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K Sandman

Publications and source records attributed to K Sandman.

At least 19 recordsLinked to original sources
PubMed2001

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.

Archaea↗
PubMed2000

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.

Amino Acid Sequence↗
PubMed2000

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.

Allosteric Site↗
PubMed2000

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.

Amino Acid Sequence↗
PubMed2000

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.

Amino Acid Sequence↗
PubMed1999

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.

Archaea↗
PubMed1998

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.

Amino Acid Sequence↗
PubMed1998

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.

Amino Acid Sequence↗
PubMed1998

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.

Amino Acid Sequence↗
PubMed1998

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.

Amino Acid Sequence↗
PubMed1996

NMR structure of HMfB from the hyperthermophile, Methanothermus fervidus, confirms that this archaeal protein is a histone.

The three-dimensional structure of the recombinant histone rHMfB from Methanothermus fervidus, an archaeon that grows optimally at 83 degrees C, has been determined by nuclear magnetic resonance methods. This is only the third structure of a protein from a hyperthermophilic organism (optimal growth at temperatures above 80 degrees C). Signal assignments were made using a combination of homonuclear-correlated, 15N-double resonance and 15N, 13C triple resonance NMR experiments. Long range dipolar interactions for the symmetric homodimer were identified from two-dimensional 13C-double half-filtered and three-dimensional 13C-filtered NMR data obtained for a heterolabeled-dimer. A family of 33 structures was calculated using DSPACE with a total of 609 NOE-derived interproton distance restraints, including 22 intraresidue, 192 sequential, 300 medium-range (two to five residues), 86 long-range intramolecular (more than five residues) and 112 intermolecular distance restraints. The monomer subunits consist of three alpha-helices, extending from residues Pro4 to Ala15 (helix I), Ser21 to Ala50 (helix II) and Lys56 to Lys68 (helix III), as well as two short segments of beta-strand comprised of residues Arg19 to Ser21 and Thr54 to Ile55. Helices I, II and III contain N-terminal capping boxes, and helices I and II contain C-terminal caps. The structure of the (rHMfB)2 dimer appears very similar to the dimer subunits within the histone core octamer of the chicken nucleosome. The presence of a canonical "histone fold" motif in rHMfB is consistent with the HMf family of archaeal histones and the eukaryal nucleosome core histones having evolved from a common ancestor. The (rHMfB)2 dimer contains several structural features that may impart thermal stability (or non-lability), including two novel hydrophobic "proline Ncaps", four interhelical hydrogen bonds and short N- and C-terminal disordered tails.

Amino Acid Sequence↗
PubMed1996

Crystallization and preliminary X-ray characterization of the Methanothermus fervidus histones HMfA and HMfB.

HMfA and HMfB are histone proteins from the thermophilic archaeon Methanothermus fervidus. They wrap DNA into nucleosome-like structures and appear to represent the basic core histone fold. HMfA was crystallized in space groups P4(2)2(1)2 and P2(1)2(1)2(1). HMfB crystallized in space group P2(1)2(1)2, while a selenomethionine-substituted variant, SeMet-HMfB, yielded crystals in C222(1). In all crystal forms HMfA, HMfB, or SeMet-HMfB may be present as homodimers.

Bacterial Proteins↗