dArchaeal 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 (⌬htkA) resulted in a T. kodakarensis strain that was no longer amenable to transformation, whereas the deletion of TK2289 (⌬htkB) 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.T he histone fold apparently evolved before the archaeal and eukaryotic lineages diverged ϳ1.5 to 1.9 billion years ago, and now almost all eukaryotes, Euryarchaea, Nanoarchaea, Thaumarchaea, and some Crenarchaea employ histone fold-based DNA binding to wrap and compact their genomic DNA (2,9,14,21,28,30,38). All transactions in these species that involve chromosomal DNA must therefore be considered in terms of histone-bound chromatin. The presence of histones in Archaea, but not in Bacteria, was a major distinction first recognized ϳ20 years ago (26), and research since then has established the detailed structure of archaeal histones (3, 19); the composition and architecture of the archaeal nucleosome (11,20,22,24,30); and the consequences of archaeal histone binding on DNA topology, replication, and transcription in vitro (7,37,43,44). Archaeal nucleosomes resemble the eukaryotic tetrasome, the structure at the center of the eukaryotic nucleosome formed by ϳ90 bp of DNA wrapped around a histone (H3ϩH4) 2 tetramer (20,28,30). Archaeal histones do not, however, have homologues of the N-and C-terminal amino acid extensions (21) that contain the targets for eukaryotic histone acetylation and methylation and thus provide the basis for epigenetic regulation. Consistent with this, scrutiny of archaeal genome sequences has failed to detect recognizable homologues of the eukaryotic histone modification systems, and to date, no archaeal histone modification has been described (5). It is therefore intriguing and important to determine if archaeal histones nevertheless participate in regulating genome functions. In this regard, in species ...