A Systematic Study of Patterns of Hydration in Nucleic Acids:(I) Guanine and Cytosine

Abstract

The hydration sites of guanine and cytosine are defined by examination of the crystal structures of bases, nucleosides, nucleotides, and three dinucleoside phosphate salts. The patterns of hydration for two guanine and cytosine containing oligonucleotides are then predicted. The relationship between these structural motifs and thermodynamic parameters is discussed.     

The role of spin in biological processes: O2, NO,nucleobases, nucleosides,nucleotides and Watson–Crick base pairs

The experimental electron affinities of adenine, guanine, cytosine, thymine and uracil have been determined from reduction potentials and negative ion photoelectron spectra. Updated values for purine, pyrimidine and other nitrogen heterocyclics, which have not been measured in the gas phase, are presented. The electron affinity of Watson–Crick guanine–cytosine is estimated empirically. The experimental values are consistent with quantum mechanical semi-empirical multiconfiguration configuration interaction calculations. The bulk hydration energies of the nucleobase anions, 2.34 eV, determined from the experimental data and sequential anion hydration energy difference of about 0.20(5) eV suggest that 10–15 water molecules complete the hydration shell. The electron affinities for the formation of doublet and quartet anions of the nucleobases, nucleosides, nucleotides and Watson–Crick base pairs are calculated. We postulate that low-lying quartet anion states and their spin distribution can and will participate in electron conduction, radiation damage, oxidation damage and repair, strand breakage and protein synthesis.     

Hydration of the DNA bases is local.

Ordered hydration sites were determined for the nucleotide bases in B-type conformations using the crystal structure data on 14 B-DNA decamer structures. A method of density representation was extended so that positions, occupancies, and distributions of the hydration sites were predicted around a B-DNA double helix by a method analogous to crystallographic refinement. The predicted hydration sites correctly reproduce the main features of hydration around the B-DNA dodecamer. In contrast to the previous observations, the newly available crystal data show the same extent of hydration of guanine and adenine, and of cytosine and thymine.     

The infrared spectrum and structure of the type I complex of silver and DNA.

Infrared spectroscopy was used to study films of the type I complex of Ag+ and DNA as a function of hydration with the following conclusions. Ag+ binds to guanine residues but not to cytosine or thymine residues. Cytosine becomes protonated as Ag+ binds to guanine. (These conclusions confirm previous models.) The type I complex remains in the B family of structures with slight modifications of the sugar-phosphate geometry. This modified B structure remains stable at lower values of hydration for which pure DNA is in the A form. Binding of Ag+ to PO2-, O-P-O or the deoxyribose oxygen is excluded.     

Structural forms and transitions for the complex of mercury(II) with poly(dG-dC)

Infrared spectroscopy was used to study hydrated double-helical poly(dG-dC) complexed with varying amounts of mercury(II). For one Hg(II) per ten nucleotide residues (r = 0.1), the B structure was stabilized and the B* structure was absent at high hydration. The Z structure did not form as hydration was reduced. For r = 0.2, the B and Z structures coexisted at high hydration and the transition to total Z structure was broad as hydration was reduced. Hg(II) was bound exclusively to the guanine residues probably at N3 or N7 for r less than or equal to 0.25. The cytosine residue did not protonate (at N3) as Hg(II) was bound to guanine. The addition of NaCl together with Hg(II) reduced the binding of Hg(II), stabilized the B structure at the highest hydration and caused a sharp transition between the B and Z structures as hydration was lowered. Hydration with D2O stabilized the Z structure for poly(dG-dC) complexed with HgCl2.     

Aqueous hydration of nucleic acid constituents: Monte Carlo computer simulation studies

Monte Carlo computer simulations were performed on dilute aqueous solutions of thymine, cytosine, uracil, adenine, guanine, the dimethyl phosphate anion in the gauche-gauche conformation and a ribose and deoxyribose derivative. The aqueous hydration of each molecule was analysed in terms of quasi-component distribution functions based on the Proximity Criterion, and partitioned into hydrophobic, hydrophilic and ionic contributions. Color stereo views of selected hydration complexes are also presented. A preliminary discussion of the transferability of functional group coordination numbers is given. The results enable to comment on two current problems related to the hydration of nucleic acids: a) the theory of Dickerson and coworkers on the role of water in the relative stability of the A and B form of DNA and b) the idea of water bridges and filaments emerging from the computer simulation results on the hydration of DNA fragments by Clementi.     

Hydration of DNA bases: analysis of crystallographic data.

We present a systematic analysis of water structure around nucleic acid bases. We have examined 28 crystal structures of oligonucleotides, and have studied the patterns of water around the four bases, guanine, cytosine, adenine, and thymine. The geometries of water positions were calculated up to 4.00 A from base atoms. We have found conformation-dependent differences in both the geometry and extent of hydration of the bases.     

Structural Forms and Transitions for the Complex of Mercury(II) with Poly(dG-dC)

Abstract

Infrared spectroscopy was used to study hydrated double-helical poly(dG-dC) complexed with varying amounts of mercury (II). For one Hg(II) per ten nucleotide residues (r = 0.1), the B structure was stabilized and the B* structure was absent at high hydration. The Z structure did not form as hydration was reduced. For r = 0.2, the B and Z structures coexisted at high hydration and the transition to total Z structure was broad as hydration was reduced. Hg(II) was bound exclusively to the guanine residues probably at N 3 orN7forr < 0.25. The cytosine residue did not protonate (at N3) as Hg(II) was bound to guanine. The addition of NaCl together with Hg(II) reduced the binding of Hg(II), stabilized the B structure at the highest hydration and caused a sharp transition between the B and Z structures as hydration was lowered. Hydration with D,0 stabilized the Z structure for poly(dG-dC) complexed with HgCl₂.     

On the hydration of DNA. II. Base composition dependence of the net hydration of DNA

The dependence of the net hydration of DNA on its base composition has been measured by density gradient ultracentrifugation of three DNA's in a series of cesium and lithium salt solutions of different water activities. Extrapolation to zero water activity showed the dependence of the partial specific volume on base composition to be very small for CsDNA and aero for LiDNA. At least 99% of the dependence of buoyant density on base composition can be accounted for on the basis of a differential hydration, with a mole of adenine–thymine pairs binding about 2 moles more water than a mole of guanine–cytosine pairs in CsCl.     

Aqueous Hydration of Nucleic Acid Constituents: Monte Carlo Computer Simulation Studies

Abstract

Monte Carlo computer simulations were performed on dilute aqueous solutions of thymine, cytosine, uracil, adenine, guanine, the dimethyl phosphate anion in the gauche-gauche conformation and a ribose and deoxyribose derivative. The aqueous hydration of each molecule was analysed in terms of quasi-component distribution functions based on the Proximity Criterion, and partitioned into hydrophobic, hydrophilic and ionic contributions. Color stereo views of selected hydration complexes are also presented. A preliminary discussion of the transferability of functional group coordination numbers is given. The results enable to comment on two current problems related to the hydration of nucleic acids: a) the theory of Dickerson and coworkers on the role of water in the relative stability of the A and B forms of DNA and b) the idea of water bridges and filaments emerging from the computer simulation results on the hydration of DNA fragments by Clementi.     

Determination of the base composition of deoxyribonucleic acid by measurement of the adenine/guanine ratio

A method is described for determination of the base composition (as guanine+cytosine or adenine+thymine content) of DNA by accurate measurement of the adenine/guanine ratio. The DNA is hydrolysed with 0.03n-hydrochloric acid for 40min. to release the purines. The hydrolysate is subjected to ion-exchange chromatography on Zeo-Karb 225. Apurinic acids are eluted with 0.03n-hydrochloric acid and then guanine and adenine are eluted separately with 2n-hydrochloric acid. Guanine and adenine are each collected as a single fraction, and the amount of base in each case is determined by measuring the volume and the extinction at suitable wavelengths. For use in the calculations, millimolar extinction coefficients in 2n-hydrochloric acid of 12.09 for adenine at 262mmu, and 10.77 for guanine at 248mmu, were determined with authentic samples of bases. The method gives extremely reproducible results: from 12 determinations with calf thymus DNA the adenine/guanine molar ratio had a standard deviation of 0.011; this corresponds to a standard deviation in guanine+cytosine content of 0.2% guanine+cytosine.     

Structural forms and transitions of poly(dG-dC) with Cd(II), Ag(I) and NaNO3

Infrared spectroscopy was used to study the structures and transitions in hydrated gels of double-helical poly(dG-dC) complexed with the metal carcinogens Cd(II) and Ag(I). For one Cd(II) per ten nucleotides (r = 0.1), the B structure was stable at high and moderate hydrations with D2O and the B and Z structures coexisted at low hydrations. For poly(dG-dC) with Cd(II) at r = 0.2 to 0.35, the Z structure was stable at high hydrations (94% r.h. for r = 0.2). At a given value of hydration, H2O gave a higher content of Z structure than D2O. Cd(II) most likely binds to guanine residues at N7 in both the B and Z forms of poly(dG-dC) but binding to guanine N3 can not be excluded. It is unlikely that Cd(II) binds to cytosine residues at the r values studied and the cytosine residues did not protonate at N3 as Cd(II) bound to guanine residues. Poly(dG-dC) with Ag(I) at r = 0.2 to 0.36, existed in a B-family structure which is different from the B-family structure of the type I complex of Ag(I) and calf-thymus DNA. Poly(dG-dC) with Ag(I) did not assume the Z structure at lower hydrations even though NO3- was present in the sample. Ag(I) differs from other soft-metal acids which promote the Z structure. Ag(I) most likely binds to the guanine N7 or N3 and not to cytosine residues. Cytosine residues did not protonate at N3 as Ag(I) was bound to guanine.(ABSTRACT TRUNCATED AT 250 WORDS)     

A purine permease in Candida glabrata

Abstract Competition experiments revealed that adenine and guanine were transported by a purine permease in both Candida glabrata 4 and a C. glabrata 4 cytosine permease negative mutant. The C. glabrata 4 cytosine permease negative mutant was isolated using 5-fluorocytosine selection. This mutant no longer transported cytosine, but transported adenine and guanine. A transport system for hypoxanthine was not detected. Hence, in addition to the cytosine permease, a purine permease exists in C. glabrata . This differs from the purine cytosine permeases in Saccharomyces cereuisiae and Candida albicans which transport adenine, cytosine, guanine and hypoxanthine.     

Analysis of difference spectra of protonated DNA: determination of degree of protonation of nitrogen bases and the fractions of disordered nucleotide pairs.

The titration curves of nitrogen bases and fractions of disordered nucleotide pairs are obtained during DNA protonation. It is shown that purine bases are the first sites of the DNA double helix protonation. The cytosine protonation is due to proton-induced conformational transition within GC pairs with the sequence proton transfer from (N-7) of guanine to (N-3) of cytosine. Within DNA with unwound regions the bases are protonated in the following order: cytosine, adenine, guanine. It is shown that GC pairs are the primary centres in which the unwinding of protonated DNAs occurs.     

Parallel-Stranded DNA Formed by New Base Pairs Related to the Isoguanine-Cytosine or Isocytosine-Guanine Motifs

Abstract

Parallel-stranded (ps) oligonucleotide duplexes containing several new base pairs formed between 7-deazaisoguanine and cytosine, 8-aza-7-deaza-isoguanine and cytosine, and 5-aza-7-deaza guanine and guanine are described. The stability of the pshybrids increased if the duplex contains 8-aza-7-deazaisoguanine instead of isoguanine and is decreased by 7-deazaisoguanine incorporation. The purine-purine base pair between 5-aza-7-deazaguanine and guanine was found to be more stable than that of 5-methylisocytosine with guanine.     

A Monte Carlo simulation study of the aqueous hydration of r(GpC)2: comparison with crystallographic ordered water sites

Monte Carlo computer simulation is described for the dinucleotide duplex rGpC together with 562 water molecules at an environmental density of 1 g/cc in a cubic cell under periodic boundary conditions. Water-water interactions were treated using the TIP4P potential and the solute water interactions by TIP4P spliced with the nonbonded interactions from the AMBER 3.0 force field. The simulation was subjected to proximity analysis to obtain solute coordinate numbers and pair interaction energies for each solute atom. Hydration density distributions partitioned into contributions from the major groove side, the minor groove side and the sugar-phosphate backbone were examined, and the probabilities of occurrence for one- and two-water bridges in the simulation were enumerated. The results were compared with observations of crystallographic ordered water sites from x-ray diffraction studies on G and C containing small molecules, and in crystal structure determinations of the sodium, calcium, and ammonium salts of rGpC. The calculated results are generally consistent with the observed sites, except for cytosine N4, where a hydration site is predicted yet none observed in rGpC salts, and for guanine N3, which appears in this calculation to compete unfavorably with the adjacent donor site at guanine N2. There is, however, a significant probability of finding a one-water G-N3-W-G-N2 bridge indicated in the simulation. An explanation for the guanine N3 discrepancy in terms of electrostatic potentials is also offered. The calculated one- and two-water bridges in the rGpC hydration complex coincide in a number of cases to those observed in the ordered water structure of the sodium rGpC crystal hydrate.     

Physiological and biochemical contributions to the taxonomy of the genus Prototheca

16 strains of the genus Prototheca do not produce extracellular amylolytic enzymes. The base composition of their DNA shows rather continuous values from 62% to 78% GC (guanine + cytosine). Their assignment to four species and their possible relationship with Chlorella protothecoides are discussed.Abbreviations Used GC guanine + cytosine - SSC saline sodium citrate     

Deoxyribonucleic Acid Base Composition of Stentor coeruleus*

SYNOPSIS. The deoxyribonucleic acid of Stentor coeruleus has of 33 moles percent guanine plus cytosine. a buoyant density in CsCl of 1.692 gcm^?3 and a base composition of 33 moles percent guanine plus cytosine.     

The nucleic acids of Drosophila melanogaster

1. Nucleic acids of whole Drosophila adults were prepared in good yield and substantially free from impurities by new modifications of the phenol method. 2. The average molar base compositions of the DNA (41% of guanine+cytosine) and transfer RNA (60% of guanine+cytosine) resemble those of mammalian nucleic acids; the ribosomal RNA has a DNA-like molar base composition (43% of guanine+cytosine), and it is considered that this is reflected in the lower stability of its secondary structure compared with mammalian ribosomal RNA. 3. The two main ribosomal forms were separated and average base compositions and sedimentation values determined.