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.     

Structure of subnucleosomal particles. Tetrameric (H3/H4)2 146 base pair DNA and hexameric (H3/H4)2(H2A/H2B)1 146 base pair DNA complexes

The tetrameric (H3/H4)2 146 base pair (bp) DNA and hexameric (H3/H4)2(H2A/H2B)1 146 bp DNA subnucleosomal particles have been prepared by depletion of chicken erythrocyte core particles using 3 or 4 M urea, 250 mM sodium chloride, and a cation-exchange resin. The particles have been characterized by cross-linking and sedimentation equilibrium. The structures of the particles, particularly the tetrameric, have been studied by sedimentation velocity, low-angle neutron scattering, circular dichroism, optical melting, and nuclease digestion with DNase I, micrococcal nuclease, and exonuclease III. It is concluded that since the radius of gyration of the DNA in the tetramer particle and its maximum dimension are very close to those of the core particle, no expansion occurs on removal of all the H2A and H2B. Nuclease digestion results indicate that histones H3/H4 in the tetramer particle protect a total of 70 bp of DNA that are centrally located within the 146 bp. Within the 70 bp DNA length, the two terminal regions of 10 bp are, however, not strongly protected from digestion. The optical melting profile of both particles can be resolved into three components and is consistent with the model of histone protection of DNA proposed from nuclease digestion. The structure proposed for the tetrameric histone complex bound to DNA is that of a compact particle containing 1.75 superhelical turns of DNA, in which the H3 and H4 histone location is the same as found for the core particle in chromatin by histone/DNA cross-linking [Shick, V. V., Belyavsky, A. V., Bavykin, S. G., & Mirzabekov, A. D. (1980) J. Mol. Biol. 139, 491-517]. Optical melting of the hexamer particle shows that each (H2A/H2B)1 dimer of the core particle protects about 22 base pairs of DNA.     

Association of nucleosome core particle DNA with different histone oligomers. Transfer of histones between DNA-(H2A,H2B) and DNA-(H3,H4) complexes

In non-denaturing low ionic strength gels, the titration of core DNA with H2A,H2B produces five well-defined bands. Quantitative densitometry and cross-linking experiments indicate that these bands are due to the successive binding of H2A,H2B dimers to core DNA. Only two bands are obtained with DNA-(H3,H4) samples. The slower of these bands is broad and presumably corresponds to two complexes containing one and two H3,H4 tetramers, respectively. In gels of higher ionic strength, DNA-(H2A,H2B) samples produce an ill-defined band, suggesting that the lifetime of the complexes containing H2A,H2B is relatively short. However, the low intensity of the free DNA band observed in these gels indicates that most of the DNA is associated with H2A,H2B. In agreement with this, our results obtained using different techniques (sedimentation, cross-linking, trypsin and nuclease digestions, and thermal denaturation) demonstrate that the association of H2A,H2B with core DNA occurs in free solution in both the absence and presence of NaCl (0.1 to 0.2 M). The low mobilities of DNA-(H2A,H2B) complexes, together with sedimentation and DNase I digestion results, indicate that the DNA in these complexes is not folded into the compact structure found in the core particle. Furthermore, non-denaturing gels have been used to study the dynamic properties of DNA-(H2A,H2B) and DNA-(H3,H4) complexes in 0.2 M-NaCl. Our results show that: (1) H2A,H2B and H3,H4 can associate, respectively, with DNA-(H3,H4) and DNA-(H2A,H2B) to produce complexes containing the four core histones; (2) DNA-(H2A,H2B) and DNA-(H3,H4) are able to transfer histones to free core DNA; (3) an exchange of histone pairs takes place between DNA-(H2A,H2B) and DNA-(H3,H4) and produces complexes with the same histone composition as that of the normal nucleosome core particle; and (4) although both histone pairs can exchange, histones H2A,H2B show a higher tendency than H3,H4 to migrate from one incomplete core particle to another. The complexes produced in these reactions have the same compact structure as reconstituted core particles containing the four core histones. Our kinetic results are consistent with a reaction mechanism in which the transfer of histones involves direct contacts between the reacting complexes. The possible participation of these spontaneous reactions on the mechanism of nucleosome assembly is discussed.     

Isolation and characterization of a spacerless dinucleosome from H1-deleted chromatin.

Calf thymus chromatin, depleted in histone H1, was digested with micrococcal nuclease and fractionated by column chromatography. 140 base pair nucleosome core particles were isolated along with an unusual particle containing 2 histone octamers and 240 base pairs of DNA. Evidence is presented that the spacer DNA region is absent from these modified dinucleosomes, which appear as stable products of the digestion process. The physical properties of both particles are presented along with brief speculation on their possible origin and function.     

The organization of histones and DNA in chromatin: Evidence for an arginine-rich histone kernel

We have examined the role played by various histones in the organization of the DNA of the nucleosome, using staphylococcal nuclease as a probe of DNA conformation. When this enzyme attacks chromatin, a series of fragments evenly spaced at 10 base pair intervals is generated, reflecting the histone-DNA interactions within the nucleosome structure. To determine what contribution the various histones make to DNA organization, we have studied the staphylococcal nuclease digestion patterns of complexes of DNA with purified histones.Virtually all possible combinations of homogeneous histones were reconstituted onto DNA. Exhaustive digestion of a complex containing the four histones H2A, H2B, H3, and H4 yields a DNA fragment pattern very similar to that of whole chromatin. The only other combinations of histones capable of inducing chromatin-like DNA organization are H2A/H2B/H4 and those mixtures containing both H3 and H4. From an examination of the kinetics of digestion of H3/H4 reconstitutes, we conclude that although the other histones have a role in DNA organization within the nucleosome, the arginine-rich histone pair, H3/H4, can organize DNA segments the length of the nucleosome core in the absence of all other histones.     

H3 Cys-110 is in close proximity to the C-terminal regions of H2B and H4 in a nucleosome core with an altered internal arrangement of histones

A particle obtained by nuclease digestion of nucleohistone complexes prepared by direct mixing of histones with DNA in 0.15 M NaCl was indistinguishable by composition and physical properties from nucleosome cores prepared under the same conditions from nucleohistone preannealed in 0.6 M NaCl. We show here that different photo-cross-links form when these particles are prepared from H3 labeled with photoaffinity reagents on the unique histone H3 cysteine. H3-H3 histone dimers were dominant when the particles were prepared by dilution of the nucleohistone from 0.6 M NaCl while H3-H2B and H3-H4 histone dimers were prominent if the nucleohistone complex was prepared directly in 0.15 M NaCl. Peptide mapping of the novel H3-H4 and H3-H2B dimers showed that Cys-110 of histone H3 is cross-linked to the 18 amino acid C-terminal end of H4 or to the 66 amino acid C-terminal half of H2B.     

Nucleosome core particle self-assembly kinetics and stability at physiological ionic strength

Micrococcal nuclease, DNase I, and trypsin have been employed to study the kinetics of core particle self-assembly by salt jump from 2.0 to 0.2 M NaCl. A few seconds after the initiation of the reassociation reaction, the bulk of core particle DNA becomes protected from digestion by micrococcal nuclease, whereas free DNA, under the same conditions, is completely hydrolyzed. The central and C-terminal regions of core histones are also protected from trypsin digestion immediately after the 2.0-0.2 M NaCl salt jump. Moreover, the extent of degradation produced by trypsin is the same for samples digested a few seconds after the salt jump and for samples digested 20 min after the salt jump. With DNase I, minor structural differences have been detected between samples obtained at different times during the reaction. However, even in this case our results indicate that many of the characteristic histone-DNA contacts within the core particle are made a few seconds after the initiation of the self-assembly reaction. Furthermore, core particles have been labeled with the fluorescent reagent N-(1-pyrenyl)maleimide (NPM), which was previously used as a sensitive probe for nucleosome conformation. Extensive DNase I or trypsin digestion of NPM-labeled core particles in 0.2 M NaCl does not produce significant changes in excimer fluorescence. This allows us to conclude that the covalent continuity of DNA is not required for the maintenance of the folded conformation of the core particle and that the trypsin-resistant domains of core histones play a fundamental role in the stabilization of this structure.     

The structure of sub-nucleosomal particles. The octameric (H3/H4)4--125-base-pair-DNA complex

Chicken erythrocyte chromatin was depleted of histones H1, H5, H2A and H2B. The resulting (H3/H4)-containing chromatin was digested with micrococcal nuclease to yield monomer, dimer, trimer etc. units, irregularly spaced on the DNA, with even-number multimers being more prominent. Sucrose density gradient centrifugation separated monomers and dimers (7.7 S and 10.5 S). Sodium dodecyl sulphate gel electrophoresis and cross-linking indicated: the monomer contains 50-base-pair (bp), 60-bp and 70-bp DNA and the dimer 125-bp DNA; the monomer contains a tetramer and the dimer an octamer of H3 and H4. Partial association of monomer units to dimers inhibits structural studies of monomers. The internal structure of the dimer, i.e. and (H3/H4)4-125-bp-DNA particle, was studied using circular dichroism, thermal denaturation and nuclease digestion. Both micrococcal nuclease and DNase I digestion indicate that, unlike core particles, accessible sites occur in the centre of the particle and it is concluded that the (H3/H4)4-125-bp-DNA particle is not a 'pseudo-core particle' in which the 'extra' H3 and H4 replace H2A and H2B. It is proposed that the octamer particle is formed by the sliding together of two 'monomer' units, each containing the (H3/H4)2 tetramer and 70 bp of DNA. Excision of this dimer unit with micrococcal nuclease results in the loss of 10 readily digestible base pairs at each end, leaving 125 bp.     

Histones H2a, H2b, H3, and H4 form a tetrameric complex in solutions of high salt.

In 2 M NaCl, histones H2b, H2a, H3, and H4 form a heterotypic tetrameric complex made up of one chain of each histone. This complex has been analyzed by hydrodynamic techniques. It is indistinguishable from histones in chromatin by its resistance to trypsin, pattern of reactivity with 125I. and ability to form specific crosslinked products after treatment with formaldehyde. It is proposed that this complex is responsible for protecting the small DNA fragments produced by exhausting nuclease digestion of nuclei and that on the average two of these complexes protect the larger 180-200 base pair unit produced by partial treatment of nuclei with nuclease.     

Contribution of histones H2A and H2B to the folding of nucleosomal DNA

We have studied the structural properties of nucleosomal particles deficient in histones H2A and H2B produced by modification of histone amino groups with dimethylmaleic anhydride [Jordano, J., Montero, F., & Palacián, E. (1984) Biochemistry (preceding paper in this issue)]. Digestion with DNase I of residual particles containing only 15% of the original H2A . H2B complement produces only discrete DNA fragments no longer than 70 nucleotides. As compared with the original nucleosomes, thermal denaturation of the residual particles shows a decrease from 140 to about 90 in the number of nucleotide base pairs per particle that melt at the highest temperature transition as well as a drop in the temperature of this transition. Circular dichroism spectra of the residual particles give ellipticity values around 275 nm, much higher than those corresponding to the control nucleosomes, which appears to indicate a loss in the compact DNA tertiary structure. When regeneration of the modified amino groups of the residual particles takes place in the presence of the complementary fraction containing histones H2A and H2B, but not in its absence, nucleosomal particles with the structural properties of the original nucleosomes are reconstituted. Therefore, the structural change observed in the residual particles can be assigned to the lack of histones H2A and H2B and not to the modified amino groups of the histones present in the residual particles. The results are consistent with the stabilization by histones H2A and H2B of a DNA length of 50-70 base pairs per nucleosome.     

Heterogeneity of chromatin subunits in vitro and location of histone H1.

Chromatin subunits ("nucleosomes") which were purified by sucrose gradient centrifugation of a staphylococcal nuclease digest of chromatin have been studied. We found that such a preparation contains nucleosomes of two discrete types which can be separated from each other by polyacrylamide gel electrophoresis. Nucleosome of the first type contains all five histones and a DNA segment of approximately 200 base pairs long, whereas nucleosome of the second type lacks histone H1 and its DNA segment is approximately 170 base pairs long, i.e., about 30 base pairs shorter than the DNA segment of the nucleosome of the first type. Purified dimer of the nucleosome also can be fractionated by gel electrophoresis into three discrete bands which correspond to dinucleosomes containing two molecules of histone H1, one and no H1. These and related findings strongly suggest that the H1 molecule is bound to a short (approximately 30 base pairs) terminal stretch of the nucleosomal DNA segment which can be removed by nuclease (possibly in the form of H1-DNA complex) without any significant disturbance of main structural features of the nucleosome.     

Remodeling of sperm chromatin after fertilization involves nucleosomes formed by sperm histones H2A and H2B and two CS histone variants

The composition of nucleosomes at an intermediate stage of male pronucleus formation was determined in sea urchins. Nucleosomes were isolated from zygotes harvested 10 min post-insemination, whole nucleoprotein particles were obtained from nucleus by nuclease digestion, and nucleosomes were subsequently purified by a sucrose gradient fractionation. The nucleosomes derived from male pronucleus were separated from those derived from female pronucleus by immunoadsorption to antibodies against sperm specific histones (anti-SpH) covalently bound to Sepharose 4B (anti-SpH-Sepharose). The immunoadsorbed nucleosomes were eluted, and the histones were analyzed by Western blots. Sperm histones (SpH) or alternatively, the histones from unfertilized eggs (CS histone variants), were identified with antibodies directed against each set of histones. It was found that these nucleosomes are organized by a core formed by sperm histones H2A and H2B combined with two major CS histone variants. Such a hybrid histone core interacts with DNA fragments of approximately 100 bp. It was also found that these atypical nucleosome cores are subsequently organized in a chromatin fiber that exhibits periodic nuclease hypersensitive sites determined by DNA fragments of 500 bp of DNA. It was found that these nucleoprotein particles were organized primarily by the hybrid nucleosomes described above. We postulate that this unique chromatin organization defines an intermediate stage of male chromatin remodeling after fertilization.     

Novel nucleosomal particles containing core histones and linker DNA but no histone H1

Eukaryotic chromosomal DNA is assembled into regularly spaced nucleosomes, which play a central role in gene regulation by determining accessibility of control regions. The nucleosome contains ∼147 bp of DNA wrapped ∼1.7 times around a central core histone octamer. The linker histone, H1, binds both to the nucleosome, sealing the DNA coils, and to the linker DNA between nucleosomes, directing chromatin folding. Micrococcal nuclease (MNase) digests the linker to yield the chromatosome, containing H1 and ∼160 bp, and then converts it to a core particle, containing ∼147 bp and no H1. Sequencing of nucleosomal DNA obtained after MNase digestion (MNase-seq) generates genome-wide nucleosome maps that are important for understanding gene regulation. We present an improved MNase-seq method involving simultaneous digestion with exonuclease III, which removes linker DNA. Remarkably, we discovered two novel intermediate particles containing 154 or 161 bp, corresponding to 7 bp protruding from one or both sides of the nucleosome core. These particles are detected in yeast lacking H1 and in H1-depleted mouse chromatin. They can be reconstituted in vitro using purified core histones and DNA. We propose that these ‘proto-chromatosomes’ are fundamental chromatin subunits, which include the H1 binding site and influence nucleosome spacing independently of H1.     

Analysis of the binding of high mobility group protein 17 to the nucleosome core particle by 1H NMR spectroscopy

The binding of high mobility group (HMG) protein 17 to the nucleosome core particle has been studied in D2O solution using 1H NMR at 500 MHz. Spectra were obtained for purified HMG 17, purified nucleosome core particles, and the reconstituted HMG 17-nucleosome core particle complex at 0.1, 0.2, 0.3, and 0.4 M NaCl. Subtraction of the core particle spectra from spectra of the core particle reconstituted with HMG 17 demonstrated those regions of HMG 17 which interact with the nucleosome at different ionic strengths; the resonance peaks of interacting groups are broadened due to their restricted mobility. At 0.1 M NaCl, the mobility of all the amino acid side chains of HMG 17 was restricted, indicating complete binding of HMG 17 to the much larger nucleosome core particle. At 0.2 M NaCl most of the amino acids were free with the exception of arginine and proline which are confined to or predominant in the basic central region of HMG 17. These amino acids were completely free only at 0.4 M NaCl. We conclude that the entire HMG 17 molecule interacts with the nucleosome core particle at physiological ionic strength. The acidic COOH-terminal region of HMG 17 is released from interaction with the core histones at an NaCl concentration between 0.1 and 0.2 M and so binds weakly at physiological ionic strength. The basic central region binds more strongly to the core particle DNA, being completely released only at much higher ionic strength, between 0.3 and 0.4 M NaCl.     

S(T)PXX motifs promote the interaction between the extended N-terminal tails of histone H2B with "linker" DNA.

The assembly of hybrid core particles onto long chicken DNA with histone H2B in the chicken histone octamer replaced with either wheat histone H2B(2) or sea urchin sperm histone H2B(1) or H2B(2) is described. All these histone H2B variants have N-terminal extensions of between 18 and 20 amino acids, although only those from sea urchin sperm have S(T)PXX motifs present. Whereas chicken histone octamers protected 167 base pairs (bp) (representing two full turns) of DNA against micrococcal nuclease digestion (Lindsey, G. G., Orgeig, S., Thompson, P., Davies, N., and Maeder, D. L. (1991) J. Mol. Biol. 218, 805-813), all the hybrid histone octamers protected an additional 17-bp DNA against nuclease digestion. This protection was more marked in the case of hybrid octamers containing sea urchin sperm histone H2B variants and similar to that described previously (Lindsey, G. G., Orgeig, S., Thompson, P., Davies, N., and Maeder, D. L. (1991) J. Mol. Biol. 218, 805-813) for hybrid histone octamers containing wheat histone H2A variants all of which also have S(T)PXX motifs present. Continued micrococcal nuclease digestion reduced the length of DNA associated with the core particle via 172-, 162-, and 152-bp intermediates until the 146-bp core particle was obtained. These DNA lengths were approximately 5 bp or half a helical turn longer than those reported previously for stripped chicken chromatin and for core particles containing histone octamers reconstituted using "normal" length histone H2B variants. This protection pattern was also found in stripped sea urchin sperm chromatin, demonstrating that the assembly/digestion methodology reflects the in vivo situation. The interaction between the N-terminal histone H2B extension and DNA of the "linker" region was confirmed by demonstrating that stripped sea urchin sperm chromatin precipitated between 120 and 500 mM NaCl in a manner analogous to unstripped chromatin whereas stripped chicken chromatin did not. Tryptic digestion to remove all the histone tails abolished this precipitation as well as the protection of DNA outside of the 167-bp core particle against nuclease digestion.     

Generation of a third-order folded structure for chromatin

A model for the initiation of the diffuse-condensed transition of chromatin induced by a change in the conformation of lysine-rich histones is proposed. Three levels of folded structures are discussed. The first-order folded structure refers to the structure of the repeat unit of chromatin, which is called the nucleosome. The nucleosome contains a nuclease resistant region in which 140 base pairs of DNA are wrapped around the surface of a histone aggregated of two copies each of the histones H2A, H2B, H3 and H4. This DNA-histone aggregate is called a core particle. The nuclease accessible region of the nucleosome is approximately 60 base pairs of DNA which link the core particle, hence the terminology “linker DNA.” The lysine-rich histones, (Hl, H5), which are more loosely bound than the core histones, are associated with the linker DNA. The second-order folded structure refers to the conformation of a polynucleosome. Based on neutron scattering and quasielastic light scattering studies the second-order folded structure is assumed to be an extended helix in solution with 5–7 nucleosome units per turn. The third-order folded structure is defined as that structure resulting from the first stage in the condensation process induced by a conformational change in the lysine-rich histones. Generation of the third-order folded structure in the proposed model is effected by an increased affinity of the lysine-rich histones for super-helical DNA in the core particles in adjacent turns of the second-order folded structure. Since the lysine-rich histones preferentially bind to A-T rich regions in DNA, the distribution of these regions would determine the third-order folded structure. The net effect of a non-random distribution of A-T rich regions as in the proposed model is the generation of a helix for the third-order folded structure. The assumption of a non-random distribution of A-T rich regions is indirectly supported by proflavine binding studies reported herein and by the existence of repetitive and non-repetitive DNA regions inferred from renaturation studies. One consequence of the proposed mechanism is that the majority of the A-T rich regions are in the interior of the third-order folded structure. Promoter sites of high A-T content would then be inaccessible to polymerases. The proposed model also suggests a role for spacer DNA in the genome. Higher order folded structures must also be present in the final state of condensed chromatin since the three orders of folded structures considered in this communication accounts for only 2% of that required in the diffuse-condensed transition.     

Structure of nucleosome core particles containing uH2A (A24)

We have purified uH2A (A24) and reconstituted it, in place of H2A, into high molecular weight nucleohistone containing the core histones and DNA. uH2A-containing core particles were then prepared by nuclease digestion and studies on these particles were carried out. We show that two uH2A molecules can be accommodated within a core particle. We also show that the presence of two uH2A molecules in a core particle does not alter significantly either the pattern or the rate of DNase I digestion as compared to both reconstituted and native core particles. Finally, we show that HMG proteins 14 and 17 can bind to uH2A-containing core particles. We conclude that uH2A has little influence on structure at the level of individual nucleosomes.     

Fragmentation of chromatin by endogenous nucleases, accumulation of the subnucleosomal fragments with high electrophoretic mobility]

Digestion of chromatin by endogenous nucleases to nucleosomes (140-160 base pairs of DNA) is accompanied by the accumulation of subnucleosomal DNP particles with high electrophoretic mobility (20-40 base pairs of DNA). All histones associate with the 140-160 base pairs fragment. The production of subnucleosomal DNP particles does not correlate with the degradation of histone H1 and the appearance of nucleosomes lacking histone H1. Degradation of the protein in this fragment is accompanied by the appearance of free DNA. The data obtained are in agreement with the hypothesis on the origin of subnucleosomes from the nucleosomal locus preferentially associated with the non-histone proteins and on the autonomy of these loci and of the loci associated with histone H1 in the nucleosome.     

DNase I site mapping and micrococcal nuclease digestion of pachytene chromatin reveal novel structural features

A comparison of the DNase I digestion products of the 32P-5'-end-labeled pachytene nucleosome core particles (containing histones H2A, TH2A, X2, H2B, TH2B, H3, and H4) and liver nucleosome core particles (containing somatic histones H2A, H2B, H3, and H4) revealed that the cleavage sites that are 30, 40, and 110 nucleotides away from the 5'-end are significantly more accessible in the pachytene core particles than in the liver core particles. These cleavage sites correspond to the region wherein H2B interacts with the nucleosome core DNA. These results, therefore, suggest that the histone-DNA interaction at these sites in the pachytene core particles is weaker, possibly because of the presence of the histone variant TH2B interacting at similar topological positions in the nucleosome core as that of its somatic counterpart H2B. Such a loosened structure may also be maintained even in the native pachytene chromatin since micrococcal nuclease digestion of pachytene nuclei resulted in a higher ratio of subnucleosomes (SN4 + SN7) to mononucleosomes than that observed in liver chromatin.     

The interaction of core histones with DNA: equilibrium binding studies.

The binding of core histone proteins to DNA, measured as a function of [NaCl[ is a reversible process. Dissociation and reassociation occurs in two stages. Between 0.7 and 1.2 M NaCl H2a H2b bind non-cooperatively as an equimolar complex with deltaGo = 1.6 Kcals/mole at 4 degree C and 1.0 M NaCl. Between 1.2 and 2.0 M NaCl H3 and H4 bind cooperatively as an equimolar complex with delta Go = 7.4 Kcal/mole at 4 degree C and 1.0 M NaCl. The proper binding of H2a and H2b requires the presence of bound H3 and H4. Nuclease digestion of the H3-H4 DNA produces a tetramer of H3-H4 bound to fragments of DNA 145, 125 and 104 base pairs long. Thus an H3-H4 tetramer can protect fragments of DNA as long as those found in complete core particles and must therefore span the nucleosome core particle.