Histone-encoding genes from Pyrococcus: evidence for members of the HMf family of archaeal histones in a non-methanogenic Archaeon

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’.

An actin homolog of the archaeon Thermoplasma acidophilum that retains the ancient characteristics of eukaryotic actin

Actin, a central component of the eukaryotic cytoskeleton, plays a crucial role in determining cell shape in addition to several other functions. Recently, the structure of the archaeal actin homolog Ta0583, isolated from the archaeon Thermoplasma acidophilum, which lacks a cell wall, was reported by Roeben et al. (J. Mol. Biol. 358:145-156, 2006). Here we show that Ta0583 assembles into bundles of filaments similar to those formed by eukaryotic actin. Specifically, Ta0583 forms a helix with a filament width of 5.5 nm and an axial repeating unit of 5.5 nm, both of which are comparable to those of eukaryotic actin. Eukaryotic actin shows a greater resemblance to Ta0583 than to bacterial MreB and ParM in terms of polymerization characteristics, such as the requirement for Mg(2+), critical concentration, and repeating unit size. Furthermore, phylogenetic analysis also showed a closer relationship between Ta0583 and eukaryotic actin than between MreB or ParM and actin. However, the low specificity of Ta0583 for nucleotide triphosphates indicates that Ta0583 is more primitive than eukaryotic actin. Taken together, our results suggest that Ta0583 retains the ancient characteristics of eukaryotic actin.

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.

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

HTz is a member of the archaeal histone family. The archaeal histones have primary sequences and structural similarity to the eukaryal histone fold domain, and are thought to resemble the archetypal ancestor of the eukaryal nucleosome core histones. The effects of growth phase on the total soluble proteins from Thermococcus zilligii, isolated after various stages of growth from mid-logarithmic to late stationary phase, were examined by denaturing polyacrylamide gel electrophoresis. On entry into stationary phase, at least 11 proteins were detected that changed considerably in level. One of these proteins was identified by Western hybridization as HTz. The level of HTz decreased dramatically as cells entered stationary phase, and it could not be detected by late stationary phase. Unexpectedly, the Western hybridization detected a second protein, with an estimated molecular mass of approximately 14 kDa, which paralleled the decrease in level of HTz. Native purified HTz was shown to retain complete activity after prolonged incubation at the growth temperature of the organism, suggesting that the decrease in HTz was a specific cell-regulated process. Analysis of native purified HTz by electrospray ionization mass spectrometry revealed the molecular masses of HTz1 and HTz2 to be 7204 +/- 3 Da and 7016 +/- 3 Da respectively. The only non-covalent species that was detected corresponded to the molecular mass of an HTz1-HTz2 heterodimer. Northern analyses of T. zilligii total RNA with an htz1 gene probe indicated a rapid decrease in expression of htz1 with progression of the growth phase, and complete repression of htz1 transcript synthesis by late logarithmic phase. Three proteins that changed in level with growth phase were identified by N-terminal sequence analysis. The first was homologous to a hypothetical protein conserved in all Archaea sequenced to date, the second to the Sac10b family of archaeal DNA-binding proteins and the third to the C-terminal region of the leucine-responsive regulatory family of DNA-binding proteins (LRPs).

Analysis of DNA compaction profile and intracellular contents of archaeal histones from Pyrococcus kodakaraensis KOD1

Two histone genes, hpkA and hpkB, from hyperthermophilic archaeon Pyrococcus kodakaraensis KOD1 strain were cloned, sequenced, and expressed in Escherichia coli cells. Both hpkA and hpkB genes encoded a protein of 67 amino acids, however they possessed the different molecular weight (HpkA, 7,378:HpkB, 7,167). Deduced amino acid sequences of HpkA and HpkB were homologous to other archaeal histones and eucaryal core histones (H2A, H4). Gel mobility shift assays by purified proteins demonstrated that HpkB possessed higher affinity to DNA and more extensive ability to compact DNA than HpkA. HpkB prevented double stranded DNA from thermal denaturation in less amount than HpkA in vitro. In order to investigate intracellular contents of HpkA and HpkB in KOD1 cells, immunoblot analysis was performed by using anti-HpkA antisera obtained from immunized BALB/c mice, showing that HpkA was less abundantly expressed than HpkB in KOD1 cells. These results suggest that HpkB plays a major role to protect double stranded DNA from thermal denaturation in vivo.

A search for extraterrestrial eukaryotes: physical and paleontological aspects

Physical and biochemical aspects of a proposed search for extraterrestrial eukaryotes (SETE) are considered. Such a program should approach the distinction between a primitive eukaryote and an archaebacteria. The emphasis on gene silencing suggests a possible assay suitable for a robotic investigation of eukaryoticity, so as to be able to decide whether the first steps towards eukaryogenesis have been taken in an extraterrestrial planet, or satellite. The experiment would consist of searching for cellular division and the systematic related delay in replication of heterochromatic chromosome segments. It should be noticed that the direct search for a membrane-bounded set of chromosomes does not necessarily determine eukaryotic identity, as there are prokaryotes that have membrane-bounded nucleoids. A closer look at the protein fraction of chromatin (mainly histones) does not help either, as there are some eukaryotes that may lack histones; there are also some bacteria as well as archaebacteria with histone-like proteins in their nucleoids. Comments on the recent suggestion of possible environments for a SETE program are discussed: the deep crust of Mars, and the Jovian satellite Europa, provided the existence of an ocean under its ice-covered surface is confirmed by the current Galileo mission.

Evidence for an early prokaryotic origin of histones H2A and H4 prior to the emergence of eukaryotes

Histones have been identified recently in many prokaryotes. These histones, unlike their eukaryotic homologs, are of a single uniform type that is thought to resemble the archetypal ancestor of the eukaryotic histone family. In this paper we report the finding, the cloning and the phylogenetic analysis of the sequence of a prokaryotic histone from the hyperthermophile Methanopyrus kandleri . Unlike previously described prokaryotic histones, the Methanopyrus sequence has a novel structure consisting of two tandemly repeated histone fold motifs in a single polypeptide. Sequence analyses indicate that the N-terminal repeat is most closely related to eukaryotic H2A and H4 histones, whereas the C-terminal repeat resembles that found in prokaryotic histones. These results imply an early divergence within the histone gene family prior to the emergence of eukaryotes and may represent an evolutionary step leading to eukaryotic histones.

Repair of extensive ionizing-radiation DNA damage at 95 degrees C in the hyperthermophilic archaeon Pyrococcus furiosus

We investigated the capacity of the hyperthermophile Pyrococcus furiosus for DNA repair by measuring survival at high levels of 60Co gamma-irradiation. The P. furiosus 2-Mb chromosome was fragmented into pieces ranging from 500 kb to shorter than 30 kb at a dose of 2,500 Gy and was fully restored upon incubation at 95 degrees C. We suggest that recombination repair could be an extremely active repair mechanism in P. furiosus and that it might be an important determinant of survival of hyperthermophiles at high temperatures.

The emergence of major cellular processes in evolution

The phylogenetic distribution of divergently related protein families into the three domains of life (archaea, bacteria and eukaryotes) can signify the presence or absence of entire cellular processes in these domains and their ancestors. We can thus study the emergence of the major transitions during cellular evolution, and resolve some of the controversies surrounding the evolutionary status of archaea and the origins of the eukaryotic cell. In view of the ongoing projects that sequence the complete genomes of several Archaea, this work forms a testable prediction when the genome sequences become available. Using the presence of the protein families as taxonomic traits, and linking them to biochemical pathways, we are able to reason about the presence of the corresponding cellular processes in the last universal ancestor of contemporary cells. The analysis shows that metabolism was already a complex network of reactions which included amino acid, nucleotide, fatty acid, sugar and coenzyme metabolism. In addition, genetic processes such as translation are conserved and close to the original form. However, other processes such as DNA replication and repair or transcription are exceptional and seem to be associated with the structural changes that drove eukaryotes and bacteria away from their common ancestor. There are two major hypotheses in the present work: first, that archaea are probably closer to the last universal ancestor than any other extant life form, and second, that the major cellular processes were in place before the major splitting. The last universal ancestor had metabolism and translation very similar to the contemporary ones, while having an operonic genome organization and archaean-like transcription. Evidently, all cells today contain remnants of the primordial genome of the last universal ancestor.

A gene, han1A, encoding an archaeal histone-like protein from the Thermococcus species AN1: homology with eukaryal histone consensus sequences and the implications for delineation of the histone fold

The han1A gene, encoding a subunit of the histone-like protein HAN1 from the Thermococcus species AN1, has been cloned and sequenced. Sequence analysis of the translation product of the gene demonstrates homology with other archaeal histone-like proteins of the 'HMf family' and eukaryal consensus sequences, particularly H4. The region of highest homology between the AN1 histone subunit, termed the HAN1A1 subunit, and the H4 consensus is suggested, by the 3-dimensional structure of the histone octamer, to interact with the minor groove of DNA. The results presented add further weight to the notion that the 'archaeal histones' and the eukaryal histones are indeed related and that the approximate 65 amino acid residue length of the archaeal histones represents the archaeal equivalent of the histone fold structural building block common to all eukaryal histones.

Histones and chromatin structure in hyperthermophilic Archaea

HMf is a histone from the hyperthermophile Methanothermus fervidus. It is the archetype and most studied member of a family of archaeal histones that have primary sequences and three-dimensional structures in common with the eukaryal nucleosome core histones and that bind and compact DNA molecules into nucleosome-like structures (NLS). HMf preparations are mixtures of two similar, small (approximately 7.5 kDa) polypeptides designated HMfA and HMfB that in vivo form both homodimers and heterodimers. HMfA synthesis predominates during exponential growth but the relative amount of HMfB increases as M. fervidus cells enter the stationary growth phase. Analyses of homogeneous preparations of recombinant (r) (HMfA)2 and (rHMfB)2 have demonstrated that these proteins have different DNA-binding and compaction properties in vitro, consistent with different roles in vivo for the (HMfA)2, (HMfB)2 and HMfA. HmfB dimers, and for the NLS that they form, in regulating gene expression and in genome compaction and stability.

Purification and characterization of a histone-like protein from the Archaeal isolate AN1, a member of the Thermococcales

We have purified and characterized the histone-like protein, termed HAN1, and an HAN1-associated DNA-binding protein (hDBP) from nucleoids of the hyperthermophilic Thermococcus-like AN1. HAN1 is shown to be composed of two subunits, to be thermally stable and to compact DNA in a reversible manner. The N-terminal sequence of HAN1 shares a high degree of homology with HMf, the histone-like protein from Methanothermus fervidus. Consistent with this, the toroidal wrapping of DNA by HAN1 resembles that described for HMf. However, significant differences in both twist and writhe components of these complexes are indicated by the 12.0 bp helical repeat produced during hydroxyl radical footprinting with HAN1. Furthermore, the increased stability of HAN1: DNA complexes allows DNA to be protected from thermal denaturation and cleavage by the restriction enzyme TaqI at 65 degrees C. The hDBP, which co-purified with HAN1,is shown to represent a major portion of the acid-washed nucleoid protein in AN1 and to enhance the mobility of DNA directly, yet decrease the mobility of HAN1:DNA complexes.

Parallel origins of the nucleosome core and eukaryotic transcription from Archaea

Computational sequence analysis of 10 available archaean histone-like proteins has shown that this family is not only divergently related to the eukaryotic core histones H2A/B, H3, and H4, but also to the central domain of subunits A and C of the CCAAT-binding factor (CBF), a transcription factor associated with eukaryotic promoters. Despite the low sequence identity, it is unambiguously shown that the core histone fold shares a common evolutionary history. Archaean histones and the two CBF families show a remarkable variability in contrast to eukaryotic core histones. Conserved residues shared between families are identified, possibly being responsible for the functional versatility of the core histone fold. The H4 subfamily is most similar to archaean proteins and may be the progenitor of the other core histones in eukaryotes. While it is not clear whether archaean histones are more actively involved in transcription regulation, the present observations link two processes, nucleosomal packing and transcription in a unique way. Both these processes, evidently hybrid in Archaea, have originated before the ermergence of the eukaryotic cell.

An abnormally acidic TATA-binding protein from a hyperthermophilic archaeon

The gene encoding the TATA-binding protein (PkTBP) from a hyperthermophilic archaeon, Pyrococcus sp. KOD1 (Pk), was cloned and sequenced. An open reading frame with homology to the conserved C-terminal core region of eukaryotic TBP was expressed in Escherichia coli. Specific DNA-binding activity of the recombinant PkTBP (190 amino acids, 21.36 kDa) was also demonstrated. Although it was composed of a structurally direct repeat sequence which is similar to eukaryotic TBP, the total net charge of archaeal TBP was amazingly negative (calculated isoelectric point (pI) was 4.66 and experimentally estimated pI was 4.8). A series of five Glu residues was found at the C terminus of archaeal TBP. These data strongly suggest that a positively charged protein is also involved in the transcription initiation event which might stabilize the structure of the genomic DNA under high-growth-temperature conditions.

Structure and stability of histone HMf from the hyperthermophilic archaeon Methanothermus fervidus

The secondary and quaternary structures and stabilities of recombinant (r) forms of the HMfA and HMfB histones from Methanothermus fervidus have been investigated by CD spectroscopy and formaldehyde-mediated protein-protein cross-linking. Both proteins were shown to be dimers in solutions containing 5-1300 mM KCl, at pH 6-10 and 25-83 degrees C, and specifically in 1 M KCl, at pH 7.5 and 83 degrees C, conditions which approximate those in vivo in M. fervidus cells. Heat treatment of a mixture of rHMfA and rHMfB homodimers resulted in the formation of rHMfA.rHMfB heterodimers, as demonstrated by two-dimensional PAGE. Heterodimer formation did not result in a CD-detectable conformational change from the homodimer states, indicating that homogeneous (rHMfA)2 and (rHMfB)2 preparations may be considered as structural models of heterodimers. At pH 2, both rHMfA and rHMfB were denatured under low-salt (< 0.2 M KCl) conditions, and their conformations were stabilized in a cooperative manner by increasing KCl concentration, with cooperativity constants for KCl uptake of 2.7 and 3.1, respectively. The alpha-helical conformations of rHMfA and rHMfB were salt-dependent, at both pH 2 and pH 7.5, with maximal helicities in 1 M KCl of 84% and 63% at pH 2, and 72% and 65% at pH 7.5, respectively. The data obtained indicate that the structures of HMfA and HMfB, in 100-200 mM KCl at pH 7.5 and 25 degrees C, are likely to be very similar to their in vivo structures, even though these conditions are far removed from those found in vivo.(ABSTRACT TRUNCATED AT 250 WORDS)

Extremozymes: expanding the limits of biocatalysis

The study of enzymes isolated from organisms inhabiting unconventional ecosystems has led to the realization that biocatalysis need not be constrained to mild conditions and can be considered at pH's, temperatures, pressures, ionic and solvent environments long thought to be destructive to biomolecules. Parallel to this, it has been demonstrated that even conventional enzymes will catalyze reactions in solvents other than water. However, the intrinsic basis for biological function under extreme conditions is only starting to be addressed, as are associated applications. This was the focus of a recent NSF/NIST-sponsored workshop on extremozymes. Given the information acquired from the study of extremozymes, modification of enzymes to improve their ranges of stability and activity remains a possibility. Ultimately, by expanding the range of conditions suitable for enzyme function, new opportunities to use biocatalysis will be created.

Methanobacterium formicicum, a mesophilic methanogen, contains three HFo histones

The mesophilic methanogen Methanobacterium formicicum JF-1 has been shown to contain three members of the HMf family of archaeal histones, designated HFoA1, HFoA2, and HFoB, and their encodinig genes (hfoA1, hfoA2, and hfoB) have been cloned and sequenced. The HFo histones have primary sequences that are 75 to 82% identical to the HMf sequences and appear to share ancestry with the core histones that form the eukaryal nucleosome. The HFo proteins bind and compact DNA molecules into nucleosome-like structures apparently identical to those formed by the HMf proteins, but, in contrast to the HMf proteins, this activity of the HFo proteins is lost after incubation at 95 degrees C for 5 h.