O exossomo é um complexo multiproteico conservado evolutivamente de archaea a eucariotos superiores que desempenha funções celulares essenciais tais como: atividade exoribonucleolítica 3\'→5\', regulação dos níveis de mRNA, maturação de RNAs estruturais e controle de qualidade de RNAs durante os vários estágios do mecanismo de expressão gênica. Em Archaea, o exossomo é composto por até quatro subunidades diferentes, duas com domínios de RNase PH, aRrp41 e aRrp42, e duas com domínios de ligação a RNAs, aCsl4 e aRrp4. Três cópias das proteínas aRrp4 e/ou aCsl4 se associam com o núcleo hexamérico catalítico do anel de RNase PH e completam a formação do complexo. A proteína PaNip7 é um cofator de regulação do exossomo da archaea Pyrococcus abyssi e atua na inibição do complexo enzimático ligando-se simultaneamente ao exossomo e a RNAs. Neste projeto, a reconstituição in vitro do exossomo da archaea Pyrococcus abyssi formado pela proteína de topo PaCsl4 foi obtida. Para tanto foram realizadas análises de interação proteica usando as técnicas de cromatografia de afinidade, gel filtração e SDS-PAGE. Em adição à formação da isoforma PaCsl4-exossomo, um fragmento peptídico correspondente à região C-terminal da PaNip7 foi sintetizado pelo método da fase sólida, purificado por RP-HPLC e o purificado foi caracterizado por LC/ESI-MS almejando realizar futuros experimentos de interação com o exossomo. / The exosome is a multiprotein complex evolutionarily conserved from archaea to higher eukaryotes that performs essential cellular functions such as: 3\'→5\' exoribonucleolytic activity, regulation of mRNA levels, maturation of structural RNAs and quality control of RNAs during the various stages of the gene expression mechanism. In Archaea, the exosome is composed of up to four different subunits, two with RNase PH domains, aRrp41 and aRrp42, and two with RNAs binding domains, aCsl4 and aRrp4. Three copies of the aRrp4 and/or aCsl4 proteins associate with the hexameric catalytic core of the RNase PH ring and complete the formation of the complex. The PaNip7 protein is a regulating cofactor of the Pyrococcus abyssi archaeal exosome and acts in the inhibition of the enzyme complex by binding simultaneously to the exosome and RNAs. In this project, the reconstitution in vitro of the Pyrococcus abyssi archaeal exosome formed by the PaCsl4 top protein was achieved. To this end protein interaction analyses were performed using affinity chromatography, gel filtration and SDS-PAGE techniques. In addition to the formation of the PaCsl4-exosome isoform, a peptide fragment corresponding to the C-terminal region of PaNip7 was synthesized by solid-phase method, purified by RP-HPLC and the purified peptide was characterized by LC/ESI-MS aiming to perform future binding experiments with the exosome.

Les virus peuvent être retrouvés dans tous les écosystèmes où de la vie est présente. Ils constituent l’entité biologique la plus abondante de la biosphère. Si de nombreuses données sont disponibles sur l’abondance et la dynamique virale dans les écosystèmes aquatiques tempérés, peu d’études ont été menées sur ces aspects dans les milieux extrêmes, dont les sources hydrothermales. Dans l’étude présentée dans ce manuscrit, les communautés procaryotiques et virales des sources hydrothermales des Terres australes et antarctiques françaises (TAAF) ont été explorées. Dans un premier temps, les cellules procaryotiques et les particules de type viral (VLP) ont été dénombrées dans plusieurs sources chaudes terrestres et marines côtières. L’abondance microbienne et virale est de l’ordre de 105 - 106 particules/ml dans les deux types de sources avec des rapports VLP/procaryotes (VPR) qui sont généralement faibles, concordant ainsi avec rares les données disponibles actuellement dans la littérature. Dans un second temps, la diversité morphologique des VLP a été analysée par observation au microscope électronique à transmission. La présence de VLP de morphologies différentes a pu être constatée dans quelques échantillons bruts, mais également dans des cultures d’enrichissement, où elles étaient associées à des Thermococcales et des Thermotogales. Finalement, quelques souches isolées de ces échantillons ont été criblées pour la présence de virus aboutissant à la description d’un nouveau bactériovirus tempéré associé à une bactérie thermophile Geobacillus. L’effet d’un choc osmotique en présence de NaCl et l’effet d’un stress anoxique sur la production virale ont également été étudiés. La caractérisation du virus GTV1 a ensuite été entamée. Il appartient à la famille des Myoviridae et a un génome composé d’ADN double brin de 38841 pb, composé de 71 ORF prédits. Enfin, l’étude de la diversité microbienne a permis de décrire une nouvelle espèce bactérienne hautement thermophile, Calditerricola clavaformis sp.nov. / Viruses thrive in all types of ecosystems where life is found. They represent the most abundant biological entity of our biosphere. Though several studies have been conducted on viral abundance and dynamics in mesophilic aquatic ecosystems, these aspects remain largely unexplored in extremophilic environments, such as hot springs. In this study, prokaryotic and associated viral communities of the French Southern and Antarctic Lands hot springs were explored. First, prokaryotic cells and Virus-like particles (VLP) were enumerated in several terrestrial and inshore hot springs. The results reveal an abundance of 105 - 106 particles/ml in both types of hot springs studied. The virus-to-prokaryote ratios (VPR) were generally low, confirming thus actual knowledge in these types of ecosystems. The morphological diversity of VLP was then studied in raw samples as well as in enrichment cultures containing Thermococcales and Thermotogales. Several isolates obtained from these samples were then screened for viral particles which led to the discovery and description of a temperate phage (GTV1) of a thermophilic bacterium belonging to the genus Geobacillus. The effect of NaCl and anoxic stress on the viral production was studied. The genomic characterization of the GTV1 was started and revealed a 38441 bp genome with 71 predicted ORF. Finally, microbial diversity studies led also to the discovery of a new extremely thermophilic bacterium, Calditerricola clavaformis sp.nov.

PII-Proteine, zu denen GlnB und GlnK zählen, sind ubiquitär verbreitete kleine Regulatorproteine, die den internen Stickstoffzustand der Zelle sensieren und weiterleiten und hierdurch maßgeblich an der Regulation des Stickstoffmetabolismus beteiligt sind.Ziel dieser Arbeit war es, das GlnK1-Protein aus dem methanogenen Archeaon Methanosarcina mazei Stamm Gö1 umfassend zu charakterisieren und seine potentielle Rolle in der Regulation des Stickstoffmetabolismus aufzuklären. Das M. mazei GlnK1-Protein weist den typischen Tyrosin51-Rest auf, der in Bakterien stickstoffabhängig posttranslationell modifiziert wird. Sowohl in vitro als auch in vivo Experimente haben jedoch gezeigt, dass GlnK1 in M. mazei nicht stickstoffabhängig modifiziert wird. Weitere strukturelle Unterschiede zu bakteriellen PII-Proteinen haben Experimente zur Bildung von Heterotrimeren aufgezeigt. Trotz dieser deutlichen Unterschiede haben Komplementationsversuche ergeben, dass das archaeelle GlnK-Protein in der Lage ist, E. coli GlnK funktionell zu komplementieren. Dieses läßt darauf schließen, dass das GlnK1-Protein in M. mazei auch in der Regulation des Stickstoffmetabolismus involviert ist. Um dieses zu bestätigen, wurde eine chromosomale M. mazei glnK1-Mutante generiert. Hierfür war es erforderlich, zunächst ein funktionelles System zur Transformation von M. mazei Gö1 zu entwickeln. Es gelang, (i) durch Selektion einer potentiellen spontanen Zellwandmutante von M. mazei, die eine stark verbesserte Plattierungseffizienz aufwies, sowie (ii) durch mehrere Modifizierungen des von W. Metcalf (Urbana) entwickelten Liposomen-vermittelten Transformationsprotokolls für Methanosarcina-Stämme M. mazei Gö1 genetisch zugänglich zu machen. Wachstumsanalysen des konstruierten M. mazei glnK1-Mutantenstamms zeigten einen partiell reduzierten Wachstumsphänotyp unter stickstofflimitierenden Bedingungen. Quantitative Reverse Transkriptions-PCR Analysen ausgewählter Gene ergaben allerdings, dass das GlnK1 keinen Einfluss auf die Transkription stickstoffregulierter Gene ausübt.Sowohl biochemische Experimente mit gereinigtem Enzym als auch in vivo Versuche zeigten jedoch, dass das GlnK1-Protein mit der Glutamin-Synthetase (GlnA) interagiert und hierdurch deren Enzymaktivität inhibiert. Ein aktivierender Effekt auf die GlnA Enzymaktivität wurde hingegen bei Anwesenheit von 2-Oxoglutarat beobachtet, welches den internen Stickstoffstatus wiederspiegelt. Aus der Gesamtheit der Ergebnisse läßt sich folgendes hypothetisches Regulationsmodel ableiten: Unter Stickstofflimitierung wird 2-Oxoglutarat akkumuliert, welches die Glutamine-Synthetase Aktivität stark stimuliert; bei einem Übergang zu Stickstoffüberschuss wird die Glutamine-Synthetase sowohl durch einen reduzierten 2-Oxoglutarat-Spiegel als auch durch direkte Protein-Interaktion mit GlnK1 inaktiviert. Letzteres dient der Feinregulation und ermöglicht schnell auf eine veränderte Stickstoffversorgung reagieren zu können.

Les nanoparticules métalliques manufacturées (NPs) sont des polluants émergents dont la concentration augmente dans les sols en raison de leur utilisation croissante dans de nombreux produits commerciaux de la vie courante (cosmétiques, aliments, peintures…). Des études in vitro ont montré la toxicité des NPs pour les microorganismes, mais il existe encore peu de données sur l'écotoxicité et le devenir de ces contaminants dans les sols. L'objectif de cette thèse est donc d'évaluer l'influence des paramètres abiotiques du sol sur (i) les caractéristiques physico-chimiques et le transfert des NPs, et (ii) sur la toxicité des NPs pour les communautés microbiennes du sol, en particulier pour des groupes fonctionnels microbiens impliqués dans le cycle du carbone et de l'azote. Nous avons mis en évidence que les propriétés du sol influençaient l'agrégation et la charge de surface des NPs de dioxyde de titane (TiO2) et d'oxyde de cuivre (CuO). Dans les six sols agricoles étudiés, nous avons observé un transport très faible des NPs testées lors d'une expérimentation en colonnes de sols. Nous avons mis en évidence une absence de toxicité des NPs de TiO2 sur les communautés microbiennes, sauf dans un sol limono-argileux à forte teneur en matière organique. Dans ce sol, des effets négatifs ont été observés après 90 jours d'exposition sur les activités microbiennes, sur l'abondance des microorganismes nitrifiants et la diversité des bactéries et des archées. Des études complémentaires en colonnes de sol, ont permis de mettre en évidence des effets délétères des NPs plus importants que la nitrification lors d'une contamination chronique au TiO2 que lors d'une contamination aigüe / Manufactured metallic nanoparticles (NPs) are emerging pollutants of soils due to their increasing utilization in numerous commercial products (cosmetics, food, paint…). In vitro studies have demonstrated NPs toxicity on microorganisms but data are still scarce on the fate and ecotoxicity of these contaminants in soils. The objective of this thesis was to assess the influence of soil properties on (i) the physicochemical characteristics and the transport of NPs, and (ii) on the NPs toxicity on soil microbial communities, especially on microbial functional groups involved in carbon and nitrogen cycles. This work highlighted that soil properties influenced the aggregation and the surface charges of titanium dioxide NPs (TiO2-NPs) and copper oxide NPs (CuO-NPs). In the six agricultural soils studied, we observed a very low transport of the two NPs in a soil column experiment. We observed a low toxicity of TiO2-NPs for soil microbial communities, except in a silty-clay soil with a high organic matter content. In this soil, microbial activities (soil respiration, nitrification and denitrification) and nitrifier abundances were strongly decreased and archaeal and bacterial community structure were altered after 90 days of exposure. Furthermore in this soil, we observed decreases of nitrification activity, even for very low TiO2-NPs concentrations (0.05 mg kg-1) which were explained by a high sensitivity of ammonia-oxidizing archaea (AOA) involved in this process. Additional studies in soil columns demonstrated that chronic contamination with TiO2-NPs caused more deleterious effects on nitrification than acute contamination

Deep subsurface rock samples from Upper Ordovician strata in the Michigan Basin were analyzed for the presence of microbial communities. High concentrations of biogenic methane were observed in the Upper and Middle Ordovician formations. Total porosity values for the shale, shale hard bed and limestone samples were 7.4%, 2.5% and 1.9%, respectively. Hydrocarbon presence ranged from petroliferous shale, to bituminous layering in shale hard beds, to hydrocarbon odour in limestone. Organic carbon content ranged from 0.5 to 2.5%, highest amount being present in the shale. Environmental DNA was extracted from core samples and PCR amplified using 16S rDNA bacterial primers. PCR performed with archaeal 16S rDNA and methanogen-specific (mcrA) primers did not yield DNA amplification. Gene analysis indicated that bacterial sequences similar to Proteobacteria, Cyanobacteria, Firmicutes, and Actinobacteria were present. Most sequences were not related to known cultivated species. Proteobacteria was the most dominant phyla at all depths and included heterotrophic, lithotrophic, acidophilic, radiotolerant, and sulphate-reducing species of bacteria. This study concludes that the observed biogenic methane is a product of ancient methanogenesis.

O presente trabalho foi desenvolvido com o objetivo de verificar a eficiência de um reator anaeróbio híbrido (RAH) alimentado com uma mistura de ácidos orgânicos acético, propiônico, butírico, e láctico, bem como do álcool metanol, perfazendo uma DQO de 6,88 g/L, e avaliar nessas condições, a degradação do pentaclorofenol (PCP) na faixa de 2,0 a 21,0 mg/L. O RAH apresentou adequada performance na ausência de PCP, tendo sido inoculado com um lodo com AME cerca de 0,57 g DQO-CH4/g SV.d. Durante os 21 meses de operação do RAH na ausência de PCP verificou-se uma remoção média de DQO de 93% produção média de metano de 84%. Através de testes de toxicidade realizadas em batelada com o lodo granulado do RAH, antes da adição de PCP no reator, calculou-se o IC50, cujos valores foram 10, 12 e 13,69 mg/L. Na presença de PCP na faixa de 2,0 a 2,1 mg/L, o RAH apresentou remoção média de DQO de 96,7%, produção média de metano de 85,5% e remoção dos ácidos voláteis próxima a 74% do acético, 93% do butírico e 64% do propiônico. Individualmente, na presença da maior concentração de PCP adicionada, ocorreu decréscimo na remoção dos ácidos voláteis, principalmente do ácido propiônico e na taxa de conversão DQO/biogás. O PCP foi removido do sistema na ordem de 99% pela ação do lodo granulado com predominância do grupo das Archaea metanogênicas, verificada por exames microscópicos e hibridação \"in situ\". Valores da ordem de grandeza microbiana para os microrganismos metanogênicos nos períodos anteriores e posteriores a adição de PCP permaneceram na faixa de 105 e 106 céls./mL, quando cultivados em metanol e lactato mais sulfato, respectivamente. Os resultados sugerem que as Archaea metanogênicas podem estar envolvidas na degradação do PCP. A velocidade de remoção do organoclorado foi igual a 1,07 mg PCP/g SV.d quando a maior concentração de PCP foi estudada (21,0 mg/L). / The present research aimed to verify the efficiency of an Anaerobic Hybrid Reactor (AHR) supplied with a mixture of fatty acids, acetic, propionic, butyric and lactic and methanol as well. The total amount of COD was 6.88 g/L. The performance of the reactor was remarkably stable and efficient during PCP additions at range from 2.0 to 21.0 mg/L. The AHR showed a great performance in the PCP absence, inoculated with sludge with an specific methanogenic (SMA) activity of 0,057 g.COD-CH4/g. VS.d. During the 21 months of operation without PCP, the reduction of COD was around 93% and methane was up to 84% in the biogas. Before PCP addiction, two toxicity batch tests conducted with the granular sludge presented IC50 values around 10.12 mg/L and 13.69 mg/L. In the presence of PCP, at the range of 2.0 to 21.0 mg/L, the efficiency of volatile fatty acids breakdown was 93%, 64% and 74% respectively for butyric, propionic and acetic acids. Individually, at the presence of the higher PCP concentration studied, a decrease in the conversion of COD to biogas and organic acids removal occurred, mainly with propionic acid. PCP total removal of more than 99% was reached by granular sludge activities formed by the total time of reactor operation with a prevalence of methanogenic Archaea, verified under direct microscopy exams and in situ hybridization. Methanogenic cells predominance was noticed with 105 to 106 cells/mL during enumeration on methanol and lactate plus sulfate culture media, respectively. The results suggest that methanogenic Archaea can be involved in PCP degradation. The organochlorine removal rate was 1.07 mg PCP.g-1 VS.d-1 during the highest PCP (21.0 mg/L) concentration addition.

Os impactos da poluição por hidrocarboneto de petróleo sobre a diversidade e funcionalidade das comunidades microbianas em manguezais não são totalmente conhecidos, principalmente devido às limitações metodológicas para acessar os microrganismos nãocultiváveis. No entanto, vários métodos moleculares independentes de cultivo têm sido utilizados para investigar a diversidade e a estrutura das comunidades microbianas em ecossistemas naturais. O objetivo deste trabalho foi avaliar as variações da estrutura das comunidades de Bacteria e Archaea e a diversidade de Bacteria em uma transeção de solo de mangue do rio Iriri (Bertioga, SP) com um gradiente de contaminação por hidrocarbonetos de petróleo. As análises por eletroforese em gel com gradiente desnaturante (DGGE) mostraram que as comunidades de Bacteria e Archaea nas diferentes posições geográficas foram mais similares entre si do que entre diferentes profundidades ao longo do perfil em uma mesma posição geográfica. A análise das seqüências de clones de rDNA 16S de Bacteria dos diferentes pontos amostrados em abril de 2000, mostrou que a diversidade genética, avaliada pelo índice de Shannon, das comunidades microbianas diferem estatisticamente somente entre ponto o P1 (ponto menos contaminado) e P3 (ponto mais contaminado). As estimativas não-paramétricas da riqueza de espécies mostraram que P1, P2 e P3 possuem mais de 3539, 2524 e 1421 espécies bacterianas, respectivamente. Já, para as amostras do ponto P2 coletadas nos anos 2000 e 2004, muito embora os valores dos índices de Shannon tenham sido semelhantes, houve uma provável dominância de grupos específicos nas amostras coletadas em 2004, verificada pelos altos valores da recíproca do índice de Simpson. Os dados mostraram também que o número estimado de espécies bacterianas no ponto P2 diminuiu com o tempo, sendo menor em amostras de 2004, se comparado com amostras de 2000. No geral, a afiliação filogenética dos clones de rDNA 16S mostrou a grande diversidade de espécies, a maioria não conhecidas. Os dados sugerem que a contaminação do solo de mangue do rio Iriri está selecionando microrganismos mais adaptados às fontes de carbono introduzidas no solo. / The impacts of petroleum hydrocarbon pollution on the diversity and functionality of the microbial communities in mangrove soils are not totally understood, mainly due to the methodological limitations to access unculturable microorganisms. However, several cultureindependent molecular methods have been used to investigate the diversity and structure of microbial communities in natural ecosystems. The aim of this work was to evaluate shifts in Bacteria and Archaea community structures and the diversity of Bacteria in a soil transection of the Iriri river mangrove (Bertioga, SP) showing a petroleum hydrocarbon contamination gradient. The analyses by denaturing gradient gel electrophoresis (DGGE) showed that the communities of Bacteria and Archaea in different geographical positions were more similar among them than the communities in different depths along the soil profile at the same geographical position. Sequence analyses of bacterial 16S rDNA clones from different points sampled in April 2000 showed that the genetic diversity of the bacterial communities, based on the Shannon index, differ statistically only between P1 (less polluted) and P3 (more polluted) locations. Nonparametric estimates of species richness showed that P1, P2 and P3 may have more than 3539, 2524 and 1421 bacterial species, respectively. For P2 sampled in years 2000 and 2004, even though the Shannon indices were similar, there was a probable dominance of specific bacterial groups in year 2004, based on the high values of the reciprocal of Simpson\'s index. The data also showed that the estimated number of bacterial species in P2 decreased with the time, being lower in samples collected in 2004, as compared to samples collected in 2000. In the general, the phylogenetic affiliation of the 16S rDNA clones showed high bacterial species diversity, and most of the bacteria were of unknown species. The data suggest that the contamination of Iriri river mangrove soil with petroleum hydrocarbon is selecting microorganisms more adapted to the introduced carbon sources into the soil.

No description available.

Les réarrangements permettent une évolution rapide du génome par l’acquisition de séquences codantes exogènes, la perte de fonctions non-essentielles ou la création de nouvelles organisations génomiques. Différents mécanismes de réarrangements impliquant des éléments génétiques mobiles (EGM) ont été identifiés chez les archées, les bactéries et les eucaryotes. En revanche, on ignore l’origine des nombreuses inversions génomiques détectées pour les espèces du genre archéen Thermococcus. Mes travaux de thèse visent à améliorer la compréhension de l’évolution génomique chez les Thermococcales à travers l’étude de deux familles d’EGM : les familles de plasmides pTN3 et pT26-2. Plus précisément, je me suis intéressée aux recombinases à tyrosine (ou intégrases) que ces plasmides encodent et qui permettent leur intégration dans le chromosome de l’hôte. J’ai montré que l’intégrase plasmidique Intᵖᵀᴺ³ est responsable d’inversions dans le chromosome de son hôte Thermococcus nautili grâce à une activité catalytique inédite de recombinaison homologue. J’ai par la suite caractérisé deux autres intégrases de Thermococcales reliés phylogénétiquement à Intᵖᵀᴺ³ dont seulement une présente une activité de recombinaison homologue. La comparaison de leurs séquences primaires et la résolution de la structure de Intᵖᵀᴺ³ vont maintenant éclairer les déterminants génétiques responsables de la spécificité de site et de l’activité de recombinaison homologue. Les trois intégrases appartiennent à une classe de recombinases spécifique des archées qui catalyse une intégration suicidaire. Lors de l’intégration, le gène de l’intégrase est fragmenté et probablement désactivé. L’EGM intégré se retrouve piégé dans le chromosome. Les avantages évolutifs d’une telle activité suicidaire restent pour l’instant mystérieux. J’ai identifié 62 intégrases hyperthermophiles suicidaires et reconstruit leur histoire évolutive. Ces intégrases sont très prévalentes et recrutées par différents EGM. De plus, j’ai montré que l’une de ces intégrases présente in vitro une activité de recombinaison site-spécifique à des températures proches de l’ébullition de l’eau, représentant un avantage dans les environnements hyperthermophiles. / Genomes rapidly evolve through rearrangements that can generate new genome organizations or lead to the acquisition of foreign coding sequences or the loss of non-essential functions. Several mechanisms of rearrangement were uncovered for Archaea, Bacteria and Eukaryotes that involve mobile genetic elements (MGE). Species from the archaeal genera Thermococcus present numerous genomic inversions but none of the previously known inversion drivers. To better understand the genomic evolution of Thermococcales, I investigated two of their MGE families: the pTN3 and pT26-2 plasmid families. Specifically, I focused on the tyrosine recombinases (or integrase) that these plasmids encode and that catalyze their site-specific integration in the host chromosome. I demonstrated that the plasmidic integrase Intᵖᵀᴺ³ is responsible for chromosomal inversions in the host Thermococcus nautili through an unprecedented homologous recombination catalytic activity. I also characterized two other related Thermococcus integrases and only one catalyzes homologous recombination. The structure resolution of Intᵖᵀᴺ³ and primary sequence comparisons will now provide clues about the genetic determinants of site specificity and of the homologous recombination activity. The three integrases all belong to an archaeal-specific class of integrases that catalyzes a suicidal integration. The integrase gene is partitioned and presumably inactivated upon integration. The integrated MGE is then trapped into the chromosome. The evolutionary benefits of this suicide activity are puzzling. I identified 62 related suicidal hyperthermophilic integrases and reconstructed their evolutionary history. They are highly prevalent and recruited by diverse MGE. I also showed that one of these integrases can catalyze in vitro site-specific recombination at near boiling water temperature, representing an advantage in hyperthermophilic environments.

Ce travail de thèse porte sur l’étude de la réplication chez les archées, qui constituent le troisième domaine du vivant avec les bactéries et les eucaryotes. L’organisme modèle que nous avons utilisé est l'archée halophile Haloferax volcanii car les outils génétiques disponibles permettent d’exprimer des protéines fusionnées à la Protéine Fluorescente Verte (GFP) dans cet organisme mésophile et aérobe et ainsi de localiser les protéines d’intérêt dans des cellules vivantes. Nous nous sommes ainsi intéressés à la localisation cellulaire de quatre protéines de la réplication qui ont été fusionnées à la GFP et exprimées sous contrôle de leur propre promoteur : (i) la protéine ‘Flap Endonuclease 1’ (FEN1), qui intervient dans la maturation des fragments d’Okazaki, (ii) la protéine ‘Origin Recognition Complex’ (ORC1) impliquée dans la reconnaissance des origines de réplication, (iii) la protéine ‘Proliferating Cellular Nuclear Antigen’ (PCNA), anneau de processivité des ADN polymérases réplicatives, et (iv) la protéine de fixation à l’ADN simple-brin ‘Replication Protein A’ (RPA2) essentielle à la réplication chez H. volcanii. Seule la protéine PCNA n’a pu être exprimée en fusion avec la GFP, suggérant que la protéine fusion n’est pas fonctionnelle. GFP::Orc1 et GFP::Fen1 ont été exprimées dans la cellule mais ne présentent pas de localisation spécifique reflétant un rôle de ces protéines dans la réplication de l’ADN. En revanche des foyers de fluorescence de la protéine fusion GFP::Rpa2 ont été observés, dont le nombre augmente significativement dans des cellules exposées à l’aphidicoline, drogue inhibant la synthèse de l’ADN et induisant ainsi un stress réplicatif. Cependant une localisation différente de la protéine GFP::Rpa2 a été observée lorsque les cellules sont exposés à la phléomycine, qui induit notamment des cassures double-brin de l‘ADN. Dans ces cellules, GFP::Rpa2 forme un foyer de fluorescence massif qui colocalise avec l’ADN compacté dans la grande majorité des cellules observées. Nos résultats suggèrent donc que la localisation spécifique observée pour GFP::Rpa2 reflète son rôle dans la réparation de l’ADN et/ou le redémarrage des fourche de réplication arrêtées. / The aim of this thesis project was to improve our understanding of DNA replication in archaea, the third domain of life with bacteria and eukarya. The model organism chosen for these studies is the halophilic archaea Haloferax volcanii, a mesophilic aerobe for which genetics tools allow studying in living cells the localization of proteins fused to the Green Fluorescent protein (GFP). Four proteins involved in DNA replication were fused to the GFP and expressed under the control of their own promoter: (i) the ‘Flap Endonuclease 1’ (FEN1), involved in Okazaki fragments maturation, (ii) the ‘Origin Recognition Complex’ (ORC1), involved in DNA replication origin recognition, (iii) the ‘Proliferating Cellular Nuclear Antigen’ (PCNA), processivity factor of replicative DNA polymerases, and (iv) the ‘Replication Protein A’ (RPA2), single-stranded DNA binding protein essential for DNA replication in H. volcanii. Only the PCNA fusion to the GFP was not successful, suggesting that the GFP hinders essential roles of PCNA in DNA replication. Fen1 and Orc1 were successfully fused to the GFP and expressed in living cells, but specific localization in cells related to growth phase, reflecting different replication dynamics, were not observed. In contrast, we could observed fluorescent foci formed by the fully functional GFP::Rpa2 protein that actively responded to DNA damage in H. volcanii cells. The number of these fluorescent foci per cell was constant during cell growth but it significantly increased in cells exposed to aphidicoline, which inhibits DNA synthesis during replication. When cells were treated with phleomycine, a DNA damaging agent mainly causing double-strand breaks, formation of a massive fluorescent focus coinciding with DNA compaction was observed. Our results suggest that the specific cellular localization of GFP::Rpa2 observed reflects Rpa2 roles in DNA repair and/or DNA replication fork restart.