The diversity, origin, and evolution of chromoviruses in Eukaryota were examined using the massive amount of genome sequence data for different eukaryotic lineages. A surprisingly large number of novel full-length chromoviral elements were found, greatly exceeding the number of the known chromoviruses. These new elements are mostly structurally intact and highly conserved. Chromoviruses in the key Amniota lineage, the reptiles, have been analyzed by PCR to explain their evolutionary dynamics in amniotes. Phylogenetic analyses provide evidence for a novel centromere-specific chromoviral clade that is widespread and highly conserved in all seed plants. Chromoviral diversity in plants, fungi, and vertebrates, as shown by phylogenetic analyses, was found to be much greater than previously expected. The age of plant chromoviruses has been significantly extended by finding their representatives in the most basal plant lineages, the green and the red algae. The evolutionary origin of chromoviruses has been found to be no earlier than in Cercozoa. The evolutionary history and dynamics of chromoviruses can be explained simply by strict vertical transmission in plants, followed by more complex evolution in fungi and in Metazoa. The currently available data clearly show that chromoviruses indeed represent the oldest and the most widespread clade of Metaviridae.

The cystatin superfamily comprises cysteine protease inhibitors that play key regulatory roles in protein degradation processes. Although they have been the subject of many studies, little is known about their genesis, evolution and functional diversification. Our aim has been to obtain a comprehensive insight into their origin, distribution, diversity, evolution and classification in Eukaryota, Bacteria and Archaea.

We have shown previously by Southern blot analysis that Bov-B long interspersed nuclear elements (LINEs) are present in different Viperidae snake species. To address the question as to whether Bov-B LINEs really have been transmitted horizontally between vertebrate classes, the analysis has been extended to a larger number of vertebrate, invertebrate, and plant species. In this paper, the evolutionary origin of Bov-B LINEs is shown unequivocally to be in Squamata. The previously proposed horizontal transfer of Bov-B LINEs in vertebrates has been confirmed by their discontinuous phylogenetic distribution in Squamata (Serpentes and two lizard infra-orders) as well as in Ruminantia, by the high level of nucleotide identity, and by their phylogenetic relationships. The horizontal transfer of Bov-B LINEs from Squamata to the ancestor of Ruminantia is evident from the genetic distances and discontinuous phylogenetic distribution. The ancestor of Colubroidea snakes is a possible donor of Bov-B LINEs to Ruminantia. The timing of horizontal transfer has been estimated from the distribution of Bov-B LINEs in Ruminantia and the fossil data of Ruminantia to be 40–50 My ago. The phylogenetic relationships of Bov-B LINEs from the various Squamata species agrees with that of the species phylogeny, suggesting that Bov-B LINEs have been maintained stably by vertical transmission since the origin of Squamata in the Mesozoic era.

This study examined the evolutionary dynamics of Bov-B LINEs in vertebrates and the evolution of the RTE clade of non-LTR retrotransposons. The first full-length reptilian Bov-B LINE element is described; it is 3.2 kb in length, with a structural organization typical of the RTE clade of non-LTR retrotransposons. The long-term evolution of Bov-B LINEs was studied in 10 species of Squamata by analysis of a PCR-amplified 1.8-kb fragment encoding part of apurinic/apyrimidinic endonuclease, the intervening domain, and the palm/fingers subdomain of reverse transcriptase. A very high level of conservation in Squamata Bov-B long interspersed nuclear elements has been found, reaching 86% identity in the nearly 600 amino acids of ORF2. The same level of conservation exists between the ancestral snake lineage and Ruminantia. Such a high level is exceptional when compared with the level of conservation observed in nuclear and mitochondrial proteins and in other transposable elements. The RTE clade has been found to be much more widely distributed than previously thought, and novel representatives have been discovered in plants, brown algae, annelids, crustaceans, mollusks, echinoderms, and teleost fishes. Evolutionary relationships in the RTE clade were deduced at the amino acid level from three separate regions of ORF2. By using different independent methods, including the divergence-versus-age analysis, several examples of horizontal transfer in the RTE clade were recognized, with important implications for the existence of HT in non-LTR retrotransposons.