Abstract.A phylogenetic analysis of the five major families of DNA polymerase is presented. Viral and plasmid sequences are included in this compilation along with cellular enzymes. The classification by Ito and Braithwaite (Ito and Braithwaite 1991) of the A, B, C, D, and X families has been extended to accommodate the "Y family" of DNA polymerases that are related to the eukaryotic RAD30 and the bacterial UmuC gene products. After analysis, our data suggest that no DNA polymerase family was universally conserved among the three biological domains and no simple evolutionary scenario could explain that observation. Furthermore, viruses and plasmids carry a remarkably diverse set of DNA polymerase genes, suggesting that lateral gene transfer is frequent and includes non-orthologous gene displacements between cells and viruses. The relationships between viral and host genes appear very complex. We propose that the gamma DNA polymerase of the mitochondrion replication apparatus is of phage origin and that this gene replaced the one in the bacterial ancestor. Often there was no obvious relation between the viral and the host DNA polymerase, but an interesting exception concerned the family B enzymes: in which ancient gene exchange can be detected between the viruses and their hosts. Additional evidence for horizontal gene transfers between cells and viruses comes from an analysis of the small damage-inducible DNA polymerases. Taken together, these findings suggest a complex evolutionary history of the DNA replication apparatus that involved significant exchanges between viruses, plasmids, and their hosts.

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Dominant coral-associated Endozoicomonas bacteria species are hypothesized to play a role in the coral sulfur cycle by metabolizing dimethylsulfoniopropionate (DMSP) into dimethylsulfide (DMS); however, no sequenced genome to date harbors genes for this process. In this study, we assembled high-quality (>95% complete) draft genomes of strains of the recently added species Endozoicomonas acroporae (Acr-14 T , Acr-1, and Acr-5) isolated from the coral Acropora sp. and performed a comparative genomic analysis on the genus Endozoicomonas. We identified DMSP CoA-transferase/lyase-a dddD gene homolog in all sequenced genomes of E. acroporae strains-and functionally characterized bacteria capable of metabolizing DMSP into DMS via the DddD cleavage pathway using RT-qPCR and gas chromatography (GC). Furthermore, we demonstrated that E. acroporae strains can use DMSP as a carbon source and have genes arranged in an operon-like manner to link DMSP metabolism to the central carbon cycle. This study confirms the role of Endozoicomonas in the coral sulfur cycle.

Both bacteria and algal symbionts (genus Symbiodinium), the two major microbial partners in the coral holobiont, respond to fluctuations in the environment, according to current reports; however, little evidence yet indicates that both populations have any direct interaction with each other in seasonal fluctuation. In this study, we present field observations of a compositional change in bacteria and Symbiodinium in the coral Isopora palifera in three separate coral colonies following monthly sampling from February to November in 2008. Using massively parallel pyrosequencing, over 200 000 bacterial V6 sequences were classified to build the bacterial community profile; in addition, the relative composition and quantity of Symbiodinium clades C and D were determined by real-time PCR. The results showed that coral-associated bacterial and Symbiodinium communities were highly dynamic and dissimilar among the tagged coral colonies, suggesting that the effect of host specificity was insignificant. The coral-associated bacterial community was more diverse (Shannon index up to 6.71) than previous estimates in other corals and showed rapid seasonal changes. The population ratios between clade C and D groups of Symbiodinium varied in the tagged coral colonies through the different seasons; clade D dominated in most of the samples. Although significant association between bacteria and symbiont was not detected, this study presents a more detailed picture of changes in these two major microbial associates of the coral at the same time, using the latest molecular approaches.

Summary HF2 is a haloarchaeal virus infecting twoHalorubrum species (Family Halobacteriaceae). It is lytic, has a head-and-tail morphology and belongs to the Myoviridae (contractile tails). The linear double-stranded DNA genome was sequenced and found to be 77 670 bp in length, with a mol% G+C of 55.8. A total of 121 likely open reading frames (ORFs) were identified, of which 37 overlapped at start and stop codons. The predicted proteins were usually acidic (average pI of 4.8), and less than about 12% of them had homologues in the sequence databases. Four complete tRNA-like sequences (tRNA-Arg, -Asx, -Pro and -Tyr) and an incomplete tRNA-Thr were detected. A transcription map showed that most of the genome was transcribed and that the synthesis of transcripts occurred in a highly organized and reproducible pattern over a 5 h infection cycle. Transcripts often spanned multiple ORFs, suggesting that viral genes were organized into operons. The predicted ORF and observed transcript directions matched well and showed that transcription is mainly directed inwards from the genome termini, meeting at about 45-48 kb, and this was also a turning point in a cumulative GCskew plot. The low point in cumulative GC-skew, near the left end, was a region rich in short repeats and lacking ORFs, which is likely to be an origin of replication. The HF2 genome is a mosaic of components from widely different sources, demonstrating clearly that viruses of haloarchaea, like their bacteriophage counterparts, are vectors for the exchange and trans-

It has been proposed that the chemical composition of a coral’s mucus can influence the associated bacterial community. However, information on this topic is rare, and non-existent for corals that are under thermal stress. This study therefore compared the carbohydrate composition of mucus in the coral Acropora muricata when subjected to increasing thermal stress from 26 to 31°C, and determined whether this composition correlated with any changes in the bacterial community. Results showed that, at lower temperatures, the main components of mucus were N-acetyl glucosamine and C6 sugars, but these constituted a significantly lower proportion of the mucus in thermally stressed corals. The change in the mucus composition coincided with a shift from a γ-Proteobacteria- to a Verrucomicrobiae- and α-Proteobacteria-dominated community in the coral mucus. Bacteria in the class Cyanobacteria also started to become prominent in the mucus when the coral was thermally stressed. The increase in the relative abundance of the Verrucomicrobiae at higher temperature was strongly associated with a change in the proportion of fucose, glucose, and mannose in the mucus. Increase in the relative abundance of α-Proteobacteria were associated with GalNAc and glucose, while the drop in relative abundance of γ-Proteobacteria at high temperature coincided with changes in fucose and mannose. Cyanobacteria were highly associated with arabinose and xylose. Changes in mucus composition and the bacterial community in the mucus layer occurred at 29°C, which were prior to visual signs of coral bleaching at 31°C. A compositional change in the coral mucus, induced by thermal stress could therefore be a key factor leading to a shift in the associated bacterial community. This, in turn, has the potential to impact the physiological function of the coral holobiont.

Halovirus PH1 infects Haloarcula hispanica and was isolated from an Australian salt lake. The burst size in single-step growth conditions was 50–100 PFU/cell, but cell density did not decrease until well after the rise (4–6 hr p.i.), indicating that the virus could exit without cell lysis. Virions were round, 51 nm in diameter, displayed a layered capsid structure, and were sensitive to chloroform and lowered salt concentration. The genome is linear dsDNA, 28,064 bp in length, with 337 bp terminal repeats and terminal proteins, and could transfect haloarchaeal species belonging to five different genera. The genome is predicted to carry 49 ORFs, including those for structural proteins, several of which were identified by mass spectroscopy. The close similarity of PH1 to SH1 (74% nucleotide identity) allowed a detailed description and analysis of the differences (divergent regions) between the two genomes, including the detection of repeat-mediated deletions. The relationship of SH1-like and pleolipoviruses to previously described genomic loci of virus and plasmid-related elements (ViPREs) of haloarchaea revealed an extensive level of recombination between the known haloviruses. PH1 is a member of the same virus group as SH1 and HHIV-2, and we propose the name halosphaerovirus to accommodate these viruses.