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Roger A Garrett

Publications and source records attributed to Roger A Garrett.

21 records · Page 2Linked to original sources

Relationships between fuselloviruses infecting the extremely thermophilic archaeon Sulfolobus: SSV1 and SSV2.

The fusellovirus SSV2 from an Icelandic Sulfolobus strain was isolated, characterized and its complete genomic sequence determined. SSV2 is very similar in morphology, replication, genome size and number of open reading frames (ORFs) to the type virus of the family, SSV1 from Japan, except in its high level of uninduced virus production. The nucleotide sequences are, however, only 55% identical to each other, much less than related bacteriophage, related animal viruses and the rudiviruses of Sulfolobus, SIRV1 and SIRV2. Nevertheless the genome architecture is very similar between the two viruses, indicating that despite this genomic dissimilarity the virus genomes are mostly homologous. Unlike SSV1, the sequence of SSV2 indicates integration into a glycyl tRNA gene and is completely missing a DNA packaging gene. There is a unique, perfectly tandemly directly repeated sequence of 62 nucleotides in SSV2 that has no similarity to known sequences or structures. By comparison to the SSV2 genome, an integrated partial fusellovirus genome was found in the Sulfolobus solfataricus P2 genome further confirming the dynamism of the Sulfolobus genome. Clustering of cysteine codon containing ORFs both in SSV1 and SSV2 indicates that these Fuselloviridae arose from a genome fusion event.

Fuselloviridae↗

Genus-specific protein binding to the large clusters of DNA repeats (short regularly spaced repeats) present in Sulfolobus genomes.

Short regularly spaced repeats (SRSRs) occur in multiple large clusters in archaeal chromosomes and as smaller clusters in some archaeal conjugative plasmids and bacterial chromosomes. The sequence, size, and spacing of the repeats are generally constant within a cluster but vary between clusters. For the crenarchaeon Sulfolobus solfataricus P2, the repeats in the genome fall mainly into two closely related sequence families that are arranged in seven clusters containing a total of 441 repeats which constitute ca. 1% of the genome. The Sulfolobus conjugative plasmid pNOB8 contains a small cluster of six repeats that are identical in sequence to one of the repeat variants in the S. solfataricus chromosome. Repeats from the pNOB8 cluster were amplified and tested for protein binding with cell extracts from S. solfataricus. A 17.5-kDa SRSR-binding protein was purified from the cell extracts and sequenced. The protein is N terminally modified and corresponds to SSO454, an open reading frame of previously unassigned function. It binds specifically to DNA fragments carrying double and single repeat sequences, binding on one side of the repeat structure, and producing an opening of the opposite side of the DNA structure. It also recognizes both main families of repeat sequences in S. solfataricus. The recombinant protein, expressed in Escherichia coli, showed the same binding properties to the SRSR repeat as the native one. The SSO454 protein exhibits a tripartite internal repeat structure which yields a good sequence match with a helix-turn-helix DNA-binding motif. Although this putative motif is shared by other archaeal proteins, orthologs of SSO454 were only detected in species within the Sulfolobus genus and in the closely related Acidianus genus. We infer that the genus-specific protein induces an opening of the structure at the center of each DNA repeat and thereby produces a binding site for another protein, possibly a more conserved one, in a process that may be essential for higher-order stucturing of the SRSR clusters.

Amino Acid Sequence↗

Mobile elements in archaeal genomes.

The recent availability of several archaeal genome sequences has provided a basis for detailed analyses of the frequency, location and phylogeny of archaeal mobile elements. All the known elements fall into two main types, autonomous insertion sequence (IS) elements and the non-autonomous miniature inverted repeat element (MITE)-like elements. Both classes are considered to be mobilized via transposases that are encoded by the IS elements, although mobility has only been demonstrated experimentally for a few elements. The number, and diversity, of the elements differs greatly between the genomes. At one extreme Sulfolobus solfataricus P2 and Halobacterium NRC-1 are very rich in elements while Methanobacterium thermoautotrophicum contains none. The former also show examples of complex clusters of interwoven elements. An analysis of the genomic distribution in S. solfataricus suggests that the putative oriC and terC regions act as barriers for the mobility of both IS and MITE-like elements. Moreover, the very high level of truncated IS elements in the genomes of S. solfataricus, Sulfolobus tokodaii and Thermoplasma volcanium suggests that there may be a cellular mechanism for selectively inactivating IS elements at a point when they become too numerous and disadvantageous for the cell. Phylogenetically, archaeal IS elements are confined to 11 of the 17 known families of bacterial and eukaryal IS elements where some generate distinct subgroups. Finally, DNA viruses, plasmids and DNA fragments can also be inserted into, and excised from, archaeal genomes by means of an integrase-mediated mechanism that has special archaeal characteristics.

Crenarchaeota↗