Archaeal histones and nucleosomes

Polyphosphate binds to human von Willebrand factor in vivo and modulates its interaction with glycoprotein Ib

BACKGROUND

Polyphosphate, a phosphate polymer released by activated platelets, has recently been described as a potent modulator of blood coagulation and fibrinolysis. In blood plasma, polyphosphate binds to and alters the biological functions of factor XII, fibrin(ogen), thrombin and factor VII activating protease.

OBJECTIVES

The aim of the present study is to investigate whether polyphosphate also binds to von Willebrand factor (VWF) and alters some of its activities.

METHODS/RESULTS

When studying patients with type 1 von Willebrand disease (VWD) and their healthy relatives, we discovered a significant correlation between von Willebrand factor (VWF) and platelet polyphosphate levels. We have also found polyphosphate in preparations of VWF isolated from normal platelets and plasma. Surface plasmon resonance and electrophoretic mobility assays indicated that polyphosphate interacts with VWF in a dose- and time-dependent manner. Treatment of normal plasma with active exopolyphosphatase decreased the VWF ristocetin cofactor (VWF:RCo) activity, a functional measure of VWF binding to platelet glycoprotein receptor Ib. VWF collagen binding and multimerization were unaltered after polyphosphate depletion. Moreover, addition of polyphosphate increased the deficient VWF:RCo activity presented by plasma from patients with type 1 VWD.

CONCLUSIONS

Our results reveal that a new role is played by polyphosphate in hemostasis by its interaction with VWF, and suggest that this polymer may be effective in the treatment of some types of VWD.

Nanoarchaeal origin of histone H3?

NEQ288, one of two archaeal histones in Nanoarchaeum equitans, has a unique four-residue insertion that closely resembles an insertion in the eukaryotic histone H3 lineage. NEQ288 bound DNA but did not compact DNA in vitro in the absence of NEQ348, the second N. equitans archaeal histone. The properties of NEQ288 suggest an intermediate between the archaeal and H3 histone lineages and an evolutionary step toward the now-mandatory assembly of eukaryotic histones into heterodimers.

Archaeal chromatin proteins histone HMtB and Alba have lost DNA-binding ability in laboratory strains of Methanothermobacter thermautotrophicus

Alignments of the sequences of the all members of the archaeal histone and Alba1 families of chromatin proteins identified isoleucine residues, I19 in HMtB and I39 in MtAlba, in Methanothermobacter thermautotrophicus, at locations predicted to be directly involved in DNA binding. In all other HMfB family members, residue 19 is an arginine (R19), and either arginine or lysine is present in almost all other Alba1 family members at the structural site equivalent to I39 in MtAlba. Electrophoretic mobility shift assays revealed that recombinant HMtB and MtAlba do not bind DNA, but variants constructed with R19 and R39, respectively, bound DNA; and whereas MtAlba(I19) did not bind RNA, MtAlba(R19) bound both single stranded RNA and tRNA. Amplification and sequencing of MT0254 (encodes HMtB) and MT1483 (encodes MtAlba) from several Methanothermobacter thermautotrophicus lineages has revealed that HMtB and MtAlba had arginine residues at positions 19 and 39, respectively, in the original isolate and that spontaneous mutations must have occurred, and been fixed, in some laboratory lineages that now have HMtB(I19) and MtAlba(I39). The retention of these variants suggests some continuing functions and fusion of the HMtB(I19) sequence to HMtA2 resulted in a protein that folds to form a histone fold heterodimer that binds and compacts DNA. The loss of DNA binding by HMtB(I19) does not therefore prevent HMtB from participating in DNA interactions as one partner of an archaeal histone heterodimer.

Deletion of the archaeal histone in Methanosarcina mazei Gö1 results in reduced growth and genomic transcription

HMm is the only archaeal histone in Methanosarcina mazei Göl and recombinant HMm, synthesized by expression of MM1825 in Escherichia coli, has been purified and confirmed to have the DNA binding and compaction properties characteristic of an archaeal histone. Insertion of a puromycin resistance conferring cassette (pac) into MM1825 was not lethal but resulted in mutants (M. mazei MM1825::pac) that have impaired ability to grow on methanol and trimethylamine. Loss of HMm also resulted in increased sensitivity to UV light and decreased transcript levels for approximately 25% of all M. mazei genes. For most genes, the transcript decrease was 3- to 10-fold, but transcripts of MM483 (small heat-shock protein), MM1688 (trimethylamine:corrinoid methyl transferase) and MM3195 (transcription regulator), were reduced 100-, 100- and 25-fold, respectively, in M. mazei MM1825::pac cells. Transcripts of only five adjacent genes that appear to constitute an aromatic amino acid biosynthetic operon were elevated in M. mazei MM1825::pac cells. Complementary synthesis of HMm from a plasmid transformed into M. mazei MM1825::pac restored wild-type growth and transcript levels.

Formation of ε-Formyllysine on Silver-stained Proteins

Considerable effort is focused presently on the detection and comprehensive assignment of post-translational modifications of proteins. Obviously attention must be paid to the possibility of chemical modifications that may occur to protein samples during sample handling and manipulation prior to analysis by tandem mass spectrometry. This is of particular concern when a modification is isobaric with the mass differential in common with a known post-translational analog. Here we provide evidence that silver staining protocols that use formaldehyde can result in epsilon-formylation of lysine residues. This modification is in fact isobaric with the important product of methyltransferases, epsilon,epsilon-dimethyllysine. Without exercising proper caution the analysis of silver-stained protein samples by mass spectrometry looking for dimethylation of lysine will yield a significant number of misassigned sites of modification. High accuracy measurements of the mass of the precursor ions and their fragments are required to eliminate this uncertainty. The occurrence of dimethylation of the epsilon-amino function of lysine residues has been reported often in histones. For histone samples excised from silver-stained gels, we found that most sites initially assigned to be dimethylated by automatic search engines under standard search parameters (100 ppm error tolerance) are actually in fact formylated. Caution must be exercised when data obtained from instruments unable to perform high accuracy mass measurements (better than 5 ppm) are to be interpreted.

Histones in crenarchaea

Archaeal histone-encoding genes have been identified in marine Crenarchaea. The protein encoded by a representative of these genes, synthesized in vitro and expressed in Escherichia coli, binds DNA and forms complexes with properties typical of an archaeal histone. The discovery of histones in Crenarchaea supports the argument that histones evolved before the divergence of Archaea and Eukarya.

A novel nuclease-ATPase (Nar71) from archaea is part of a proposed thermophilic DNA repair system

We have identified a novel structure-specific nuclease in highly fractionated extracts of the thermophilic archaeon Methanothermobacter thermautotrophicus (Mth). The 71 kDa protein product of open reading frame mth1090 is a nuclease with ATPase activity, which we call Nar71 (Nuclease-ATPase in Repair, 71 kDa). The nar71 gene is located in a gene neighbourhood proposed by genomics to encode a novel DNA repair system conserved in thermophiles. The biochemical characterization of Nar71 presented here is the first analysis from within this neighbourhood, and it supports the insight from genomics. Nuclease activity of Nar71 is specific for 3' flaps and flayed duplexes, targeting single-stranded DNA (ssDNA) regions. This activity requires Mg2+ or Mn2+ and is greatly reduced in ATP. In ATP, Nar71 displaces ssDNA, also with high specificity for 3' flap and flayed duplex DNA. Strand displacement is weak compared with nuclease activity, but in ATPS it is abolished, suggesting that Nar71 couples ATP hydrolysis to DNA strand separation. ATPase assays confirmed that Nar71 is stimulated by ssDNA, though not double-stranded DNA. Mutation of Lys-117 in Nar71 abolished ATPase and nuclease activity, and we describe a separation-of-function mutant (K68A) that has lost ATPase activity but retains nuclease activity. A model of possible Nar71 function in DNA repair is presented.

Transcription by an archaeal RNA polymerase is slowed but not blocked by an archaeal nucleosome

Archaeal RNA polymerases (RNAPs) are closely related to eukaryotic RNAPs, and in Euryarchaea, genomic DNA is wrapped and compacted by histones into archaeal nucleosomes. In eukaryotes, transcription of DNA bound into nucleosomes is facilitated by histone tail modifications and chromatin remodeling complexes, but archaeal histones do not have histone tails and archaeal genome sequences provide no evidence for archaeal homologs of eukaryotic chromatin remodeling complexes. We have therefore investigated the ability of an archaeal RNAP, purified from Methanothermobacter thermautotrophicus, to transcribe DNA bound into an archaeal nucleosome by HMtA2, an archaeal histone from M. thermautotrophicus. To do so, we constructed a template that allows transcript elongation to be separated from transcription initiation, on which archaeal nucleosome assembly is positioned downstream from the site of transcription initiation. At 58 degrees C, in the absence of an archaeal nucleosome, M. thermautotrophicus RNAP transcribed this template DNA at a rate of approximately 20 nucleotides per second. With an archaeal nucleosome present, transcript elongation was slowed but not blocked, with transcription pausing at sites before and within the archaeal nucleosome. With additional HMtA2 binding, complexes were obtained that also incorporated the upstream regulatory region. This inhibited transcription presumably by preventing archaeal TATA-box binding protein, general transcription factor TFB, and RNAP access and thus inhibiting transcription initiation.

The two faces of Alba: the evolutionary connection between proteins participating in chromatin structure and RNA metabolism

The Alba superfamily of chromosomal proteins appear to have originated as RNA-binding proteins and to have been recruited to chromosomes possibly only within the crenarchaeal lineage.

Background

There is considerable heterogeneity in the phyletic patterns of major chromosomal DNA-binding proteins in archaea. Alba is a well-characterized chromosomal protein from the crenarchaeal genus Sulfolobus. While Alba has been detected in most archaea and some eukaryotic taxa, its exact functions in these taxa are not clear. Here we use comparative genomics and sequence profile analysis to predict potential alternative functions of the Alba proteins.

Results

Using sequence-profile searches, we were able to unify the Alba proteins with RNase P/MRP subunit Rpp20/Pop7, human RNase P subunit Rpp25, and the ciliate Mdp2 protein, which is implicated in macronuclear development. The Alba superfamily contains two eukaryote-specific families and one archaeal family. We present different lines of evidence to show that both eukaryotic families perform functions related to RNA metabolism. Several members of one of the eukaryotic families, typified by Mdp2, are combined in the same polypeptide with RNA-binding RGG repeats. We also investigated the relationships of the unified Alba superfamily within the ancient RNA-binding IF3-C fold, and show that it is most closely related to other RNA-binding members of this fold, such as the YhbY and IF3-C superfamilies. Based on phyletic patterns and the principle of phylogenetic bracketing, we predict that at least some of the archaeal members may also possess a role in RNA metabolism.

Conclusions

The Alba superfamily proteins appear to have originated as RNA-binding proteins which formed various ribonucleoprotein complexes, probably including RNase P. It was recruited as a chromosomal protein possibly only within the crenarchaeal lineage. The evolutionary connections reported here suggest how a diversity of functions based on a common biochemical basis emerged in proteins of the Alba superfamily.

Comparative genomics of Archaea: how much have we learned in six years, and what's next?

Archaea comprise one of the three distinct domains of life (with bacteria and eukaryotes). With 16 complete archaeal genomes sequenced to date, comparative genomics has revealed a conserved core of 313 genes that are represented in all sequenced archaeal genomes, plus a variable 'shell' that is prone to lineage-specific gene loss and horizontal gene exchange. The majority of archaeal genes have not been experimentally characterized, but novel functional pathways have been predicted.

Conserved eukaryotic histone-fold residues substituted into an archaeal histone increase DNA affinity but reduce complex flexibility

Although the archaeal and eukaryotic nucleosome core histones evolved from a common ancestor, conserved lysine residues are present at DNA-binding locations in all four eukaryotic histones that are not present in the archaeal histones. Introduction of lysine residues at the corresponding locations into an archaeal histone, HMfB, generated a variant with increased affinity for DNA that formed more compact complexes with DNA. However, these complexes no longer facilitated the circularization of short DNA molecules and had lost the flexibility to wrap DNA alternatively in either a negative or positive supercoil.

Structure based hyperthermostability of archaeal histone HPhA from Pyrococcus horikoshii

The histone protein HPhA from the hyperthermophilic archaeon Pyrococcus horikoshii, shows hyperthermostability, as required for optimal growth of the organism at 95 degrees C. The structure of recombinant P.horikoshii HPhA has been determined to 2.3A resolution by molecular replacement, and refined to R(work) and R(free) values of 20.7% and 27.3%, respectively. The HPhA monomer structure is characterized by the histone fold and assembles into a homodimer like other archaeal histones. There are four anions found in the dimer structure, giving rise to clues as to where DNA might bind. A detailed comparison of four known structures of archaeal histones, which evolve and exist under different temperatures, shows that the thermophilic archaeal histone HPhA has a larger hydrophobic contact area, an increased number of hydrogen bonds and a reduced solvent-accessible area. We also observe a unique network of tyrosine residues located at the crossover point of the two HPhA monomers, which locks them together and stabilizes the dimer. These factors together account for the increased thermal stability.

Archaeal histone tetramerization determines DNA affinity and the direction of DNA supercoiling

DNA binding and the topology of DNA have been determined in complexes formed by >20 archaeal histone variants and archaeal histone dimer fusions with residue replacements at sites responsible for histone fold dimer:dimer interactions. Almost all of these variants have decreased affinity for DNA. They have also lost the flexibility of the wild type archaeal histones to wrap DNA into a negative or positive supercoil depending on the salt environment; they wrap DNA into positive supercoils under all salt conditions. The histone folds of the archaeal histones, HMfA and HMfB, from Methanothermus fervidus are almost identical, but (HMfA)(2) and (HMfB)(2) homodimers assemble into tetramers with sequence-dependent differences in DNA affinity. By construction and mutagenesis of HMfA+HMfB and HMfB+HMfA histone dimer fusions, the structure formed at the histone dimer:dimer interface within an archaeal histone tetramer has been shown to determine this difference in DNA affinity. Therefore, by regulating the assembly of different archaeal histone dimers into tetramers that have different sequence affinities, the assembly of archaeal histone-DNA complexes could be localized and used to regulate gene expression.

Both DNA and histone fold sequences contribute to archaeal nucleosome stability

The roles and interdependence of DNA sequence and archaeal histone fold structure in determining archaeal nucleosome stability and positioning have been determined and quantitated. The presence of four tandem copies of TTTAAAGCCG in the polylinker region of pLITMUS28 resulted in a DNA molecule with increased affinity (DeltaDeltaG of approximately 700 cal mol(-1)) for the archaeal histone HMfB relative to the polylinker sequence, and the dominant, quantitative contribution of the helical repeats of the dinucleotide TA to this increased affinity has been established. The rotational and translational positioning of archaeal nucleosomes assembled on the (TTTAAAGCCG)(4) sequence and on DNA molecules selectively incorporated into archaeal nucleosomes by HMfB have been determined. Alternating A/T- and G/C-rich regions were located where the minor and major grooves, respectively, sequentially faced the archaeal nucleosome core, and identical positioning results were obtained using HMfA, a closely related archaeal histone also from Methanothermus fervidus. However, HMfA did not have similarly high affinities for the HMfB-selected DNA molecules, and domain-swap experiments have shown that this difference in affinity is determined by residue differences in the C-terminal region of alpha-helix 3 of the histone fold, a region that is not expected to directly interact with DNA. Rather this region is thought to participate in forming the histone dimer:dimer interface at the center of an archaeal nucleosome histone tetramer core. If differences in this interface do result in archaeal histone cores with different sequence preferences, then the assembly of alternative archaeal nucleosome tetramer cores could provide an unanticipated and novel structural mechanism to regulate gene expression.