Archaeal histones: structures, stability and DNA binding.

Structures, stability and DNA-binding properties have been established for archaeal histones from mesophiles, thermophiles and hyperthermophiles. Most archaeal histones are simply histone folds that are stabilized by dimer formation. Archaeal histones and the histone folds of the eukaryotic nucleosome core histones share a common ancestry and bind and wrap DNA similarly using conserved residues. The histone-fold residues that stabilize dimer-dimer interactions within an archaeal histone core contribute to determining archaeal histone-DNA affinity.

Molecular components of the archaeal nucleosome.

Here we describe the organization of the archaeal nucleosome, in which four archaeal histones are circumscribed by approximately 80 bp of DNA. Through a combination of sequence comparisons, 3D structural studies, site-directed mutagenesis and assays for DNA binding, we have assigned functions to most of the individual residues in the histone fold of the representative archaeal histone rHMfB. By SELEX selection, the sequences of DNA molecules that are most readily bound and wrapped by rHMfB into archaeal nucleosomes in vitro have been identified, and these define DNA structures that position archaeal nucleosome assembly.

Crystal structures of recombinant histones HMfA and HMfB from the hyperthermophilic archaeon Methanothermus fervidus.

The hyperthermophilic archaeon Methanothermus fervidus contains two small basic proteins, HMfA (68 amino acid residues) and HMfB (69 residues) that share a common ancestry with the eukaryal nucleosome core histones H2A, H2B, H3, and H4. HMfA and HMfB have sequences that differ at 11 locations, they have different structural stabilities, and the complexes that they form with DNA have different electrophoretic mobilities. Here, crystal structures are documented for recombinant (r) HMfA at a resolution of 1.55 A refined to a crystallographic R-value of 19.8 % (tetragonal form) and at 1.48 A refined to a R-value of 18.8 % (orthorhombic form), and for rHMfB at 1.9 A refined to a R-value of 18.0 %. The rHMfA and rHMfB monomers have structures that are just histone folds in which a long central alpha-helix (alpha2; 29 residues) is separated from shorter N-terminal (alpha1; 11 residues) and C-terminal (alpha3; 10 residues) alpha-helices by two loops (L1 and L2; both 6 residues). Within L1 and L2, three adjacent residues are in extended (beta) conformation. rHMfA and rHMfB assemble into homodimers, with the alpha2 helices anti-parallel aligned and crossing at an angle of close to 35 degrees, and with hydrogen bonds formed between the extended, parallel regions of L1 and L2 resulting in short beta-ladders. Dimerization creates a novel N-terminal structure that contains four proline residues, two from each monomer. As prolines are present at these positions in all archaeal histone sequences, this proline-tetrad structure is likely to be a common feature of all archaeal histone dimers. Almost all residues that participate in monomer-monomer interactions are conserved in HMfA and HMfB, consistent with the ability of these monomers to form both homodimers and (HMfA+HMfB) heterodimers. Differences in side-chain interactions that result from non-conservative residue differences in HMfA and HMfB are identified, and the structure of a (rHMfA)(2)-DNA complex is presented based on the structures documented here and modeled by homology to histone-DNA interactions in the eukaryal nucleosome.

Structure and functional relationships of archaeal and eukaryal histones and nucleosomes.

A decade after the discovery of histones in Archaea, there is now also a biochemical description of the archaeal nucleosome. A tetrameric core of archaeal histones is encircled by approximately 80 bp of DNA, and nuclease digestions indicate that adjacent archaeal nucleosomes exist in vivo compacting archaeal genomic DNA. Most Eukarya employ a similar structure to organize their chromosomal DNA, the eukaryal nucleosome, with a histone octamer and 146 bp of DNA. Here we compare the properties of both nucleosomes in terms of DNA packaging and the accessibility of the packaged DNA for transcription.

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 alpha-helices separated by two beta-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 (rMJ1647delta) 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 (rMJ1647delta)4. The presence of the C-terminal extension increased the thermostability of rMJ1647 when compared with rMJ1647delta 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.

Mutational analysis of archaeal histone-DNA interactions.

Site-specific mutagenesis of the hmfB gene cloned from the archaeon Methanothermus fervidus, followed by expression in Escherichia coli, has been used to generate approximately 90 recombinant (r) variants of the archaeal histone HMfB. The abilities of these variants to form stable archaeal nucleosome-containing complexes with linear pBR322 DNA, and with an 89 bp restriction fragment of this DNA have been determined. Variants that failed to form such complexes, based on negative gel-shift assays, had substitutions at the N terminus or within the alpha1, L1 and L2 regions of the rHMfB histone fold, at sites predicted to be homologous to eucaryal histone fold residues that contact the DNA in the eucaryal nucleosome. Variants that failed to give gel shifts were further assayed for their abilities to facilitate ligase-catalyzed circularization of a linear 88 bp DNA molecule, and to reduce the ellipticity of a DNA solution at 275 nm (theta(275)). Consistent with cooperative but independent sites of DNA binding, a combination of three residue substitutions, one each in alpha1, L1 and L2, was required to generate a rHMfB variant with no detectable DNA binding based on gel shift, circularization and theta(275) reduction assays.

The efficiency of Escherichia coli selenocysteine insertion is influenced by the immediate downstream nucleotide.

Selenocysteine (Sec) incorporation requires the TGA opal codon and a downstream Sec insertion sequence (SECIS), which can be partially randomized and cloned into M13 pIII fusion constructs for phage display. This combinatorial approach provides a convenient non-radioactive assay that couples phage production to opal suppression. Two SECIS libraries were prepared, with the immediate downstream nucleotide either randomized (TGAN) or fixed as thymidine (TGAT). The TGAN library resulted in a majority of clones with a downstream purine and selenium-independent phage production, implicating the endo-genous tryptophan-inserting opal suppression pathway. Although the addition of sodium selenite to the growth medium did not affect phage production, it did increase the level of Sec insertion, as shown by the chemical reactivity of the resulting phage. The TGAT phage library yielded clones with strictly selenium-dependent phage production and reactivity consistent with the presence of Sec. These clones were prone to spontaneous mutation upon further propagation, however, resulting in loss of the selenium-dependent phenotype. We conclude that the immediate downstream nucleotide determines whether the endogenous opal suppression pathway competes with co-translational Sec insertion.

Toxicity of platinum(II) amino acid (N,O) complexes parallels their binding to DNA as measured in a new solid phase assay involving a fluorescent HMG1 protein construct readout.

The compound [Pt(lysine)Cl2] (Kplatin) was previously identified in a study of platinum amino acid complexes as a potential antitumor drug candidate. The DNA binding properties, high mobility group (HMG)-domain protein affinity for the platinated DNA, and cytotoxicity against HeLa cells of Kplatin and three related (N,O) chelated platinum(II) amino acid complexes, [Pt(arginine)Cl2] (Rplatin), K[Pt(Nepsilon-acetyllysine)Cl2] (NacKplatin), and K[Pt(norleucine)Cl2] (Norplatin), are reported. The four complexes have identical PtCl2(N,O) coordination environments. A new solid phase screening methodology was devised in which platinated DNA probes are covalently attached to a nylon support and tested for their ability to bind a fluorescently labeled HMG-domain protein. The fluorescent HMG-domain protein was generated by expressing a fusion of the green fluorescent protein (GFP) with recombinant rat HMG1. Binding revealed by the solid phase method correlated well with the results of gel mobility shift and HeLa cytotoxicity assays. These results suggest that the net charge on the complex, rather than the nature of the side chain, is the most important factor underlying the DNA binding properties and toxicity of amino acid (N,O) chelated platinum complexes. This property explains why Kplatin was previously selected from the pool of platinum amino acid complexes based on the ability of its DNA adducts to bind HMG1.

Rapid fluorescence-based reporter-gene assays to evaluate the cytotoxicity and antitumor drug potential of platinum complexes.

BACKGROUND: The need for new platinum antitumor drugs is underscored by the usefulness of cisplatin and carboplatin in chemotherapy and the resistance of many tumors to these compounds. Combinatorial chemistry could aid in the search for cisplatin analogs if fast, high-throughput assays were available. Our goal was to develop rapid cell-based assays suitable for high-throughput screening that accurately predict the cytotoxicity of platinum complexes. We examined the effects of platinum complexes and other agents on reporter-gene expression in cancer cells. RESULTS: HeLa Tet-On cells with inducible enhanced green fluorescent protein (EGFP) were prepared. Cisplatin and other cis-disubstituted platinum complexes inhibited EGFP expression, with a strong positive correlation between EGFP inhibition and cytotoxicity. By contrast, trans-[Pt(NH(3))(2)Cl(2)], other trans-platinum complexes, methyl methanesulfonate or heat shock stimulated EGFP expression. Northern and nuclear run-on analyses revealed that the changes in EGFP expression were at the level of transcription. In another reporter-gene assay in Jurkat cells, cisplatin, but not trans-[Pt(NH(3))(2)Cl(2)] or K(2)[PtCl(4)], inhibited beta-lactamase expression, as measured by hydrolysis of the fluorescent substrate CCF2. CONCLUSIONS: The EGFP results indicate that cytotoxic stress enhances transcription from the inducible promoter, whereas compounds able to form the 1,2-intrastrand platinum-DNA cross-links repress transcription. Both fluorescence-based reporter-gene assays afford promising new approaches to platinum anticancer drug discovery.

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.

Thermodynamic stability of archaeal histones.

The temperature, salt, and pH dependencies of unfolding of four recombinant (r) archaeal histones (rHFoB from the mesophile Methanobacterium formicicum, and rHMfA, rHMfB, and rHPyA1 from the hyperthermophiles Methanothermus fervidus and Pyrococcus strain GB-3a) have been determined by circular dichroism spectroscopy (CD) and differential scanning calorimetry (DSC). The thermal unfolding of these proteins is > 90% reversible, with concentration-dependent apparent Tm values and asymmetric unfolding transitions that are fit well by a two-state unfolding model in which a histone dimer unfolds to two random coil monomers. rHPyA1 dimers are stable in the absence of salt, whereas rHMfA, rHMfB, and rHFoB dimers unfold at 20 degrees C and pH 2 in solutions containing < 200 mM, < 400 mM, and < 1.5 M KCl, respectively. rHMfA, rHMfB, and rHFoB also experience significant cold denaturation in low salt concentrations and at low pH. The midpoint of thermal unfolding of a 1 M protein solution (T degree value) and the temperature dependency of the free energy of unfolding have been established for each histone, and both parameters correlate with the growth temperature of the originating archaeon. The changes in heat capacity upon unfolding are similar for the four histones, indicating that enhanced thermostability is not obtained by altering the curvature of the stability curve. Rather, the stability curves for the histones from the hyperthermophiles are displaced vertically to higher energies and laterally to higher Tmax values relative to the stability curve for rHFoB. The maximal free energies of unfolding for rHFoB, rHMfA, rHMfB, and rHPyA1 are 7.2, 15.5, 14.6, and 17.2 kcal/mol at 32, 35, 40, and 44 degrees C, respectively. T degree values for rHFoB, rHMfA, rHMfB, and rHPyA1 are 75, 104, 113, and 114 degrees C, respectively, at pH 5 in 0.2 M KCl. Structural features within the conserved histone fold that might confer these stability differences are discussed.

NMR structure and comparison of the archaeal histone HFoB from the mesophile Methanobacterium formicicum with HMfB from the hyperthermophile Methanothermus fervidus.

The solution-state structure of the recombinant archaeal histone rHFoB, from the mesophile Methanobacterium formicicum, has been determined by two- and three-dimensional (3D) proton homonuclear correlated nuclear magnetic resonance (NMR) methods. On the basis of 951 nuclear Overhauser effect (NOE)-derived distance restraints, rHFoB monomers form the histone fold and assemble into symmetric (rHFoB)2 dimers that have a structure consistent with assembly into archaeal nucleosomes. rHFoB exhibits approximately 78% sequence homology with rHMfB from the hyperthermophile Methanothermus fervidus, and the results obtained demonstrate that these two proteins have very similar 3D structures, with a root-mean-square deviation for backbone atoms of 0.65 +/- 0.13 A2. (rHFoB)2 dimers however unfold at lower temperatures and require a higher salt environment for stability than (rHMfB)2 dimers, and comparing the structures, we predict that these differences result from unfavorable surface-located ionic interactions and a larger, more solvent-accessible cavity adjacent to residue G36 in the hydrophobic core of (rHFoB)2.

Archaeal histone stability, DNA binding, and transcription inhibition above 90 degrees C.

The DNA binding and compacting activities of the recombinant (r) archaeal histones rHMfA and rHMfB from Methanothermus fervidus, and rHPyA1 from Pyrococcus species GB-3a, synthesized in Escherichia coli, have been shown to be completely resistant to incubation for 4h at 95 degrees C in the presence of 1M KCl. Continued incubation of rHMfA and rHMfB at 95 degrees C resulted in a gradual loss of these activities, and rHMfA and rHMfB lost activity more rapidly at 95 degrees C when the salt environment was reduced to 200 mM K Cl. rHPyA1, in contrast, retained full activity even after a 60-h incubation at 95 degrees C in 1 M KCl, and reducing the salt concentration did not affect the heat resistance of rHPyA1. rHPya1-DNA complexes remained intact at 100 degrees C, and rHPyA1 bound to the template DNA in in vitro transcription reaction mixtures assembled using Pyrococcus furiosus components at 90 degrees C. Transcription in vitro from the P. furiosus gdh promoter was reduced by rHPyA1 binding, in a manner that was dependent on the histone-to-DNA ratio and on the topology of the DNA template. Transcription from circular templates was more sensitive to rHPyA1 binding than transcription from a linear template, consistent with rHPyA1 binding introducing physical barriers to transcription and causing changes in the topology of circular templates that also reduced transcription.

Diversity of prokaryotic chromosomal proteins and the origin of the nucleosome.

All cells employ architectural proteins to confine and organize their chromosomes, and to prevent the otherwise thermodynamically favored collapse of concentrated DNA into compact structures. To accomplish this, prokaryotes have evolved a variety of phylogenetically unrelated, small, basic, sequence-independent DNA-binding proteins that include histones in Euryarchaeota, and members of the HU family in many Bacteria. In contrast, virtually, all Eukarya employ histones, and recently a metabolism-based hypothesis proposed that the eukaryal nucleus originated from a hydrogen-consuming, histone-containing Archaeon. Histones may have prevailed during the evolution of the Eukarya because of their extended interactions with DNA and, as noted, the histone fold now exists not only in histones but also as a structural motif in eukaryal transcription factors.

Large scale preparation of positively supercoiled DNA using the archaeal histone HMf.

A technique to prepare relatively large quantities (>/=100 microg) of highly positively supercoiled DNA is reported. This uses a recombinant archaeal histone (rHMfB) to introduce toroidal supercoils, and an inexpensive chicken blood extract to relax unrestrained superhelical tension. Preparation of positively supercoiled pUC19 DNA molecules, >50% of which have linking number changes ranging from+8 to+17, is demonstrated. Advantages include the high degree of positive supercoiling that can be achieved, control over the extent of supercoiling, easy production of relatively large quantities of supercoiled DNA, and low cost.