, and 24 other Mg(2+) and Ca(2+) bound B-DNA structures, we conclude that sequence-specific and strand-specific binding of Mg(2+) and Ca(2+) to the major groove causes DNA bending by base-roll compression towards the major groove, while sequence-specific binding of Mg(2+) and Ca(2+) in the minor groove has a negligible effect on helix curvature. The minor groove opens and closes to accommodate Mg(2+) and Ca(2+) without the necessity for significant bending of the overall helix.The program Shelxdna was written to facilitate refinement and analysis of X-ray crystal structures by Shelxl-97 and to plot and analyze one or more Curves and Freehelix output files.     

Binding of Hoechst 33258 to the minor groove of B-DNA

An X-ray crystallographic structure analysis has been carried out on the complex between the antibiotic and DNA fluorochrome Hoechst 33258 and a synthetic B-DNA dodecamer of sequence C-G-C-G-A-A-T-T-C-G-C-G. The drug molecule, which can be schematized as: phenol-benzimidazole-benzimidazole-piperazine, sits within the minor groove in the A-T-T-C region of the DNA double helix, displacing the spine of hydration that is found in drug-free DNA. The NH groups of the benzimidazoles make bridging three-center hydrogen bonds between adenine N-3 and thymine O-2 atoms on the edges of base-pairs, in a manner both mimicking the spine of hydration and calling to mind the binding of the auti-tumor drug netropsin. Two conformers of Hoechst are seen in roughly equal populations, related by 180 degrees rotation about the central benzimidazole-benzimidazole bond: one form in which the piperazine ring extends out from the surface of the double helix, and another in which it is buried deep within the minor groove. Steric clash between the drug and DNA dictates that the phenol-benzimidazole-benzimidazole portion of Hoechst 33258 binds only to A.T regions of DNA, whereas the piperazine ring demands the wider groove characteristic of G.C regions. Hence, the piperazine ring suggests a possible G.C-reading element for synthetic DNA sequence-reading drug analogs.     

Exocyclic groups in the minor groove influence the backbone conformation of DNA

Exocyclic groups in the minor groove of DNA modulate the affinity and positioning of nucleic acids to the histone protein. The addition of exocyclic groups decreases the formation of this protein–DNA complex, while their removal increases nucleosome formation. On the other hand, recent theoretical results show a strong correlation between the B_I/B_II phosphate backbone conformation and the hydration of the grooves of the DNA. We performed a simulation of the d(CGCGAATTCGCG)₂ Drew Dickerson dodecamer and one simulation of the d(CGCIAATTCGCG)₂ dodecamer in order to investigate the influence of the exocyclic amino group of guanine. The removal of the amino group introduces a higher intrinsic flexibility to DNA supporting the suggestions that make the enhanced flexibility responsible for the enlarged histone complexation affinity. This effect is attributed to changes in the destacking interactions of both strands of the DNA. The differences in the hydration of the minor groove could be the explanation of this flexibility. The changed hydration of the minor groove also leads to a different B_I/B_II substate pattern. Due to the fact that the histone preferentially builds contacts with the backbone of the DNA, we propose an influence of these B_I/B_II changes on the nucleosome formation process. Thus, we provide an additional explanation for the enhanced affinity to the histone due to removal of exocyclic groups. In terms of B_I/B_II we are also able to explain how minor groove binding ligands could affect the nucleosome assembly without disrupting the structure of DNA.     

DNA B to D transition can be explained in terms of hydration economy of the minor groove atoms

Adjacent phosphate oxygen atoms in A and Z-DNA are located much closer together than in the B form and can be hydrated more economically due to the formation of water bridges between them, whereas in the B form phosphates are hydrated individually. This principle of hydration economy of phosphate groups discovered by Saenger and colleagues could not be applied to the B-D transition, which, like the B-A and B-Z transitions, occurs in a situation of water deficiency, because the distances between adjacent phosphates of individual polynucleotide chains in the D form are not much different from B-DNA. It follows from our calculations of B and D-DNA accessibility to solvent performed by the method of Lee & Richards, and from a simulation of solvent structure near DNA, that there is an economy of hydration only for the minor groove atoms. This feature and some experimental data can explain why only a limited range of sequences consisting of A.T or I.C pairs undergo the transition to the D form. The conformational transition in DNAs with such sequences to a poly[d(A]).poly[d(T])-like conformation (Bh-DNA), which is accompanied by a narrowing of the minor groove, can be explained in the same way. Calculations suggest that in the D-form minor groove of different A-T or I-C DNAs there is a double-layer hydration spine similar to that observed by Drew & Dickerson in the A-T tract of the d(C-G-C-G-A-A-T-T-C-G-C-G) dodecamer. The B-D and B-Bh transitions in A + T-rich DNAs can have biological implications, e.g. they can facilitate DNA bending upon the interaction with proteins.