Thermoplasma acidophilum histone-like protein. Partial amino acid sequence suggestive of homology to eukaryotic histones

The chromatin landscape of the euryarchaeon Haloferax volcanii

BACKGROUND

Archaea, together with Bacteria, represent the two main divisions of life on Earth, with many of the defining characteristics of the more complex eukaryotes tracing their origin to evolutionary innovations first made in their archaeal ancestors. One of the most notable such features is nucleosomal chromatin, although archaeal histones and chromatin differ significantly from those of eukaryotes, not all archaea possess histones and it is not clear if histones are a main packaging component for all that do. Despite increased interest in archaeal chromatin in recent years, its properties have been little studied using genomic tools.

RESULTS

Here, we adapt the ATAC-seq assay to archaea and use it to map the accessible landscape of the genome of the euryarchaeote Haloferax volcanii. We integrate the resulting datasets with genome-wide maps of active transcription and single-stranded DNA (ssDNA) and find that while H. volcanii promoters exist in a preferentially accessible state, unlike most eukaryotes, modulation of transcriptional activity is not associated with changes in promoter accessibility. Applying orthogonal single-molecule footprinting methods, we quantify the absolute levels of physical protection of H. volcanii and find that Haloferax chromatin is similarly or only slightly more accessible, in aggregate, than that of eukaryotes. We also evaluate the degree of coordination of transcription within archaeal operons and make the unexpected observation that some CRISPR arrays are associated with highly prevalent ssDNA structures.

CONCLUSIONS

Our results provide the first comprehensive maps of chromatin accessibility and active transcription in Haloferax across conditions and thus a foundation for future functional studies of archaeal chromatin.

Structure and function of archaeal histones

The genomes of all organisms throughout the tree of life are compacted and organized in chromatin by association of chromatin proteins. Eukaryotic genomes encode histones, which are assembled on the genome into octamers, yielding nucleosomes. Post-translational modifications of the histones, which occur mostly on their N-terminal tails, define the functional state of chromatin. Like eukaryotes, most archaeal genomes encode histones, which are believed to be involved in the compaction and organization of their genomes. Instead of discrete multimers, in vivo data suggest assembly of “nucleosomes” of variable size, consisting of multiples of dimers, which are able to induce repression of transcription. Based on these data and a model derived from X-ray crystallography, it was recently proposed that archaeal histones assemble on DNA into “endless” hypernucleosomes. In this review, we discuss the amino acid determinants of hypernucleosome formation and highlight differences with the canonical eukaryotic octamer. We identify archaeal histones differing from the consensus, which are expected to be unable to assemble into hypernucleosomes. Finally, we identify atypical archaeal histones with short N- or C-terminal extensions and C-terminal tails similar to the tails of eukaryotic histones, which are subject to post-translational modification. Based on the expected characteristics of these archaeal histones, we discuss possibilities of involvement of histones in archaeal transcription regulation.

Both Archaea and eukaryotes express histones, but whereas the tertiary structure of histones is conserved, the quaternary structure of histone–DNA complexes is very different. In a recent study, the crystal structure of the archaeal hypernucleosome was revealed to be an “endless” core of interacting histones that wraps the DNA around it in a left-handed manner. The ability to form a hypernucleosome is likely determined by dimer–dimer interactions as well as stacking interactions between individual layers of the hypernucleosome. We analyzed a wide variety of archaeal histones and found that most but not all histones possess residues able to facilitate hypernucleosome formation. Among these are histones with truncated termini or extended histone tails. Based on our analysis, we propose several possibilities of archaeal histone involvement in transcription regulation.

Breaking through a phylogenetic impasse: a pair of associated archaea might have played host in the endosymbiotic origin of eukaryotes

For over a century, the origin of eukaryotes has been a topic of intense debate among scientists. Although it has become widely accepted that organelles such as the mitochondria and chloroplasts arose via endosymbiosis, the origin of the eukaryotic nucleus remains enigmatic. Numerous models for the origin of the nucleus have been proposed over the years, many of which use endosymbiosis to explain its existence. Proposals of microbes whose ancestors may have served as either a host or a guest in various endosymbiotic scenarios abound, none of which have been able to sufficiently incorporate the cell biological as well as phylogenetic data which links these organisms to the nucleus. While it is generally agreed that eukaryotic nuclei share more features in common with archaea rather than with bacteria, different studies have identified either one or the other of the two major groups of archaea as potential ancestors, leading to somewhat of a stalemate. This paper seeks to resolve this impasse by presenting evidence that not just one, but a pair of archaea might have served as host to the bacterial ancestor of the mitochondria. This pair may have consisted of ancestors of both Ignicoccus hospitalis as well as its ectosymbiont/ectoparasite ‘Nanoarchaeum equitans’.

The last eukaryotic common ancestor (LECA): acquisition of cytoskeletal motility from aerotolerant spirochetes in the Proterozoic Eon

We develop a symbiogenetic concept of the origin of eukaryotic intracellular motility systems from anaerobic but aerotolerant spirochetes in sulfide-rich environments. The last eukaryotic common ancestors (LECAs) have extant archaeprotist descendants: motile nucleated cells with Embden-Meyerhof glycolysis and substrate-level phosphorylation that lack the alpha-proteobacterial symbiont that became the mitochondrion. Swimming and regulated O(2)-tolerance via sulfide oxidation already had been acquired by sulfidogenic wall-less archaebacteria (thermoplasmas) after aerotolerant cytoplasmic-tubule-containing spirochetes (eubacteria) attached to them. Increasing stability of sulfide-oxidizing/sulfur-reducing consortia analogous to extant sulfur syntrophies (Thiodendron) led to fusion. The eubacteria-archaebacteria symbiosis became permanent as the nucleus evolved by prokaryotic recombination with membrane hypertrophy, analogous to Gemmata obscuriglobus and other delta-proteobacteria with membrane-bounded nucleoids. Histone-coated DNA, protein-synthetic RNAs, amino-acylating, and other enzymes were contributed by the sulfidogen whereas most intracellular motility derives from the spirochete. From this redox syntrophy in anoxic and microoxic Proterozoic habitats LECA evolved. The nucleus originated by recombination of eu- and archaebacterial DNA that remained attached to eubacterial motility structures and became the microtubular cytoskeleton, including the mitotic apparatus. Direct LECA descendants include free-living archaeprotists in anoxic environments: archamoebae, metamonads, parabasalids, and some mammalian symbionts with mitosomes. LECA later acquired the fully aerobic Krebs cycle-oxidative phosphorylation-mitochondrial metabolism by integration of the protomitochondrion, a third alpha-proteobacterial symbiont from which the ancestors to most protoctists, all fungi, plants, and animals evolved. Secondarily anaerobic eukaryotes descended from LECA after integration of this oxygen-respiring eubacterium. Explanatory power and experimental predictions for molecular biology of the LECA concept are stated.

The chimeric eukaryote: origin of the nucleus from the karyomastigont in amitochondriate protists

We present a testable model for the origin of the nucleus, the membrane-bounded organelle that defines eukaryotes. A chimeric cell evolved via symbiogenesis by syntrophic merger between an archaebacterium and a eubacterium. The archaebacterium, a thermoacidophil resembling extant Thermoplasma, generated hydrogen sulfide to protect the eubacterium, a heterotrophic swimmer comparable to Spirochaeta or Hollandina that oxidized sulfide to sulfur. Selection pressure for speed swimming and oxygen avoidance led to an ancient analogue of the extant cosmopolitan bacterial consortium "Thiodendron latens." By eubacterial-archaebacterial genetic integration, the chimera, an amitochondriate heterotroph, evolved. This "earliest branching protist" that formed by permanent DNA recombination generated the nucleus as a component of the karyomastigont, an intracellular complex that assured genetic continuity of the former symbionts. The karyomastigont organellar system, common in extant amitochondriate protists as well as in presumed mitochondriate ancestors, minimally consists of a single nucleus, a single kinetosome and their protein connector. As predecessor of standard mitosis, the karyomastigont preceded free (unattached) nuclei. The nucleus evolved in karyomastigont ancestors by detachment at least five times (archamoebae, calonymphids, chlorophyte green algae, ciliates, foraminifera). This specific model of syntrophic chimeric fusion can be proved by sequence comparison of functional domains of motility proteins isolated from candidate taxa.

Overproduction of Sac7d and Sac7e reveals only Sac7e to be a DNA-binding protein with ribonuclease activity from the extremophilic archaeon Sulfolobus acidocaldarius

Genomic DNA from Sulfolobus acidocaldarius was screened using a degenerate oligodeoxyribonucleotide, derived from the sequence of 16 N-terminal amino acids from SaRD protein. SaRD protein was previously isolated in our laboratory and identified as a protein from S. acidocaldarius exhibiting ribonuclease activity as well as DNA-binding properties. On the basis of Southern hybridization analysis two genes from S. acidocaldarius have been cloned, sequenced and overproduced in Escherichia coli. The deduced amino acid sequences revealed that one gene encodes Sac7d and the other one Sac7e; two small, previously described basic proteins from S. acidocaldarius, and furthermore the N-termini of Sac7e and SaRD are identical. Northern blot analysis demonstrated that the genes are transcribed separately. After expression of sac7d and sac7e genes in E. coli it was shown that only recombinant Sac7e protein exhibits RNase activity and is catalytically indistinguishable from SaRD protein. Western blot analysis using a polyclonal antiserum raised against purified SaRD protein further confirmed that Sac7e and SaRD are identical proteins endowed with RNase activity and DNA-binding properties. A new RNA cleavage mechanism has to be postulated for Sac7e since, in contrast to common RNases (e.g. RNase A and T1), no histidines are present in the amino acid sequence. Differences between the very closely related 7 kDa proteins from two Sulfolobus strains converting DNA-binding proteins into RNases are pointed out and discussed, whereas substitutions of Glu by Gln (S. solfataricus) or by Lys (S. acidocaldarius) seem to be crucial.

Gene cloning, expression, and characterization of the Sac7 proteins from the hyperthermophile Sulfolobus acidocaldarius

The genes for two Sac7 DNA-binding proteins, Sac7d and Sac7e, from the extremely thermophilic archaeon Sulfolobus acidocaldarius have been cloned into Escherichia coli and sequenced. The sac7d and sac7e open reading frames encode 66 amino acid (7608 Da) and 65 amino acid (7469 Da) proteins, respectively. Southern blots indicate that these are the only two Sac7 protein genes in S. acidocaldarius, each present as a single copy. Sac7a, b, and c proteins appear to be carboxy-terminal modified Sac7d species. The transcription initiation and termination regions of the sac7d and sac7e genes have been identified along with the promoter elements. Potential ribosome binding sites have been identified downstream of the initiator codons. The sac7d gene has been expressed in E. coli, and various physical properties of the recombinant protein have been compared with those of native Sac7. The UV absorbance spectra and extinction coefficients, the fluorescence excitation and emission spectra, the circular dichroism, and the two-dimensional double-quantum filtered 1H NMR spectra of the native and recombinant species are essentially identical, indicating essentially identical local and global folds. The recombinant and native proteins bind and stabilize double-stranded DNA with a site size of 3.5 base pairs and an intrinsic binding constant of 2 x 10(7) M-1 for poly[dGdC].poly[dGdC] in 0.01 M KH2PO4 at pH 7.0. The availability of the recombinant protein permits a direct comparison of the thermal stabilities of the methylated and unmethylated forms of the protein. Differential scanning calorimetry demonstrates that the native protein is extremely thermostable and unfolds reversibly at pH 6.0 with a Tm of approximately 100 degrees C, while the recombinant protein unfolds at 92.7 degrees C.

Nucleoid proteins

This article examines the published evidence in support of the classification of organisms into three groups (Bacteria, Archae, and Eukarya) instead of two groups (prokaryotes and eukaryotes) and summarizes the comparative biochemistry of each of the known histone-like, nucleoid DNA-binding proteins. The molecular structures and amino acid sequences of Archae are more similar to those of Eukarya than of Bacteria, with a few exceptions. Cytochemical methodology employed for localizing these proteins in archaeal and bacterial cells has also been reviewed. It is becoming increasingly apparent that these proteins participate both in the organization of DNA and in the control of gene expression. Evidence obtained from biochemical properties, structural and functional differences, and the ultrastructural location of these proteins, as well as from gene mutations clearly justifies the division of prokaryotes into bacterial and archaeal groups. Indeed, chromosomes, whether they be nuclear, prokaryotic, or organellar, are invariably complexed with abundant, small, basic proteins that bind to DNA with low sequence specificity. These proteins include the histones, histone-like proteins, and nonhistone high mobility group (HMG) proteins.

Amino acid substitution in the C-terminal arm domain of HU-2 results in an enhanced affinity for DNA

Three mutants of the Escherichia coli hupA gene, encoding the HU-2 protein, were constructed by synthetic oligodeoxyribonucleotide-directed, site-specific mutagenesis on M13mp18 vectors. The resulting HupAN10, HupAN11 and HupAN12 proteins contained Thr59-->Lys, Gln64-->Lys and Asn53-->Arg substitutions, respectively. These amino acid (aa) changes increased the positive charge of the N-terminal half of the two-strand, antiparallel beta-ribbon of the arm structure, which is believed to be a domain for DNA binding. The three mutant proteins bound to DNA more tightly than wild-type HU-2, and their affinities for DNA increased in the order of HupAN10, HupAN11, HupAN12. The mutant proteins showed a slightly increased HU activity for supporting Mu phage development. A mutant HU-2 protein with increased basicity, but with an altered aa sequence in the arm region due to a frameshift mutation, was also constructed. This mutant protein showed a reduced affinity to DNA and was unable to support Mu growth, suggesting that a unique aa sequence of the arm domain, rather than mere basicity of this domain, is required for efficient binding to DNA.

DNA binding by the archaeal histone HMf results in positive supercoiling

HMf, a histone from the hyperthermophilic archaeon Methanothermus fervidus binds double-stranded DNA molecules in vitro, forming compact structures that visibly resemble eukaryal nucleosomes. We show here that HMf binding increases the helical periodicity of DNA molecules to approximately 11 base pairs (bp) per turn and that DNA molecules in these nucleosome-like structures are constrained in positive toroidal supercoils. Based on the mass of HMf needed to cause a change in linking number (delta Lk), the maximum delta Lk introduced into circular DNA molecules of known sizes, and electron microscopy, we estimate that each HMf-DNA structure contains between 90 and 150 bp of DNA wrapped in 1.5 positive toroidal supercoils around a core of four HMf molecules. A model and pathway for the formation of these structures in vitro are presented and the possible role of positive toroidal wrapping of the M. fervidus genome in vivo is discussed.

HMf, a DNA-binding protein isolated from the hyperthermophilic archaeon Methanothermus fervidus, is most closely related to histones

Methanothermus fervidus grows optimally at 83 degrees C. A protein designated HMf (histone M. fervidus) has been isolated from this archaeal hyperthermophile that binds to double-stranded DNA molecules and increases their resistance to thermal denaturation. HMf binding to linear double-stranded DNA molecules of greater than 2 kilobase pairs also increases their electrophoretic mobilities through agarose gels. Visualization of this compaction process by electron microscopy has demonstrated the formation of quasispherical, macromolecular HMf-DNA complexes. HMf is a mixture of approximately equal amounts of two very similar polypeptides designated HMf-1 and HMf-2. Determination of the DNA sequence of the gene encoding HMf-2 (hmfB) has revealed that over 30% of the amino acid residues in HMf-2 are conserved in the consensus sequences derived for eucaryal histones H2A, H2B, H3, and H4. These archaeal polypeptides and eucaryal histones appear therefore to have evolved from a common ancestor and are likely to have related structures and functions.

Characterization of HU-like protein from Bifidobacterium longum

A HU-like protein (HBl) of Bifidobacterium longum was purified and characterized. HBl is heat-stable and acid-resistant, and has a molecular weight of about 9.1 kDa as estimated by its mobility on electrophoresis. HBl is intermediate in basicity (pI 9.8) between the HU-1 and HU-2 proteins of Escherichia coli, and is dissociated from a calf thymus DNA-cellulose column at 300-400 mM NaCl. Its amino acid composition shows many similarities with that of E coli HU. The NH2-terminal amino acid sequence of HBl also shows significant similarities to the consensus sequence deduced from the sequences of eleven HU-like proteins from prokaryotic sources. Chemical crosslinking analysis indicated that the HBl protein predominantly forms a homotypic dimer.

Gene structure, organization, and expression in archaebacteria

Major advances have recently been made in understanding the molecular biology of the archaebacteria. In this review, we compare the structure of protein and stable RNA-encoding genes cloned and sequenced from each of the major classes of archaebacteria: the methanogens, extreme halophiles, and acid thermophiles. Protein-encoding genes, including some encoding proteins directly involved in methanogenesis and photoautotrophy, are analyzed on the basis of gene organization and structure, transcriptional control signals, codon usage, and evolutionary conservation. Stable RNA-encoding genes are compared for gene organization and structure, transcriptional signals, and processing events involved in RNA maturation, including intron removal. Comparisons of archaebacterial structures and regulatory systems are made with their eubacterial and eukaryotic homologs.

Histonelike proteins of bacteria

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Histones and their modifications

Histones constitute the protein core around which DNA is coiled to form the basic structural unit of the chromosome known as the nucleosome. Because of the large amount of new histone needed during chromosome replication, the synthesis of histone and DNA is regulated in a complex manner. During RNA transcription and DNA replication, the basic nucleosomal structure as well as interactions between nucleosomes must be greatly altered to allow access to the appropriate enzymes and factors. The presence of extensive and varied post-translational modifications to the otherwise highly conserved histone primary sequences provides obvious opportunities for such structural alterations, but despite concentrated and sustained effort, causal connections between histone modifications and nucleosomal functions are not yet elucidated.

Cell symbiosis [correction of symbioisis] theory: status and implications for the fossil record

Recent geological treatises have presented three alternative models of the origins of eukaryotes as if they merited equal treatment. However, modern biological techniques, especially nucleic acid and protein sequencing, have clearly established the validity of the symbiotic theory of the origin of eukaryotic organelles. The serial endosymbiotic theory in its most extreme form states that three classes of eukaryotic cell organelles (mitochondria, plastids and undulipodia) originated as free-living bacteria (aerobic respirers, phototrophic bacteria and spirochetes respectively) in association with hosts that become the nucleocytoplasm (Thermoplasma-like archaebacterial hosts). Molecular biological information, primarily derived from ribosomal RNA nucleotide sequencing studies leads to the conclusion that the symbiotic origin theory for both mitochondria and plastids has been proven. The probability of an ancestral archaebacterial-Thermoplasma-like host for the nucleocytoplasm has been rendered more likely by discoveries by Dennis Searcy and his colleagues and Carl Woese and his colleagues. The most equivocal postulate of the symbiotic theory, the origin of undulipodia (cilia and other organelles of motility that develop from kinetosomes is under investigation now. The status of these postulates, as well as their implications for the fossil record, is briefly summarized here.

Histone-like protein in the Archaebacterium Sulfolobus acidocaldarius

The Archaebacterium Thermoplasma acidophilum contains a basic chromosomal protein remarkably similar to the histones of eukaryotes. Therefore, it was of interest to examine a different Archaebacterium for similar proteins. We chose to examine Sulfolobus acidocaldarius because it is thermophilic, like T. acidophilum, but nevertheless the two organisms are not particularly closely related. Two major chromosomal proteins were found in S. acidocaldarius. The smaller of these was soluble in 0.2 M H2SO4 and had a molecular weight of 14500. The larger was acid-insoluble and had a molecular weight of about 36000. Together, the proteins protected about 5% of the DNA against nuclease digestion and stabilized about 50% against thermal denaturation. Overall, the properties of these proteins were intermediate between those of the Escherichia coli protein HU and T. acidophilum protein HTa.