Modernsierung von Steuerungssystem von Simatic S5 auf Simatic S7 der VSG1 Anlagen

[s.c.]

Pore-forming pyocin S5 utilizes the FptA ferripyochelin receptor to kill Pseudomonas aeruginosa.

Pyocins are toxic proteins produced by some strains of Pseudomonas aeruginosa that are lethal for related strains of the same species. Some soluble pyocins (S2, S3 and S4) were previously shown to use the pyoverdine siderophore receptors to enter the cell. The P. aeruginosa PAO1 pore-forming pyocin S5 encoding gene (PAO985) was cloned into the expression vector pET15b, and the affinity-purified protein product tested for its killing activity against different P. aeruginosa strains. The results, however, did not show any correlation with a specific ferripyoverdine receptor. To further identify the S5 receptor, transposon mutants were generated. Pooled mutants were exposed to pyocin S5 and the resistant colonies growing in the killing zone were selected. The majority of S5-resistant mutants had an insertion in the fptA gene encoding the receptor for the siderophore pyochelin. Complementation of an fptA transposon mutant with the P. aeruginosa fptA gene in trans restored the sensitivity to S5. In order to define the receptor-binding domain of pyocin S5, two hybrid pyocins were constructed containing different regions from pyocin S5 fused to the C-terminal translocation and DNase killing domains of pyocin S2. Only the protein containing amino acid residues 151 to 300 from S5 showed toxicity, indicating that the pyocin S5 receptor-binding domain is not at the N-terminus of the protein as in other S-type pyocins. Pyocin S5 was, however, unable to kill Burkholderia cenocepacia strains producing a ferripyochelin FptA receptor, nor was the B. cenocepacia fptA gene able to restore the sensitivity of the resistant fptA mutant P. aeruginosa strain.

Couplage entre les régions IIS4-S5 et IIS6 lors de l’activation du canal calcique CaV2.3

Les canaux calciques dépendants du voltage CaV font partie de la famille structurale des canaux ioniques à 6 segments transmembranaires. Tout comme les canaux potassiques Kv, les canaux CaV possèdent une série de résidus chargés dans l’hélice S4 de chaque domaine ou sous-unité qui conférerait à la protéine une sensibilité aux changements de voltage. De plus les hélices S6 tapissent la paroi du pore et forment la porte d’activation de la protéine. Comment le mouvement des hélices S4 se traduit par l’ouverture de la porte d’activation des hélices S6 demeure une question encore non résolue. Suite à la publication de la structure cristalline du canal Kv1.2 en 2005, le groupe de MacKinnon a proposé que le mouvement des hélices S4 est mécaniquement couplé à la porte d’activation S6 à travers le glissement de l’hélice amphiphile S4-S5 selon un mécanisme nommé couplage électromécanique (Long et al. 2005b). Dans le but de déterminer si la région S4-S5 joue un rôle dans l’activation du canal calcique CaV2.3, nous avons étudié, par la méthode d’analyse cyclique de mutations doubles (« Double Mutant Cycle Analysis », (Horovitz 1996)), le couplage entre la boucle S4-S5 et l’hélice S6 du domaine II de ce canal. Les mesures d’énergies d’activation, ΔGact, obtenues en présence des sous-unités auxiliaires CaVα2δ et CaVβ3 ont affiché un couplage significatif pour l’activation entre les paires de résidus V593G/L699G, V593G/A700G, V593G/A702G, S595G/V703G L596G/L699G, L596G/A700G, L596G/I701G, L596G/A702G, L596G/V703G, L596G/D704G, M597G/I701G, et S602G/I701G. Aucune de ces paires de résidus n’a affiché de couplage lors de l’inactivation, suggérant que les effets observés sont spécifiques au mécanisme d’activation. Mis ensemble, ces résultats suggèrent que la boucle IIS4-S5 et l’hélice IIS6 interagissent et jouent un rôle déterminant dans l’activation de CaV2.3.

Influence des glycines du lien S4-S5 sur le couplage électromécanique des canaux ioniques dépendants du voltage

Les canaux potassiques dépendants du voltage sont formés de quatre sous-unités, chacune possédant six segments transmembranaires (S1-S6) et une boucle (p-loop) qui se trouve entre le cinquième et le sixième segment au niveau du pore. Il est connu que le segment senseur du voltage (S1-S4) subit un mouvement lorsque le potentiel membranaire change. Pour ouvrir le canal, il est nécessaire de transférer l'énergie du senseur du voltage (généré par le mouvement des charges positives de S4) au pore. Le mécanisme exact de ce couplage électromécanique est encore sous étude. Un des points de liaison entre le senseur de voltage et le pore est le lien physique fait par le segment S4-S5 (S45L). Le but de cette étude est de déterminer l'influence de la flexibilité du segment S45L sur le processus de couplage. Dans le S45L, trois glycines sont distribuées dans des positions différentes. Elles sont responsables de la flexibilité des hélices-alpha. Ces glycines (mais pas leurs positions exactes) sont conservées pour tous les canaux potassiques dépendants de potentiel. En utilisant la technique de mutagènes dirigé, la glycine a été remplacée dans chacune de ces différentes positions par une alanine et dans une deuxième étape, par une proline (pour introduire un angle dans l'hélice). Pour étudier le comportement des canaux dans cette nouvelle conformation, on a appliqué la technique de « patch clamp » pour déterminer les effets lors de l'ouverture du pore (courant ionique). Avec le « cut-open oocyte voltage-clamp », nous avons étudié les effets sur le mouvement du senseur de voltage (courant “gating”) et la coordination temporelle avec l'ouverture du pore (courant ionique). Les données ont montré qu’en réduisant la flexibilité dans le S45L, il faut avoir plus d'énergie pour faire ouvrir le canal. Le changement pour une proline suggère que le mouvement du senseur est indépendant du pore pendant l'ouverture du canal.

One loop conformal invariance of the superstring in an AdS5 × S5 background

It is proven that the pure spinor superstring in an AdS5 × S5 background remains conformally invariant at one loop level in the sigma model perturbation theory. © SISSA/ISAS 2003.

Flat currents in the classical AdS5 × S5 pure spinor superstring

It is proven that the classical pure spinor superstring in an AdS 5 × S5 back-ground has a flat current depending on a continuous parameter. This generalizes the recent result of Bena, et al. for the classical Green-Schwarz superstring. © SISSA/ISAS 2004.

Harmonic superspace from the AdS5 × S5 pure spinor formalism

On-shell supergravity vertex operators in an AdS 5 × S 5 background are described in the pure spinor formalism by the zero mode cohomology of a BRST operator. After expanding the pure spinor BRST operator in terms of the AdS 5 radius variable, this cohomology is computed using $ \mathcal{N}=4 $ harmonic superspace variables and explicit super-field expressions are obtained for the behavior of supergravity vertex operators near the boundary of AdS 5. © 2013 SISSA, Trieste, Italy.

Nd isotope data for planktonic foraminifera from within and around sapropels S1 and S5 from ODP Site 160-967

The development of widespread anoxic conditions in the deep oceans is evidenced by the accumulation and preservation of organic-carbon-rich sediments, but its precise cause remains controversial. The two most popular hypotheses involve (1) circulation-induced increased stratification resulting in reduced oxygenation of deep waters or (2) enhanced productivity in the surface ocean, increasing the raining down of organic matter and overwhelming the oxic remineralization potential of the deep ocean. In the periodic development of deep-water anoxia in the Pliocene-Pleistocene Mediterranean Sea, increased riverine runoff has been implicated both as a source for nutrients that fuel enhanced photic-zone productivity and a source of a less dense freshwater cap leading to reduced circulation, basin-wide stagnation, and deep-water oxygen starvation. Monsoon-driven increases in Nile River discharge and increased regional precipitation due to enhanced westerly activity-two mechanisms that represent fundamentally different climatic driving forces-have both been suggested as causes of the altered freshwater balance. Here we present data that confirm a distinctive neodymium (Nd) isotope signature for the Nile River relative to the Eastern Mediterranean-providing a new tracer of enhanced Nile outflow into the Mediterranean in the past. We further present Nd isotope data for planktonic foraminifera that suggest a clear increase in Nile discharge during the central intense period of two recent anoxic events. Our data also suggest, however, that other regional freshwater sources were more important at the beginning and end of the anoxic events. Taken at face value, the data appear to imply a temporal link between peaks in Nile discharge and enhanced westerly activity.

High-resolution stratigraphic framework for Mediterranean sapropel S5

A high-resolution stratigraphic framework is presented for sapropel S5, which represents the low-mid latitude climate optimum of the previous interglacial period (Eemian). The framework is based on three sites along a transect from west to east through the eastern Mediterranean, and is further validated using a fourth site. This method allows expression of S5-based proxy records of Eemian climate variability along a standardised depth scale that offers unprecedented possibilities for assessment of spatial gradients and signal leads and lags in an interval where highresolution (radiocarbon-style) dating cannot be performed. Our lateral comparison of S5 sapropels suggests that the onset of S5 in ODP site 967C (Eratosthenes seamount) was 1-6 centuries delayed relative to the onsets in more westerly sites.

Planktonic assemblages during sapropel S5 deposits in the Urania Basin

A micropaleontological study of planktonic assemblages on the partially laminated sapropel S5 (late Pleistocene, marine isotope stage (MIS) 5e) was performed in two piston cores from Urania Basin area (eastern Mediterranean, west of Crete): UM94PC16 and UM94PC31 recovered during a PALEOFLUX Project Cruise. The abundance of Florisphaera profunda indicates the development of a deep chlorophyll maximum (DCM) before the anoxic condition at bottom were established, whereas patterns of upper photic zone coccoliths suggest extreme oligotrophy in surface water. The short appearance of Globorotalia scitula and the presence of Globigerinoides ruber in the lower part of sapropel testify to a thermal stratification, also recorded by changes in primary producers. During G. scitula occurrence, diatoms, mainly represented by Pseudosolenia calcar-avis, appear and bloom because of their capability in using nutrients from DCM. Scanning electron microscope analyses performed on selected intervals from UM94PC16 show that the sapropel is organized in microlaminae mostly composed by siliceous microfossils. In particular, sapropel S5 could be related to an enhanced nutrient availability in the lower-middle part of the photic zone, stratified conditions, and a higher continental input.