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In Archaea and Bacteria, the arrays called CRISPRs for ‘clustered regularly interspaced short palindromic repeats’ and the CRISPR associated genes or cas provide adaptive immunity against viruses, plasmids and transposable elements. Short sequences called spacers, corresponding to fragments of invading DNA, are stored in-between repeated sequences. The CRISPR–Cas systems target sequences homologous to spacers leading to their degradation. To facilitate investigations of CRISPRs, we developed 12 years ago a website holding the CRISPRdb. We now propose CRISPRCasdb, a completely new version giving access to both CRISPRs and cas genes. We used CRISPRCasFinder, a program that identifies CRISPR arrays and cas genes and determine the system's type and subtype, to process public whole genome assemblies. Strains are displayed either in an alphabetic list or in taxonomic order. The database is part of the CRISPR-Cas++ website which also offers the possibility to analyse submitted sequences and to download programs. A BLAST search against lists of repeats and spacers extracted from the database is proposed. To date, 16 990 complete prokaryote genomes (16 650 bacteria from 2973 species and 340 archaea from 300 species) are included. CRISPR–Cas systems were found in 36% of Bacteria and 75% of Archaea strains. CRISPRCasdb is freely accessible at https://crisprcas.i2bc.paris-saclay.fr/.

International audience; Single-stranded (ss) DNA-binding proteins are found in all three domains of life where they play vital roles in nearly all aspects of DNA metabolism by binding to and stabilizing exposed ssDNA and acting as platforms onto which DNA-processing activities can assemble. The ssDNA-binding factors SSB and RPA are extremely well conserved across bacteria and eukaryotes, respectively, and comprise one or more OB-fold ssDNA-binding domains. In the third domain of life, the archaea, multiple types of ssDNA-binding protein are found with a variety of domain architectures and subunit compositions, with OB-fold ssDNA-binding domains being a characteristic of most, but not all. This chapter summarizes current knowledge of the distribution, structure, and biological function of the archaeal ssDNA-binding factors, highlighting key features shared between clades and those that distinguish the proteins of different clades from one another. The likely cellular functions of the proteins are discussed and gaps in current knowledge identified.

Background Shark Bay, Australia, harbours one of the most extensive and diverse systems of living microbial mats that are proposed to be analogs of some of the earliest ecosystems on Earth. These ecosystems have been shown to possess a substantial abundance of uncultivable microorganisms. These enigmatic microbes, jointly coined as ‘microbial dark matter’ (MDM), are hypothesised to play key roles in modern microbial mats. Results We reconstructed 115 metagenome-assembled genomes (MAGs) affiliated to MDM, spanning 42 phyla. This study reports for the first time novel microorganisms (Zixibacterial order GN15) putatively taking part in dissimilatory sulfate reduction in surface hypersaline settings, as well as novel eukaryote signature proteins in the Asgard archaea. Despite possessing reduced-size genomes, the MDM MAGs are capable of fermenting and degrading organic carbon, suggesting a role in recycling organic carbon. Several forms of RuBisCo were identified, allowing putative CO2 incorporation into nucleotide salvaging pathways, which may act as an alternative carbon and phosphorus source. High capacity of hydrogen production was found among Shark Bay MDM. Putative schizorhodopsins were also identified in Parcubacteria, Asgard archaea, DPANN archaea, and Bathyarchaeota, allowing these members to potentially capture light energy. Diversity-generating retroelements were prominent in DPANN archaea that likely facilitate the adaptation to a dynamic, host-dependent lifestyle. Conclusions This is the first study to reconstruct and describe in detail metagenome-assembled genomes (MAGs) affiliated with microbial dark matter in hypersaline microbial mats. Our data suggests that these microbial groups are major players in these systems. In light of our findings, we propose H2, ribose and CO/CO2 as the main energy currencies of the MDM community in these mat systems.

A synthesis of phenotypic and quantitative genomic traits is provided for bacteria and archaea, in the form of a scripted, reproducible workflow that standardizes and merges 26 sources. The resulting unified dataset covers 14 phenotypic traits, 5 quantitative genomic traits, and 4 environmental characteristics for approximately 170,000 strain-level and 15,000 species-aggregated records. It spans all habitats including soils, marine and fresh waters and sediments, host-associated and thermal. Trait data can find use in clarifying major dimensions of ecological strategy variation across species. They can also be used in conjunction with species and abundance sampling to characterize trait mixtures in communities and responses of traits along environmental gradients., Measurement(s)Trait • phenotypic trait • quantitative genomic traitTechnology Type(s)digital curationFactor Type(s)habitat • speciesSample Characteristic - OrganismArchaea • BacteriaSample Characteristic - Locationglobal Machine-accessible metadata file describing the reported data: 10.6084/m9.figshare.12221732

Replicative DNA polymerases are nano-machines essential to life, which have evolved the ability to copy the genome with high fidelity and high processivity. In contrast with cellular transcriptases and ribosome machines, which evolved by accretion of complexity from a conserved catalytic core, no replicative DNA polymerase is universally conserved. Strikingly, four different families of DNA polymerases have evolved to perform DNA replication in the three domains of life. In Bacteria, the genome is replicated by DNA polymerases belonging to the A- and C-families. In Eukarya, genomic DNA is copied mainly by three distinct replicative DNA polymerases, Polα, Polδ, and Polε, which all belong to the B-family. Matters are more complicated in Archaea, which contain an unusual D-family DNA polymerase (PolD) in addition to PolB, a B-family replicative DNA polymerase that is homologous to the eukaryotic ones. PolD is a heterodimeric DNA polymerase present in all Archaea discovered so far, except Crenarchaea. While PolD is an essential replicative DNA polymerase, it is often underrepresented in the literature when the diversity of DNA polymerases is discussed. Recent structural studies have shown that the structures of both polymerase and proofreading active sites of PolD differ from other structurally characterized DNA polymerases, thereby extending the repertoire of folds known to perform DNA replication. This review aims to provide an updated structural classification of all replicative DNAPs and discuss their evolutionary relationships, both regarding the DNA polymerase and proofreading active sites.

Clustered regularly interspaced short palindromic repeat (CRISPR)-Cas systems are well-known acquired immunity systems that are widespread in archaea and bacteria. The RNA-guided nucleases from CRISPR-Cas systems are currently regarded as the most reliable tools for genome editing and engineering. The first hint of their existence came in 1987, when an unusual repetitive DNA sequence, which subsequently was defined as a CRISPR, was discovered in the Escherichia coli genome during an analysis of genes involved in phosphate metabolism. Similar sequence patterns were then reported in a range of other bacteria as well as in halophilic archaea, suggesting an important role for such evolutionarily conserved clusters of repeated sequences. A critical step toward functional characterization of the CRISPR-Cas systems was the recognition of a link between CRISPRs and the associated Cas proteins, which were initially hypothesized to be involved in DNA repair in hyperthermophilic archaea. Comparative genomics, structural biology, and advanced biochemistry could then work hand in hand, not only culminating in the explosion of genome editing tools based on CRISPR-Cas9 and other class II CRISPR-Cas systems but also providing insights into the origin and evolution of this system from mobile genetic elements denoted casposons. To celebrate the 30th anniversary of the discovery of CRISPR, this minireview briefly discusses the fascinating history of CRISPR-Cas systems, from the original observation of an enigmatic sequence in E. coli to genome editing in humans.

Background Analysis of metagenomic sequences has become the principal approach for the study of the diversity of viruses. Many recent, extensive metagenomic studies on several classes of viruses have dramatically expanded the visible part of the virosphere, showing that previously undetected viruses, or those that have been considered rare, actually are important components of the global virome. Results We investigated the provenance of viruses related to tail-less bacteriophages of the family Tectiviridae by searching genomic and metagenomics sequence databases for distant homologs of the tectivirus-like Double Jelly-Roll major capsid proteins (DJR MCP). These searches resulted in the identification of numerous genomes of virus-like elements that are similar in size to tectiviruses (10–15 kilobases) and have diverse gene compositions. By comparison of the gene repertoires, the DJR MCP-encoding genomes were classified into 6 distinct groups that can be predicted to differ in reproduction strategies and host ranges. Only the DJR MCP gene that is present by design is shared by all these genomes, and most also encode a predicted DNA-packaging ATPase; the rest of the genes are present only in subgroups of this unexpectedly diverse collection of DJR MCP-encoding genomes. Only a minority encode a DNA polymerase which is a hallmark of the family Tectiviridae and the putative family "Autolykiviridae". Notably, one of the identified putative DJR MCP viruses encodes a homolog of Cas1 endonuclease, the integrase involved in CRISPR-Cas adaptation and integration of transposon-like elements called casposons. This is the first detected occurrence of Cas1 in a virus. Many of the identified elements are individual contigs flanked by inverted or direct repeats and appear to represent complete, extrachromosomal viral genomes, whereas others are flanked by bacterial genes and thus can be considered as proviruses. These contigs come from metagenomes of widely different environments, some dominated by archaea and others by bacteria, suggesting that collectively, the DJR MCP-encoding elements have a broad host range among prokaryotes. Conclusions The findings reported here greatly expand the known host range of (putative) viruses of bacteria and archaea that encode a DJR MCP. They also demonstrate the extreme diversity of genome architectures in these viruses that encode no universal proteins other than the capsid protein that was used as the marker for their identification. From a supposedly minor group of bacterial and archaeal viruses, these viruses are emerging as a substantial component of the prokaryotic virome. Electronic supplementary material The online version of this article (10.1186/s12985-018-0974-y) contains supplementary material, which is available to authorized users.

Our growing awareness of the microbial world's importance and diversity contrasts starkly with our limited understanding of its fundamental structure. Despite recent advances in DNA sequencing, a lack of standardized protocols and common analytical frameworks impedes comparisons among studies, hindering the development of global inferences about microbial life on Earth. Here we present a meta-analysis of microbial community samples collected by hundreds of researchers for the Earth Microbiome Project. Coordinated protocols and new analytical methods, particularly the use of exact sequences instead of clustered operational taxonomic units, enable bacterial and archaeal ribosomal RNA gene sequences to be followed across multiple studies and allow us to explore patterns of diversity at an unprecedented scale. The result is both a reference database giving global context to DNA sequence data and a framework for incorporating data from future studies, fostering increasingly complete characterization of Earth's microbial diversity. Fil: Thompson, Luke R.. University of California at San Diego; Estados Unidos. University of Southern Mississippi; Estados Unidos. National Oceanic and Atmospheric Administration; Estados Unidos Fil: Sanders, Jon G.. University of California at San Diego; Estados Unidos Fil: McDonald, Daniel. University of California at San Diego; Estados Unidos Fil: Amir, Amnon. University of California at San Diego; Estados Unidos Fil: Ladau, Joshua. University of California San Francisco; Estados Unidos Fil: Locey, Kenneth J.. Indiana University; Estados Unidos Fil: Prill, Robert J.. IBM Almaden Research Center; Estados Unidos Fil: Tripathi, Anupriya. University of California at San Diego; Estados Unidos Fil: Gibbons, Sean M.. Massachusetts Institute of Technology; Estados Unidos Fil: Ackermann, Gail. University of California San Diego; Estados Unidos Fil: Navas Molina, Jose A.. University of California at San Diego; Estados Unidos Fil: Janssen, Stefan. University of California at San Diego; Estados Unidos Fil: Kopylova, Evguenia. University of California at San Diego; Estados Unidos Fil: Vázquez Baeza, Yoshiki. University of California at San Diego; Estados Unidos Fil: González, Antonio. University of California at San Diego; Estados Unidos Fil: Morton, James T.. University of California at San Diego; Estados Unidos Fil: Mirarab, Siavash. University of California at San Diego; Estados Unidos Fil: Xu, Zhenjiang Zech. University of California at San Diego; Estados Unidos Fil: Jiang, Lingjing. University of California at San Diego; Estados Unidos Fil: Haroon, Mohamed F.. Harvard University; Estados Unidos Fil: Kanbar, Jad. University of California at San Diego; Estados Unidos Fil: Zhu, Qiyun. University of California at San Diego; Estados Unidos Fil: Song, Se Jin. University of California at San Diego; Estados Unidos Fil: Kosciolek, Tomasz. University of California at San Diego; Estados Unidos Fil: Bokulich, Nicholas A.. Northern Arizona University; Estados Unidos Fil: Lefler, Joshua. University of California at San Diego; Estados Unidos Fil: Brislawn, Colin J.. Earth and Biological Sciences Directorate; Estados Unidos Fil: Humphrey, Gregory. University of California at San Diego; Estados Unidos Fil: Owens, Sarah M.. Argonne National Laboratory; Estados Unidos Fil: Hampton Marcell, Jarrad. Argonne National Laboratory; Estados Unidos. University of Illinois at Chicago; Estados Unidos Fil: Berg Lyons, Donna. University of Colorado; Estados Unidos Fil: McKenzie, Valerie. University of Colorado; Estados Unidos Fil: Fierer, Noah. University of Colorado; Estados Unidos Fil: Fuhrman, Jed A.. University of Colorado; Estados Unidos Fil: Clauset, Aaron. University of Colorado; Estados Unidos Fil: Stevens, Rick L.. Argonne National Laboratory; Estados Unidos. University of Chicago; Estados Unidos Fil: Shade, Ashley. Michigan State University; Estados Unidos Fil: Pollard, Katherine S.. The Gladstone Institutes; Estados Unidos. University of California San Francisco; Estados Unidos Fil: Goodwin, Kelly D.. National Oceanic and Atmospheric Administration; Estados Unidos Fil: Jansson, Janet K.. Earth and Biological Sciences Directorate; Estados Unidos Fil: Gilbert, Jack A.. Argonne National Laboratory; Estados Unidos. University of Chicago; Estados Unidos Fil: Knight, Rob. University of California San Diego; Estados Unidos Fil: Dionisi, Hebe Monica. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Centro Nacional Patagónico. Centro para el Estudio de Sistemas Marinos; Argentina Fil: Lozada, Mariana. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Centro Nacional Patagónico. Centro para el Estudio de Sistemas Marinos; Argentina Fil: Mac Cormack, Walter Patricio. Universidad de Buenos Aires; Argentina. Ministerio de Relaciones Exteriores, Comercio Interno y Culto. Dirección Nacional del Antártico. Instituto Antártico Argentino; Argentina

International audience; Bacteriophages and archaeal viruses contribute, through lysogenic conversion or transduction, to the horizontal transfer of genetic material between cellular genomes. Recent works using a variety of approaches have shown that lysogenic conversion is widespread and provides hosts with adaptive traits often associated with biotic interactions. The quantification of the evolutionary impact of transduction has lagged behind and still requires further theoretical and experimental work. Nevertheless, recent studies have suggested that generalized transduction could play a role in the transfer of antibiotic resistance genes and in gene acquisition during intra-specific competition. Phage-mediated horizontal transfer has specific characteristics that complement other mechanisms of transfer. Notably, they could play a key role in the spread of adaptive genes between communities.

International audience; A casposon, a member of a distinct superfamily of archaeal and bacterial self-synthesizing transposons that employ a recombinase (casposase) homologous to the Cas1 endonuclease, appears to have given rise to the adaptation module of CRISPR-Cas systems as well as the CRISPR repeats themselves. Comparison of the mechanistic features of the reactions catalyzed by the casposase and the Cas1-Cas2 heterohexamer, the CRISPR integrase, reveals close similarity but also important differences that explain the requirement of Cas2 for integration of short DNA fragments, the CRISPR spacers.

Viruses cause the mortality of a large fraction of deep-sea benthic archaea, thereby influencing overall ecosystem functions., Viruses are the most abundant biological entities in the world’s oceans, and they play a crucial role in global biogeochemical cycles. In deep-sea ecosystems, archaea and bacteria drive major nutrient cycles, and viruses are largely responsible for their mortality, thereby exerting important controls on microbial dynamics. However, the relative impact of viruses on archaea compared to bacteria is unknown, limiting our understanding of the factors controlling the functioning of marine systems at a global scale. We evaluate the selectivity of viral infections by using several independent approaches, including an innovative molecular method based on the quantification of archaeal versus bacterial genes released by viral lysis. We provide evidence that, in all oceanic surface sediments (from 1000- to 10,000-m water depth), the impact of viral infection is higher on archaea than on bacteria. We also found that, within deep-sea benthic archaea, the impact of viruses was mainly directed at members of specific clades of Marine Group I Thaumarchaeota. Although archaea represent, on average, ~12% of the total cell abundance in the top 50 cm of sediment, virus-induced lysis of archaea accounts for up to one-third of the total microbial biomass killed, resulting in the release of ~0.3 to 0.5 gigatons of carbon per year globally. Our results indicate that viral infection represents a key mechanism controlling the turnover of archaea in surface deep-sea sediments. We conclude that interactions between archaea and their viruses might play a profound, previously underestimated role in the functioning of deep-sea ecosystems and in global biogeochemical cycles.

It was previously demonstrated that microbial communities of pig manure were composed of both bacteria and archaea. Recent studies have shown that bacteria are aerosolized from pig manure, but none have ever focused on the airborne archaeal burden. We sought here to develop and apply molecular ecology approaches to thoroughly characterize airborne archaea from swine confinement buildings (SCBs). Eight swine operations were visited, twice in winter and once during summer. Institute of Occupational Medicine cassettes loaded with 25-mm gelatin filters were used to capture the inhalable microbial biomass. The total genomic DNA was extracted and used as a template for PCR amplification of the archaeal 16S rRNA gene. High concentrations of archaea were found in SCB bioaerosols, being as high as 10 8 16S rRNA gene copies per cubic meter of air. Construction and sequencing of 16S rRNA gene libraries revealed that all sequences were closely related to methanogenic archaea, such as Methanosphaera stadtmanae (94.7% of the archaeal biodiversity). Archaeal community profiles were compared by 16S rRNA gene denaturing gradient gel electrophoresis. This analysis showed similar fingerprints in each SCB and confirmed the predominance of methanogenic archaea in the bioaerosols. This study sheds new light on the nature of bioaerosols in SCBs and suggests that archaea are also aerosolized from pig manure.

En libre-accès sur Archimer : http://archimer.ifremer.fr/doc/2009/publication-6977.pdf; International audience; A hyperthermophilic, anaerobic, dissimilatory Fe(III)-reducing, facultatively chemolithoautotrophic archaeon (strain SBH6(T)) was isolated from a hydrothermal sample collected from the deepest of the known World Ocean hydrothermal fields, Ashadze field (1 degrees 58' 21'' N 4 degrees 51' 47'' W) on the Mid-Atlantic Ridge, at a depth of 4100 m. The strain was enriched using acetate as the electron donor and Fe(III) oxide as the electron acceptor. Cells of strain SBH6(T) were irregular cocci, 0.3-0.5 mum in diameter. The temperature range for growth was 50-85 degrees C, with an optimum at 81 degrees C. The pH range for growth was 5.0-7.5, with an optimum at pH 6.8. Growth of SBH6(T) was observed at NaCl concentrations ranging from 1 to 6 % (w/v) with an optimum at 2.5 % (w/v). The isolate utilized acetate, formate, pyruvate, fumarate, malate, propionate, butyrate, succinate, glycerol, stearate, palmitate, peptone and yeast extract as electron donors for Fe(III) reduction. It was also capable of growth with H(2) as the sole electron donor, CO(2) as a carbon source and Fe(III) as an electron acceptor without the need for organic substances. Fe(III) [in the form of poorly crystalline Fe(III) oxide or Fe(III) citrate] was the only electron acceptor that supported growth. 16S rRNA gene sequence analysis revealed that the closest relative of the isolated organism was Geoglobus ahangari 234(T) (97.0 %). On the basis of its physiological properties and phylogenetic analyses, the isolate is considered to represent a novel species, for which the name Geoglobus acetivorans sp. nov. is proposed. The type strain is SBH6(T) (=DSM 21716(T) =VKM B-2522(T)).

International audience; Adaptive immune systems in prokaryotes and animals give rise to long-term memory through modification of specific genomic loci, such as by insertion of foreign (viral or plasmid) DNA fragments into clustered regularly interspaced short palindromic repeat (CRISPR) loci in prokaryotes and by V(D)J recombination of immunoglobulin genes in vertebrates. Strikingly, recombinases derived from unrelated mobile genetic elements have essential roles in both prokaryotic and vertebrate adaptive immune systems. Mobile elements, which are ubiquitous in cellular life forms, provide the only known, naturally evolved tools for genome engineering that are successfully adopted by both innate immune systems and genome-editing technologies. In this Opinion article, we present a general scenario for the origin of adaptive immunity from mobile elements and innate immune systems.

International audience; Type II DNA topoisomerases are divided into two families, IIA and IIB. Types IIA and IIB enzymes share homologous B subunits encompassing the ATP-binding site, but have non-homologous A subunits catalyzing DNA cleavage. Type IIA topoisomerases are ubiquitous in Bacteria and Eukarya, whereas members of the IIB family are mostly present in Archaea and plants. Here, we report the detection of genes encoding type IIB enzymes in which the A and B subunits are fused into a single polypeptide. These proteins are encoded in several bacterial genomes, two bacterial plasmids and one archaeal plasmid. They form a monophyletic group that is very divergent from archaeal and eukaryotic type IIB enzymes (DNA topoisomerase VI). We propose to classify them into a new subfamily, denoted DNA topoisomerase VIII. Bacterial genes encoding a topoisomerase VIII are present within integrated mobile elements, most likely derived from conjugative plasmids. Purified topoisomerase VIII encoded by the plasmid pPPM1a from Paenibacillus polymyxa M1 had ATP-dependent relaxation and decatenation activities. In contrast, the enzyme encoded by mobile elements integrated into the genome of Ammonifex degensii exhibited DNA cleavage activity producing a full-length linear plasmid and that from Microscilla marina exhibited ATP-independent relaxation activity. Topoisomerases VIII, the smallest known type IIB enzymes, could be new promising models for structural and mechanistic studies.

Opinion; International audience; It has been claimed that giant DNA viruses represent a separate, fourth domain of life in addition to the domains of Bacteria, Archaea, and Eukarya. Such classification disregards fundamental differences between the two types of living entities - viruses and cells - and results in confusion and controversies in evolutionary scenarios. We highlight these problems and emphasize the importance of restricting the term 'domain' to the descendants of the last universal cellular ancestor (LUCA), based on the shared ribosome structure. We suggest tracing phylogeny of viruses along evolutionary lineages primarily defined by virion architectures and the structures of the major capsid proteins.

International audience; The replicon model has initiated a major research line in molecular biology: the study of DNA replication mechanisms. Until now, the majority of studies have focused on a limited set of model organisms, mainly from Bacteria or Opisthokont eukaryotes (human, yeasts) and a few viral systems. However, molecular evolutionists have shown that the living world is more complex and diverse than believed when the operon model was proposed. Comparison of DNA replication proteins in the three domains, Archaea, Bacteria, and Eukarya, have surprisingly revealed the existence of two distinct sets of non-homologous cellular DNA replication proteins, one in Bacteria and the other in Archaea and Eukarya, suggesting that the last universal common ancestor possibly still had an RNA genome. A major puzzle is the presence in eukaryotes of the unfaithful DNA polymerase alpha (Pol α) to prime Okazaki fragments. Interestingly, Pol α is specifically involved in telomere biosynthesis, and its absence in Archaea correlates with the absence of telomeres. The recent discovery of telomere-like GC quartets in eukaryotic replication origins suggests a link between Pol α and the overall organization of the eukaryotic chromosome. As previously proposed by Takemura, Pol α might have originated from a mobile element of viral origin that played a critical role in the emergence of the complex eukaryotic genomes. Notably, most large DNA viruses encode DNA replication proteins very divergent from their cellular counterparts. The diversity of viral replication machineries compared to cellular ones suggests that DNA and DNA replication mechanisms first originated and diversified in the ancient virosphere, possibly explaining why they are so many different types of replication machinerie.

International audience; Viruses are ubiquitous and can infect any of the three existing cellular lineages (Archaea, Bacteria and Eukarya). Despite the persisting negative public perception of these entities, scientists learnt how to domesticate some of them. The study of molecular mechanisms essential to the completion of viral cycles has greatly contributed to deciphering fundamental processes in biology. Nowadays, viruses have entered the biotechnological era and numerous applications have already been developed. Viral-derived tools are used to manipulate genetic information, detect, diagnose, control and cure infectious diseases, or even design new structural assemblies. With the recent advances in the field of metagenomics, an overwhelming amount of information on novel viruses has become available. As current tools have been historically developed from a limited number of viruses, the potential of discoveries from new archaeal, bacterial and eukaryotic viruses may be limited only by our understanding of the multiple facets of viral cycles.

The definitive version is available at ww3.interscience.wiley.com; International audience; Diversity and function in microbial mats from the Lucky Strike hydrothermal vent field (Mid-Atlantic Ridge) were investigated using molecular approaches. DNA and RNA were extracted from mat samples overlaying hydrothermal deposits and Bathymodiolus azoricus mussel assemblages. We constructed and analyzed libraries of 16S rRNA gene sequences and sequences of functional genes involved in autotrophic carbon fixation [forms I and II RuBisCO (cbbL/M), ATP-citrate lyase B (aclB)]; methane oxidation [particulate methane monooxygenase (pmoA)] and sulfur oxidation [adenosine-5'-phosphosulfate reductase (aprA) and soxB]. To gain new insights into the relationships between mats and mussels, we also used new domain-specific 16S rRNA gene primers targeting Bathymodiolus sp. symbionts. All identified archaeal sequences were affiliated with a single group: the marine group 1 Thaumarchaeota. In contrast, analyses of bacterial sequences revealed much higher diversity, although two phyla Proteobacteria and Bacteroidetes were largely dominant. The 16S rRNA gene sequence library revealed that species affiliated to Beggiatoa Gammaproteobacteria were the dominant active population. Analyses of DNA and RNA functional gene libraries revealed a diverse and active chemolithoautotrophic population. Most of these sequences were affiliated with Gammaproteobacteria, including hydrothermal fauna symbionts, Thiotrichales and Methylococcales. PCR and reverse transcription-PCR using 16S rRNA gene primers targeted to Bathymodiolus sp. symbionts revealed sequences affiliated with both methanotrophic and thiotrophic endosymbionts.

oceanographic cruise MARNAUT; International audience; To extend comparative metagenomic analyses of the deep-sea, we produced metagenomic data by direct 454 pyrosequencing from bathypelagic plankton (1000m depth) and bottom sediment of the Sea of Marmara, the gateway between the Eastern Mediterranean and the Black Seas. Data from small subunit ribosomal RNA (SSU rRNA) gene libraries and direct pyrosequencing of the same samples indicated that Gamma- and Alpha-proteobacteria, followed by Bacteroidetes, dominated the bacterial fraction in Marmara deep-sea plankton, whereas Planctomycetes, Delta- and Gammaproteobacteria were the most abundant groups in high bacterial-diversity sediment. Group I Crenarchaeota/Thaumarchaeota dominated the archaeal plankton fraction, although group II and III Euryarchaeota were also present. Eukaryotes were highly diverse in SSU rRNA gene libraries, with group I (Duboscquellida) and II (Syndiniales) alveolates and Radiozoa dominating plankton, and Opisthokonta and Alveolates, sediment. However, eukaryotic sequences were scarce in pyrosequence data. Archaeal amo genes were abundant in plankton, suggesting that Marmara planktonic Thaumarchaeota are ammonia oxidizers. Genes involved in sulfate reduction, carbon monoxide oxidation, anammox and sulfatases were over-represented in sediment. Genome recruitment analyses showed that Alteromonas macleodii ‘surface ecotype', Pelagibacter ubique and Nitrosopumilus maritimus were highly represented in 1000 m-deep plankton. A comparative analysis of Marmara metagenomes with ALOHA deep-sea and surface plankton, whale carcasses, Peru subsurface sediment and soil metagenomes clustered deep-sea Marmara plankton with deep-ALOHA plankton and whale carcasses, likely because of the suboxic conditions in the deep Marmara water column. The Marmara sediment clustered with the soil metagenome, highlighting the common ecological role of both types of microbial communities in the degradation of organic matter and the completion of biogeochemical cycles.

International audience; Tailed double-stranded DNA viruses (order Caudovirales) represent the dominant morphotype among viruses infecting bacteria. Analysis and comparison of complete genome sequences of tailed bacterial viruses provided insights into their origin and evolution. Structural and genomic studies have unexpectedly revealed that tailed bacterial viruses are evolutionarily related to eukaryotic herpesviruses. Organisms from the third domain of life, Archaea, are also infected by viruses that, in their overall morphology, resemble tailed viruses of bacteria. However, high-resolution structural information is currently unavailable for any of these viruses, and only a few complete genomes have been sequenced so far. Here we identified nine proviruses that are clearly related to tailed bacterial viruses and integrated into chromosomes of species belonging to four different taxonomic orders of the Archaea. This more than doubled the number of genome sequences available for comparative studies. Our analyses indicate that highly mosaic tailed archaeal virus genomes evolve by homologous and illegitimate recombination with genomes of other viruses, by diversification, and by acquisition of cellular genes. Comparative genomics of these viruses and related proviruses revealed a set of conserved genes encoding putative proteins similar to virion assembly and maturation, as well as genome packaging proteins of tailed bacterial viruses and herpesviruses. Furthermore, fold prediction and structural modeling experiments suggest that the major capsid proteins of tailed archaeal viruses adopt the same topology as the corresponding proteins of tailed bacterial viruses and eukaryotic herpesviruses. Data presented in this study strongly support the hypothesis that tailed viruses infecting archaea share a common ancestry with tailed bacterial viruses and herpesviruses.

International audience; The strategies organisms use to decode synonymous codons in cytosolic protein synthesis are not uniform. The complete isoacceptor tRNA repertoire and the type of modified nucleoside found at the wobble position 34 of their anticodons were analyzed in all kingdoms of life. This led to the identification of four main decoding strategies that are diversely used in Bacteria, Archaea and Eukarya. Many of the modern tRNA modification enzymes acting at position 34 of tRNAs are present only in specific domains and obviously have arisen late during evolution. In an evolutionary fine-tuning process, these enzymes must have played an essential role in the progressive introduction of new amino acids, and in the refinement and standardization of the canonical nuclear genetic code observed in all extant organisms (functional convergent evolutionary hypothesis).

International audience; Background: To understand the evolutionary role of Lateral Gene Transfer (LGT), accurate methods are needed to identify transferred genes and infer their timing of acquisition. Phylogenetic methods are particularly promising for this purpose, but the reconciliation of a gene tree with a reference (species) tree is computationally hard. In addition, the application of these methods to real data raises the problem of sorting out real and artifactual phylogenetic conflict. Results: We present Prunier, a new method for phylogenetic detection of LGT based on the search for a maximum statistical agreement forest (MSAF) between a gene tree and a reference tree. The program is flexible as it can use any definition of "agreement" among trees. We evaluate the performance of Prunier and two other programs (EEEP and RIATA-HGT) for their ability to detect transferred genes in realistic simulations where gene trees are reconstructed from sequences. Prunier proposes a single scenario that compares to the other methods in terms of sensitivity, but shows higher specificity. We show that LGT scenarios carry a strong signal about the position of the root of the species tree and could be used to identify the direction of evolutionary time on the species tree. We use Prunier on a biological dataset of 23 universal proteins and discuss their suitability for inferring the tree of life. Conclusions: The ability of Prunier to take into account branch support in the process of reconciliation allows a gain in complexity, in comparison to EEEP, and in accuracy in comparison to RIATA-HGT. Prunier's greedy algorithm proposes a single scenario of LGT for a gene family, but its quality always compares to the best solutions provided by the other algorithms. When the root position is uncertain in the species tree, Prunier is able to infer a scenario per root at a limited additional computational cost and can easily run on large datasets.; Pour comprendre le rôle des transferts horizontaux de gènes dans l'évolution, on doit savoir les détecter. Et pour ce faire, utiliser des méthodes phylogénétiques qui réconcilient les histoires de gènes et les histoires des organismes qui les portent. Mais non seulement les problèmes computationnels soulevés sont complexes, mais ils se heurtent aussi à la difficulté de séparer le signal biologique du signal artefactuel lors de la reconstruction phylogénétique. Nous présentons Prunier, une nouvelle méthode pour la détection phylogénétique des transferts, fondée sur la recherche d'une sous-forêt en accord statistique avec un arbre de gène et un arbre de référence. Le choix de la définition de l'accord statistique entre deux arbres est donné à l'utilisateur. Nous décrivons l'évaluation de la performance de Prunier et de deux autres programmes (EEEP and RIATA-HGT). Prunier montre une sensibilité comparable, et une meilleure spécificité. Nous montrons que les transferts horizontaux portent un signal phylogénétique et peuvent être utilisés pour donner une direction à l'évolution dans un arbre d'espèce (identifier une racine). Nous discutons également de l'utilisation possible de Prunier por la reconstruction de l'arbre de la vie.

Background Ribonucleotide reduction is the only de novo pathway for synthesis of deoxyribonucleotides, the building blocks of DNA. The reaction is catalysed by ribonucleotide reductases (RNRs), an ancient enzyme family comprised of three classes. Each class has distinct operational constraints, and are broadly distributed across organisms from all three domains, though few class I RNRs have been identified in archaeal genomes, and classes II and III likewise appear rare across eukaryotes. In this study, we examine whether this distribution is best explained by presence of all three classes in the Last Universal Common Ancestor (LUCA), or by horizontal gene transfer (HGT) of RNR genes. We also examine to what extent environmental factors may have impacted the distribution of RNR classes. Results Our phylogenies show that the Last Eukaryotic Common Ancestor (LECA) possessed a class I RNR, but that the eukaryotic class I enzymes are not directly descended from class I RNRs in Archaea. Instead, our results indicate that archaeal class I RNR genes have been independently transferred from bacteria on two occasions. While LECA possessed a class I RNR, our trees indicate that this is ultimately bacterial in origin. We also find convincing evidence that eukaryotic class I RNR has been transferred to the Bacteroidetes, providing a stunning example of HGT from eukaryotes back to Bacteria. Based on our phylogenies and available genetic and genomic evidence, class II and III RNRs in eukaryotes also appear to have been transferred from Bacteria, with subsequent within-domain transfer between distantly-related eukaryotes. Under the three-domains hypothesis the RNR present in the last common ancestor of Archaea and eukaryotes appears, through a process of elimination, to have been a dimeric class II RNR, though limited sampling of eukaryotes precludes a firm conclusion as the data may be equally well accounted for by HGT. Conclusions Horizontal gene transfer has clearly played an important role in the evolution of the RNR repertoire of organisms from all three domains of life. Our results clearly show that class I RNRs have spread to Archaea and eukaryotes via transfers from the bacterial domain, indicating that class I likely evolved in the Bacteria. However, against the backdrop of ongoing transfers, it is harder to establish whether class II or III RNRs were present in the LUCA, despite the fact that ribonucleotide reduction is an essential cellular reaction and was pivotal to the transition from RNA to DNA genomes. Instead, a general pattern of ongoing horizontal transmission emerges wherein environmental and enzyme operational constraints, especially the presence or absence of oxygen, are likely to be major determinants of the RNR repertoire of genomes.

International audience; Contrary to a widespread opinion, horizontal gene transfer (HGT) between distantly related microorganisms (such as Bacteria and Archaea) has not been demonstrated to occur on a large scale. Except for transfer of mobile elements between closely related organisms, most alleged HGT events reflect phylogenetic discrepancies that can be explained by a variety of artefacts or by the differential loss of paralogous gene copies either originally present in the Last Universal Common Ancestor (LUCA) to the three Domains (a sophisticated, genetically redundant and promiscuous community of protoeukaryotes), or created by duplications having occurred at later times. Besides, (i) there is no experimental evidence for the facile acquisition of foreign DNA between distant taxa and (ii) important biological constraints operate on the phenotypic success of genetic exchange at several levels, including protein-protein interactions involved in metabolic channelling; stable integration and expression of foreign DNA is, therefore, expected to require strong selection. Explaining phylogenetic discrepancies by artefacts or loss of paralogs does not eliminate difficulties in retracing species genealogy but maintains the picture of a universal tree of life, HGT between distant organisms being reduced to a trickle. We illustrate our thesis by the phylogenetic analysis of carbamoyltransferases, a family of paralogous proteins. Among higher eukaryotes HGT appears of limited scope except in asexual organisms. We suggest that meiotic sexuality (a hallmark of eukaryotes) emerged in the genetically redundant and protoeukaryotic LUCA as a molecular identity check providing a defence mechanism against the deleterious effects of HGT.

International audience; DNA-SIP (stable isotope probing) was conducted on anaerobic municipal solid waste samples incubated with (13)C-cellulose, (13)C-glucose and (13)C-acetate under mesophilic conditions. A total of 567 full-length bacterial and 448 1100-bp-length archaeal 16S rRNA gene sequences were analysed. In the clone libraries derived from 'heavy' DNA fractions, the most abundant sequences were affiliated with the phyla Firmicutes, Bacteroidetes, the gamma-subclass of Proteobacteria and methanogenic orders Methanomicrobiales and Methanosarcinales. Sequences related to the genus Acetivibrio (phylum Firmicutes) were recovered only in the 'heavy' DNA fraction derived from the (13)C-cellulose incubation. An oligonucleotide probe (UCL284) targeting specifically Acetivibrio was designed and used for fluorescent in situ hybridization (FISH) experiments. Interestingly, hybridization of the probe was detected in microorganisms aggregated around cellulose fibres, strengthening the conclusion that these microorganisms were major cellulose degraders. Sequences related to genus Clostridium (phylum Firmicutes) and to the family Porphyromonadaceae (phylum Bacteroidetes) were retrieved in large numbers from the 'heavy' DNA library of (13)C-Glucose incubation, suggesting their involvement in saccharide fermentation. Design and hybridization of specific FISH-probes confirmed the abundant representation of Clostridium (CLO401, CLO1248) and Porphyromonadaceae (BAC1040), which were mostly observed in the planktonic phase. Surprisingly, in the (13)C-acetate experiment, the 'heavy' DNA archaeal library was dominated by sequences related to the strictly hydrogenotrophic methanogenic genus Methanoculleus. One single operational taxonomic unit containing 70 sequences, affiliated to the gamma-subclass of Proteobacteria, was retrieved in the corresponding bacterial library. FISH observations with a newly designed specific probe (UGA64) confirmed the dominance of this bacterial group. Our results show that combination of DNA-SIP and FISH applied with a series of functionally connected substrates can shed light on the networks of uncultured microbes catalysing the methanization of the most abundant chemical renewable energy source on Earth.

En libre-accès sur Archimer : http://archimer.ifremer.fr/doc/2008/publication-4209.pdf; International audience; Sub-sea-floor sediments may contain two-thirds of Earth's total prokaryotic biomass. However, this has its basis in data extrapolation from ~500-meter to 4-kilometer depths, whereas the deepest documented prokaryotes are from only 842 meters. Here, we provide evidence for low concentrations of living prokaryotic cells in the deepest (1626 meters below the sea floor), oldest (111 million years old), and potentially hottest (~100 degrees C) marine sediments investigated. These Newfoundland margin sediments also have DNA sequences related to thermophilic and/or hyperthermophilic Archaea. These form two unique clusters within Pyrococcus and Thermococcus genera, suggesting unknown, uncultured groups are present in deep, hot, marine sediments (~54 degrees to 100 degrees C). Sequences of anaerobic methane-oxidizing Archaea were also present, suggesting a deep biosphere partly supported by methane. These findings demonstrate that the sub-sea-floor biosphere extends to at least 1600 meters below the sea floor and probably deeper, given an upper temperature limit for prokaryotic life of at least 113 degrees C and increasing thermogenic energy supply with depth.

Summary: BAGET (Bacterial and Archaeal Gene Exploration Tool) is a web service designed to facilitate extraction, by molecular geneticists and phylogeneticists, of specific gene and protein sequences from completely determined prokaryotic genomes. Upon selection of a particular prokaryotic organism and gene, two levels of visual gene context information are provided on a single dynamic page: (i) a graphical representation of a user defined portion of the chromosome centered on the gene of interest and (ii) the DNA sequence of the query gene, of the immediate neighboring genes and the intergenic regions each identified by a consistent color code. The aminoacid sequence is provided for protein-coding query genes. Query results can be exported as a rich text format (RTF) word processor file for printing, archival or further analysis. Availability: http://archaea.u-psud.fr/bin/baget.dll

International audience; The Pyrococcus abyssi genome displays two genes possibly coding for S-adenosyl-l-methionine-dependent RNA(uracil, C5)-methyltransferases (PAB0719 and PAB0760). Their amino acid sequences are more closely related to Escherichia coli RumA catalysing the formation of 5-methyluridine (m(5)U)-1939 in 23S rRNA than to E. coli TrmA (tRNA methyltransferase A) methylating uridine-54 in tRNA. Comparative genomic and phylogenetic analyses show that homologues of PAB0719 and PAB0760 occur only in a few Archaea, these genes having been acquired via a single horizontal gene transfer from a bacterial donor to the common ancestor of Thermococcales and Nanoarchaea. This transfer event was followed by a duplication event in Thermococcales leading to two closely related genes. None of the gene products of the two P. abyssi paralogues catalyses in vitro the formation of m(5)U in a P. abyssi rRNA fragment homologous to the bacterial RumA substrate. Instead, PAB0719 enzyme (renamed (Pab)TrmU54) displays an identical specificity to TrmA, as it catalyses the in vitro formation of m(5)U-54 in tRNA. Thus, during evolution, at least one of the two P. abyssi RumA-type enzymes has changed of target specificity. This functional shift probably occurred in an ancestor of all Thermococcales. This study also provides new evidence in favour of a close relationship between Thermococcales and Nanoarchaea.

Submarine mud volcanoes are formed by expulsions of mud, fluids, and gases from deeply buried subsurface sources. They are highly reduced benthic habitats and often associated with intensive methane seepage. In this study, the microbial diversity and community structure in methane-rich sediments of the Haakon Mosby Mud Volcano (HMMV) were investigated by comparative sequence analysis of 16S rRNA genes and fluorescence in situ hybridization. In the active volcano center, which has a diameter of about 500 m, the main methane-consuming process was bacterial aerobic oxidation. In this zone, aerobic methanotrophs belonging to three bacterial clades closely affiliated with Methylobacter and Methylophaga species accounted for 56% ± 8% of total cells. In sediments below Beggiatoa mats encircling the center of the HMMV, methanotrophic archaea of the ANME-3 clade dominated the zone of anaerobic methane oxidation. ANME-3 archaea form cell aggregates mostly associated with sulfate-reducing bacteria of the Desulfobulbus (DBB) branch. These ANME-3/DBB aggregates were highly abundant and accounted for up to 94% ± 2% of total microbial biomass at 2 to 3 cm below the surface. ANME-3/DBB aggregates could be further enriched by flow cytometry to identify their phylogenetic relationships. At the outer rim of the mud volcano, the seafloor was colonized by tubeworms ( Siboglinidae , formerly known as Pogonophora ). Here, both aerobic and anaerobic methane oxidizers were found, however, in lower abundances. The level of microbial diversity at this site was higher than that at the central and Beggiatoa species-covered part of the HMMV. Analysis of methyl-coenzyme M-reductase alpha subunit ( mcrA ) genes showed a strong dominance of a novel lineage, mcrA group f, which could be assigned to ANME-3 archaea. Our results further support the hypothesis of Niemann et al. (54), that high methane availability and different fluid flow regimens at the HMMV provide distinct niches for aerobic and anaerobic methanotrophs.

Background The evolutionary characterization of species and lifestyles at global levels is nowadays a subject of considerable interest, particularly with the availability of many complete genomes. Are there specific properties associated with lifestyles and phylogenies? What are the underlying evolutionary trends? One of the simplest analyses to address such questions concerns characterization of proteomes at the amino acids composition level. Results In this work, amino acid compositions of a large set of 208 proteomes, with significant number of representatives from the three phylogenetic domains and different lifestyles are analyzed, resorting to an appropriate multidimensional method: Correspondence analysis. The analysis reveals striking discrimination between eukaryotes, prokaryotic mesophiles and hyperthemophiles-themophiles, following amino acid usage. In sharp contrast, no similar discrimination is observed for psychrophiles. The observed distributional properties are compared with various inferred chronologies for the recruitment of amino acids into the genetic code. Such comparisons reveal correlations between the observed segregations of species following amino acid usage, and the separation of amino acids following early or late recruitment. Conclusion A simple description of proteomes according to amino acid compositions reveals striking signatures, with sharp segregations or on the contrary non-discriminations following phylogenies and lifestyles. The distribution of species, following amino acid usage, exhibits a discrimination between [high GC]-[high optimal growth temperatures] and [low GC]-[moderate temperatures] characteristics. This discrimination appears to coincide closely with the separation of amino acids following their inferred early or late recruitment into the genetic code. Taken together the various results provide a consistent picture for the evolution of proteomes, in terms of amino acid usage.

Mud volcanism is an important natural source of the greenhouse gas methane to the hydrosphere and atmosphere(1,2). Recent investigations show that the number of active submarine mud volcanoes might be much higher than anticipated ( for example, see refs 3 - 5), and that gas emitted from deep-sea seeps might reach the upper mixed ocean(6-8). Unfortunately, global methane emission from active submarine mud volcanoes cannot be quantified because their number and gas release are unknown(9). It is also unclear how efficiently methane-oxidizing microorganisms remove methane. Here we investigate the methane-emitting Haakon Mosby Mud Volcano (HMMV, Barents Sea, 72 degrees N, 14 degrees 44' E; 1,250 m water depth) to provide quantitative estimates of the in situ composition, distribution and activity of methanotrophs in relation to gas emission. The HMMV hosts three key communities: aerobic methanotrophic bacteria (Methylococcales), anaerobic methanotrophic archaea (ANME-2) thriving below siboglinid tubeworms, and a previously undescribed clade of archaea (ANME-3) associated with bacterial mats. We found that the upward flow of sulphate- and oxygen-free mud volcano fluids restricts the availability of these electron acceptors for methane oxidation, and hence the habitat range of methanotrophs. This mechanism limits the capacity of the microbial methane filter at active marine mud volcanoes to

One of the most important outcomes of modern biology has been the demonstration of the unity of life. All living beings are in fact descendants of a unique ancestor commonly referred to as Luca (the Last universal common ancestor). The discovery - nearly 30 years ago by Carl Woese - that present-day life on our planet can be assigned to only three domains: two of prokaryotic nature (Archaea and Bacteria), and one eukaryoyic (Eucarya), has given birth to a new field of investigation aimed at determining the nature of Luca. Today, thanks to the accumulation of genomic data, we can loop back into the past and infer a few characters of Luca by comparing what present-day organisms have in common. For example, it is now clear that Luca was a cellular organism provided with a cytoplasmic membrane, and that it harboured already a quite sophisticated translation apparatus. However, the inference of other characters of Luca from comparative genomics is less straightforward: for instance, a few key molecular mechanisms for DNA replication are non-homologous across the three domains and their distribution is often puzzling. This evidence has been embraced by proponents of the hypothesis that Luca harboured an RNA genome and that its replacement by DNA and the appearance of the corresponding molecular systems would have occurred independently in the three life domains after their divergence. However, an equally likely scenario would be that of a Luca with a DNA genome and of a subsequent replacement of its DNA-replication systems by non-homologous counterparts either in the bacterial or in the archaeal/eukaroytic branch. Nevertheless, including the viral world into the picture of the tree of life may thus provide us with precious insights into our most distant past since the invention and spread potential of viruses may have played a key role in early evolution.

Operons coding for the enzyme arsenite oxidase have been detected in the genomes from Archaea and Bacteria by Blast searches using the amino acid sequences of the respective enzyme characterized in two different beta-proteobacteria as templates. Sequence analyses show that in all these species, arsenite oxidase is transported over the cytoplasmic membrane via the tat system and most probably remains membrane attached by an N-terminal transmembrane helix of the Rieske subunit. The biochemical and biophysical data obtained for arsenite oxidase in the green filamentous bacterium Chloroflexus aurantiacus allow a structural model of the enzyme's membrane association to be proposed. Phylogenies for the two constituent subunits (i.e., the molybdopterin-containing and the Rieske subunit) of the heterodimeric enzyme and their respective homologs in DMSO-reductase, formate dehydrogenase, nitrate reductase, and the Rieske/cytb complexes were calculated from multiple sequence alignments. The obtained phylogenetic trees indicate an early origin of arsenite oxidase before the divergence of Archaea and Bacteria. Evolutionary implications of these phylogenies are discussed.