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.

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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