Negative constrained DNA supercoiling in archaeal nucleosomes

Archaeal histones have significant sequence and structural similarity to their eukaryal counterparts. However, whereas DNA is wrapped in negatively constrained supercoils in eukaryal nucleosomes, it has been reported that DNA is positively supercoiled by archaeal nucleosomes. This was inferred from experiments performed at low temperature and low salt concentrations, conditions markedly different from those expected for many archaea in vivo. Here, we report that the archaeal histones HMf and HTz wrap DNA in negatively constrained supercoils in buffers containing potassium glutamate (K-Glu) above 300 mM, either at 37 degrees C or at 70 degrees C. This suggests that high salt concentrations allow an alternate archaeal nucleosome topology: a left-handed tetramer rather than the right-handed tetramer seen in low salt conditions. In contrast, the archaeal histone MkaH produces DNA negative supercoiling at all salt concentrations, suggesting that this duality of structure is not possible for this atypical protein, which is formed by the association of two histone folds in a single polypeptide. These results extend the already remarkable similarity between archaeal and eukaryal nucleosomes, as it has been recently shown that DNA can be wrapped into either positive or negative supercoils around the H3/H4 tetramer. Negative supercoiling could correspond to the predominant physiological mode of DNA supercoiling in archaeal nucleosomes.     

Histone stoichiometry and DNA circularization in archaeal nucleosomes.

Recombinant (r)HMfB (archaealhistone B fromMethanothermusfervidus) formed complexes with increasing stability with DNA molecules increasing in length from 52 to 100 bp, but not with a 39 bp molecule. By using125I-labeled rHMfB-YY (an rHMfB variant with I31Y and M35Y replacements) and32P-labeled 100 bp DNA, these complexes, designated archaeal nucleosomes, have been shown to contain an archaeal histone tetramer. Consistent with DNA bending and wrapping, addition of DNA ligase to archaeal nucleosomes assembled with 88 and 128 bp DNAs resulted in covalently-closed monomeric circular DNAs which, following histone removal, were positively supercoiled based on their electrophoretic mobilities in the presence of ethidium bromide before and after relaxation by calf thymus topoisomerase I. Ligase addition to mixtures of rHMfB with 53 or 30 bp DNA molecules also resulted in circular DNAs but these were circular dimers and trimers. These short DNA molecules apparently had to be ligated into longer linear multimers for assembly into archaeal nucleosomes and ligation into circles. rHMfB assembled into archaeal nucleosomes at lower histone to DNA ratios with the supercoiled, circular ligation product than with the original 88 bp linear version of this molecule. Archaeal histones are most similar to the globular histone fold region of eukaryal histone H4, and the results reported are consistent with archaeal nucleosomes resembling the structure formed by eukaryal histone (H3+H4)2tetramers.     

Archaeal Nucleosome Positioning by CTG Repeats

DNA shape recognition determines the preferred binding sites for sequence-independent DNA binding proteins, and here we document that archaeal histones assemble archaeal nucleosomes in vitro centered preferentially within (CTG)₆ and (CTG)₈ repeats, close to junctions with flanking mixed-sequence DNA. Archaeal nucleosomes were not positioned by (CTG)₄-, (CTG)₅-, or (CTG)₃AA(CTG)₃-containing DNA sequences. The features of CTG repeat-containing sequences that direct eucaryal nucleosome positioning may also be similarly recognized by archaeal histones.     

Archaeal histone selection of nucleosome positioning sequences and the procaryotic origin of histone-dependent genome evolution

Archaeal histones and the eucaryal (eucaryotic) nucleosome core histones have almost identical histone folds. Here, we show that DNA molecules selectively incorporated by rHMfB (recombinant archaeal histone B from Methanothermus fervidus) into archaeal nucleosomes from a mixture of approximately 10(14) random sequence molecules contain sequence motifs shown previously to direct eucaryal nucleosome positioning. The dinucleotides GC, AA (=TT) and TA are repeated at approximately 10 bp intervals, with the GC harmonic displaced approximately 5 bp from the AA and TA harmonics [(GCN(3)AA or TA)(n)]. AT and CG were not strongly selected, indicating that TA not equalAT and GC not equalCG in terms of facilitating archaeal nucleosome assembly. The selected molecules have affinities for rHMfB ranging from approximately 9 to 18-fold higher than the level of affinity of the starting population, and direct the positioned assembly of archaeal nucleosomes. Fourier-transform analyses have revealed that AA dinucleotides are much enriched at approximately 10. 1 bp intervals, the helical repeat of DNA wrapped around a nucleosome, in the genomes of Eucarya and the histone-containing Euryarchaeota, but not in the genomes of Bacteria and Crenarchaeota, procaryotes that do not have histones. Facilitating histone packaging of genomic DNA has apparently therefore imposed constraints on genome sequence evolution, and since archaeal histones have no structure in addition to the histone fold, these constraints must result predominantly from histone fold-DNA contacts. Based on the three-domain universal phylogeny, histones and histone-dependent genome sequence evolution most likely evolved after the bacterial-archaeal divergence but before the archaeal-eucaryal divergence, and were subsequently lost in the Crenarchaeota. However, with lateral gene transfer, the first histone fold could alternatively have evolved after the archaeal-eucaryal divergence, early in either the euryarchaeal or eucaryal lineages.     

MJ1647, an open reading frame in the genome of the hyperthermophile Methanococcus jannaschii, encodes a very thermostable archaeal histone with a C-terminal extension

All archaeal histones studied to date have similar lengths, 66 to 69 amino acid residues that form three α-helices separated by two β-strand loop regions which together constitute a histone fold. In contrast, the eukaryal nucleosome core histones are larger, 102 to 135 residues in length, with N-terminal and C-terminal extensions flanking the histone fold that participate in gene regulation and higher-order chromatin assembly. In the Methanococcus jannaschii genome, MJ1647 was annotated as an open reading frame predicted to encode an archaeal histone with an approximately 27-amino-acid C-terminal extension, and we here document the DNA binding and assembly properties and thermodynamic stability parameters of the recombinant product of MJ1647 synthesized in Escherichia coli with (rMJ1647) and without (rMJ1647Δ) the C-terminal extension. The presence of the C-terminal extension did not prevent homodimer formation or inhibit DNA binding, but the complexes formed by rMJ1647, presumably archaeal nucleosomes containing a (rMJ1647)₄ tetramer, were apparently less stable than those formed by (rMJ1647Δ)₄. The presence of the C-terminal extension increased the thermostability of rMJ1647 when compared with rMJ1647Δ in 0.2 M KCl at pH 4 but not in the absence of KCl at pH 1. Based on thermal unfolding transitions, rMJ1647 and rHAfB generated by expression of AF0337 cloned from the genome of the related hyperthermophile Archaeoglobus fulgidus in E. coli were found to have higher thermodynamic stabilities than all previously studied archaeal histones. Received: September 2, 1999 / Accepted: October 18, 1999     

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.     

Chemical acetylation, trypsinolysis and stability of nucleosomes

Gel electrophoretic analysis of the histone chemical acetylation in the nucleosome core particles with acetic andydride revealed availability of about 14 lysine residues of histone H2A, 15-21 of H2B, 8-11--H3 and 6-9--H4. Moderately lysine-rich histones H2A and H2B were found to be more susceptible to acetylation than arginine-rich H3 and H4. Chemical acetylation enhanced the rate of trypsin digestion in acetylated nucleosomes as evidenced by gel electrophoresis of histone fragments. A more pronounced trypsin digestion was evident at acetylation of only 3-5 histone amino groups per nucleosome. However, even heavily acetylated nucleosomes yielded in familiar trypsin limit digest pattern of histone fragments thus indicating persistence of histone octamer. Nucleosomes which were trace acetylated (up to 3-5 histone amino groups neutralized per nucleosome) and treated with trypsin to remove highly charged terminal histone regions revealed remarkable unfolding and partial dissociation when analyzed by gel electrophoresis. The same trace acetylated nucleosomes did not show such destabilization prior to trypsin digestion.     

ATP dependent histone phosphorylation and nucleosome assembly in a human cell free extract.

Physiologically spaced nucleosome formation in HeLa cell extracts is ATP dependent. ATP hydrolysis is required for chromatin assembly on both linear and covalently closed circular DNA. The link between the phosphorylation state of histones and nucleosome formation has been examined and we demonstrate that in the absence of histone phosphorylation no stable and regularly spaced nucleosomes are formed. Phosphorylated H3 stabilizes the nucleosome core; while phosphorylation of histone H2a is necessary to increase the linker length between nucleosomes from 0 to approximately 45 bp. Histone H1 alone, whether phosphorylated or unphosphorylated, does not increase the nucleosome repeat length in the absence of core histone phosphorylation. Phosphorylations of H1 and H3 correlate with condensation of chromatin. Maximum ATP hydrolysis which is necessary to increase the periodicity of nucleosomes from approximately 150 to approximately 185 bp, not only inhibits H1 and H3 phosphorylation but facilitates their dephosphorylation.     

Replication-independent nucleosome exchange is enhanced by local and specific acetylation of histone H4

We used a novel single-cell strategy to examine the fate of histones during G₂-phase. Consistent with previous results, we find that in G₂-phase, the majority of nuclear histones are assembled into chromatin, whereas a small fraction comprises an unassembled pool. Small increases in the amount of histones within the free pool affect the extent of exchange, suggesting that the free pool is in dynamic equilibrium with chromatin proteins. Unexpectedly, acetylated H4 is preferentially partitioned to the unassembled pool. Although an increase in global histone acetylation did not affect overall nucleosome dynamics, an H4 containing lysine to glutamine substitutions as mimics of acetylation significantly increased the rate of exchange, but did not affect the acetylation state of neighbouring nucleosomes. Interestingly, transcribed regions are particularly predisposed to exchange on incorporation of H4 acetylation mimics compared with surrounding regions. Our results support a model whereby histone acetylation on K8 and K16 specifically marks nucleosomes for eviction, with histones being rapidly deacetylated on reassembly.     

Archaeal nucleosome positioning sequence from Methanothermus fervidus.

DNA in Methanothermus fervidus, a hyperthermophilic archaeon, is constrained into archaeal nucleosomes in vivo by the archaeal histones HMfA and HMfB. Here, we document the translational and rotational positioning of archaeal nucleosome assembly in vitro by a sequence from the 7S RNA encoding region of the M. fervidus genome. The minor groove of the DNA at the center of the DNA sequence, protected from micrococcal nuclease digestion by incorporation into a positioned archaeal nucleosome, faces away from the archaeal histone core.     

Role of histone tyrosines in nucleosome formation and histone-histone interaction

We have studied the functional properties of iodinated histones. Isolated, denatured histones were iodinated at trace levels and then renatured together with carrier histones and high molecular weight DNA to form nucleohistone. Nucleosomes were prepared from the reconstitute using micrococcal nuclease, and the relative representations of the individual iodinated tyrosines of the histones in the reconstituted nucleosomes were determined. Our principal findings are 1) that denatured histones can be iodinated at any tyrosine without interfering in subsequent nucleosome reconstitution and 2) that the resulting reconstituted nucleosomes nevertheless possess histone cores of altered stability, being either more or less stable depending on the particular tyrosine which is iodinated. We show that tyrosines 37, 40, and 42 of H2B are protected from iodination in intact core particles, as expected since these tyrosines lie within the H2B-H2A binding site. Yet iodination of these tyrosines in denatured H2B does not interfere with nucleosome assembly. However, the histone cores isolated from these reconstituted nucleosomes are of diminished stability as assayed by Sephadex column chromatography in 2 M salt. In contrast, iodination of tyrosines 83 and 121 of H2B, as well as iodination of the tyrosines of H2A, increases the stability of the histone octamer core. Iodination of H4 tyrosine 72 is without effect on histone octamer stability. Tyrosine iodination constitutes a profound amino acid alteration in the context of the absolute evolutionary conservation of most histone tyrosines. For example, all H2Bs sequenced to date, from fungi to mammals, possess tyrosines at positions 37, 40, and 42. Our results suggest that the immutability of these tyrosines reflects some sophisticated function of the nucleosome histone core beyond the assembly and mere maintenance of a compact structure.