Chicken erythrocyte polynucleosomes which are soluble at physiological ionic strength and contain linker histones are highly enriched in beta-globin gene sequences.

Mature chicken erythrocyte polynucleosomes which are soluble at physiological ionic strength are enriched in beta-globin DNA sequences. Vitellogenin chromatin, which is not expressed in this tissue, is found in aggregation prone, salt insoluble chromatin. There is a direct correlation between the size of soluble fragments and the degree of globin gene enrichment, with the largest fragments being most highly enriched. The highly globin enriched (about 50 fold) polynucleosomes contain significantly elevated levels of acetylated histones H4, H2A.Z, and H2B, and ubiquitinated (prefix "u") histones H2A and H2B (with a significant relative increase of uH2B over uH2A). These polynucleosomes were complexed with histones H1 and H5 but at a lower level than that found in unfractionated chromatin.     

Formation and characterization of soluble complexes of histone H1 with supercoiled DNA

We have analyzed the interaction of rat liver histone H1 with superhelical DNA. Depending on the ratio of H1 to DNA and the concentration of salt, two different types of complexes were found. Above a critical ratio of H1 to DNA, called the aggregation point, large aggregates are formed, which have a cable-like appearance in the electron microscope. Below the aggregation point, individual soluble complexes are formed, which are the subject of this study. With increasing ionic strength, the aggregation point is shifted towards lower ratios of H1 to DNA. In the soluble complexes, H1 appears to bind along superhelically intertwined DNA strands, forming a polymer. Partial digestion of the complexes with protease suggests protection of the N-terminal tail and the globular domain of H1. Similar soluble complexes were observed with various H1 fragments but not with the core histones. In the soluble complexes, similar regions of the H1 molecule are considered to be protected from cleavage by protease, as in chromatin. Therefore, these complexes appear to be a valuable model for the interaction of H1 in chromatin fibers.     

Interaction of histone H1 from sea urchin sperm with superhelical and relaxed DNA

Complexes of histone H1 from sea urchin sperm (H1S) and calf thymus (H1T) with superhelical DNA I and relaxed circular DNA II have been analyzed by analytical sedimentation. Similar to H1T, the highly basic and relatively arginine-rich histone H1S preferentially interacts with DNA I compared to DNA II under competition conditions. However, H1S induces a stronger aggregation of bothforms of DNA than H1T. Below 0.05 M NaCl, the soluble complexes formed by both histones have similar properties, but aggregation proceeds in a different manner: H1S induces a stronger aggregation of DNA II as compared to DNA I, whereas H1T fails to aggregate DNA I.The results are explained on the basis of differences in amino acid sequence and structure of the two histones and related to the special chromatin condensing ability of histone H1S.     

H1 histone exchange is limited to particular regions of chromatin that differ in aggregation properties

Chromatin fragments produced by mild nuclease digestion were chromatographed on Bio-Gel A-50m to give fractions ranging in size from 0.4 to 30 kilobase pair-DNA. The fragments that were larger than about 8-10 nucleosomes accounted for 80% of the chromatin, and the H1/core histone ratio was constant throughout these fractions. When adjusted to 150 mM NaCl, aggregates precipitated in each fraction, the largest fragments yielding 60% and the smallest 25%. In all of these fractions, after aggregation was induced by NaCl, the H1/core histone ratio in the aggregation-resistant chromatin (S) was 0.7 that in the aggregated chromatin (P). To show that the H1 deficiency and aggregation resistance were not produced by transfer of H1 from little fragments to bigger one, big aggregation-resistant fragments were incubated with little aggregation-prone fragments in 75 mM NaCl for 2 h, and readjusted to 150 mM. The little aggregation-prone fragments retained their aggregatibility after exposure to big aggregation-resistant fragments. By mixing [3H]P with [14C]S and vice versa, incubating at 75 mM NaCl for 2 h, and separating P from S with 150 mM NaCl, it was demonstrated that H1 histone did not equilibrate between S and P. Similarly, mixing combinations of radioactive and unlabeled, big and little, S and P fractions, and fractionating by size after 2 h or more incubation at 75 mM NaCl, it was shown that H1 equilibrates between different S fragments, and between different P fragments, but not between S and P. The distribution of H1 variants between S and P fractions was not correlated with the affinity of the variants for DNA. The order of binding affinities was H10 greater than H1ab = H1c, but the deficits of H1's in the aggregation-resistant S fractions were ranked H1ab greater than H1c greater than H10. It is suggested that chromatin is a mosaic of aggregation-resistant and aggregation-prone regions which differ in H1 content quantitatively and qualitatively.     

Fractionation of chromatin fragments on columns of Biogel A50-m at different salt concentrations

Nuclease fragmented chromatin was chromatographed on Biogel at various NaCl concentrations. The yield of eluted chromatin, and its H1/core histone ratio was minimal at 0.18 M NaCl where the ratio of H1 subtypes H1c/H1ab was maximal. Therefore, the eluted material was aggregation-resistant chromatin while aggregatable chromatin remained on the columns. Previous results were interpreted as H1 depletion of chromatin by ion-exchange properties of Biogel, but the primary phenomenon is now seen as a separation of classes of chromatin that differ in sensitivity to salt-induced aggregation. At very low salt concentrations, Biogel chromatography can be used without concern for H1 depletion.     

Studies on the role and mode of operation of the very-lysine-rich histone H1 (F1) in eukaryote chromatin. The properties of the N-terminal and C-terminal halves of histone H1.

Restricted chymotrypsin digestion of calf thymus H1 histone gives two fragments, residues 1--106 and 107--C-terminal. These were studied by proton magnetic resonance and circular dichroism. The N-terminal fragment exhibited some salt-induced structure in aqueous solution, but this did not parallel the globular structure of the intact H1 molecule. Comparison of circular dichroism results with helix predictions for this portion of the molecule suggests that the secondary structure may be the same in this fragment as it is in the corresponding region of the whole molecule. The C-terminal fragments show very little salt-induced structure. The N-terminal fragments binds to DNA very weakly, but the C-terminal fragment binds as strongly as the whole molecule. In the C-terminal fragment, about one quarter of the lysine residues are not bound to the DNA in water, but initial increase of salt concentration causes them to become bound. This increasing binding occurs under the same ionic conditions that cause chromatin condensation and condensation of H1 - DNA complexes, and it is suggested that there may be a connection between these phenomena.     

Interactions of H1 and H5 histones with polynucleotides of B- and Z-DNA conformations

Interactions of chicken H1 and H5 histones with poly(dA-dT), poly(dG-dC), and the Z-DNA structure brominated poly(dG-dC) were measured by a nitrocellulose filter binding assay and circular dichroism. At low protein:DNA ratios, both H1 and H5 bound more Z-DNA than B-DNA, and binding of Z-DNA was less sensitive to interference by an increase in ionic strength (to 600 mM NaCl). H5 histone bound a higher percentage of all three polynucleotides than did H1 and caused more profound CD spectral changes as well. For spectral studies, histones and DNA were mixed in 2.0 M NaCl and dialyzed stepwise to low ionic strength. Prepared in this way or by direct mixing in 150 mM NaCl, complexes made with right-handed poly(dG-dC) showed a deeply negative psi spectrum (deeper with H5 than with H1). Complexes of histone and Br-poly(dG-dC) showed a reduction in the characteristic Z-DNA spectral features, with H5 again having a greater effect. Complexes of poly(dA-dT) and H5, prepared by mixing them at a protein:DNA ratio of 0.5, displayed a distinctive spectrum that was not achieved with H1 even at higher protein:DNA ratios. It included a new negative band at 287 nm and a large positive band at 255 nm, giving the appearance of an inverted spectrum relative to spectra of various forms of B-DNA. These findings may reflect an ability of the different lysine-rich histones to cause varying conformational changes in the condensation of chromatin in DNA regions of highly biased base sequence.     

Aggregation of mono- and dinucleosomes into chromatin-like fibers

Three classes of chicken erythrocyte chromatin particles differing in their content of lysine-rich histones and/or spacer DNA have been studied in order to determine their ability to aggregate into complexes resembling those observed in native chromatin. The complexes have been obtained in the presence of MgCl₂ and NaCl and studied by electron microscopy. Mononucleosomes, containing spacer DNA and histones H1 and H5, give rise to thick (about 70 nm) ellipsoidal particles in the presence of 0.5 mM MgCl₂. These particles are disrupted by the addition of small amounts of NaCl (5–20 mM). On the other hand in 0.5 mM MgCl₂ dinucleosomes give rise to regular fibrous complexes of about 40 nm in diameter which are very similar to native chromatin fibers. These complexes are much more stable when NaCl is added. We conclude that for the stability of nucleosomal aggregates, similar to native chromatin fibers, a continuity of DNA structure is not required, but the presence of divalent cations, spacer DNA and lysine-rich histones is essential.     

Erythroid-specific gene chromatin has an altered association with linker histones.

The chromatin of several genes was assayed for sensitivity to DNAase I and for solubility as polynucleosomes in 0.15 M NaCl. The degree of solubility of chromatin fragments as polynucleosomes in 0.15 M NaCl correlates well with the sensitivity to DNAase I for several genes. Chromatin of repressed, housekeeping and erythroid-specific genes can be distinguished as distinct groups by the degree to which they display these properties. NaCl precipitation of chromatin fragments stripped and then reconstituted with varying quantities of H1 and H5 (linker) histones indicate that the polynucleosomes of erythroid-specific genes have altered interaction with these histones. Linker histones interacted with bulk chromatin and in the chromatin of the repressed ovalbumin and vitellogenin genes to form salt precipitable structures. Chromatin of erythroid-specific genes (histone H5 and beta-globin) as well as that of the histone H2A.F gene was resistant to linker histone induced precipitation.     

The ubiquitinated histone species are enriched in histone H1-depleted chromatin regions

Bovine thymus and trout testis chromatin were fractionated into regions which differed in their micrococcal nuclease accessibility and solubility properties, and the distribution of the ubiquitinated histone species among these chromatin regions was elucidated. Ubiquitinated (u) species of histones H2A and H2B were enriched in the nuclease-sensitive, low-ionic-strength, soluble fraction of both chromatins. These results indicate that the presence of ubiquitinated histones may alter nucleosome-nucleosome interactions and destabilize higher-order chromatin structures. Bovine thymus chromatin was separated into aggregation-resistant, salt-soluble and aggregation-prone, salt-insoluble chromatin fractions. The aggregation-resistant chromatin fraction depleted in H1 histones was enriched in uH2A and uH2B, with uH2B showing the greater enrichment. The chromatin fragments were also stripped and reconstituted with the H1 histones prior to fractionation. The results were the same as above: uH2A and uH2B were preferentially localized in the aggregation-resistant. H1-depleted chromatin fraction, suggesting that chromatin regions enriched in ubiquitinated histone species have a reduced affinity for the H1 histones. Thus, ubiquitinated histone species may be one of the contributing factors in the differential assembly of various parts of the genome.     

Co-existence of two different types of soluble histone complexes in nuclei of Xenopus laevis oocytes

The nuclear pool of soluble histones in Xenopus laevis oocytes is organized into two major types of acidic histone complexes separable by sucrose density gradient centrifugation. One type of complex sediments at 5 S (Mr approximately 120,000), is isoelectric at pH 4.6, and contains histones H3 and/or H4 tightly bound to one polypeptide of a pair of very acidic polypeptides, designated N1 and N2 (Kleinschmidt, J. A., and Franke, W. W. (1982) Cell 29, 799-809). This complex can be selectively immunoprecipitated by guinea pig antibodies against purified protein N1/N2. In contrast, a larger complex of 7 S contains four histones and nucleoplasmin (the purified protein exists as a pentamer of a polypeptide of Mr approximately 30,000), is isoelectric over the pH range of 5-7, and can be immunoprecipitated by nucleoplasmin antibodies. Its relative molecular weight of 130,000-170,000, as determined by gel filtration, sucrose density gradient centrifugation, and sodium dodecyl sulfate-polyacrylamide gel electrophoresis of the cross-linked complexes, excludes the association of a histone octamer with nucleoplasmin. In addition to histones H2A and H2B, two histones (designated H3 and H4) which are similar in their electrophoretic mobilities to histones H3 and H4 but have lower isoelectric pH values are enriched in immuno-precipitates obtained with nucleoplasmin antibodies. Cross-linking of complexes present in intact nuclei, using 1% formaldehyde at near-physiological ionic strength and pH, indicates the coexistence of these two soluble histone complexes in the living cell. In chromatin assembly experiments using SV 40 DNA, both histone fractions are able to transfer histones to DNA, resulting in an increase of DNA superhelicity and the formation of beaded nucleoprotein complexes of nucleosome-like morphology. The common principle governing both types of complexes, i.e. the association of one or two histone molecules with a karyophilic large acidic histone-binding protein is emphasized. We discuss the possible role of these complexes in storing histones utilized in chromatin assembly during early amphibian embryogenesis as well as the possible existence of similar complexes, albeit at lower concentrations, in somatic cells.     

The sites of deposition of newly synthesized histone.

The chromosomal fragments produced by nuclease digestion of freshly replicated chromatin migrate more rapidly relative to bulk chromatin when analyzed in nucleoprotein gels. The cause of the anomalous migration has been studied and the evidence indicates that rather than reflecting a shorter nucleosomal repeat in vivo that it may be a consequence of nucleosome sliding during the digestion itself. The distinct electrophoretic characteristics of nucleosomal material containing newly replicated DNA have enabled us to examine their histone composition by two dimensional electrophoresis. We find that nucleosomes containing new DNA also contain newly synthesized histones H3 and H4. In contrast more than 50% of newly synthesized H2A and H2B, and essentially all of new H1, are deposited at sites on the bulk chromatin distinct from that material containing newly replicated DNA. In addition we show that newly synthesized histones H3 and H4 are bound unusually weakly when they first become associated with the chromatin.     

An H1-like protein from the macronucleus of Euplotes eurystomus

An H1-like protein has been purified from the macronucleus (MAC) of the hypotrichous ciliated protozoan, Euplotes eurystomus. It is present in amounts comparable to the inner histones and is extracted by treatment with 5% perchloric acid or 0.65 M NaCl, but not by 0.35 M NaCl. Treatment of soluble MAC chromatin with the ionic exchange resin AG 50W-X2 in 80 mM NaCl removes MAC H1 and yields H1-depleted chromatin. Mac H1 is lysine-rich and deficient in acidic amino acids. The stoichiometry of the H1 protein is reduced in mononucleosome preparations, consistent with its postulated interaction with linker DNA regions. Thermal denaturation and circular dichroism studies reveal that H1-depleted chromatin contains a larger portion of destabilized DNA than control chromatin. The molecular weight of Euplotes MAC H1 is significantly smaller than most reported H1 proteins. Comparisons are made with extracts of macronuclei from other hypotrichous ciliated protozoa and published reports of other lower eukaryotes.     

Assembly of newly replicated chromatin.

Mild staphylococcal nuclease digestions under isotonic conditions release fragments of a 200 Å diameter fiber from nuclei of Drosophila melanogaster tissue culture cells. These soluble fragments have high sedimentation coefficients (30–100S) and show tightly packed nucleosomes in the electron microscope. Under the same conditions, newly replicated chromatin is released as more slowly sedimenting fragments (14S). Within 20 min after DNA replication, the nascent chromatin gradually matures into compact supranucleosomal structures which are indistinguishable from bulk chromatin on the isokinetic sucrose gradients.We have used this fractionation technique to examine the question of the fate and assembly of the new histones. After short pulses with either ³⁵S-methionine or ³H-lysine, the radioactive histones do not co-sediment with the bulk chromatin but appear instead in the fractions where the newly replicated DNA is found. Furthermore, the various nascent histones appear in different fractions on the gradient: histones H3 and H4 in 10–15S structures, histones H2A and H2B in 15–50S structures and histone H1 in 30–100S structures. These results, together with the analysis of pulse and pulse-chase experiments of both nascent DNA and histones, strongly suggest that histones H3 and H4 are deposited first on the nascent DNA (during or slightly after the DNA is replicated), histones H2A and H2B are deposited next (2–10 min later) and histone H1 is deposited last (10–20 min after DNA replication). A high turnover 20,000 dalton protein is also associated with the newly replicated chromatin.     

Structural transition in chromatin induced by ions in solution

Structural transition in chromatin was measured as a function of counter ions in solution (NaCl or MgCl(2)) and of histones bound on the DNA. The addition of counter ions to aqueous solutions of chromatin, partially dehistonized chromatin, and DNA caused a drastic reduction in viscosity and a significant increase in sedimentation coefficient. Transitions occurred primarily at about 2 x 10(-3) M NaCl and 1 x 10(-5) M MgCl(2) and are interpreted as a change in structure of chromatin induced by tight binding of cations (Na(+) or Mg(++)) to DNA, either free or bound by histones, and is an intrinsic property of DNA rather than of the type of histone bound. At a given ionic condition, removal of histone H1 from chromatin had only a minor effect on the hydrodynamic properties of chromatin while removal of other histones caused a drastic change in these properties. An increase in the sedimentation coefficient of DNA was observed also for protamine. DNA complexes wherein the bound protein contains only unordered coil rather than the alpha-helices found in histones.