Crystal structure of the translation recovery factor Trf from Sulfolobus solfataricus.

During translation initiation, the heterotrimeric archaeal translation initiation factor 2 (aIF2) recruits the initiator tRNAi to the small ribosomal subunit. In the stationary growth phase and/or during nutrient stress, Sulfolobus solfataricus aIF2 has a second function: It protects leaderless mRNAs against degradation by binding to their 5'-ends. The S. solfataricus protein Sso2509 is a translation recovery factor (Trf) that interacts with aIF2 and is responsible for the release of aIF2 from bound mRNAs, thereby enabling translation re-initiation. It is a member of the domain of unknown function 35 (DUF35) protein family and is conserved in Sulfolobales as well as in other archaea. Here, we present the X-ray structure of S. solfataricus Trf solved to a resolution of 1.65 Å. Trf is composed of an N-terminal rubredoxin-like domain containing a bound zinc ion and a C-terminal oligosaccharide/oligonucleotide binding fold domain. The Trf structure reveals putative mRNA binding sites in both domains. Surprisingly, the Trf protein is structurally but not sequentially very similar to proteins linked to acyl-CoA utilization-for example, the Sso2064 protein from S. solfataricus-as well as to scaffold proteins found in the acetoacetyl-CoA thiolase/high-mobility group-CoA synthase complex of the archaeon Methanothermococcus thermolithotrophicus and in a steroid side-chain-cleaving aldolase complex from the bacterium Thermomonospora curvata. This suggests that members of the DUF35 protein family are able to act as scaffolding and binding proteins in a wide variety of biological processes.

Structure and dynamics study of translation initiation factor 1 from Staphylococcus aureus suggests its RNA binding mode.

Translation initiation, the rate-limiting step in the protein synthesis, is tightly regulated. As one of the translation initiation factors, translation initiation factor 1 (IF1) plays crucial roles not only in translation but also in many cellular processes that are important for genomic stability, such as the activity of RNA chaperones. Here, we characterize the RNA interactions and dynamics of IF1 from Staphylococcus aureus Mu50 (IF1Sa) by NMR spectroscopy. First, the NMR-derived solution structure of IF1Sa revealed that IF1Sa adopts an oligonucleotide/oligosaccharide binding (OB)-fold. Structural comparisons showed large deviations in the α-helix and the following loop, which are potential RNA-binding regions of the OB-fold, as well as differences in the electrostatic potential surface among bacterial IF1s. Second, the 15N NMR relaxation data for IF1Sa indicated the flexible nature of the α-helix and the following loop region of IF1Sa. Third, RNA-binding properties were studied using FP assays and NMR titrations. FP binding assays revealed that IF1Sa binds to RNAs with moderate affinity. In combination with the structural analysis, the NMR titration results revealed the RNA binding sites. Taken together, these results show that IF1Sa binds RNAs with moderate binding affinity via the residues that occupy the large surface area of its ß-barrel. These findings suggest that IF1Sa is likely to bind RNA in various conformations rather than only at a specific site and indicate that the flexible RNA binding mode of IF1Sa is necessary for its interaction with various RNA substrates.

Cryo-EM structure of the archaeal 50S ribosomal subunit in complex with initiation factor 6 and implications for ribosome evolution.

Translation of mRNA into proteins by the ribosome is universally conserved in all cellular life. The composition and complexity of the translation machinery differ markedly between the three domains of life. Organisms from the domain Archaea show an intermediate level of complexity, sharing several additional components of the translation machinery with eukaryotes that are absent in bacteria. One of these translation factors is initiation factor 6 (IF6), which associates with the large ribosomal subunit. We have reconstructed the 50S ribosomal subunit from the archaeon Methanothermobacter thermautotrophicus in complex with archaeal IF6 at 6.6 Å resolution using cryo-electron microscopy (EM). The structure provides detailed architectural insights into the 50S ribosomal subunit from a methanogenic archaeon through identification of the rRNA expansion segments and ribosomal proteins that are shared between this archaeal ribosome and eukaryotic ribosomes but are mostly absent in bacteria and in some archaeal lineages. Furthermore, the structure reveals that, in spite of highly divergent evolutionary trajectories of the ribosomal particle and the acquisition of novel functions of IF6 in eukaryotes, the molecular binding of IF6 on the ribosome is conserved between eukaryotes and archaea. The structure also provides a snapshot of the reductive evolution of the archaeal ribosome and offers new insights into the evolution of the translation system in archaea.

Prokaryotic community structure in algal photosynthetic biofilms from extreme acidic streams in Río Tinto (Huelva, Spain)

Four algal photosynthetic biofilms were collected from the Río Tinto (SW Spain) at four localities: AG, Euglena and Pinnularia biofilms; ANG, Chlorella and Pinnularia biofilms; RI, Cyanidium and Dunaliella biofilms; and CEM, Cyanidium, Euglena and Pinnularia biofilms. Community composition and structure were studied by a polyphasic approach consisting of 16S rRNA analysis, scanning electron microscopy by back-scattered electron detection mode (SEM-BSE), and fluorescence in-situ hybridization (FISH). Acidophilic prokaryotes associated with algal photosynthetic biofilms included sequences related to the Alpha-, Beta-, and Gammaproteobacteria (phylum Proteobacteria) and to the phyla Nitrospira, Actinobacteria, Acidobacteria and Firmicutes. Sequences from the Archaea domain were also identified. No more than seven distinct lineages were detected in any biofilm, except for those from RI, which contained fewer groups of Bacteria. Prokaryotic communities of the thinnest algal photosynthetic biofilms (-100 microm) were more related to those in the water column, including Leptospirillum populations. In general, thick biofilms (200 microm) generate microniches that could facilitate the development of less-adapted microorganisms (coming from the surrounding environment) to extreme conditions, thus resulting in a more diverse prokaryotic biofilm (AU)

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