Biomedical subjects

Fabrice Confalonieri

Publications and source records attributed to Fabrice Confalonieri.

4 recordsLinked to original sources

PubMed2005

A diversity of bacteriophage forms and genomes can be isolated from the surface sands of the Sahara Desert.

The surface sands of the Sahara Desert are exposed to extremes of ultraviolet light irradiation, desiccation and temperature variation. Nonetheless, the presence of bacteria has recently been demonstrated in this environment by cultivation methods and by 16S rDNA analyses from total DNA isolated from surface sands. To discern the presence of bacteriophages in this harsh environment, we searched for extracellular phages and intracellularly located phages present as prophages or within pseudolysogens. Mild sonication of the sand, in different liquid culture media, incubated with and without Mitomycin-C, was followed by differential centrifugation to enrich for dsDNA phages. The resulting preparations, examined by electron microscopy, revealed the presence of virus-like particles with a diversity of morphotypes representative of all three major double-stranded DNA bacteriophage families (Myoviridae, Siphoviridae and Podoviridae). Moreover, pulsed-field gel electrophoresis of DNA, extracted from the enriched bacteriophage preparations, revealed the presence of distinct bands suggesting the presence of putative dsDNA phage genomes ranging in size from 45 kb to 270 kb. Characterization of the bacteriophages present in the surface sands of the Sahara Desert extends the range of environments from which bacteriophages can be isolated, and provides an important point of departure for the study of phages in extreme terrestrial environments.

Africa, Northern↗

PubMed2005

Nanoarchaea: representatives of a novel archaeal phylum or a fast-evolving euryarchaeal lineage related to Thermococcales?

BACKGROUND: Cultivable archaeal species are assigned to two phyla -- the Crenarchaeota and the Euryarchaeota -- by a number of important genetic differences, and this ancient split is strongly supported by phylogenetic analysis. The recently described hyperthermophile Nanoarchaeum equitans, harboring the smallest cellular genome ever sequenced (480 kb), has been suggested as the representative of a new phylum -- the Nanoarchaeota -- that would have diverged before the Crenarchaeota/Euryarchaeota split. Confirming the phylogenetic position of N. equitans is thus crucial for deciphering the history of the archaeal domain. RESULTS: We tested the placement of N. equitans in the archaeal phylogeny using a large dataset of concatenated ribosomal proteins from 25 archaeal genomes. We indicate that the placement of N. equitans in archaeal phylogenies on the basis of ribosomal protein concatenation may be strongly biased by the coupled effect of its above-average evolutionary rate and lateral gene transfers. Indeed, we show that different subsets of ribosomal proteins harbor a conflicting phylogenetic signal for the placement of N. equitans. A BLASTP-based survey of the phylogenetic pattern of all open reading frames (ORFs) in the genome of N. equitans revealed a surprisingly high fraction of close hits with Euryarchaeota, notably Thermococcales. Strikingly, a specific affinity of N. equitans and Thermococcales was strongly supported by phylogenies based on a subset of ribosomal proteins, and on a number of unrelated molecular markers. CONCLUSION: We suggest that N. equitans may more probably be the representative of a fast-evolving euryarchaeal lineage (possibly related to Thermococcales) than the representative of a novel and early diverging archaeal phylum.

Crenarchaeota↗

PubMed2003

The 62-kb upstream region of Bombyx mori fibroin heavy chain gene is clustered of repetitive elements and candidate matrix association regions.

We sequenced an 80 kb DNA region containing the complete sequence of the silkworm Bombyx mori fibroin gene and its flanking, especially the upstream, regions (-62 kb). About 30% of the 62 kb upstream region is composed of repetitive elements including short interspersed elements Bm1, long interspersed elements L1Bm and mariner-like elements Bmmar1 which are widespread over the silkworm genome. This 62 kb region is also enriched of commonly considered matrix association region (MAR) motifs. A total of 25 individual MAR recognition signatures (MRSs) were identified, with 24 at the upstream and one at the downstream region. Combining two newly developed MAR prediction programs (MAR-finder and Chrclass), ten candidate MARs were predicted, with five containing MRS and seven related to the repetitive elements. The wide distribution of nested repetitive elements, candidate MARs, DNase I hypersensitive sites and other potential regulatory factors recognition sites indicates this region is probably a unique huge cis-acting element contributing to the regulation of the spatial and temporal specificity and efficiency of fibroin gene expression.

5' Flanking Region↗

PubMed2002

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↗