Growth phase-dependent expression and degradation of histones in the thermophilic archaeon Thermococcus zilligii

The origin of chromosomal histones in a 30S ribosomal protein

Histones are genes that regulate chromatin structure. They are present in both eukaryotes and archaea, and form nucleosomes with DNA, but their exact evolutionary origins have hitherto remained a mystery. A longstanding hypothesis is that they have precursors in ribosomal proteins with whom they share much in common in terms of size and chemistry. By examining the proteome of the Asgard archaeon, Lokiarchaeum, the most conserved of all the histones, H4, is found to plausibly be homologous with one of its 30S ribosomal proteins, RPS6. This is based on both sequence identity and statistical analysis. The N-terminal tail, containing key sites involved in post-translational modifications, is notably present in the precursor gene. Although other archaeal groups possess similar homologs, these are not as close to H4 as the one found in Lokiarchaeum. The other core histones, H2A, H2B and H3, appear to have also evolved from the same ribosomal protein. Parts of H4 are also similar to another ribosomal protein, namely RPS15, suggesting that the ancestral precursor could have resembled both. Eukaryotic histones, in addition, appear to have an independent origin to that of their archaeal counterparts that evolved from similar, but still different, 30S subunit proteins, some of which are much more like histones in terms of their physical structure. The nucleosome may, therefore, be not only of archaeal but also of ribosomal origin.

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.

Transcription Regulation in Archaea

The known diversity of metabolic strategies and physiological adaptations of archaeal species to extreme environments is extraordinary. Accurate and responsive mechanisms to ensure that gene expression patterns match the needs of the cell necessitate regulatory strategies that control the activities and output of the archaeal transcription apparatus. Archaea are reliant on a single RNA polymerase for all transcription, and many of the known regulatory mechanisms employed for archaeal transcription mimic strategies also employed for eukaryotic and bacterial species. Novel mechanisms of transcription regulation have become apparent by increasingly sophisticated in vivo and in vitro investigations of archaeal species. This review emphasizes recent progress in understanding archaeal transcription regulatory mechanisms and highlights insights gained from studies of the influence of archaeal chromatin on transcription.

The Proteome and Lipidome of Thermococcus kodakarensis across the Stationary Phase

The majority of cells in nature probably exist in a stationary-phase-like state, due to nutrient limitation in most environments. Studies on bacteria and yeast reveal morphological and physiological changes throughout the stationary phase, which lead to an increased ability to survive prolonged nutrient limitation. However, there is little information on archaeal stationary phase responses. We investigated protein- and lipid-level changes in Thermococcus kodakarensis with extended time in the stationary phase. Adaptations to time in stationary phase included increased proportion of membrane lipids with a tetraether backbone, synthesis of proteins that ensure translational fidelity, specific regulation of ABC transporters (upregulation of some, downregulation of others), and upregulation of proteins involved in coenzyme production. Given that the biological mechanism of tetraether synthesis is unknown, we also considered whether any of the protein-level changes in T. kodakarensis might shed light on the production of tetraether lipids across the same period. A putative carbon-nitrogen hydrolase, a TldE (a protease in Escherichia coli) homologue, and a membrane bound hydrogenase complex subunit were candidates for possible involvement in tetraether-related reactions, while upregulation of adenosylcobalamin synthesis proteins might lend support to a possible radical mechanism as a trigger for tetraether synthesis.

The Alba protein family: Structure and function

Alba family proteins are small, basic, dimeric nucleic acid-binding proteins, which are widely distributed in archaea and a number of eukaryotes. This family of proteins bears the distinct features of regulation through acetylation/deacetylation, hence named as acetylation lowers binding affinity (Alba). Alba family proteins bind DNA cooperatively with no apparent sequence specificity. Besides DNA, Alba proteins also interact with diverse RNA species and associate with ribonucleo-protein complexes. Initially, Alba proteins were recognized as chromosomal proteins and supposed to be involved in the maintenance of chromatin architecture and transcription repression. However, recent studies have shown increasing evidence of functional plasticity among Alba family of proteins that widely range from genome packaging and organization, transcriptional and translational regulation, RNA metabolism, and development and differentiation processes. In recent years, Alba family proteins have attracted growing interest due to their widespread occurrence in large number of organisms. Presence in multiple copies, functional crosstalk, differential binding affinity, and posttranslational modifications are some of the key factors that might regulate the biological functions of Alba family proteins. In this review article, we present an overview of the Alba family proteins, their salient features and emphasize their functional role in different organisms reported so far.

The interplay between nucleoid organization and transcription in archaeal genomes

The archaeal genome is organized by either eukaryotic-like histone proteins or bacterial-like nucleoid-associated proteins. Recent studies have revealed novel insights into chromatin dynamics and their effect on gene expression in archaeal model organisms. In this Progress article, we discuss the interplay between chromatin proteins, such as histones and Alba, and components of the basal transcription machinery, as well as between chromatin structure and gene-specific transcription factors in archaea. Such an interplay suggests that chromatin might have a role in regulating gene expression on both a global and a gene-specific level. Moreover, several archaeal transcription factors combine a global gene regulatory role with an architectural role, thus contributing to chromatin organization and compaction, as well as gene expression. We describe the emerging principles underlying how these factors cooperate in nucleoid structuring and gene regulation.

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.

Interactions of archaeal chromatin proteins Alba1 and Alba2 with nucleic acids

BACKGROUND

Architectural proteins have important roles in compacting and organising chromosomal DNA. There are two potential histone counterpart peptide sequences (Alba1 and Alba2) in the Aeropyrum pernix genome (APE1832.1 and APE1823).

METHODOLOGY/PRINCIPAL FINDINGS

THESE TWO PEPTIDES WERE EXPRESSED AND THEIR INTERACTIONS WITH VARIOUS DNAS WERE STUDIED USING A COMBINATION OF VARIOUS EXPERIMENTAL TECHNIQUES: surface plasmon resonance, UV spectrophotometry, circular dichroism-spectropolarimetry, gel-shift assays, and isothermal titration calorimetry.

CONCLUSIONS/SIGNIFICANCE

Our data indicate that there are significant differences in the properties of the Alba1 and Alba2 proteins. Both of these Alba proteins can thermally stabilise DNA polynucleotides, as seen from UV melting curves. Alba2 and equimolar mixtures of Alba1/Alba2 have greater effects on the thermal stability of poly(dA-dT).poly(dA-dT). Surface plasmon resonance sensorgrams for binding of Alba1, Alba2, and equimolar mixtures of Alba1/Alba2 to DNA oligonucleotides show different binding patterns. Circular dichroism indicates that Alba2 has a less-ordered secondary structure than Alba1. The secondary structures of the Alba proteins are not significantly influenced by DNA binding, even at high temperatures. Based on these data, we conclude that Alba1, Alba2, and equimolar mixtures of Alba1/Alba2 show different properties in their binding to various DNAs.

An archaeal histone is required for transformation of Thermococcus kodakarensis

Archaeal histones wrap DNA into complexes, designated archaeal nucleosomes, that resemble the tetrasome core of a eukaryotic nucleosome. Therefore, all DNA interactions in vivo in Thermococcus kodakarensis, the most genetically versatile model species for archaeal research, must occur in the context of a histone-bound genome. Here we report the construction and properties of T. kodakarensis strains that have TK1413 or TK2289 deleted, the genes that encode HTkA and HTkB, respectively, the two archaeal histones present in this archaeon. All attempts to generate a strain with both TK1413 and TK2289 deleted were unsuccessful, arguing that a histone-mediated event(s) in T. kodakarensis is essential. The HTkA and HTkB amino acid sequences are 84% identical (56 of 67 residues) and 94% similar (63 of 67 residues), but despite this homology and their apparent redundancy in terms of supporting viability, the absence of HTkA and HTkB resulted in differences in growth and in quantitative and qualitative differences in genome transcription. A most surprising result was that the deletion of TK1413 (ΔhtkA) resulted in a T. kodakarensis strain that was no longer amenable to transformation, whereas the deletion of TK2289 (ΔhtkB) had no detrimental effects on transformation. Potential roles for the archaeal histones in regulating gene expression and for HTkA in DNA uptake and recombination are discussed.

Genome sequence of an oligohaline hyperthermophilic archaeon, Thermococcus zilligii AN1, isolated from a terrestrial geothermal freshwater spring

Thermococcus zilligii, a thermophilic anaerobe in freshwater, is useful for physiological research and biotechnological applications. Here we report the high-quality draft genome sequence of T. zilligii AN1(T). The genome contains a number of genes for an immune system and adaptation to a microbial biomass-rich environment as well as hydrogenase genes.

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.

Replication-biased genome organisation in the crenarchaeon Sulfolobus

BACKGROUND

Species of the crenarchaeon Sulfolobus harbour three replication origins in their single circular chromosome that are synchronously initiated during replication.

RESULTS

We demonstrate that global gene expression in two Sulfolobus species is highly biased, such that early replicating genome regions are more highly expressed at all three origins. The bias by far exceeds what would be anticipated by gene dosage effects alone. In addition, early replicating regions are denser in archaeal core genes (enriched in essential functions), display lower intergenic distances, and are devoid of mobile genetic elements.

CONCLUSION

The strong replication-biased structuring of the Sulfolobus chromosome implies that the multiple replication origins serve purposes other than simply shortening the time required for replication. The higher-level chromosomal organisation could be of importance for minimizing the impact of DNA damage, and may also be linked to transcriptional regulation.

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.

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.

Archaeal chromatin proteins: different structures but common function?

Chromatin proteins promote chromosome flexibility in vivo, maintaining a compact yet decondensed template that permits polymerase accessibility. All Archaea have at least two types of chromatin proteins, and diversity in the chromatin protein population appears to prevent polymerization of a single type of protein. Of the numerous chromatin proteins that have been described in Archaea, only two--histones and Alba homologs--are present in all archaeal phyla. Although their structures and complexes with DNA have no similarities, their functions probably overlap as mutants that lack single chromatin proteins are viable.

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.

Archaeal chromatin and transcription

Archaea contain a variety of sequence-independent DNA binding proteins consistent with the evolution of several different, sometimes overlapping and exchangeable solutions to the problem of genome compaction. Some of these proteins undergo residue-specific post-translational lysine acetylation or methylation, hinting at analogues of the histone modifications that regulate eukaryotic chromatin structure and transcription. Archaeal transcription initiation most closely resembles the eukaryotic RNA polymerase II (RNAPII) system, but Archaea do not appear to have homologues of the multisubunit complexes that remodel eukaryotic chromatin and activate RNAPII initiation. In contrast, they have sequence-specific regulators that repress and perhaps activate archaeal transcription by mechanisms superficially similar to the bacterial paradigm of regulating promoter binding by RNAP. Repressors compete with archaeal TATA-box binding protein (TBP) and TFB for the TATA-box and TFB-recognition elements (BRE) of the archaeal promoter, or with archaeal RNAP for the site of transcription initiation. Transcript-specific regulation by repressors binding to sites of transcript initiation is consistent with such sites having very little sequence conservation. However, most Archaea have only one TBP and/or TFB that presumably must therefore bind to similar TATA-box and BRE sequences upstream of most genes. Repressors that function by competing with TBP and/or TFB binding must therefore also make additional contacts with transcript-specific regulatory sites adjacent or remote from the TATA-box/BRE region. The fate of the archaeal TBP and TFB following transcription initiation remains to be determined. Based on functional homology with their eukaryotic RNAPII-system counterparts, archaeal TBP and possibly also TFB should remain bound to the TATA-box/BRE region after transcription initiation. However, this seems unlikely as it might limit repressor competition at this site to only the first round of transcription initiation.

Controlling the double helix

Chromatin is the complex of DNA and proteins in which the genetic material is packaged inside the cells of organisms with nuclei. Chromatin structure is dynamic and exerts profound control over gene expression and other fundamental cellular processes. Changes in its structure can be inherited by the next generation, independent of the DNA sequence itself.

Archaeal genome organization and stress responses: implications for the origin and evolution of cellular life

For DNA to be used as an informational molecule it must exist in the cell on the edge of stability because all genomic processes require local controlled melting. This presents mechanistic opportunities and problems for genomic DNA from hyperthermophilic organisms, whose unpackaged DNA could melt at optimal temperatures for growth. Hyperthermophiles are suggested to employ the novel positively supercoiling topoisomerase enzyme reverse gyrase (RG) to form positively supercoiled DNA that is intrinsically resistant to thermal denaturation. RG is presently the only archaeal gene that is uniquely found in hyperthermophiles and therefore is central to hypotheses suggesting a hypothermophilic origin of life. However, the suggestion that RG has evolved by the fusion of two pre-existing enzymes has led to hypotheses for a lower temperature for the origin of life. In addition to the action of topoisomerases, DNA packaging and the intracellular ionic environment can also manipulate DNA topology significantly. In the Euryarchaeota, nucleosomes containing minimal histones can adopt two alternate DNA topologies in a salt-dependent manner. From this we hypothesize that since internal salt concentrations are increased following an increase in temperature, the genomic effects of temperature fluctuations could also be accommodated by changes in nucleosome organization. In addition, stress-induced changes in the nucleoid proteins could also play a role in maintaining the genome in the optimal topological state in changing environments. The function of these systems could therefore be central to temperature adaptation and thus be implicated in origin of life scenarios involving hyperthermophiles.