Liquid crystalline ordering of nucleosome core particles under macromolecular crowding conditions: evidence for a discotic columnar hexagonal phase.

Macromolecular crowding conditions occurring inside the cell nucleus were reproduced experimentally with solutions of mononucleosome core particles to study their supramolecular organization. We report here that under these conditions, and over a large range of monovalent salt concentrations, mononucleosome core particles self-assemble to form a discotic liquid crystalline phase characterized in polarizing and freeze-fracture electron microscopy. Mononucleosomes are stacked on each other to form columns, which are themselves closely packed into an hexagonal array. The nucleosome concentration, estimated from the network parameters, falls in the range of values measured in cell nuclei. We suggest that these concentrated solutions, although their organization cannot be immediately compared to the organization of chromatin in vivo, may be used to investigate the nucleosome-nucleosome interactions. Furthermore, this approach may be complexified to take into account the complexity of the eucaryotic chromatin.     

X-ray diffraction characterization of the dense phases formed by nucleosome core particles

Multiple dense phases of nucleosome core particles (NCPs) were formed in controlled ionic conditions (15-160 mM monovalent salt, no divalent ions), under osmotic pressures ranging from 4.7 x 10(5) to 2.35 x 10(6) Pa. We present here the x-ray diffraction analysis of these phases. In the lamello-columnar phase obtained at low salt concentration (<25 mM), NCPs stack into columns that align to form bilayers, kept separated from one another by a layer of solvent. NCPs form a monoclinic lattice in the plane of the bilayer. For high salt concentration (>50 mM), NCPs order into either a two-dimensional columnar hexagonal phase or into three-dimensional orthorhombic (quasi-hexagonal) crystals. The lamellar and hexagonal (or quasi-hexagonal) organizations coexist in the intermediate salt range; their demixing requires a long time. For an applied pressure P = 4.7 10(5) Pa, the calculated NCPs concentration ranges from approximately 280 to 320 mg/ml in the lamello-columnar phase to 495 to 585 mg/ml in the three-dimensional orthorhombic phase. These concentrations cover the concentration of the living cell.     

Bilayers of nucleosome core particles

Among the multiple effects involved in chromatin condensation and decondensation processes, interactions between nucleosome core particles are suspected to play a crucial role. We analyze them in the absence of linker DNA and added proteins, after the self-assembly of isolated nucleosome core particles under controlled ionic conditions. We describe an original lamellar mesophase forming tubules on the mesoscopic scale. High resolution imaging of cryosections of vitrified samples reveals how nucleosome core particles stack on top of one another into columns which themselves align to form bilayers that repel one another through a solvent layer. We deduce from this structural organization how the particles interact through attractive interactions between top and bottom faces and lateral polar interactions that originate in the heterogeneous charge distribution at the surface of the particle. These interactions, at work under conditions comparable with those found in the living cell, should be of importance in the mechanisms governing chromatin compaction in vivo.     

Salt-induced structural changes of nucleosome core particles.

The effects of sodium chloride concentration on the structure of chicken erythrocyte nucleosome core particles have been studied by the use of fluorescently labelled histones. Histone H3 was modified with two sulfhydryl-specific dyes and reconstituted into core nucleosomes. Between 10^?4 m and 0.6 M-NaCl four different states were observed by the fluorescent techniques of collisional quenching, polarization and energy transfer. Below 5 × 10^?4 m-NaCl the nucleosome is flexible, with the single cysteine residues of the two H3 species about 48 Å apart and somewhat exposed. Between 5 × 10^?3 m and 10^?1 m-NaCl the nucleosome is rigid and non-spherical. The cysteine residues are close together and buried. Between 10^?1 m and 4 × 10^?1 m-NaCl, the cysteines become slightly more exposed but remain close together. At 6 × 10^?1 m-NaCl the nucleosome is very flexible. The cysteines are more than 70 Å apart and are quite exposed. The dramatic structural changes that are observed in core nucleosomes are consistent with the variety of functions in which they must participate in the cell.     

Phase diagram of nucleosome core particles

We present a phase diagram of the nucleosome core particle (NCP) as a function of the monovalent salt concentration and applied osmotic pressure. Above a critical pressure, NCPs stack on top of each other to form columns that further organize into multiple columnar phases. An isotropic (and in some cases a nematic) phase of columns is observed in the moderate pressure range. Under higher pressure conditions, a lamello-columnar phase and an inverse hexagonal phase form under low salt conditions, whereas a 2D hexagonal phase or a 3D orthorhombic phase is found at higher salt concentration. For intermediate salt concentrations, microphase separation occurs. The richness of the phase diagram originates from the heterogeneous distribution of charges at the surface of the NCP, which makes the particles extremely sensitive to small ionic variations of their environment, with consequences on their interactions and supramolecular organization. We discuss how the polymorphism of NCP supramolecular organization may be involved in chromatin changes in the cellular context.     

Maintenance DNA methylation of nucleosome core particles

The enzyme responsible for maintenance methylation of CpG dinucleotides in vertebrates is DNMT1. The presence of DNMT1 in DNA replication foci raises the issue of whether this enzyme needs to gain access to nascent DNA before its packaging into nucleosomes, which occurs very rapidly behind the replication fork. Using nucleosomes positioned along the 5 S rRNA gene, we find that DNMT1 is able to methylate a number of CpG sites even when the DNA major groove is oriented toward the histone surface. However, we also find that the ability of DNMT1 to methylate nucleosomal sites is highly dependent on the nature of the DNA substrate. Although nucleosomes containing the Air promoter are refractory to methylation irrespective of target cytosine location, nucleosomes reconstituted onto the H19 imprinting control region are more accessible. These results argue that although DNMT1 is intrinsically capable of methylating some DNA sequences even after their packaging into nucleosomes, this is not the case for at least a fraction of DNA sequences whose function is regulated by DNA methylation.     

Self-assembly of single and closely spaced nucleosome core particles.

Self-assembly of DNA with the four core histones but in the absence of H1 generates nucleosome core particles which are spaced randomly over large distances. Closely spaced core particles, however, exhibit a preferred short linkage which is not a multiple of 10 base pairs. They bind about 140 base pairs whereas apparently shorter DNA lengths per nucleosome observed after digestion with micrococcal nuclease are the result of degradation from the ends. The DNA length of one superhelical turn in the core particle is 83 +/- 4 base pairs. Single core particles may bind more DNA than closely spaced core particles but probably less than two full turns of 168 base pairs. The internal structures of single and of native core particles are very similar as judged by their amount of DNA, sedimentation coefficient, appearance in the electron microscope, and digestion with DNase I. In addition to core particles, a particle is described which sediments at 9 S and consists of 108 base pairs of DNA bound to the histone octamer. It appears to be the smallest stable "core particle" but it is not a degradation product of the 146-base-pair core particle. Digestion of end-labeled 9 S and nucleosome core particles with DNase I shows distinct differences.     

Different mechanism for in vitro formation of nucleosome core particles

The interaction of different histone oligomers with nucleosomes has been investigated by using nondenaturing gel electrophoresis. In the presence of 0.2 M NaCl, the addition of the pairs H2A,H2B or H3,H4 or the four core histones to nucleosome core particles produces a decrease in the intensity of the core particle band and the appearance of aggregated material at the top of the gel, indicating that all these histone oligomers are able to associate with nucleosomes. Equivalent results were obtained by using oligonucleosome core particles. Additional electrophoretic results, together with second-dimension analysis of histone composition and fluorescence and solubility studies, indicate that H2A,H2B, H3,H4, and the four core histones can migrate spontaneously from the aggregated nucleosomes containing excess histones to free core DNA. In all cases the estimated yield of histone transfer is very high. Furthermore, the results obtained from electron microscopy, solubility, and supercoiling assays demonstrate the transfer of excess histones from oligonucleosomes to free circular DNA. However, the extent of solubilization obtained in this case is lower than that observed with core DNA as histone acceptor. Our results demonstrate that nucleosome core particles can be formed in 0.2 M NaCl by the following mechanisms: (1) transfer of excess core histones from oligonucleosomes of free DNA, (2) transfer to excess H2A,H2B and H3,H4 associated separately with oligonucleosomes to free DNA, (3) transfer to excess H2A,H2B initially associated with oligonucleosomes to DNA, followed by the reaction of the resulting DNA-(H2A,H2B) complex with oligonucleosomes containing excess H3,H4, and (4) a two-step transfer reaction similar to that indicated in (3), in which excess histones H3,H4 are transferred to DNA before the reaction with oligonucleosomes containing excess H2A,H2B. The possible biological implications of these spontaneous reactions are discussed in the context of the present knowledge of the nucleosome function.     

Wrapping of genomic polydA.polydT tracts around nucleosome core particles.

Five human clones containing genomic regions of polydA have been isolated by their ability to form intermolecular triple helices with agarose cross-linked polyU. All of these clones contain Alu repetitive DNA sequences. End-labelled DNA fragments containing these sequences have been successfully reconstituted onto nucleosome core particles by salt exchange. The structure of these has been examined by digesting with DNase I, hydroxyl radicals or diethylpyrocarbonate. DNase I cleavage of the polydA tracts is poor in the free DNA but is markedly enhanced at certain positions when complexed with nucleosome cores. Phased digestion patterns are observed which continue through the (A)n blocks and reveal an average helical periodicity of about 10 base pairs. The distance between adjacent maxima varies between 8-12 base pairs, suggesting that the exact helical repeat is not necessarily constant. One fragment containing the sequence (TA)11T34 reveals a 12 base pair repeat within the (AT)n region. A pUC19 polylinker fragment containing a block of A69.T69 cloned into the Smal site could also be reconstituted onto nucleosome cores and reveals the same phased DNaseI digestion pattern. The DNase I cleavage pattern is not identical at each of the maxima, suggesting that the structural distortions imposed by the core particles are not constant along the DNA.     

Chiral discotic columnar germs of nucleosome core particles

In concentrated solution and in the presence of high concentrations of monovalent cations, nucleosome core particles order into a discotic columnar mesophase. This phase is limited to finite-sized hexagonal germs that further divide into six coiled branches, following an iterative process. We show how the structure of the germs comes from the competition between hexagonal packing and chirality with a combination of dendritic facetting and double-twist configurations. Geometrical considerations lead us to suspect that the chirality of the eukaryotic chromosomes may originate from the same competition.     

Transport of nucleosome core particles in semidilute DNA solutions

We studied the diffusion of native and trypsinized nucleosome core particles (NCPs), in aqueous solution and in concentrated DNA solutions (0.25-100 mg/ml) using fluorescence correlation spectroscopy (FCS). The highest DNA concentrations studied mimic the DNA density inside the cell nucleus. The diffusion coefficient of freely diffusing NCPs depends on the presence or absence of histone tails and is affected by the salt concentration due to the relaxation effect of counterions. NCPs placed in a network of long DNA molecules (30-50 kbp) reveal anomalous diffusion. We demonstrate that NCPs diffusion is in agreement with known particle transport in entangled macromolecular solutions as long as the histone tails are folded onto the particles. In contrast, when these tails are unfolded, the reversible adsorption of NCPs onto the DNA network has to be taken into account. This is confirmed by the fact that removal of the tails leads to reduction of the interaction between NCPs and the DNA network. The findings suggest that histone tail bridging plays an important role in chromatin dynamics.     

31P-NMR studies of DNA in nucleosome core particles

³¹P Nmr parameters (δ, T₁, W_1/2, and NOE) were measured for the DNA in nucleosome core particles at three frequencies and compared with similar data for the histone-free DNA. An essentially linear relationship was found between the frequency of observation and line-width for the single broad envelope of ³¹P resonances of the DNA in the nucleosome cores. We attributed this largely to chemical shift dispersion, with smaller contributions from chemical shift anisotropy and dipolar broadening. These results suggest the presence of different environments for phosphorus atoms in the core particles. However, within the accuracy of the method, no asymmetry in the resonance could be detected, which would tend to rule out any significant degree of DNA “kinking.” To investigate the interactions of the DNA and histones within the core particles we also studied transitions induced by urea and by temperature. Urea caused two stepwise increases in linewidth, which we attributed to conformational changes. A biphasic transition was also observed in the temperature profile, consistent with previous optical studies [Weischet et. al. (1978) Nucleic Acids Res. 5 , 139]. Various models with different types of local mobility were examined by the relaxation theory. A model of isotropic motion having a broad distribution of correlation times gave a fairly good fit to the ³¹P-nmr data.     

Hydrodynamic studies of the interaction between nucleosome core particles and core histones

We have studied the hydrodynamic properties of the complexes formed by interaction of nucleosome core particles with excess histone octamers containing two each of the four core histones. The results are consistent with tight binding of two to three octamers to the exterior of each core particle. The binding is dependent upon the presence of the H3/H4 histone pair: when H3/H4 alone are added to nucleosome core particles, tight binding is observed, but H2A/H2B alone are bound only weakly. We have also examined the properties of the nucleosome core in solutions containing 0·1 m to 0·7 M-NaCl. We show that in this salt range the core particle undergoes some changes in shape, reflected in a 14% increase in the frictional coefficient. Even at the highest salt concentrations used, however, the nucleosome core is still a compact, folded structure.     

The structure of nucleosome core particles as revealed by difference Raman spectroscopy.

Raman spectra have been observed of nucleosome core particles (I) prepared from chicken erythrocyte chromatin, its isolated 146 bp DNA (II), and its isolated histone octamer (H2A+H2B+H3+H4)2 (III). By examining the difference Raman spectra, (I)-(II), (I)-(III), and (I)-(II)-(III), several pieces of information have been obtained on the conformation of the DNA moiety, the conformation of the histone moiety, and the DNA-histone interaction in the nucleosome core particles. In the nucleosome core particles, about 15 bp (A.T rich) portions of the whole 146 bp DNA are considered to take an A-form conformation. These are considered to correspond to its bent portions which appear at intervals of 10 bp.     

Site-specific aflatoxin B1 adduction of sequence-positioned nucleosome core particles

The question of how the presence of nucleosomal packing of DNA modifies carcinogen interaction at specific sites cannot be answered by studies on whole chromatin or bulk nucleosomes because of the heterogeneity of DNA sequences in the particles. We have circumvented this problem by using nucleosomes that are homogenous in DNA sequence and hence in DNA-histone contact points. A cloned DNA fragment containing a sea urchin 5 S gene which precisely positions a histone octamer was employed. By using 32P end-labeled DNA and genotoxins that allow cleavage at sites of attack, the frequency of adduction at every susceptible nucleotide can be determined on sequencing gels. The small methylating agent dimethyl sulfate and the bulky alkylating agent aflatoxin B1-dichloride (AFB1-Cl2) were used to probe the influence of DNA-histone interactions on DNA alkylation patterns in the sequence-positioned core particle. We find dimethyl sulfate to bind with equal preference to naked or nucleosomal DNA. In contrast, AFB1-Cl2 binding is suppressed an average of 2.4-fold at guanyl sites within nucleosomes compared with AFB1-Cl2 affinity at the corresponding site in naked DNA. The DNA is more accessible in regions near the particle boundary. We observe no other histone-imposed localized changes in AFB1-Cl2 sequence specificity. Further, sites of DNase I cleavage or proposed DNA bending show neither enhanced nor reduced AFB1-Cl2 adduction to N7-guanine. Since AFB1-Cl2 binding sites lie in the major groove, nucleosomal DNA appears accessible to AFB1-Cl2 at all points of analysis but with an access which is uniformly restricted in the central 100 nucleotides of the core particle. The data available do not indicate further localized or site-specific perturbations in DNA interactions with the two carcinogens studied.     

Stability of the primary organization of nucleosome core particles upon some conformational transitions.

The sequential arrangement of histones along DNA in nucleosome core particles was determined between 0.5 and 600 mM salt and from 0 to 8 M urea. These concentrations of salt and urea up to 6 M had no significant effect on the linear order of histones along DNA but 8 M urea caused the rearrangement of histones. Conformational changes in cores have been identified within these ranges of conditions by several laboratories 8-21. Also, abrupt structural changes in the cores, apparently their unfolding, were found by gel electrophoresis to occur at urea concentration, between 4 and 5 M. 600 mM salt and 6 M urea were shown to relax the binding of histones to DNA in cores but do not however release histones or some part of their molecules from DNA. It appears therefore that nucleosomal cores can undergo some conformational transitions and unfolding whereas their primary organization remains essentially unaffected. These results are consistent with a model of the core particles in which the histone octamer forms something like a helical "rim" along the superhelical DNA and histone-histone interactions beyond the "rim" are rather weak in comparison with those within the "rim".