Laser-induced crosslinking of histones to DNA in chromatin and core particles: implications in studying histone-DNA interactions.

UV laser irradiation has been used to covalently crosslink histones to DNA in nuclei, chromatin and core particles and the presence of the different histone species in the covalently linked material was detected immunochemically. When nuclei were irradiated and then trypsinized to cleave the N- and C- terminal histone tails, no histones have been found covalently linked to DNA. This finding shows that UV laser-induced crosslinking of histones to DNA is accomplished via the non-structured domains only. This unexpected way of crosslinking operated in chromatin, H1-depleted chromatin and core particles, i.e. independently of the chromatin structure. The efficiency of crosslinking, however, showed such a dependence: whilst the yield of crosslinks was similar in total and H1-depleted chromatin, in core particles the efficiency was 3-4 times lower for H2A, H2B and H4 and 10-12 times lower for H3. The decreased crosslinking efficiency, especially dramatic in the case of H3, is attributed to a reduced number of binding sites, and, respectively, is considered as a direct evidence for interaction of nonstructured tails of core histones with linker DNA.     

Primary organization of nucleosomes containing all five histories and DNA 175 and 165 base-pairs long

The sequential arrangement of histones along DNA in nucleosomes containing all five histones and DNA about 165 and 175 base-pairs in length has been determined. The data provide evidence that core histones (H2A, H2B, H3 and H4) are arranged in nucleosomes and nucleosome core particles in a largely similar way with the following differences. (1) On nucleosomal DNA about 175 basepairs long core histones are probably shifted by 20 nucleotides on one DNA strand and by 10 nucleotides on the complementary DNA strand from the 5′ end. On nucleosomal DNA 165 base-pairs long, histones appear to be shifted by 10 nucleotides from the 5′ end of DNA on both the DNA strands. (2) Histone H3 is extended beyond core DNA and is bound to the 3′ end of DNA about 175 nucleotides long. Thus, core histones span the whole length of nucleosomal DNA. (3) Histone H2A seems to be absent from the central region of nucleosomal DNA. These results indicate that during the preparation of core particles, some rearrangement of histones or some of their regions occurs.Histone H1 has been shown to be bound mainly to the ends of nucleosomal DNA and, along the whole DNA length, to the gap regions that are free of core histones.     

Localization of testis-variant histones in rat testis chromatin.

Nucleosome core particles and oligonucleosomes were isolated by digesting rat testis nuclei with micrococcal nuclease to 20% acid-solubility, followed by fractionation of the digest on a Bio-Gel A-5m column. The core particles thus isolated were characterized on the basis of their DNA length of 151 +/- 5 base-pairs and sedimentation coefficient of 11.4S. Analysis of the acid-soluble proteins of the core particles indicated that histones TH2B and X2 are constituents of the core particles, in addition to the somatic histones H2A, H2B, H3 and H4. The acid-soluble proteins of the oligonucleosomes comprised all the histones, including both the somatic (H1, H2A, H2B, H3, H4 and X2) and the testis-specific ones (TH1 and TH2B). It was also observed that histones TH1 and H1 are absent from the core particles and were readily extracted from the chromatin by 0.6 M-NaCl, which indicated that both of them are bound to the linker DNA.     

Condensation of DNA and chromatin by histones H1, H5 and protamines. The influence of a protein phosphorylation

A mutual displacement of the DNA crosslinking protiens, protamines, histones H1 and H5, is observed if cell nuclei are incubated in solutions containing one of these species. While their competition is in accord with their specific positive charge, a displacement of the core histones does not occur. Crosslinking proteins give rise to the formation of macrocomplexes from DNA and core particles, respectively which in the present study are investigated by stray-light and centrifugation methods. It is shown than the reduction of electrostatic affinities, which in vivo is achieved by a protein phosphorylation, serves to enhance complex sizes, probably by permitting at thermodynamically controlled, ordered association of DNA segments.     

Primary organization of the nucleosome core particles sequential arrangement of histones along DNA

A high-resolution map for the arrangement of histones along DNA in the nucleosome core particles has been determined by a new sequencing procedure. The lysine groups of histones were crosslinked to partly depurinated DNA at neutral pH. One strand of DNA was split at the points of crosslinking, thus leaving the 5′-terminal DNA fragments bound to histones. The lengths of these crosslinked DNA fragments were measured to determine the position of histones on one strand of the core DNA from its 5′ end.The results demonstrate that histones are bound to regularly arranged, discrete DNA segments about six nucleotides long. These segments are separated by histone-free gaps about four nucleotides wide located at a distance of about 10n nucleotides from the 5′ end of DNA. The first 20 nucleotides from the 5′ ends of DNA seem to be free of histones. Histones appear to be arranged symmetrically and in a similar way on both DNA strands. Any one histone, being bound predominantly to discrete segments on one or other of the strands, can oscillate at the same time between the two strands across the major DNA groove. Two symmetrical models for the arrangement of two molecules of each core histone on linearized and folded DNA are proposed.     

Primary organization of nucleosomes. Interaction of non-histone high mobility group proteins 14 and 17 with nucleosomes, as revealed by DNA-protein crosslinking and immunoaffinity isolation

The binding sites for histones and high mobility group proteins (HMG) 14 and 17 have been located on DNA in the nucleosomal cores and H1/H5-containing nucleosomes. The nucleosomes were specifically associated with two molecules of the non-histone proteins HMG 14 and/or HMG 17 when followed by DNA-protein crosslinking and immunoaffinity isolation of the crosslinked HMG-DNA complexes. HMGs 14 and 17 were shown to be crosslinked in a similar manner to each core DNA strand at four sites: to both 3' and 5' DNA ends and also at distances of about 25 and 125 nucleotides from the 5' termini of the DNA. These sites are designated as HMG(143), (0), (25) and (125). The site HMG(125) is located at the place where no significant histone-DNA crosslinking was observed. The HMG(125) and HMG(25) sites lie opposite one another on the complementary DNA strands across the minor DNA groove and are placed, similarly to histones, on the inner side of the DNA superhelix in the nucleosome. The crosslinking of HMG 17 to the 3' ends of the DNA is much weaker than that of HMG 14. These data indicate that each of two molecules of HMG 14 and/or HMG 17 is bound to the double-stranded core DNA at two discrete sites: to the 3' and 5' ends of the DNA and at a distance of 20 to 25 base-pairs from each DNA terminus inside the nucleosome on a histone-free DNA region. Binding of HMG 14 or 17 does not induce any detectable rearrangement of histones on DNA and both HMGs seem to choose the same sites for attachment in nucleosomal cores and H1/H5-containing nucleosomes.     

Nucleosomes from normal and regenerating rat liver

Micrococcal-nuclease digestion of rat liver nuclei selectively released mononucleosomes associated with ADP-ribosylated [Caplan, Ord & Stocken (1978) Biochem. J.174, 475-483] histone H1. Two classes of mononucleosome were detected, those that leaked out during digestion and those that were subsequently released by 5mm-sodium phosphate buffer (pH6.8)/0.2mm-NaEDTA. The former, from which histone H1 had been dissociated, contained 140-base-pair-length DNA and core histones;the latter contained core particles and mononucleosomes with histone H1 and 200-base-pair-length DNA. When normal liver nuclei were phosphorylated with [gamma-(32)P]ATP, dissociated histone H1, which could be separated from core particles with Sephadex G-200, showed (32)P uptake. (32)P uptake into histones H2A and poly(ADP-ribosyl)ated H3 was appreciable in core particles, but was less evident in nucleosomes still containing histone H1. When [(3)H]-thymidine was given to partially hepatectomized rats in S-phase, 5-10min pulses in animals of over 300g body wt. showed the presence of high-specific-radioactivity DNA in released core particles and mononucleosomes compared with DNA retained in the nuclear pellets. Mononucleosomes from rat livers in S-phase with new, [(3)H]lysine-containing histones, had higher (32)P incorporation in histones H1 and their core histones, than for di- or tri-nucleosomes. Thermal-denaturation properties of control and phosphorylated mononucleosomes and core particles were very similar; removal of histone H1 and non-histone chromosomal proteins in 0.5m-NaCl markedly increased the proportion of DNA ;melting' below 70 degrees C.     

Neutron-scattering studies of accurately reconstituted nucleosome core particles and the effect of ionic strength on core particle structure

Chicken erythrocyte nucleosome core particles can be dissociated quantitatively into histones (H3, H4)2 bound to 146 base pairs of DNA, and 2(H2A, H2B). Reconstitution of core particles from the two components produces an 85% yield of particles which neutron scattering studies show to be accurate stoichiometrically and indistinguishable from native core particles: the radii of gyration of the shape, the protein components and the DNA components of the particles are 4.02 nm, 3.3 nm and 4.95 nm respectively. The largest distance and most probable distance which can be drawn in the particles are 11.5 nm and 4.3 nm respectively. The molecular weight of the particles is identical to that of control 'native' core particles. All of these values, within limits of error, are the same as known values for 'native' core particles. These experiments confirm the essential role of histones H3 and H4 in the initial organisation of core-particle structure, make possible the manufacture of perfectly pure and homogeneous core-particle preparations and allow the 100% incorporation of labelled or modified histones. Neutron scattering studies of core particles at high contrast (in D2O and H2O) have been carried out over a range of ionic strengths and pH. No change in structure is detected down to pH 5.5 in 20 mM NaCl or down to ionic strength 2.0 mM at pH 7.     

Structural organization of the meiotic prophase chromatin in the rat testis

Pachytene nuclei were isolated from rat testes by the unit gravity sedimentation technique and contained histone variants H1a, H1t, TH2A, TH2B, and X2 in addition to the somatic histones H1bde, H1c, H2A, H2B, H3, and H4. The basic organization of the pachytene chromatin namely the nucleosome repeat length and the accessibility to micrococcal nuclease, was similar to that of rat liver interphase chromatin. However, when digested by DNase I, the susceptibility of pachytene chromatin was 25% more than liver chromatin under identical conditions. Nucleosome core particles were isolated from both liver and pachytene nuclei and were characterized for their DNA length and integrity of the nucleoprotein on low ionic strength nucleoprotein gels. While liver core particles contained all the somatic histones H2A, H2B, H3, and H4, in the pachytene core particles, histone variants TH2A, X2, and TH2B had replaced nearly 60% of the respective somatic histones. A comparison of the circular dichroism spectra obtained for pachytene and liver core particles indicated that the pachytene core particles were less compact than the liver core particles. Studies on the thermal denaturation properties of the two types of core particles revealed that the fraction of the pachytene core DNA melting at the premelting temperature region of 55-60 degrees C was significantly higher than that of the liver core DNA.     

DNA folding by histones: the kinetics of chromatin core particle reassembly and the interaction of nucleosomes with histones.

The kinetics of the chromatin core particle reassembly reaction in solution were quantitatively studied under conditions such that nucleohistone aggregation did not occur. Core particles, salt-jumped rapidly by dilution from 2.5 m-NaCl (in which DNA and histones do not interact) to 0.6 m-NaCl (in which core particles are nearly intact), reassemble in two distinct time ranges. Approximately 75% of the DNA refolds into core particle-like structures “instantaneously” as measured by several physical and chemical techniques with dead times in the seconds to minutes time range. The remaining DNA refolds with relaxation times ranging from 250 minutes at 0 °C to 80 minutes at 37 °C; this slow effect cannot be attributed to sample heterogeneity. The fraction of slowly refolding DNA and the slow relaxation time are independent of the core particle concentration. Transient intermediates present during the slow phase of refolding were identified as free DNA and core particle-like structures containing excess histone. Mixing experiments with DNA, histones, and core particles showed that core particle-histone interactions are responsible for the slow kinetics of DNA refolding. Upon treatment of reassembling core particles with the protein crosslinking reagent, dimethylsuberimidate, the slow phase of the reassembly reaction was arrested and a 13 S particle containing DNA and two octamers of histone was isolated. Consistent with the nature of this kinetic intermediate, it is shown that in 0.6 m-NaCl, core particles co-operatively bind at least one additional equivalent of histones with high affinity in the form of excess octamers. Also, core particles continue to adsorb considerably more histones with a weaker association constant of the order 10⁵m^?1 (in units of octamers) to a maximum value of 12 ± 2 equivalents (octamers) per core particle. The sedimentation coefficient increases with the two-thirds power of the molecular weight of the complex, as it would in the case of clustered spheres.A reassembly mechanism consistent with the data is presented, and other simple mechanisms are excluded. In the proposed mechanism, core particles reassemble very rapidly and compete effectively with DNA for histones such that approximately one-third of the particles initially formed are complexed with an excess octamer of histones, and 25% of the total DNA remains uncomplexed. The amount of this unusual reaction intermediate decays slowly to an equilibrium value of about 10%, thereby leaving 9% of the total DNA uncomplexed. Approximate values are calculated for the free energies, rate constants, and two of the activation energies which characterize this migrating octamer mechanism. This mechanism provides a means whereby histone octamers can be temporarily stripped off DNA at a modest free energy cost, approximately 2.6 kcal per nucleosome. Also, the properties of excess histone adsorption by chromatin and octamer migration suggest an efficient mechanism, consistent with observations by others, for nucleosome assembly in vivo during replication.     

Specific folding and contraction of DNA by histones H3 and H4.

We demonstrate that the arginine-rich histones H3 and H4 can introduce torsional constraints on closed circular DNA with a concomitant compaction of the nucleic acid. SV40 DNA I complexed with H3 and H4 appears relaxed in electron micrographs and contains particles of 75 +/- 10 A in diameter along the DNA. SV40 DNA I is contracted 2.75 +/- 0.25 fold by all the four smaller histones and 2.6 +/- 0.4 fold by H3 and H4 alone. The arginine-rich histones can cause the topological equivalent of unwinding the DNA close to one Watson-Crick turn per particle formed. Spherical nucleoprotein complexes morphologically similar to isolated nu bodies or nucleosomes are obtained by association of H3 and H4 with 140 base pair length DNA isolated from chromatin core particles. These reconstituted particles sediment at 9.8S, as compared to 10.8S for native core particles, and contain a tetramer of the arginine-rich histones. None of these specific alterations in DNA structure is seen om complexing the slightly lysine rich-histones H2A and H2B to DNA. Our data provide further evidence indicating that the arginine-rich histones are the major determinants of the architecture of DNA within the chromatin core particle.     

Rearrangement of nucleosomal components by modification of histone amino groups. Structural role of lysine residues

Modification of nucleosomal particles from chicken erythrocytes with the reagents for protein amino groups acetic and dimethylmaleic anhydrides causes a rearrangement of nucleosomal components. Treatment with both reagents is accompanied by liberation of free DNA and formation of residual particles with anomalous histone composition. The residual particles obtained with acetic anhydride contain an excess of histones corresponding to the free DNA produced. In contrast, dimethylmaleic anhydride causes release of histones H1, H5, H2A and H2B and formation of residual particles deficient in these histones but containing an excess of H3 and H4 corresponding to the liberated DNA. Regeneration of the modified amino groups of nucleosomal preparations treated with dimethylmaleic anhydride is accompanied by reconstitution of nucleosomal particles with the sedimentation coefficient and composition of core histones of the original nucleosomes. This reconstitution does not occur when the released fraction containing histones H2A and H2B and free DNA is separated from the residual particles. The studied disassembly of nucleosomal particles obtained by specifically blocking lysine-DNA interactions with these reagents appears to indicate that lysine residues are essential for the binding of DNA to histones with formation of nucleosomal particles.     

The role of H2B histones from the sea urchin sperm in the formation of supranucleosome structures

The structural role of histone H2B from sea urchin sperm (H2Bsp) has been examined in experiments on reconstitution of chromatin from DNA and core histones taken in three variants: (1) four core histones from sea urchin sperm; (2) four core histones from calf thymus; (3) (H3, H4, H2A) from calf thymus and H2Bsp. It is shown that H2Bsp when present in reconstituted chromatin induces its aggregation. Fidelity of the reconstitution of nucleosomes has been tested using DNase I probe, one- and two-dimensional electrophoresis and electron microscopy. The reconstitutes that contain H2Bsp appear under electron microscope mainly as regular closely spaced large granules, about 450 A in diameter, which are very similar to the granules found in "native" sea urchin sperm chromatin. The reconstitutes formed by four core histones from calf thymus appear as randomly arranged particles, about 100 A in diameter. We conclude that histone H2Bsp participates in interactions between nucleosomes and is involved in the formation of the condensed supranucleosomal structure in sea urchin sperm chromatin.     

DNA-protein interactions in nucleosomes and in chromatin. Structural studies of chromatin stabilized by ultraviolet-light induced crosslinking.

Crosslinking induced by ultraviolet light irradiation at 254 nm has been utilized to investigate the structure of chromatin and isolated nucleosomes. The results presented here imply that the four core histones, as well as histone H1, have reactive groups within a bond length of the DNA bases. In nucleosomes depleted of H1, all of the core histones react similarly with the DNA and form crosslinks. In chromatin, the rate of crosslinking of all histones to DNA is essentially similar. Comparison of mononucleosomes, dinucleosomes and whole chromatin shows that the rate of crosslinking increases significantly with increasing number of connected nucleosomes. These differences in the rate of crosslinking are interpreted in terms of interactions between neighbouring nucleosomes on the chromatin fiber, which are absent in an isolated mononucleosome.     

Nucleosome reconstitution: effect of DNA length on nuclesome structure.

Core histones (H2A, H2B, H3, and H4) are reconstituted by salt gradient dialysis with DNA molecules ranging in length from 177 bp down to 50 bp. While reconstituted particles containing 125 bp are very similar to native particles, those particles containing a single piece of shorter DNA tend to aggregate. The aggregation depends on the ionic strength and DNA length. The DNA placement on the histone core is not random as determined by pancreatic DNase I digestions of particles containing 32P 5'-end-labeled DNA. Rather, it is found that all DNA molecules, up to 161 bp in length, reassociate with core histones in such a way as to produce defined patterns of DNase I cutting with respect to the 5' ends. Particles were made that contained two pieces of 65-bp DNA. These particles are very similar to native particles under most conditions but tended to dissociation results in the production of two half-nucleosomes (hemisones).     

Distribution of the core histones H2A.H2B.H3 and H4 during cell replication.

The distribution of newly synthesized core histones H2A, H2B, H3 and H4 relative to the DNA strand synthesized in the same generation has been examined in replicating Chinese Hamster ovary cells. Cells are grown for one generation in [14C]-lysine and thymidine, and then for one generation in [3H]-lysine and 5-bromodeoxyuridine (BrUdRib) and a further generation in unlabeled lysine and thymidine. This protocol produces equal amounts of unifilarly substituted and unsubstituted DNA. Monomer nucleosomes isolated from chromatin containing these two types of DNA can be distinguished by crosslinking with formaldehyde and banding to equilibrium in CsCl density gradients. The results indicate that the core histones are equally distributed between the two types of DNA. These findings are discussed in terms of current models for chromatin replication; they do not support any long term association of newly replicated histones with either the leading or lagging side of the replication fork.     

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.