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

Histone variants in archaea - An undiscovered country

Exchanging core histones in the nucleosome for paralogous variants can have important functional ramifications. Many of these variants, and their physiological roles, have been characterized in exquisite detail in model eukaryotes, including humans. In comparison, our knowledge of histone biology in archaea remains rudimentary. This is true in particular for our knowledge of histone variants. Many archaea encode several histone genes that differ in sequence, but do these paralogs make distinct, adaptive contributions to genome organization and regulation in a manner comparable to eukaryotes? Below, we review what we know about histone variants in archaea at the level of structure, regulation, and evolution. In all areas, our knowledge pales when compared to the wealth of insight that has been gathered for eukaryotes. Recent findings, however, provide tantalizing glimpses into a rich and largely undiscovered country that is at times familiar and eukaryote-like and at times strange and uniquely archaeal. We sketch a preliminary roadmap for further exploration of this country; an undertaking that may ultimately shed light not only on chromatin biology in archaea but also on the origin of histone-based chromatin in eukaryotes.

Deep conservation of histone variants in Thermococcales archaea

Histones are ubiquitous in eukaryotes where they assemble into nucleosomes, binding and wrapping DNA to form chromatin. One process to modify chromatin and regulate DNA accessibility is the replacement of histones in the nucleosome with paralogous variants. Histones are also present in archaea but whether and how histone variants contribute to the generation of different physiologically relevant chromatin states in these organisms remains largely unknown. Conservation of paralogs with distinct properties can provide prima facie evidence for defined functional roles. We recently revealed deep conservation of histone paralogs with different properties in the Methanobacteriales, but little is known experimentally about these histones. In contrast, the two histones of the model archaeon Thermococcus kodakarensis, HTkA and HTkB, have been examined in some depth, both in vitro and in vivo. HTkA and HTkB exhibit distinct DNA-binding behaviors and elicit unique transcriptional responses when deleted. Here, we consider the evolution of HTkA/B and their orthologs across the order Thermococcales. We find histones with signature HTkA- and HTkB-like properties to be present in almost all Thermococcales genomes. Phylogenetic analysis indicates the presence of one HTkA- and one HTkB-like histone in the ancestor of Thermococcales and long-term maintenance of these two paralogs throughout Thermococcales diversification. Our results support the notion that archaea and eukaryotes have convergently evolved histone variants that carry out distinct adaptive functions. Intriguingly, we also detect more highly diverged histone-fold proteins, related to those found in some bacteria, in several Thermococcales genomes. The functions of these bacteria-type histones remain unknown, but structural modeling suggests that they can form heterodimers with HTkA/B-like histones.

Archaea: The Final Frontier of Chromatin

The three domains of life employ various strategies to organize their genomes. Archaea utilize features similar to those found in both eukaryotic and bacterial chromatin to organize their DNA. In this review, we discuss the current state of research regarding the structure-function relationships of several archaeal chromatin proteins (histones, Alba, Cren7, and Sul7d). We address individual structures as well as inferred models for higher-order chromatin formation. Each protein introduces a unique phenotype to chromatin organization, and these structures are put into the context of in vivo and in vitro data. We close by discussing the present gaps in knowledge that are preventing further studies of the organization of archaeal chromatin, on both the organismal and domain level.

Chromatinization of Escherichia coli with archaeal histones

Nucleosomes restrict DNA accessibility throughout eukaryotic genomes, with repercussions for replication, transcription, and other DNA-templated processes. How this globally restrictive organization emerged during evolution remains poorly understood. Here, to better understand the challenges associated with establishing globally restrictive chromatin, we express histones in a naive system that has not evolved to deal with nucleosomal structures: Escherichia coli. We find that histone proteins from the archaeon Methanothermus fervidus assemble on the E. coli chromosome in vivo and protect DNA from micrococcal nuclease digestion, allowing us to map binding footprints genome-wide. We show that higher nucleosome occupancy at promoters is associated with lower transcript levels, consistent with local repressive effects. Surprisingly, however, this sudden enforced chromatinization has only mild repercussions for growth unless cells experience topological stress. Our results suggest that histones can become established as ubiquitous chromatin proteins without interfering critically with key DNA-templated processes.

New protein-DNA complexes in archaea: a small monomeric protein induces a sharp V-turn DNA structure

MC1, a monomeric nucleoid-associated protein (NAP), is structurally unrelated to other DNA-binding proteins. The protein participates in the genome organization of several Euryarchaea species through an atypical compaction mechanism. It is also involved in DNA transcription and cellular division through unknown mechanisms. We determined the 3D solution structure of a new DNA-protein complex formed by MC1 and a strongly distorted 15 base pairs DNA. While the protein just needs to adapt its conformation slightly, the DNA undergoes a dramatic curvature (the first two bend angles of 55° and 70°, respectively) and an impressive torsional stress (dihedral angle of 106°) due to several kinks upon binding of MC1 to its concave side. Thus, it adopts a V-turn structure. For longer DNAs, MC1 stabilizes multiple V-turn conformations in a flexible and dynamic manner. The existence of such V-turn conformations of the MC1-DNA complexes leads us to propose two binding modes of the protein, as a bender (primary binding mode) and as a wrapper (secondary binding mode). Moreover, it opens up new opportunities for studying and understanding the repair, replication and transcription molecular machineries of Archaea.

The Role of Archaeal Chromatin in Transcription

Genomic organization impacts accessibility and movement of information processing systems along DNA. DNA-bound proteins dynamically dictate gene expression and provide regulatory potential to tune transcription rates to match ever-changing environmental conditions. Archaeal genomes are typically small, circular, gene dense, and organized either by histone proteins that are homologous to their eukaryotic counterparts, or small basic proteins that function analogously to bacterial nucleoid proteins. We review here how archaeal genomes are organized and how such organization impacts archaeal gene expression, focusing on conserved DNA-binding proteins within the clade and the factors that are known to impact transcription initiation and elongation within protein-bound genomes.

Evidence of an Epigenetics System in Archaea

Changes in the phenotype of a cell or organism that are heritable but do not involve changes in DNA sequence are referred to as epigenetic. They occur primarily through the gain or loss of chemical modification of chromatin protein or DNA. Epigenetics is therefore a non-Mendelian process. The study of epigenetics in eukaryotes is expanding with advances in knowledge about the relationship between mechanism and phenotype and as a requirement for multicellularity and cancer. However, life also includes other groups or domains, notably the bacteria and archaea. The occurrence of epigenetics in these deep lineages is an emerging topic accompanied by controversy. In these non-eukaryotic organisms, epigenetics is critically important because it stimulates new evolutionary theory and refines perspective about biological action.

Archaeal DNA on the histone merry-go-round

How did the nucleosome, the fundamental building block of all eukaryotic chromatin, evolve? This central question has been impossible to address because the four core histones that make up the protein core of the nucleosome are so highly conserved in all eukaryotes. With the discovery of small, minimalist histone-like proteins in most known archaea, the likely origin of histones was identified. We recently determined the structure of an archaeal histone-DNA complex, revealing that archaeal DNA topology and protein-DNA interactions are astonishingly similar compared to the eukaryotic nucleosome. This was surprising since most archaeal histones form homodimers which consist only of the minimal histone fold and are devoid of histone tails and extensions. Unlike eukaryotic H2A-H2B and H3-H4 heterodimers that assemble into octameric particles wrapping ~ 150 bp DNA, archaeal histones form polymers around which DNA coils in a quasi-continuous superhelix. At any given point, this superhelix has the same geometry as nucleosomal DNA. This suggests that the architectural role of histones (i.e. the ability to bend DNA into a nucleosomal superhelix) was established before archaea and eukaryotes diverged, while the ability to form discrete particles, together with signaling functions of eukaryotic chromatin (i.e. epigenetic modifications) were secondary additions.

Structure of histone-based chromatin in Archaea

Small basic proteins present in most Archaea share a common ancestor with the eukaryotic core histones. We report the crystal structure of an archaeal histone-DNA complex. DNA wraps around an extended polymer, formed by archaeal histone homodimers, in a quasi-continuous superhelix with the same geometry as DNA in the eukaryotic nucleosome. Substitutions of a conserved glycine at the interface of adjacent protein layers destabilize archaeal chromatin, reduce growth rate, and impair transcription regulation, confirming the biological importance of the polymeric structure. Our data establish that the histone-based mechanism of DNA compaction predates the nucleosome, illuminating the origin of the nucleosome.

Structural Interface Forms and Their Involvement in Stabilization of Multidomain Proteins or Protein Complexes

The presented analysis concerns the inter-domain and inter-protein interface in protein complexes. We propose extending the traditional understanding of the protein domain as a function of local compactness with an additional criterion which refers to the presence of a well-defined hydrophobic core. Interface areas in selected homodimers vary with respect to their contribution to share as well as individual (domain-specific) hydrophobic cores. The basic definition of a protein domain, i.e., a structural unit characterized by tighter packing than its immediate environment, is extended in order to acknowledge the role of a structured hydrophobic core, which includes the interface area. The hydrophobic properties of interfaces vary depending on the status of interacting domains—In this context we can distinguish: (1) Shared hydrophobic cores (spanning the whole dimer); (2) Individual hydrophobic cores present in each monomer irrespective of whether the dimer contains a shared core. Analysis of interfaces in dystrophin and utrophin indicates the presence of an additional quasi-domain with a prominent hydrophobic core, consisting of fragments contributed by both monomers. In addition, we have also attempted to determine the relationship between the type of interface (as categorized above) and the biological function of each complex. This analysis is entirely based on the fuzzy oil drop model.

Transcriptional Repressor TrmBL2 from Thermococcus kodakarensis Forms Filamentous Nucleoprotein Structures and Competes with Histones for DNA Binding in a Salt- and DNA Supercoiling-dependent Manner

Architectural DNA proteins play important roles in the chromosomal DNA organization and global gene regulation in living cells. However, physiological functions of some DNA-binding proteins from archaea remain unclear. Recently, several abundant DNA-architectural proteins including histones, Alba, and TrmBL2 have been identified in model euryarchaeon Thermococcus kodakarensis. Although histones and Alba proteins have been previously characterized, the DNA binding properties of TrmBL2 and its interplay with the other major architectural proteins in the chromosomal DNA organization and gene transcription regulation remain largely unexplored. Here, we report single-DNA studies showing that at low ionic strength (<300 mM KCl), TrmBL2 binds to DNA largely in non-sequence-specific manner with positive cooperativity, resulting in formation of stiff nucleoprotein filamentous patches, whereas at high ionic strength (>300 mM KCl) TrmBL2 switches to more sequence-specific interaction, suggesting the presence of high affinity TrmBL2-filament nucleation sites. Furthermore, in vitro assays indicate the existence of DNA binding competition between TrmBL2 and archaeal histones B from T. kodakarensis, which can be strongly modulated by DNA supercoiling and ionic strength of surrounding solution. Overall, these results advance our understanding of TrmBL2 DNA binding properties and provide important insights into potential functions of architectural proteins in nucleoid organization and gene regulation in T. kodakarensis.

Chromatin structure and dynamics in hot environments: architectural proteins and DNA topoisomerases of thermophilic archaea

In all organisms of the three living domains (Bacteria, Archaea, Eucarya) chromosome-associated proteins play a key role in genome functional organization. They not only compact and shape the genome structure, but also regulate its dynamics, which is essential to allow complex genome functions. Elucidation of chromatin composition and regulation is a critical issue in biology, because of the intimate connection of chromatin with all the essential information processes (transcription, replication, recombination, and repair). Chromatin proteins include architectural proteins and DNA topoisomerases, which regulate genome structure and remodelling at two hierarchical levels. This review is focussed on architectural proteins and topoisomerases from hyperthermophilic Archaea. In these organisms, which live at high environmental temperature (>80 °C <113 °C), chromatin proteins and modulation of the DNA secondary structure are concerned with the problem of DNA stabilization against heat denaturation while maintaining its metabolic activity.

Chromatin organization, epigenetics and differentiation: an evolutionary perspective

Genome packaging is a universal phenomenon from prokaryotes to higher mammals. Genomic constituents and forces have however, travelled a long evolutionary route. Both DNA and protein elements constitute the genome and also aid in its dynamicity. With the evolution of organisms, these have experienced several structural and functional changes. These evolutionary changes were made to meet the challenging scenario of evolving organisms. This review discusses in detail the evolutionary perspective and functionality gain in the phenomena of genome organization and epigenetics.

Archaeal chromatin proteins

Archaea, along with Bacteria and Eukarya, are the three domains of life. In all living cells, chromatin proteins serve a crucial role in maintaining the integrity of the structure and function of the genome. An array of small, abundant and basic DNA-binding proteins, considered candidates for chromatin proteins, has been isolated from the Euryarchaeota and the Crenarchaeota, the two major phyla in Archaea. While most euryarchaea encode proteins resembling eukaryotic histones, crenarchaea appear to synthesize a number of unique DNA-binding proteins likely involved in chromosomal organization. Several of these proteins (e.g., archaeal histones, Sac10b homologs, Sul7d, Cren7, CC1, etc.) have been extensively studied. However, whether they are chromatin proteins and how they function in vivo remain to be fully understood. Future investigation of archaeal chromatin proteins will lead to a better understanding of chromosomal organization and gene expression in Archaea and provide valuable information on the evolution of DNA packaging in cellular life.

Transcriptional activation in the context of repression mediated by archaeal histones

Many archaea (including all the methanogens, nearly all euryarchaeotes, and some crenarchaeotes) use histones as components of the chromatin that compacts their genomes. The archaeal histones are homo- and heterodimers that pair on DNA to form tetrasomes (as the eukaryotic histones H3 and H4 do). The resulting DNA packaging is known to interfere with assembly of the archaeal transcription apparatus at promoters; the ability of transcriptional activation to function in repressive archaeal chromatin has not yet been explored in vitro. Using four of the Methanocaldococcus jannaschii (Mja) histones, we have examined activation of the model Mja rb2 transcription unit by the Mja transcriptional activator Ptr2 in this simplified-chromatin context. Using hydroxyl radical footprinting, we find that the Ptr2-specific rb2 upstream activating site is a preferred histone-localizing site that nucleates histone: DNA-binding radiating from the rb2 promoter. Nevertheless, Ptr2 competes effectively with histones for access to the rb2 promoter and most potently activates transcription in vitro at histone concentrations that extensively coat DNA and essentially silence basal transcription.

An improved method for large-scale preparation of negatively and positively supercoiled plasmid DNA

A rigorous understanding of the biological function of superhelical tension in cellular DNA requires the development of new tools and model systems for study. To this end, an ethidium bromide[#x02013]free method has been developed to prepare large quantities of either negatively or positively super-coiled plasmid DNA. The method is based upon the known effects of ionic strength on the direction of binding of DNA to an archaeal histone, rHMfB, with low and high salt concentrations leading to positive and negative DNA supercoiling, respectively. In addition to fully optimized conditions for large-scale (>500 microg) supercoiling reactions, the method is advantageous in that it avoids the use of mutagenic ethidium bromide, is applicable to chemically modified plasmid DNA substrates, and produces both positively and negatively supercoiled DNA using a single set of reagents.

The major architects of chromatin: architectural proteins in bacteria, archaea and eukaryotes

The genomic DNA of all organisms across the three kingdoms of life needs to be compacted and functionally organized. Key players in these processes are DNA supercoiling, macromolecular crowding and architectural proteins that shape DNA by binding to it. The architectural proteins in bacteria, archaea and eukaryotes generally do not exhibit sequence or structural conservation especially across kingdoms. Instead, we propose that they are functionally conserved. Most of these proteins can be classified according to their architectural mode of action: bending, wrapping or bridging DNA. In order for DNA transactions to occur within a compact chromatin context, genome organization cannot be static. Indeed chromosomes are subject to a whole range of remodeling mechanisms. In this review, we discuss the role of (i) DNA supercoiling, (ii) macromolecular crowding and (iii) architectural proteins in genome organization, as well as (iv) mechanisms used to remodel chromosome structure and to modulate genomic activity. We conclude that the underlying mechanisms that shape and remodel genomes are remarkably similar among bacteria, archaea and eukaryotes.

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.

A thermodynamic model for Nap1-histone interactions

The yeast nucleosome assembly protein 1 (yNap1) plays a role in chromatin maintenance by facilitating histone exchange as well as nucleosome assembly and disassembly. It has been suggested that yNap1 carries out these functions by regulating the concentration of free histones. Therefore, a quantitative understanding of yNap1-histone interactions also provides information on the thermodynamics of chromatin. We have developed quantitative methods to study the affinity of yNap1 for histones. We show that yNap1 binds H2A/H2B and H3/H4 histone complexes with low nm affinity, and that each yNap1 dimer binds two histone fold dimers. The yNap1 tails contribute synergistically to histone binding while the histone tails have a slightly repressive effect on binding. The (H3/H4)(2) tetramer binds DNA with higher affinity than it binds yNap1.

Unique fluorophores in the dimeric archaeal histones hMfB and hPyA1 reveal the impact of nonnative structure in a monomeric kinetic intermediate

Homodimeric archaeal histones and heterodimeric eukaryotic histones share a conserved structure but fold through different kinetic mechanisms, with a correlation between faster folding/association rates and the population of kinetic intermediates. Wild-type hMfB (from Methanothermus fervidus) has no intrinsic fluorophores; Met35, which is Tyr in hyperthermophilic archaeal histones such as hPyA1 (from Pyrococcus strain GB-3A), was mutated to Tyr and Trp. Two Tyr-to-Trp mutants of hPyA1 were also characterized. All fluorophores were introduced into the long, central alpha-helix of the histone fold. Far-UV circular dichroism (CD) indicated that the fluorophores did not significantly alter the helical content of the histones. The equilibrium unfolding transitions of the histone variants were two-state, reversible processes, with DeltaG degrees (H2O) values within 1 kcal/mol of the wild-type dimers. The hPyA1 Trp variants fold by two-state kinetic mechanisms like wild-type hPyA1, but with increased folding and unfolding rates, suggesting that the mutated residues (Tyr-32 and Tyr-36) contribute to transition state structure. Like wild-type hMfB, M35Y and M35W hMfB fold by a three-state mechanism, with a stopped-flow CD burst-phase monomeric intermediate. The M35 mutants populate monomeric intermediates with increased secondary structure and stability but exhibit decreased folding rates; this suggests that nonnative interactions occur from burial of the hydrophobic Tyr and Trp residues in this kinetic intermediate. These results implicate the long central helix as a key component of the structure in the kinetic monomeric intermediates of hMfB as well as the dimerization transition state in the folding of hPyA1.

Solution structure of inhibitor-free human metalloelastase (MMP-12) indicates an internal conformational adjustment

Macrophage metalloelastase or matrix metalloproteinase-12 (MMP-12) appears to exacerbate atherosclerosis, emphysema, aortic aneurysm, rheumatoid arthritis, and inflammatory bowel disease. An inactivating E219A mutation, validated by crystallography and NMR spectra, prevents autolysis of MMP-12 and allows us to determine its NMR structure without an inhibitor. The structural ensemble of the catalytic domain without an inhibitor is based on 2813 nuclear Overhauser effects (NOEs) and has an average RMSD to the mean structure of 0.25 A for the backbone and 0.61 A for all heavy atoms for residues Trp109-Gly263. Compared to crystal structures of MMP-12, helix B (hB) at the active site is unexpectedly more deeply recessed under the beta-sheet. This opens a pocket between hB and beta-strand IV in the active-site cleft. Both hB and an internal cavity are shifted toward beta-strand I, beta-strand III, and helix A on the back side of the protease. About 25 internal NOE contacts distinguish the inhibitor-free solution structure and indicate hB's greater depth and proximity to the sheet and helix A. Line broadening and multiplicity of amide proton NMR peaks from hB are consistent with hB undergoing a slow conformational exchange among subtly different environments. Inhibitor-binding-induced perturbations of the NMR spectra of MMP-1 and MMP-3 map to similar locations across MMP-12 and encompass the internal conformational adjustments. Evolutionary trace analysis suggests a functionally important network of residues that encompasses most of the locations adjusting in conformation, including 18 residues with NOE contacts unique to inhibitor-free MMP-12. The conformational change, sequence analysis, and inhibitor perturbations of NMR spectra agree on the network they identify between structural scaffold and the active site of MMPs.

Archaeal histones and the origin of the histone fold

Histone sequences have been identified in many archaeal genomes and in environmental samples, and they constitute a family of proteins that are structural homologs of the eukaryotic core histones. Most archaeal histones conform to the single histone-fold structural models that have been described, but a few histone variants exhibit short insertions, additional domains or fusions. Interpretation of these structural variations offers clues to the steps that might have occurred during the evolution and specialization of eukaryotic core histones.

Stabilization mechanism of the tryptophan synthase alpha-subunit from Thermus thermophilus HB8: X-ray crystallographic analysis and calorimetry

In order to elucidate the thermo-stabilization mechanism of the tryptophan synthase alpha-subunit from the extreme thermophile Thermus thermophilus HB8 (Tt-alpha-subunit), its crystal structure was determined and its stability was examined using DSC. The results were compared to those of other orthologs from mesophilic and hyperthermophilic organisms. The denaturation temperature of the Tt-alpha-subunit was higher than that of the alpha-subunit from S. typhimurium (St-alpha-subunit) but lower than that of the alpha-subunit from P. furiosus (Pf-alpha-subunit). Specific denaturation enthalpy and specific denaturation heat capacity values of the Tt-alpha-subunit were the lowest among the three proteins, suggesting that entropy effects are responsible for the stabilization of the Tt-alpha-subunit. Based on a structural comparison with the St-alpha-subunit, two deletions in loop regions, an increase in the number of ion pairs and a decrease in cavity volume seem to be responsible for the stabilization of the Tt-alpha-subunit. The results of structural comparison suggest that the native structure of the Tt-alpha-subunit is better adapted to an ideally stable structure than that of the St-alpha-subunit, but worse than that of the Pf-alpha-subunit. The results of calorimetry suggest that the residual structure of the Tt-alpha-subunit in the denatured state contributes to the stabilization.

Effect of polyamines on histone-induced DNA compaction of hyperthermophilic archaea

The effect of polyamines on histone-mediated DNA compaction was examined in vitro with archaeal histone HpkA from Pyrococcus kodakaraensis KOD1. An agarose gel mobility-shift experiment indicated that histone-bound DNA (compacted DNA) was further compacted by addition of a polyamine (putrescine, spermidine, or spermine) or its acetylated form (N-acetylputrescine, N1-acetylspermidine, N8-acetylspermidine, or N1-acetylspermine) when the mixture was incubated at above 75 degrees C. Spermine was most effective in compaction enhancement among all the polyamines tested. A high concentration of potassium ion (1.0 M) did not stabilize the compacted form of DNA even though double-stranded DNA was stably maintained against thermal denaturation at elevated temperatures under this condition. It appears likely that multivalent polyamines have a nucleosome maintenance function in hyperthermophilic archaea in high-temperature environments.

Posttranslational protein modification in Archaea

One of the first hurdles to be negotiated in the postgenomic era involves the description of the entire protein content of the cell, the proteome. Such efforts are presently complicated by the various posttranslational modifications that proteins can experience, including glycosylation, lipid attachment, phosphorylation, methylation, disulfide bond formation, and proteolytic cleavage. Whereas these and other posttranslational protein modifications have been well characterized in Eucarya and Bacteria, posttranslational modification in Archaea has received far less attention. Although archaeal proteins can undergo posttranslational modifications reminiscent of what their eucaryal and bacterial counterparts experience, examination of archaeal posttranslational modification often reveals aspects not previously observed in the other two domains of life. In some cases, posttranslational modification allows a protein to survive the extreme conditions often encountered by Archaea. The various posttranslational modifications experienced by archaeal proteins, the molecular steps leading to these modifications, and the role played by posttranslational modification in Archaea form the focus of this review.

Folding mechanism of the (H3-H4)2 histone tetramer of the core nucleosome

To further understand oligomeric protein assembly, the folding and unfolding kinetics of the H3-H4 histone tetramer have been examined. The tetramer is the central protein component of the core nucleosome, which is the basic unit of DNA compaction into chromatin in the eukaryotic nucleus. This report provides the first kinetic folding studies of a protein containing the histone fold dimerization motif, a motif observed in several protein-DNA complexes. Previous equilibrium unfolding studies have demonstrated that, under physiological conditions, there is a dynamic equilibrium between the H3-H4 dimer and tetramer species. This equilibrium is shifted predominantly toward the tetramer in the presence of the organic osmolyte trimethylamine-N-oxide (TMAO). Stopped-flow methods, monitoring intrinsic tyrosine fluorescence and far-UV circular dichroism, have been used to measure folding and unfolding kinetics as a function of guanidinium hydrochloride (GdnHCl) and monomer concentrations, in 0 and 1 M TMAO. The assignment of the kinetic phases was aided by the study of an obligate H3-H4 dimer, using the H3 mutant, C110E, which destabilizes the H3-H3' hydrophobic four-helix bundle tetramer interface. The proposed kinetic folding mechanism of the H3-H4 system is a sequential process. Unfolded H3 and H4 monomers associate in a burst phase reaction to form a dimeric intermediate that undergoes a further, first-order folding process to form the native dimer in the rate-limiting step of the folding pathway. H3-H4 dimers then rapidly associate with a rate constant of > or =10(7) M(-1)sec(-1) to establish a dynamic equilibrium between the fully assembled tetramer and folded H3-H4 dimers.

Stability and folding mechanism of mesophilic, thermophilic and hyperthermophilic archael histones: the importance of folding intermediates

The equilibrium stabilities to guanidinium chloride (GdmCl)-induced denaturation and kinetic folding mechanisms have been characterized for three archael histones: hFoB from the mesophile Methanobacterium formicicum; hMfB from the thermophile Methanothermus fervidus; and hPyA1 from the hyperthermophile Pyrococcus strain GB-3a. These histones are homodimers of 67 to 69 residues per monomer. The equilibrium unfolding transitions, as measured by far-UV circular dichroism (CD) are highly reversible, two-state processes. The mesophilic hFoB is very unstable and requires approximately 1 M trimethyl-amine-N-oxide (TMAO) to completely populate the native state. The thermophilic histones are more stable, with deltaG degrees (H2O) values of 14 and 16 kcal mol(-1) for hMfB and hPyA1, respectively. The kinetic folding of hFoB and hPyA1 are two-state processes, with no detectable transient kinetic intermediates. For hMfB, there is significant development of CD signal in the stopped-flow dead time, indicative of the formation of a monomeric intermediate, which then folds/associates in a single, second-order step to form the native dimer. While the equilibrium stability to chemical denaturation correlates very well with host growth temperature, there is no simple relationship between folding rates and stability for the archael histones. In the absence of denaturant, the log of the unfolding rates correlate with equilibrium stability. The folding/association of the moderately stable hMfB is the most rapid, with a rate constant in the absence of GdmCl of 3 x 10(6) M(-1) s(-1), compared to 9 x 10(5) M(-1) s(-1) for the more stable hPyA1. It appears that the formation of the hMfB burst-phase monomeric ensemble serves to enhance folding efficiency, rather than act as a kinetic trap. The folding mechanism of the archael histones is compared to the folding of other intertwined, segment-swapped, alpha-helical, DNA-binding dimers (ISSADD), including the eukaryotic heterodimeric histones, which fold more rapidly. The importance of monomeric and dimeric kinetic intermediates in accelerating ISSADD folding reactions is discussed.

Tandem histone folds in the structure of the N-terminal segment of the ras activator Son of Sevenless

The Ras activator Son of Sevenless (Sos) contains a Cdc25 homology domain, responsible for nucleotide exchange, as well as Dbl/Pleckstrin homology (DH/PH) domains. We have determined the crystal structure of the N-terminal segment of human Sos1 (residues 1-191) and show that it contains two tandem histone folds. While the N-terminal domain is monomeric in solution, its structure is surprisingly similar to that of histone dimers, with both subunits of the histone "dimer" being part of the same peptide chain. One histone fold corresponds to the region of Sos that is clearly similar in sequence to histones (residues 91-191), whereas the other is formed by residues in Sos (1-90) that are unrelated in sequence to histones. Residues that form a contiguous patch on the surface of the histone domain of Sos are conserved from C. elegans to humans, suggesting a potential role for this domain in protein-protein interactions.

Crystal structure of a DNA binding protein from the hyperthermophilic euryarchaeon Methanococcus jannaschii

The Sac10b family consists of a group of highly conserved DNA binding proteins from both the euryarchaeotal and the crenarchaeotal branches of Archaea. The proteins have been suggested to play an architectural role in the chromosomal organization in these organisms. Previous studies have mainly focused on the Sac10b proteins from the crenarchaeota. Here, we report the 2.0 A resolution crystal structure of Mja10b from the euryarchaeon Methanococcus jannaschii. The model of Mja10b has been refined to an R-factor of 20.9%. The crystal structure of an Mja10b monomer reveals an alpha/beta structure of four beta-strands and two alpha-helices, and Mja10b assembles into a dimer via an extensive hydrophobic interface. Mja10b has a similar topology to that of its crenarchaeota counterpart Sso10b (also known as Alba). Structural comparison between the two proteins suggests that structural features such as hydrophobic inner core, acetylation sites, dimer interface, and DNA binding surface are conserved among Sac10b proteins. Structural differences between the two proteins were found in the loops. To understand the structural basis for the thermostability of Mja10b, the Mja10b structure was compared to other proteins with similar topology. Our data suggest that extensive ion-pair networks, optimized accessible surface area and the dimerization via hydrophobic interactions may contribute to the enhanced thermostability of Mja10b.

Recombinant expression and characterization of an extremely hyperthermophilic archaeal histone from Pyrococcus horikoshii OT3

A histone-like gene, PHS051 from hyperthermophilic archaeon Pyrococcus horikoshii OT3 strain, was cloned, sequenced, and expressed in Escherichia coli. The recombinant histone, HPhA, encodes a protein of 70 amino acids with a molecular weight of 7868Da. Amino acid sequence analysis of HPhA showed high homology with other archaeal histones and eukaryal core histones. The HPhA was purified to homogeneity by heat precipitation and affinity chromatography. Gel electrophoresis mobility shift assays demonstrate that the purified HPhA has high affinity to DNA. The complex of the HPhA and DNA allows DNA to be protected from cleavage by the restriction enzyme TaqI at 65 degrees C. Circular dichroism spectra reveal that the conformation of the recombinant histone HPhA becomes looser when temperatures increase from 25 to 90 degrees C. The HPhA has inherited a remarkable thermostability especially in the presence of 1M KCl and retained DNA binding activity at extreme temperature, which is consistent with our previous report about its structure stability analyzed by X-ray crystallography.

Surface histidine residue of archaeal histone affects DNA compaction and thermostability

Archaeal histone, which possesses only the core domain part of eukaryal histone, induced DNA compaction by binding to DNA. Based on structural modeling, tetramer formation by dimer-dimer interaction is considered to require two intermolecular ion pairs formed between histidine and aspartate. To examine the role of the ion pairs on DNA compaction, mutant histones were constructed and analyzed using HpkB from Thermococcus kodakaraensis KOD1 as a model protein. The mutant histones, HpkB-H50A, HpkB-H50V, and HpkB-H50G were constructed by replacing conserved surface His50 with Ala, Val, and Gly, respectively. Circular dichroism analysis indicated no significant difference between wild-type and mutants in their structures. Gel mobility shift assays showed that all mutants possessed DNA binding ability, like wild-type HpkB, however all mutants compacted DNA less efficiently than the wild-type. Moreover, all mutants could not maintain the nucleosome-like structure (compacted form of DNA) above 80 degrees C. These results suggest that surface ion pairs between His and Asp play an important role in maintenance of nucleosome structure and DNA stabilization at high temperature.

Hinge-mediated dimerization of SMC protein is essential for its dynamic interaction with DNA

Structural maintenance of chromosomes (SMC) proteins play central roles in regulating higher order chromosome dynamics from bacteria to humans. As judged by electron microscopy, the SMC homodimer from Bacillus subtilis (BsSMC) is composed of two antiparallel, coiled-coil arms with a flexible hinge. Site-directed cross-linking experiments show here that dimerization of BsSMC is mediated by a hinge-hinge interaction between self-folded monomers. This architecture is conserved in the eukaryotic SMC2-SMC4 heterodimer. Analysis of different deletion mutants of BsSMC unexpectedly reveals that the major DNA-binding activity does not reside in the catalytic ATPase domains located at the ends of a dimer. Instead, point mutations in the hinge domain that disturb dimerization of BsSMC drastically reduce its ability to interact with DNA. Proper hinge function is essential for BsSMC to recognize distinct DNA topology, and mutant proteins with altered hinge angles cross-link double-stranded DNA in a nucleotide-dependent manner. We propose that the hinge domain of SMC proteins is not a simple dimerization site, but rather it acts as an essential determinant of dynamic SMC-DNA interactions.

Nucleosome-like complex of the histone from the hyperthermophile Methanopyrus kandleri (MkaH) with linear DNA

The MkaH protein from the archaeon Methanopyrus kandleri, an unusual assembly of two histone-fold domains in a single polypeptide chain, demonstrates high structural similarity to eukaryal histones. We studied the DNA binding and self-association properties of MkaH by means of the electrophoretic mobility shift assay (EMSA), electron microscopy (EM), chemical cross-linking, and analytical gel filtration. EMSA showed an increased mobility of linear DNA complexed with MkaH protein with a maximum at a protein-DNA weight ratio (R(w)) of approximately 3; the mobility decreased at higher protein concentration. EM of the complexes formed at Rw <or= 3 revealed formation of isometric loops encompassing 71 +/- 7 bp of DNA duplex. At high values of Rw (>or=9) thickened compact nucleoprotein structures were observed; no individual loops were seen within the complexes. Gel filtration chromatography and chemical fixation indicated that in the absence of DNA the dominant form of the MkaH in solution, unlike other archaeal histones, is a stable dimer (pseudo-tetramer of the histone-fold domain) apparently resembling the eukaryal (H3-H4)(2) tetramer. Similarly, dimers are the dominant form of the protein interacting with DNA. The properties of MkaH supporting the assignment of its intermediate position between other archaeal and eukaryal histones are discussed.

A recombinant RNA polymerase II-like enzyme capable of promoter-specific transcription

RNA polymerases (RNAPs) are core components of the cellular transcriptional machinery. Progress with functional studies of eukaryotic RNAPs has been delayed by the fact that it has not yet been possible to assemble active enzymes from individual subunits. Archaeal RNAPs are directly comparable to eukaryotic RNAPII in terms of primary sequence homology and quaternary structure. Here we report the successful in vitro assembly of a recombinant archaeal RNAP from purified subunits. The recombinant enzyme displays full activity in transcription assays and is capable, in the presence of two other basal factors, of promoter-specific transcription. The assembly of mutant enzymes yielded several unexpected insights into the structural and functional contributions of various subunits toward overall RNAP activity.

Ionic network at the C-terminus of the beta-glycosidase from the hyperthermophilic archaeon Sulfolobus solfataricus: Functional role in the quaternary structure thermal stabilization

Biochemical, crystallographic, and computational data support the hypothesis that electrostatic interactions are among the dominant forces in stabilizing hyperthermophilic proteins. The thermostable beta-glycosidase from the hyperthermophile Sulfolobus solfataricus (Ssbeta-gly) is an interesting model system for the study of protein adaptation to high temperatures. The largest ion-pair network of Ssbeta-gly is located at the tetrameric interface of the molecule; in this paper, key residues in this region were modified by site-directed mutagenesis and the stability of the mutants was analyzed by kinetics of thermal denaturation. All mutations produced faster enzyme inactivation, suggesting that the C-terminal ionic network prevents the dissociation into monomers, which is the limiting step in the mechanism of Ssbeta-gly inactivation. Moreover, the calculated reaction order showed that the mechanism of inactivation depends on the mutation introduced, suggesting that intermediates maintaining enzymatic activity are produced during the inactivation transition of some, but not all, mutants. Molecular models of each mutant allow us to rationalize the experimental evidence and give support to the current theories on the mechanism of ion pair stabilization in proteins from hyperthermophiles.

The archaeal histone-fold protein HMf organizes DNA into bona fide chromatin fibers

BACKGROUND

The discovery of histone-like proteins in Archaea urged studies into the possible organization of archaeal genomes in chromatin. Despite recent advances, a variety of structural questions remain unanswered.

RESULTS

We have used the atomic force microscope (AFM) with traditional nuclease digestion assays to compare the structure of nucleoprotein complexes reconstituted from tandemly repeated eukaryal nucleosome-positioning sequences and histone octamers, H3/H4 tetramers, and the histone-fold archaeal protein HMf. The data unequivocally show that HMf reconstitutes are indeed organized as chromatin fibers, morphologically indistinguishable from their eukaryal counterparts. The nuclease digestion patterns revealed a clear pattern of protection at regular intervals, again similar to the patterns observed with eukaryal chromatin fibers. In addition, we studied HMf reconstitutes on mononucleosome-sized DNA fragments and observed a great degree of similarity in the internal organization of these particles and those organized by H3/H4 tetramers. A difference in stability was observed at the level of mono-, di-, and triparticles between the HMf particles and canonical octamer-containing nucleosomes.

CONCLUSIONS

The in vitro reconstituted HMf-nucleoprotein complexes can be considered as bona fide chromatin structures. The differences in stability at the monoparticle level should be due to structural differences between HMf and core histone H3/H4 tetramers, i.e., to the complete absence in HMf of histone tails beyond the histone fold. We speculate that the existence of core histone tails in eukaryotes may provide a greater stability to nucleosomal particles and also provide the additional ability of chromatin structure to regulate DNA function in eukaryotic cells by posttranslational histone tail modifications.

Thermodynamic studies of the core histones: stability of the octamer subunits is not altered by removal of their terminal domains

We have investigated the role of the labile terminal domains of the core histones on the stability of the subunits of the protein core of the nucleosome by studying the thermodynamic behavior of the products of limited trypsin digestion of these subunits. The thermal stabilities of the truncated H2A-H2B dimer and the truncated (H3-H4)/(H3-H4)(2) system were studied by high-sensitivity differential scanning calorimetry and circular dichroism spectroscopy. The thermal denaturation of the truncated H2A-H2B dimer at pH 6.0 and low ionic strength is centered at 47.3 degrees C. The corresponding enthalpy change is 35 kcal/mol of 11.5 kDa monomer unit, and the heat capacity change upon unfolding is 1.2 kcal/(K mol of 11.5 kDa monomer unit). At pH 4.5 and low ionic strength, the truncated (H3-H4)/(H3-H4)(2) system, like its full-length counterpart, is quantitatively dissociated into two truncated H3-H4 dimers. The thermal denaturation of the truncated H3-H4 dimer is characterized by the presence of a single calorimetric peak centered at 60 degrees C. The enthalpy change is 25 kcal/mol of 10 kDa monomer unit, and the change in heat capacity upon unfolding is 0.5 kcal/(K mol of 10 kDa monomer unit). The thermal stabilities of both types of truncated dimers exhibit salt and pH dependencies similar to those of the full-length proteins. Finally, like their full-length counterparts, both truncated core histone dimers undergo thermal denaturation as highly cooperative units, without the involvement of any significant population of melting intermediates. Therefore, removal of the histone "tails" does not generally affect the thermodynamic behavior of the subunits of the core histone complex, indicating that the more centrally located regions of the histone fold and the extra-fold structured elements are primarily responsible for their stability and responses to parameters of their chemical microenvironment.

An ancestral nuclear protein assembly: crystal structure of the Methanopyrus kandleri histone

Eukaryotic histone proteins condense DNA into compact structures called nucleosomes. Nucleosomes were viewed as a distinguishing feature of eukaryotes prior to identification of histone orthologs in methanogens. Although evolutionarily distinct from methanogens, the methane-producing hyperthermophile Methanopyrus kandleri produces a novel, 154-residue histone (HMk). Amino acid sequence comparisons show that HMk differs from both methanogenic and eukaryotic histones, in that it contains two histone-fold ms within a single chain. The two HMk histone-fold ms, N and C terminal, are 28% identical in amino acid sequence to each other and approximately 21% identical in amino acid sequence to other histone proteins. Here we present the 1.37-A-resolution crystal structure of HMk and report that the HMk monomer structure is homologous to the eukaryotic histone heterodimers. In the crystal, HMk forms a dimer homologous to [H3-H4](2) in the eukaryotic nucleosome. Based on the spatial similarities to structural ms found in the eukaryotic nucleosome that are important for DNA-binding, we infer that the Methanopyrus histone binds DNA in a manner similar to the eukaryotic histone tetramer [H3-H4](2).

Entropic stabilization of the tryptophan synthase alpha-subunit from a hyperthermophile, Pyrococcus furiosus. X-ray analysis and calorimetry

The structure of the tryptophan synthase alpha-subunit from Pyrococcus furiosus was determined by x-ray analysis at 2.0-A resolution, and its stability was examined by differential scanning calorimetry. Although the structure of the tryptophan synthase alpha(2)beta(2) complex from Salmonella typhimurium has been already determined, this is the first report of the structure of the alpha-subunit alone. The alpha-subunit from P. furiosus (Pf-alpha-subunit) lacked 12 and 6 residues at the N and C termini, respectively, and one residue each in two loop regions as compared with that from S. typhimurium (St-alpha-subunit), resulting in the absence of an N-terminal helix and the shortening of a C-terminal helix. The structure of the Pf-alpha-subunit was essentially similar to that of the St-alpha-subunit in the alpha(2)beta(2) complex. The differences between both structures were discussed in connection with the higher stability of the Pf-alpha-subunit and the complex formation of the alpha- and beta-subunits. Calorimetric results indicated that the Pf-alpha-subunit has extremely high thermostability and that its higher stability is caused by an entropic effect. On the basis of structural information of both proteins, we analyzed the contributions of each stabilization factor and could conclude that hydrophobic interactions in the protein interior do not contribute to the higher stability of the Pf-alpha-subunit. Rather, the increase in ion pairs, decrease in cavity volume, and entropic effects due to shortening of the polypeptide chain play important roles in extremely high stability in Pf-alpha-subunit.

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.

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.

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.

Cloning and characterization of the histone-fold proteins YBL1 and YCL1

Histones are among the most conserved proteins in evolution, sharing a histone fold motif. A number of additional histonic proteins exist and are involved in the process of transcriptional regulation. We describe here the identification, cloning and characterization of two small members of the H2A-H2B sub-family (YBL1 and YCL1) related to the NF-YB and NF-YC subunits of the CCAAT-binding activator NF-Y and to the TATA-binding protein (TBP) binding repressor NC2. Unlike the latters, YBL1 and YCL1 have no intrinsic CCAAT or TATA-binding capacity. In nucleosome reconstitution assays, they can form complexes with histones in solution and on DNA and they are part of relatively large complexes, as determined by glycerol gradient experiments. Our data support the idea that YBL1 and YCL1 are divergent with respect to NF-YB and NF-YC for specific functions, but have coevolved the capacity to interact with nucleosomal structures.