Conformation of nucleosome core particles and chromatin in high salt concentration

A New Fluorescence Resonance Energy Transfer Approach Demonstrates That the Histone Variant H2AZ Stabilizes the Histone Octamer within the Nucleosome

Nucleosomes are highly dynamic macromolecular complexes that are assembled and disassembled in a modular fashion. One important way in which this dynamic process can be modulated is by the replacement of major histones with their variants, thereby affecting nucleosome structure and function. Here we use fluorescence resonance energy transfer between fluorophores attached to various defined locations within the nucleosome to dissect and compare the structural transitions of a H2A.Z containing and a canonical nucleosome in response to increasing ionic strength. We show that the peripheral regions of the DNA dissociate from the surface of the histone octamer at relatively low ionic strength, under conditions where the dimer-tetramer interaction remains unaffected. At around 550 mm NaCl, the (H2A-H2B) dimer dissociates from the (H3-H4)(2) tetramer-DNA complex. Significantly, this latter transition is stabilized in nucleosomes that have been reconstituted with the essential histone variant H2A.Z. Our studies firmly establish fluorescence resonance energy transfer as a valid method to study nucleosome stability, and shed new light on the biological function of H2A.Z.

Structural states of the nucleosome

The nucleosome is the fundamental component of the eukaryotic chromosome, participating in the packaging of DNA and in the regulation of gene expression. Its numerous interactions imply a structural dynamism. Previous biophysical studies under limited sets of conditions have not been able to reconcile structural differences and transitions observed. We have determined a series of nucleosome conformations over a >10,000-fold range in salt concentration using a combination of biochemical methods, spectroscopic electron microscopy, and three-dimensional reconstruction techniques for randomly oriented single particles. This study indicates several ionic strength-dependent nucleosome conformations and also reconciles the differences between currently existing divergent models for the nucleosome. At low ionic environments, the particle appears highly elongated, becoming more compact and prolate ellipsoidal as ionic strength is increased to 10 mm NaCl. At 30 mM NaCl, the particle exhibits a spheroidal conformation. As ionic strength is increased to 150 mM NaCl, the nucleosome conformation changes and becomes oblate. Above 450 mM NaCl, the structure becomes highly elongated again. The result of this study is a unifying concept in which the three-dimensional structure of the nucleosome is inferred to be dynamic in response to ionic interactions and in accord with biochemical and genetic studies.

Inhibition of CpG methylation in linker DNA by H1 histone

H1 exerts a specific in vitro inhibitory effect on enzymic DNA methylation. The experiments reported in this paper were undertaken in order to assess whether the lower methylation level found in internucleosomal DNA compared to core DNA is the in vivo consequence of the well-known localization of this histone in the linker region, as opposed to a possible deficiency of CpG dinucleotides in linker DNA. The methyl-accepting ability of H1-depleted oligonucleosomes from human placenta and of the corresponding core particles were assayed by addition of purified DNA methyltransferase, using S-adenosylmethionine as the methyl group donor. We have found that approx. 80% of newly-incorporated methyl groups are localized in linker DNA, which is indeed a good potential substrate for enzymic DNA methylation. Addition of quasi-physiological amounts of H1 to H1-depleted oligonucleosomes markedly reduced their methyl-accepting ability, while exerting a re-condensing effect on these particles, as revealed by the distortions of their circular dichroism spectra.

Analysis of the changes in the structure and hydration of the nucleosome core particle at moderate ionic strengths

In order to better understand the conformational changes induced in the nucleosome core particle by changes in the ionic strength of the media in the range from 0.1 to 0.6 M NaCl, we have conducted a very detailed structural analysis, combining circular dichroism, DNase I digestion, and sedimentation equilibrium. The results of such analysis indicate that the secondary structure of both DNA and histones exhibits small (approximately 5%) but noticeable changes as the salt increases within this range. In the case of DNA, the data are consistent with a trend toward a more relaxed secondary structure. The DNase I pattern of digestion is also altered by the salt and suggests a DNA relaxation around the flanking ends. From the hydrodynamic measurements, we also observe a significant change in the virial coefficients of the particle as the salt increases, which in turn are in very good agreement with the theoretically expected values. Furthermore, the preferential hydration parameter is also found to increase with the salt. We believe that the self-dependent conformational change of the nucleosome core particle is the result of the conjunction of all these subtle changes. Yet, from the present data, their exact relationship to the tertiary structure of the whole particle at the different ionic strengths cannot be exactly defined.

Spectroscopic studies on histone-DNA interactions. II. Three transitions in nucleosomes resolved by salt-titration

The multiple-step transitions in DNA-histone interactions in chicken erythrocyte nucleosomes with increasing ionic strength are resolved by salt-titration spectroscopy. Both the circular dichroism of the DNA and the fluorescence of the histones in nucleosomes change during the titration process with concentrations of NaCl from 0.1 M to 2.5 M. By differentiating the titration curves, three distinct peaks corresponding to three structural transitions are observed. The two peaks near 0.95 M and 1.45 M-NaCl are common to the circular dichroism and fluorescence curves. The circular dichroism curve has another peak near 0.55 M-NaCl. Because the derivative of the fluorescence titration curve for the DNA-(H3, H4) complex has only one peak near 1.45 M-NaCl, that peak is attributed to the dissociation of the histone dimer (H3, H4). The peak near 0.95 M-NaCl corresponds to the dissociation of the dimer (H2A, H2B) from the DNA-(H3, H4) complex, as shown by binding experiments of (H2A, H2B) to the DNA-(H3, H4) complex at the salt concentration near this peak. The peak near 0.55 M-NaCl reflects some inner-core structural change. As the change of the circular dichroism signal is reversible, salt-titration spectroscopy is applicable to equilibrium studies of the physical chemical properties of DNA-histone interactions. By the assumption of a non-co-operative model, the binding constant for the chicken erythrocyte (H2A, H2B) dimer to the DNA-(H3, H4) complex is calculated as 2.8 X 10(6) M-1 at 1.0 M-NaCl (20 degrees C, pH 7.6). The DNA sequence dependence of the stability of the DNA-(H3, H4) interaction is observed in the salt-titration profiles of reconstituted material. Decreasing stability of the interaction of (H3, H4) is observed following the order: poly[(dG)-(dC)] much greater than chicken erythrocyte DNA greater than poly[(dA)-(dT)]. It is concluded that histones (H3, H4) have a different DNA sequence dependence from histones (H2A, H2B).

The effect of preincubation of HeLa cell nuclei with ATP on the degradation of mononucleosomal DNA by micrococcal nuclease

HeLa cell nuclei with DNA labeled with [3H] thymidine have been preincubated under varying conditions and then incubated with micrococcal nuclease. Aliquots, removed at increasing times, were analyzed for mononucleosomal size DNA and for acid-soluble DNA, the ratios were plotted and a slope was determined. Preincubation with ATP and a regenerating system increased the slope 2 fold. Optimum ATP concentrations were above 0.25 mM. The ATP effect was reversed by novobiocin. No inhibition of the ATP effect was observed with nalidixic acid, coumermycin, oxolinic acid, VM-26, aphidicolin, or 3 amino-benzamide. NAD or cAMP or cGMP had no effect with or without ATP. Other nucleoside triphosphates could substitute to varying degrees for ATP as could ATP analogues. Nuclei from log phase cells showed no ATP effect, but log phase cells, partially depleted of ATP by incubation with deoxyglucose, showed the effect. The effect was lost in nuclei on long-term storage. No evidence was found for differential degradation of core histones, histone H-1 or DNA, and there was no evidence of nucleosome sliding.

Nucleosome core particle stability and conformational change. Effect of temperature, particle and NaCl concentrations, and crosslinking of histone H3 sulfhydryl groups

We have studied the reversible dissociation of core size DNA from chicken erythrocyte nucleosome core particles in solutions containing 0 X 1 M to 0 X 6 M-NaCl. Dissociation increases with increasing NaCl concentration, increasing temperature and decreasing particle concentration. At high particle concentrations, no free DNA is observed below 0 X 3 M-NaCl, whereas above 0 X 3 M-NaCl a lower limit of dissociation is reached. A theoretical analysis based on the migrating-octamer mechanism of Stein is in disagreement with his conclusions concerning dependence of core particle dissociation on particle concentration, but provides a good explanation for our observations, and those of others, using salt concentrations up to 1 M-NaCl. It appears that the core particle is not stabilized primarily by electrostatic interactions. DNA length is not critical for core particle stabilization. The conformation of remaining intact nucleosome core particles changes only moderately within the range of NaCl concentrations studied. Crosslinking by copper phenanthroline of the Cys110 histone H3 single sulfhydryl groups in the intact nucleosome core particle leads to a decrease in stability, yet essentially unchanged hydrodynamic properties are maintained at 0 X 6 M-NaCl, confirming conclusions derived from the behavior of the native core particles. Values for density increments of nucleosome core particles over a range of NaCl concentrations are also given. A method is described for studying binding of histones to nucleosome core particles in the ultracentrifuge by scanning at 230 and 260 nm.

Effects of pH on the stability of chromatin core particles

Chromatin core particles near physiological ionic strength undergo a reversible transition induced by changes in pH near neutrality. While sedimentation studies indicate no significant effect on size or shape, changes in tyrosine fluorescence anisotropy and in circular dichroism suggest a somewhat looser structure at high pH. Further support of this suggestion is given by high salt dissociation experiments; at pH 8 core particles begin to show changes at lower salt concentration than at pH 6. The pH transition appears unaffected by the presence of Mg2+ but can be blocked by crosslinking of the histones. A possible relationship is suggested between this transition and increases in intracellular pH which correlate with enhancement in several aspects of cellular activity including DNA replication.

Fractionation by micrococcal nuclease digestion of Drosophila embryo chromatin: isolation of a fraction enriched in two major nonhistone proteins

Limited digestion of Drosophila melanogaster embryo nuclei with mitochondrial nuclease, followed by selective solubilization in 0.1 M NaCl, yields a soluble nucleoprotein fraction (S3) enriched in two dominant protein bands of apparent molecular weight of 44000 and 48000. The analysis of the nucleosome monomer and multimer peaks, separated on sucrose gradients after slight digestion with micrococcal nuclease, shows that these proteins are associated with chromatin subunits, and that they are principally found in the subnucleosome region of fraction S3. This doublet is tentatively identified as a member of the noncanonical HMG of Drosophila. The thermal denaturation and the circular dichroism spectra of the fraction soluble in 0.1 M NaCl (S3) and insoluble fraction (P3) show that both fractions are also structurally different.

Nucleosomal particles open as the histone core becomes hyperacetylated

Lymphoblastoid cells grown in the presence of the deacetylase inhibitor butyrate were used to isolate nucleosomal particles in a hyperacetylated state. During a non-denaturing gel electrophoresis these particles revealed a heterogeneity which is only in part due to the presence of nonhistone proteins. Monomers that are free from histone H1 and high-mobility-group (HMG) proteins 14 and 17 yield a subfractionation according to the degree of core histone acetylation beyond a limiting value of 10 acetyl groups/particle. It is shown that hyperacetylation provides particles with low mobilities and a considerable conformational freedom in contrast to HMG protein 14 which locks them in a conformation that has a similar electrophoretic behaviour but is more defined.

The binding sites for large and small high-mobility-group (HMG) proteins. Studies on HMG-nucleosome interactions in vitro

Studies in vitro of binding high-mobility-group (HMG) proteins to nucleosomal particles that differ in their DNA contents reflect several aspects pertinent to their function in vivo. Two molecules of HMG 14 or 17 are accommodated by particles with 140 or 180 base pairs of DNA whereas HMG 1 or 2 are only bound by the larger specimens irrespective of the presence of HMG 14/17. It is concluded that one molecule of HMG 1 or 2 binds to the 40 base pairs of linker DNA whereas the HMG 14 or 17 molecules associate with the nucleosomal core. At physiological ionic strength, HMG 14 binding is cooperative, probably by triggering a conformational change in the nucleosomal particle. The phenomenon has been studied by two independent techniques. Besides the common gel-electrophoretic system, a centrifugation assay is described, which permits the derivation of a Hill coefficient nH = 1.3 and dissociation constants in the range of 30-90 nM at 0.15 M NaCl, pH 6.8.

Effects of pH on low-salt transition of chromatin core particles

The low-salt transition of chicken erythrocyte core particles containing uniform 145 base pair DNA was studied as a function of pH and of salt concentration. Intrinsic tyrosine fluorescence was used to follow the changes. Potassium salts of the anions C1-, H2PO4-, and SO4(2-) were indistinguishable in their ability to affect the transition. Divalent cations (Mg2+, Mn2+, Ca2+) were effective at 36-fold lower total concentration than monovalent cations (Li+, Na+, K+, Tris+), but no significant differences were observed within the two classes of cations. These results indicate that cation binding to the core particle is involved in the transition. At pH 9 the transition was broadened and shifted to higher monovalent cation concentration as compared to that at pH 6. At both pHs the fluorescence changes could be resolved into two steps by numerical least-squares analysis. On the basis of what is known about histone--histone interactions, a two-step mechanism is suggested, involving changes in the interactions between dimers of histones 2a and 2b with a tetramer of histones 3 and 4. The pH-induced changes appear to be correlated with a structural transition, which was detected as a function of pH at near physiological ionic strength (0.1 M). This structural change was accompanied by a small decrease in the tyrosine fluorescence anisotropy. An apparent pKa value near 7 is indicated, suggesting that the structural changes involved may be of physiological significance.

Conformational change of core particles studied by quasielastic light scattering

The diffusion translational coefficient Dt of core particles in monodisperse solutions has been measured by the quasielastic light scattering method in a large scale of salinities over the range 6.10(-4) to 2M Na+ or K+. The observed values of DT are independent of particle concentration in the range 0.1-2 mg/ml and do not vary with the scattering vector q corresponding to scattering angles between 40 degrees -120 degrees. When the salinity is progressively raised an increase of DT from 1.9.10(-7) cm2s-1 to 3.2.10(-7) cm2s-1 was observed at about 2.10(-3) M NaCl followed by a decrease of DT beyond 0.6 M NaCl.