The early melting of closed duplex DNA: analysis by banding in buoyant neutral rubidium trichloroacetate.

Aqueous RbTCA permits the buoyant banding of both native and denatured DNA at room temperature and neutral pH. A unique property of this solvent is the bouyant resolution of closed circular, underwound DNA (I) from the corresponding nicked (II) species. Conditions are reported here in which PM-2 DNA I is physically resolved from native PM-2 DNA II, the buoyant separation being 1.27 mq/ml in 3.3 M RbTCA at 25 degrees C. The separation between nicked and closed DNAs increases with temperature up to 35.5 degrees C, at which PM-2 DNA II cooperatively melts and subsequently pellets. The isothermal buoyant density of a cloed DNA increases linearly as the linking number (Lk) of the closed DNA decreases. The early melting of closed DNA may be monitored with high precision by buoyant banding in RbTCA, it being possible to detect the disruption of as few as 40 base pairs in PM-2 DNA (10,000 base pairs). The constraint that the linking number be conserved in closed DNA requires that a change in duplex winding be accompanied by a compensating change in supercoiling. We estimate the linking number deficiency of PM-2 DNA I to be 0.094 turns per decibase pair. This result permits the estimation of the EtdBr unwinding angle, phi, by comparison with alternative determinations of the linking number deficiency which depend upom the value of phi. The result obtained here is that phi = 27.7 degrees +/- 0.5 degrees and is approximately independent of temperature over the range 15 degrees-35 degrees.     

The helix-coil transition of closed and nicked DNAs in aqueous neutral trichloroacetate solutions.

The melting transition for closed, underwound DNAs and for nicked or linear DNAs was monitored by velocity sedimentation and by absorbance spectroscopy in aqueous NaCCl3CO2 (NaTCA) and RbTCA. The addition of neutral trichloroacetate lowers the midpoint of the helix-coil transition by 26% C/M for RbTCA and by 32% C/M for NaTCA, depressing the denaturation region to near room temperature at neutral pH. The melting of nicked DNA is cooperative, occurring over a temperature range of about 5.6 degrees C. The melting profile for closed DNA is broad and noncooperative with a transition breadth greater than 45 degrees. Closed DNAs undergo a structural alteration, as revealed by velocity sedimentation, resulting in a reduction in the number of superhelical turns at temperatures and salt concentrations substantially below the melting temperatures and salt concentrations substantially below the melting temperature of the nicked DNA. The reduction in the extent of supercoiling continues upon isothermal addition of salt up to the salt concentration at which all superhelical turns are removed. The salt concentration at the principal minimum in the sedimentation velocity profile (3.16 M NaTCA for PM-2 DNA) is approximately the same as that at the midpoint of the helix-coil transition for the nicked DNA.     

Temperature dependence of the photosynthetic activities in the thylakoid membranes from the blue-green alga Anacystis nidulans.

The effects of temperature and ethidium bromide on the banding of heat-denatured DNA was studied during equilibrium centrifugation in density gradients of NaI. Centrifugation at 10 degrees C prevents the partial renaturation of Escherichia coli DNA and Clostridium perfringens DNA that occurs at 20 degrees C. A centrifugation temperature of --5 degrees C is required to prevent renaturation of T7 phage DNA. Ethidium bromide decreases renaturation of Escherichia coli DNA during centrifugation at 20 degrees C and causes a small shift in the buoyant density of both denatured and native DNA. Equilibrium centrifugation at lower temperatures prevents DNA renaturation and permits increased utilization of the large buoyant density difference between native and heat-denatured DNA in gradients of NaI.     

Volume changes accompanying the thermal denaturation of deoxyribonucleic acid. I. Denaturation at neutral pH

Dilatometric measurements were made to determine the change in apparent specific volume φ of DNA resulting from thermal denaturation in neutral solution, φ increased continuously with temperature in the range 10–85°C. No deviations from a monotonically rising curve were observed in the φ versus temperature profile in the region of the melting temperature. The results are interpreted in terms of a partial loss of the preferentially bound DNA hydration shell. The nature of the well known buoyant density difference between native and denatured DNA was investigated by evaluating the densities in a series of cesium salt gradients at constant temperature. Extrapolation of the results to zero water activity indicates that the partial specific volumes of anhydrous native and denatured DNA are equal. The density difference at nonzero water activities is attributed to decreased hydration in the denatured state. The absence of a related change in φ accompanying the denaturation in the dilatometric experiments suggests that the probable volume change associated with loss of bound water during denaturation is accompanied by other compensatory volume effects. The possible nature of these volume effects is discussed.     

Complexing and denaturation of DNA by methylmercuric hydroxide. II. Ultracentrifugation studies

When increasing concentrations of methylmercuric hydroxide are added to a Cs₂SO₄ solution of native DNA, the buoyant density of DNA is unaltered until a critical concentration is reached above which there is a cooperative transition to denatured DNA which now binds so much CH₃HgOH that it becomes very dense and nonbuoyant. As increasing concentrations of methylmercuric hydroxide are added to a Cs₂So₄ solution of denatured DNA, the buoyant density gradually increases, indicating a gradual increase in the amount of methylmercury cation bound. The denatured DNA methylmercury complex becomes nonbuoyant at the same concentration of methylmercuric hydroxide as does the native DNA. These results support our previous interpretation that CH₃HgOH reacts with the imino NH bonds of thymine and guanine in nucleic acids. The reaction occurs more or less independently at the different binding sites for denatured DNA, but it occurs cooperatively with simultaneous denaturation for native DNA. The nature of the transition of denatured DNA to the nonbuoyant state is not known, but it is probably due to an abrupt decrease in the degree of hydration of the DNA when its density and hydrophobic character are sufficiently increased by the binding of the methylmercury cation. Direct measurements of the amount of methylmercury bound by DNA, as observed by preparative ultracentrifugation, confirm approximately the buoyant density results as to the amount of methylmercury bound. The possibility of using methylmercuric hydroxide as a reagent for the separation of complementary strands, depending on then thymine of their thymine plus guanine content, is discussed.     

Fate of Transforming Deoxyribonucleate in Bacillus subtilis

The majority of donor deoxyribonucleate (DNA) at early stages after uptake was found in a complex with a cell component which changes its buoyant behavior on equilibrium density gradients. Analysis of the recipient cell lysates, after treatment to dissociate the complex, showed about two-thirds of the donor molecules in denatured form and the rest associated with recipient DNA. Incubation of cells after DNA uptake leads to the disappearance of denatured donor DNA and to the increase of donor label associated with recipient DNA. Some characteristics of a component from intact cells or spheroplasts with affinity for denatured Bacillus subtilis DNA are described.     

Unusual properties of the DNA from Xanthomonas phage XP-12 in which 5-methylcytosine completely replaces cytosine.

Xanthomonas phage XP-12 contains 5-methylcytosine completely replacing cytosine. This substitution confers several unusual properties upon XP-12 DNA. The buoyant density of XP-12 DNA in CsCl gradients is 1.710 g/cm-3, 0.16 g/cm-3 lower than that expected for a normal DNA with the same percentage of adenine plus thymine. The melting temperature for XP-12 DNA in 0.012 M Na+ is the highest reported for any naturally occurring DNA, 83.2 degrees C, 6.1 degrees C higher than that of normal DNAs with the same percentage of adenine plus thymine. Unlike the minor amounts of 5-methylcytosine found in most plant and animal DNAs, the 5-methylcytosine residues of XP-12 derive their methyl group from the 3-carbon of serine instead of from the thiomethyl carbon of methionine. .     

Effect of ligand binding on the buoyant density of DNA in Nycodenz gradients.

The effect of ligand binding upon the buoyant density of DNA in Nycodenz gradients has been studied using DNAs of differing base compositions. The effect of both intercalating ligands (ethidium bromide and proflavin) and non-intercalating ligands (distamycin A, DAPI and netropsin) has been studied. The binding of intercalating ligands to DNA has essentially no effect on the buoyant density of DNA in Nycodenz gradients. The non-intercalating ligands were found to increase the buoyant density of DNA in a base specific manner. The increase in buoyant density can be interpreted in terms of disruption of the hydration shell of the DNA molecule caused by the binding of the ligand along the minor groove of the DNA helix.     

A study of DNA denaturation in the ultracentrifuge

The melting transition of DNA in alkaline CsCl can be followed in the analytical ultracentrifuge. Equilibrium partially denatured states can be observed. These partially denatured DNA bands have bandwidths of up to several times those of native DNA. Less stable molecules melt early and are found at heavier densities in the melting region. An idealized ultracentrifuge melting transition is described. The melting transition of singly nicked PM-2 DNA resembles the idealized curve. The DNA profile is a Gaussian band at all points in the melt. DNA's from mouse, D. Melanogaster, M. lysodeikticus, T4, and T7 also show equilibrium bands at partially denatured densities, some of which are highly asymmetric. Simple sequence satellite DNA shows an all-or-none transition with no equilibrium bands at partially denatured densities. The temperature at which a DNA denatures is an increasing function of the (G + C) content of the DNA. The T_m does not show a molecular-weight dependence in the range 1.2 × 10⁶–1.5 × 10⁷ daltons (single strand) for mouse, M. lysodeikticus, or T4 DNA. The mouse DNA partially denatured bands do not change shape as a function of molecular weight. The T4 DNA intermediate band develops a late-melting tail at low molecular weight. M. lysodeikticus DNA bands at partially denatured densities become broader as the molecular weight is decreased. Mouse DNA is resolved into six Gaussian components at each point in the melting transition.     

On the hydration of DNA. I. Preferential hydration and stability of DNA in concentrated trifluoroacetate solution

The hydration of DNA is an important factor in the stability of its secondary structure. Methods for measuring the hydration of DNA in solution and the results of various techniques are compared and discussed critically. The buoyant density of native and denatured T-7 bacteriophage DNA in potassium trifluoroacetate (KTFA) solution has been measured as a function of temperature between 5 and 50°C. The buoyant density of native DNA increased linearly with temperature, with a dependence of (2.3 ± 0.5) × 10^?4 g/cc-°C. DNA which has been heat denatured and quenched at 0°C in the salt solution shows a similar dependence of buoyant density on temperature at temperatures far below the T_m, and above the T_m. However, there is an inflection region in the buoyant density versus T curve over a wide range of temperatures below the T_m. Optical density versus temperature studies showed that this is due to the. inhibition by KTFA of recovery of secondary structure on quenching. If the partial specific volume is assumed to be the same for native and denatured DNA, the loss of water of hydration on denaturation is calculated to be about 20% in KTFA at a water activity of 0.7 at 25°C. By treating the denaturation of DNA as a phase transition, an equation has immmi derived relating the destabilizing effect of trifluoroacetate to the loss of hydration on denaturation. The hydration of native DNA is abnormally high in the presence of this anion, and the loss of hydration on denaturation is greater than in CsCl. In addition, trifluoroacetate appears to decrease the ΔHof denaturation.     

Transformation in Bacillus subtilis: characterization of an intermediate in recombination observed during transformation.

Summary From recombination-proficient competent cells of Bacillus subtilis in which the donor DNA entered at 17°, and which were kept at the same temperature, a complex of donor DNA and the recipient chromosome can be obtained which has a relatively high buoyant density in CsCl gradients. Exposure of the isolated complex to nuclease S1 liberates donor radioactivity. The limited biological activity of DNA re-extracted from cells attempting to recombine at 17° is decreased upon incubation with nuclease S1. If recombination is allowed to proceed at 30°, the high buoyant density of the donor-recipient complex decreases to normal values and less radioactivity can be liberated from the complex by nuclease S1. Concomitantly the biological activity of re-extracted DNA becomes less vulnerable to nuclease S1 under these conditions. On the basis of these observations we assume that the intermediate complex partly consists of unpaired single-stranded donor DNA.Support for the correctness of this assumption is derived from experiments with a mutant, which is delayed in the processing of high buoyant density donor-recipient complex to normal buoyant density donor-recipient complex. This delay is reflected in the time of acquisition of resistance to nuclease S1 digestion of the isolated complex.     

Partial denaturation of mouse DNA in preparative CsCl density gradients at alkaline pH.

A new technique--partial denaturation of DNA in equilibrium CsCl density gradients at pH 11.4--is used to determine the distribution of intermediate states in the melting of mouse DNA. When the technique is applied in the preparative ultracentrifuge, the DNA is fractionated according to stability. Neutralization of the partially denatured fractions results in the recovery of most of the DNA in its native form. The individual fractions are more homogeneous than the total DNA: they have decreased density heterogeneity (smaller band widths), neutral CsCl buoyant densities that differ from the average, and more homogeneous melting profiles with melting temperatures that differ from the average.     

Chromosomal DNA denaturation and reassociation in situ.

The degree of chromosomal DNA (cDNA) denaturation and renaturation on polytene chromosomes has been measured by UV microspectrophotometry. Also DNA losses occurring upon denaturation have been quantified by Feulgen, gallocyanin-chromalum and UV. It has been observed that denaturation in alkali (0.07 N NaOH at room temperature) and formamide (90% formamide; 0.1 SSC, pH 7.2) at 65 °C removes about 30% of the DNA. Low DNA loss occurs upon denaturation in HCl (0.24 M) at room temperature and 60% formamide: 2 × 10^?4 M EDTA (pH 8) at 55 °C. The presence of 4% formaldehyde in the denaturation buffer prevents DNA loss. After denaturation of chromosomes in 0.1 × SSC containing 4% formaldehyde at 100 °C for 30 sec, an hyperchromicity of 39 °C is observed. The denaturation efficiency varies with the denaturation treatment. The percentage reassociation was measured from the difference in the UV absorption of renatured chromosomes and that of denatured chromosomes from the same set. It seems that in our conditions DNA:DNA reassociation does not occur. The efficiency of hybridization is proportional to the denaturation extent of the DNA. However, the entire fraction of DNA which has been denatured is not available for hybridization.     

Spectrophotometric,potentiometric, and density gradient ultracentrifugation studies of the binding of silver ion by DNA

The equilibrium and the stoichiometry for the reversible complexing of silver ion by DNA have been studied by potentiometric titrations, proton release pH-stat titrations, and by spectrophotometry. The complexing reactions involve primarily the purine and pyrimidine residues, not the phosphate groups. There are at least three types of binding (types I, II, and III), of which the first two have been intensively studied in this work. The sum of type I and type II binding saturates at one silver atom per two nucleotide residues. In the type I and type II reactions, zero and one proton, respectively, are displaced per silver ion bound. At pH 5.6, the reactions occur stepwise, type I being first, while at pH 8.0, they occur simultaneously. The silver ion binding curve is very sharp at pH 8, indicating a cooperative reaction. The strength of the binding increases with increasing GC content. Type I binding is more important for GC-rich DNA's than for GC-poor ones. Denatured DNA binds more strongly than does native DNA. The silver ion complexing reaction is chemically and biologically reversible. We propose that type II binding essentially involves the conversion of an \documentclass{article}\pagestyle{empty}\begin{document}$ {\rm N} - {\rm H} \cdots {\rm N} $\end{document} hydrogen bond of a complementary base pair to an N—Ag—N bond. The nature of type I binding is less clear, but it may involve a π interaction with stacked bases. The buoyant density (ρ₀) of DNA in a Cs₂SO₄ density gradient increases when the DNA reacts with silver ion. The buoyant density change is about 0.15 g./ml. for 0.5 silver bound per nucleotide. The large buoyant density changes and the selective nature of the complexing reaction make it possible to perform good separations between native and denatured DNA or between GC-rich and GC-poor native DNA's by density gradient centrifugation.     

Interaction of polyribonucleotides with plant mitochondrial DNA

DNA is extracted from purified mitochondria of potato tubers. This DNA cannot be resolved into two strands by alkaline CsCl gradients in our experiments. Poly (G), poly (U) and poly (I,G) interact with the plant mitochondrial DNA as shown by the marked shift in buoyant density that they produce on denatured DNA. Poly (A) and poly (C) do not lead to detectable interactions in standard conditions whereas a slight fixation of poly (C) occurs at acidic pH. These results suggest that the plant mitochondrial DNA contains d-A and d-C rich clusters and, in a lesser extent, d-G rich clusters.     

Restricted uptake of ethidium bromide and propidium diiodide by denatured closed circular DNA in buoyant cesium chloride

Alkali-denatured closed circular DNA forms, on neutralization, a relatively stable species first described by Pouwels et al. (1968). In contrast to single-stranded DNA, this denatured two-stranded closed circular DNA species bands densely and co-bands approximately with closed circular duplex DNA in ethidium bromide-CsCl equilibrium density gradients. In CsCl gradients containing propidium diiodide, denDNA I is denser than DNA I, nicked circular DNA and single-stranded φX174 viral DNA. The magnitude of the separations between the above DNAs allows preparative isolation of each when all four are present in the same gradient. The denDNA I has a novel open circular appearance in the electron microscope when cast on standard aqueous hypophases. This species becomes tightly twisted when cast on either aqueous or formamide hypophases containing ethidium bromide. We have concluded from these observations that the high buoyant density of denDNA I in dye-CsCl gradients, relative to single-stranded DNA, is the result of a restricted uptake of dye.     

Distribution of histones in alkali-denatured chromatin studied by isopycnic centrifugation in alkaline metrizamide density gradients.

Three types of density gradients - neutral metrizamide, alkaline NaOH-metrizamide and alkaline triethanolamine-metrizamide - were used for studying the distribution of histones between the two DNA strands in alkali-denatured chromatin. It was found possible to avoid both protein redistribution and dissociation by using triethanolamine-metrizamide density gradients at pH 10.5. Under these conditions an alkali-denatured mixture of DNA and chromatin was well separated into the original DNA and DNP. When native or sonicated chromatin was denatured at pH 12.2 and centrifuged in a triethanolamine-metrizamide density gradient at pH 10.5 no peak of free DNA appeared. These results show that both DNA strands remain associated with histone molecules upon alkaline denaturation of chromatin.     

Density gradient ultracentrifugation method of studying sibiromycin interaction with linear and circular DNA]

Sibiromycin added to linear chromosomal E. coli DNA in vitro leads to the decrease of bouyant density in neutral CsCl density gradient. This decrease is a linear function of sibiromycin/DNA ratio and amounts to about 32 mg/ml at the ratio equal to 0.1. Binding sibiromycin does not change the degree of hydration of DNA as revealed by centrifugation in metrizamide density gradients. When added to the covalently closed or open circular DNA of PM-2 phage, sibiromycin decreased the bouyant density of these DNA species to a similiar extent. The antibiotic does not induce single-strand breaks in DNA in vitro as follows from the results of ethidium bromide-CsCl density gradient centrifugation of covalently closed PM-2 DNA.     

Sedimentation equilibrium of proteins in density gradients.

The technique of sedimentation equilibrium in density gradients in the analytical ultracentrifuge has been applied to the study of proteins. A variety of effects and procedures including the use of density marker beads, the effects of pressure on buoyant density and pH, and the calculation of compositional density gradient proportionality constants and density--refractive index relations have been developed. The buoyant densities of twenty-four proteins have been measured and hydration values computed. The buoyant titrations of six proteins have been measured. These data have been interpreted in terms of the buoyant titrations which have been obtained for six ionizable homopolypeptides, five copolypeptides, two non-ionizable homopolypeptides and three chemically modified proteins. Spectropolarimetry and potentiometric titrations were employed to further interpret these data. Approximate values for dissociation constants, numbers of ionizable residues, and the nature of ions bound or dissociated upon ionization have been obtained. The relation between potentiometric and buoyant titrations and the use of density gradient centrifugation as a probe for protein structure have been explored.     

Natural Occurrence of Cross-Linked Vaccinia Virus Deoxyribonucleic Acid

The molecular weight of native vaccinia deoxyribonucleic acid (DNA) is 1 to 1.17 times that of native T4 DNA. Sedimentation of denatured vaccinia DNA through alkaline sucrose gradients yields an apparent molecular weight greater than twice that of denatured T4 DNA, implying that the complementary strands of vaccinia DNA do not separate upon denaturation. When alkali-denatured vaccinia DNA is neutralized, it has the physical chemical properties of native DNA when tested by sedimentation through neutral sucrose gradients, banding in CsCl, and by hydroxylapatite chromatography. We conclude that almost all mature vaccinia DNA molecules contain a small number of naturally occurring cross-links.