Group Of Mobile Elements Research Articles

The identification of retro-DNAs in primate genomes as DNA transposons mobilizing via retrotransposition.

Mobile elements (MEs) constitute a major portion of the genome in primates and other higher eukaryotes, and they play important role in genome evolution and gene function. MEs can be divided into two fundamentally different classes: DNA transposons which transpose in the genome in a "cut-and-paste" style, and retrotransposons which propagate in a "copy-and-paste" fashion via a process involving transcription and reverse-transcription. In primate genomes, DNA transposons are mostly dead, while many retrotransposons are still highly active. We report here the identification of a unique group of MEs, which we call "retro-DNAs", for their combined characteristics of these two fundamentally different ME classes. A comparative computational genomic approach was used to analyze the reference genome sequences of 10 primate species consisting of five apes, four monkeys, and marmoset. From our analysis, we identified a total of 1,750 retro-DNAs, representing 748 unique insertion events in the genomes of ten primate species including human. These retro-DNAs contain sequences of DNA transposons but lack the terminal inverted repeats (TIRs), the hallmark of DNA transposons. Instead, they show characteristics of retrotransposons, such as polyA tails, longer target-site duplications (TSDs), and the "TT/AAAA" insertion site motif, suggesting the use of the L1-based target- primed reverse transcription (TPRT) mechanism. At least 40% of these retro-DNAs locate into genic regions, presenting potentials for impacting gene function. More interestingly, some retro-DNAs, as well as their parent sites, show certain levels of expression, suggesting that they have the potential to create more retro-DNA copies in the present primate genomes. Although small in number, the identification of these retro-DNAs reveals a new mean for propagating DNA transposons in primate genomes without active canonical DNA transposon activity. Our data also suggest that the TPRT machinery may transpose a wider variety of DNA sequences in the genomes.

Chromium resistance genetic element flanked by XerC/XerD recombination sites and its distribution in environmental and clinical Acinetobacter strains.

A novel mobile genetic element has been identified in small plasmids isolated from permafrost strains of Acinetobacter lwoffii. This element, designated the chrAB dif module, contains the chromium resistance genes chrA and chrB, functionally active both in the original host strains and after transfer into Acinetobacter baylyi. The 3011 bp chrAB dif module is flanked by XerC/XerD recombination sites highly homologous to those of the site-specific recombination system dif/Xer. Analysis of public databases revealed almost identical variants of the chrAB dif module in different plasmids in strains of various Acinetobacter species predominantly inhabiting the environment (A. lwoffii, Acinetobacter indicus, Acinetobacter idrijaensis, Acinetobacter shindleri and Acinetobacter nosocomialis). Together with previously described Acinetobacter antibiotic resistance elements, the chrAB dif module defines a new group of mobile elements that rely on the dif/Xer system for their mobility. Our observations suggest an ancient origin of the mobile elements flanked by dif sites and their participation in the mobilization of plasmid genes bearing adaptive functions.

The peculiarities of piRNA expression upon heat shock exposure in Drosophila melanogaster.

Different types of stress including heat shock may induce genomic instability, due to the derepression and amplification of mobile elements (MEs). It remains unclear, however, whether piRNA-machinery regulating ME expression functions normally under stressful conditions. The aim of this study was to explore the features of piRNA expression after heat shock (HS) exposure in Drosophila melanogaster. We also evaluated functioning of piRNA-machinery in the absence of major stress protein Hsp70 in this species. We analyzed the deep sequence data of piRNA expression after HS treatment and demonstrated that it modulates the expression of certain double-stranded germinal piRNA-clusters. Notable, we demonstrated significant changes in piRNA levels targeting a group of MEs after HS only in the strain containing normal set of hsp70 genes. Surprisingly, we failed to detect any correlation between the levels of piRNAs and the transcription of complementary MEs in the studied strains. We propose that modulation of certain piRNA-clusters expression upon HS exposure in D. melanogaster occurs due to HS-induced altering of chromatin state at certain chromosome regions.

Integrative conjugative elements (ICEs) of microorganisms

Integrative conjugative elements (ICEs) are a large group of mobile elements found in Gram-positive and Gram-negative bacteria. These genetic elements are replicated by incorporation into the host chromosome, but retain the capability of excision and conjugative transfer. A set of genes in ICEs enables conjugative transfer and control of element removal and integration into the host chromosome. These features indicate that ICEs are directly involved in processes of horizontal transfer of genetic determinants, which increase the adaptive potential of bacterial species, and can also function as universal mobilizing factors for other genetic elements.

Normal and defective mariner-like elements in Rhynchosciara species (Sciaridae, Diptera)

Mariner-like elements are widely present in diverse organisms. These elements constitute a large fraction of the eukaryotic genome; they transpose by a "cut-and-paste" mechanism with their own transposase protein. We found two groups of mobile elements in the genus Rhynchosciara. PCR using primers designed from R. americana transposons (Ramar1 and Ramar2) were the starting point for this comparative study. Genomic DNA templates of four species: R. hollaenderi, R. millerii, R. baschanti, and Rhynchosciara sp were used and genomic sequences were amplified, sequenced and the molecular structures of the elements characterized as being putative mariner-like elements. The first group included the putative full-length elements. The second group was composed of defective mariner elements that contain a deletion overlapping most of the internal region of the transposase open reading frame. They were named Rmar1 (type 1) and Rmar2 (type 2), respectively. Many conserved amino acid blocks were identified, as well as a specific D,D(34)D signature motif that was defective in some elements. Based on predicted transposase sequences, these elements encode truncated proteins and are phylogenetically very close to mariner-like elements of the mauritiana subfamily. The inverted terminal repeat sequences that flanked the mariner-like elements are responsible for their mobility. These inverted terminal repeat sequences were identified by inverse PCR.

A new family of polymerases related to superfamily A DNA polymerases and T7-like DNA-dependent RNA polymerases

Using sequence profile methods and structural comparisons we characterize a previously unknown family of nucleic acid polymerases in a group of mobile elements from genomes of diverse bacteria, an algal plastid and certain DNA viruses, including the recently reported Sputnik virus. Using contextual information from domain architectures and gene-neighborhoods we present evidence that they are likely to possess both primase and DNA polymerase activity, comparable to the previously reported prim-pol proteins. These newly identified polymerases help in defining the minimal functional core of superfamily A DNA polymerases and related RNA polymerases. Thus, they provide a framework to understand the emergence of both DNA and RNA polymerization activity in this class of enzymes. They also provide evidence that enigmatic DNA viruses, such as Sputnik, might have emerged from mobile elements coding these polymerases.This article was reviewed by Eugene Koonin and Mark Ragan.

XylellaandXanthomonasMobil'omics

The gamma-proteobacterium Xanthomonadales groups two closely related genera of plant pathogens, Xanthomonas and Xylella. Whole genome sequencing and comparative analyses disclosed a high degree of identity and co-linearity of the chromosome backbone between species and strains. Differences observed are usually clustered into genomic islands, most of which are delimited by genetic mobile elements. Focus is given in this paper to describe which groups of mobile elements are found and what is the relative contribution of these elements to Xanthomonas and Xylella genomes. Insertion sequence (IS) elements have invaded the Xanthomonas genome several times, whereas Xylella is rich in phage-related regions. Also, different plasmids are found inhabiting the bacterial cells studied here. Altogether, these results suggest that the integrative elements such as phages and transposable elements as well as the episomal plasmids are important drivers of the genome evolution of this important group of plant pathogens.

Local hopping of IS 3 elements into the A+T-rich part of the high-pathogenicity island in Yersinia enterocolitica 1B, O:8

The high-pathogenicity island (Yen HPI) of Yersinia enterocolitica biogroup (BG) 1B strains is associated with mouse virulence. Three repeated sequences are clustered on the A+T-rich part of the Yen HPI downstream of the fyuA yersiniabactin receptor gene in Y. enterocolitica O:8 strains WA-314 and 8081. In addition to IS 1328 and IS 1400, the RS3 repeated sequence consists of a novel insertion sequence, IS 1329, inserted into the remnants of IS 1222. This partial IS retains both 44-bp inverted terminal repeats (ITRs) of IS 1222 but has suffered deletions of different sizes in strains WA-314 and 8081. IS 1329 is 1243-bp long, carries 25-bp imperfect ITRs and two consecutive orfs capable to encode 110-amino acid (aa) and 249-aa proteins, respectively. IS 1329 is present only in BG 1B Y. enterocolitica strains. Similarly to IS 1400, IS 1329 and IS 1222 belong to the IS 3 group of mobile elements and seem to have preference for the ‘local hopping’ into the A+T-rich part of the Yen HPI. These insertion sequences may be responsible for the imprecise deletions of the Yen HPI in strain WA-314.

Local hopping of IS3 elements into the A+T-rich part of the high-pathogenicity island in Yersinia enterocolitica 1B, O:8.

The high-pathogenicity island (Yen HPI) of Yersinia enterocolitica biogroup (BG) 1B strains is associated with mouse virulence. Three repeated sequences are clustered on the A+T-rich part of the Yen HPI downstream of the fyuA yersiniabactin receptor gene in Y. enterocolitica O:8 strains WA-314 and 8081. In addition to IS1328 and IS1400, the RS3 repeated sequence consists of a novel insertion sequence, IS1329, inserted into the remnants of IS1222. This partial IS retains both 44-bp inverted terminal repeats (ITRs) of IS1222 but has suffered deletions of different sizes in strains WA-314 and 8081. IS1329 is 1243-bp long, carries 25-bp imperfect ITRs and two consecutive orfs capable to encode 110-amino acid (aa) and 249-aa proteins, respectively. IS1329 is present only in BG 1B Y. enterocolitica strains. Similarly to IS1400, IS1329 and IS1222 belong to the IS3 group of mobile elements and seem to have preference for the 'local hopping' into the A+T-rich part of the Yen HPI. These insertion sequences may be responsible for the imprecise deletions of the Yen HPI in strain WA-314.

Geochemistry of the M'Passa Pb-Zn deposit (Niari syncline, People's Republic of the Congo). Arguments in favor of a hydrothermal origin

The Pb-Zn deposits of the M'Passa mine are located on faults running in a Combian (i.e., N50°E) direction. The interpretation preferred by most authors over the last decade is that synsedimentary ore concentrations have been redistributed in the vicinity of fault zones. This paper presents the results of a detailed study of the behavior of 11 metallic elements (V, Mn, Fe, Co, Cu, Zn, Mo, Ag, Cd, Sb, Pb) systematically measured along a well-exposed section (94 samples, in 28 of which As was also measured). Principal component analysis of the data shows a regular decrease in the total metal content with increasing distance from the fault zones; it also brings to light groupings of metallic elements into a group of mobile elements (Pb, Zn, Cd) and a group of less mobile elements (Ag, Cu, Mo, Fe, Co). The latter are concentrated in and near the fault zone. This distribution corroborates a normal thermal zoning of elements issued from the faults rather than a lateral leaching of a preexisting ore concentration down the fault zone. A gradient in Fe content in sphalerite observed over both ore trends could also indicate regularly decreasing thermal conditions during ore formation. In addition, exploratory measurements of sulfur isotopes clearly indicate an ore concentration process different from an euxinic process. Other synsedimentary metal concentrations related to organic matter evolution seem difficult to reconcile with the total residual organic carbon content, and characteristic ratios regarding organic carbon do not show at the present time any relation with organic matter evolution. Rather than assuming that all organic indicators were erased during the geological evolution of the M'Passa deposit, a model is preferred in which local hydrothermal deposition issued from the fault and diffused through specific dolomitic strata. Paleokarstic features may be regarded as passive ore reservoirs or could be the result of alteration associated with hydrothermal fluids.