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Updated: Aug 13, 2026

X-Ray Crystallography to Study the Oligomeric State Transition of the Thermotoga maritima M42 Aminopeptidase TmPep1050
Published on: May 13, 2020
Crystal structures of recombinant histones HMfA and HMfB from the hyperthermophilic archaeon Methanothermus fervidus
K Decanniere1, A M Babu, K Sandman
1Forschungsgruppe Kristallographie, Max-Delbrück-Centrum für Molekulare Medizin, Robert-Rössle-Str. 10, Berlin, D-13125, Germany.
Abstract:
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.
Insights
Structural analysis of archaeal histones HMfA and HMfB reveals conserved features and unique dimer interfaces. These findings provide insights into the evolution of histone proteins and their interaction with DNA in hyperthermophilic archaea.
Area of Science:
- Structural biology
- Archaeal genomics
- Molecular evolution
Background:
- Methanothermus fervidus, a hyperthermophilic archaeon, possesses two small basic proteins, HMfA and HMfB.
- These proteins are evolutionarily related to eukaryal nucleosome core histones (H2A, H2B, H3, H4).
- HMfA and HMfB exhibit sequence variations, differing stabilities, and distinct DNA complex mobilities.
Purpose of the Study:
- To elucidate the crystal structures of recombinant HMfA and HMfB.
- To characterize the structural basis of their dimerization and DNA interactions.
- To compare archaeal histone structures with their eukaryal counterparts.
Main Methods:
- X-ray crystallography was employed to determine the structures of recombinant HMfA (tetragonal and orthorhombic forms) and rHMfB.
- Structure refinement was performed to high resolutions (1.48–1.9 Å).
- Homology modeling was used to present a model of the (rHMfA)2-DNA complex.
Main Results:
- Crystal structures reveal that HMfA and HMfB monomers adopt histone folds with three alpha-helices and two loops containing beta-extended conformations.
- Both proteins form homodimers through anti-parallel alignment of their central alpha-helices, stabilized by beta-ladders.
- A novel N-terminal proline-tetrad structure is formed upon dimerization, likely conserved across archaeal histones.
- Differences in side-chain interactions were identified between HMfA and HMfB, influencing their structural stability and DNA binding.
Conclusions:
- The determined structures provide detailed insights into the folding and dimerization of archaeal histones.
- The conserved proline-tetrad structure suggests a common mechanism for archaeal histone dimerization.
- The study offers a structural basis for understanding histone-DNA interactions in archaea and their evolutionary relationship to eukaryotes.
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