Accessory phases as a tool to investigate magmatic underplating in polymetamorphic metasediments : an example from a fossil lower crust : Ivrea Verbano zne, NW Italy

The Ivrea and the Strona-Ceneri zones, NW italy and S Switzerland, offer the possibility to study the continental crust of the Southern Alps. Because of its high metamorphic degree and the abundant Permo- Carboniferous mafic intrusions, the Ivrea Zone is classically interpreted an exposed section trough the Permian lower crust. The present work is focused here on metasedimentary slices (septa) intercalated within Permian gabbro (mafic complex). In particular I studied the evolution of accessory phases such as rutile and zircon and the chemistry of the metasediments. The septa build an irregular and discontinuous band that cut obliquely the mafic complex from its deepest part (N) to its roof (S). The chemistry of the metasediments evolves along the band and the chemical evolution can be compared with that observed in the country-rock surrounding the mafic intrusion to the NE and overprinted by a main regional metamorphic event. This suggests that the degree of chemical depletion of the septa was mainly established during the same regional metamorphic event. Moreover it suggests that incorporation of the septa within the gabbro did not modify their original stratigraphie distribution within the crust. It implies that the mafic complex has been emplaced following a dynamic substantially different from the classic model of « gabbro glacier » (Quick et al., 1992; Quick et al., 1994). It is more likely that it has been emplaced by repeated injections of sills at different depths during a protracted period of time. Zircon trace elements and U-Pb ages suggest that regional metamorphism occurred 330-320Ma, the first sills in the deepest part of the Mafic Complex are injected at ~300Ma, the mafic magmas reached higher levels in the crust at 285Ma and the magmatic activity continued locally until 275Ma. The ages of detrital cores in zircons fix the maximal sedimentation age at ~370Ma, this age corresponds therefore with the maximal age of the incorporation of the Ivrea zone within the lower crust. I propose that the Ivrea zone has been accreted to the lower crust during the Hercynian orogeny sensu lato. The analysis of detrital ages suggests that the source terrains for the Ivrea zone and those for the Strona-Ceneri zone have a completely different Palaeozoic history. The systematic analysis of rutile in partially molten metasediments of the Ivrea zone reveals the occurrence of two generations. The two generations are characterized by a different chemistry and textural distribution. A first generation is formed during pro-grade metamorphism in the restitic counterpart. The second generation is formed in the melts during cooling at the same time that part of the first generation re-equilibrate. Re-equilibration of the first generation seems to be spatially controlled by the presence of fluids. Locally the second generation forms overgrowths on the first generation. Considered the different diffusivity of U and Pb in rutile, U heterogeneities have important implication for U-Pb dating of rutile. ID-TIMS and LA-ICPMS dating coupled with a careful textural investigation (SEM) suggest that rutile grains are characterized by multiple path along which Pb diffusion can occur: volume diffusion is an important process, but intragrain and subgrain boundaries provide additional high diffusivity pathways for Pb escape and reduce drastically the effective diffusion length. -- La zone d'Ivrea et la zone de Strona-Ceneri, en Italie nord-occidentale et Suisse méridionale, offrent la possibilité d'étudier la croûte continentale des Alpes du Sud. En raison du haut degré métamorphique et l'abondance d'intrusions mafiques d'âge Permo-Carbonifère [complexe mafique), la zone d'Ivrea est interprétée classiquement comme de la croûte inférieure permienne. Ce travail ce concentre sur des bandes metasédimentaires (septa) incorporées dans les magmas mafiques lors de l'intrusion. Les septa forment une bande irrégulière qui coupe obliquement le complexe mafique du bas (N) vers le haut (S). La chimie des septa évolue du bas vers le haut et l'évolution chimique se rapproche de l'évolution observé dans la roche encaissante l'intrusion affecté par un événement métamorphique régionale. Cette relation suggère que le degré d'appauvrissement chimique des septa a été établit principalement lors de l'événement métamorphique régional. De plus l'incorporation dans les gabbros n'a pas perturbée la distribution stratigraphique originelle des septa. Ces deux observations impliquent que le métamorphisme dans la roche encaissante précède la mise en place du gabbro et que cette dernière ne se fait pas selon le modèle classique (« gabbro glacier » de Quick et al., 1992, 1994), mais se fait plutôt par injections répétées de sills a différentes profondeurs. Les âges U-Pb et les éléments traces des zircons suggèrent que le métamorphisme régionale a eu lieu 330-320Ma, alors que les premiers sills dans la partie profonde du Mafic Complex s'injectent à ~300Ma, le magmatisme mafique atteigne des niveaux supérieurs à 285Ma et continue localement jusqu'à 270Ma. Les âges des coeurs détritiques des zircons permettent de fixer l'âge maximale de sédimentation à ~370Ma ce qui correspond donc à l'âge maximale de l'incorporation de la zone d'Ivrea dans la croûte inférieur. L'analyse systématique des rutiles, nous a permit de montrer l'existence de plusieurs générations qui ont une répartition texturale et une chimie différente. Une génération se forme lors de l'événement UHT dans les restites, une autre génération se forme dans les liquides lors du refroidissement, au même temps qu'une partie de la première génération se rééquilibre au niveau du Zr. Localement la deuxième génération peut former des surcroissances autour de la première génération. Dans ces cas, des fortes différences en uranium entre les deux générations ont des importantes implications pour la datation U-Pb sur rutile. Classiquement les ratios Pb/U dans le rutile sont interprétés comme indiquant l'âges du refroidissement du minéral sous une température à la quelle la diffusion du Pb dans le minéral n'est plus détectable et la diffusion à plus hautes températures est assumée se faire par «volume diffusion» dans le grain (Mezger et al., 1989). Par des datations ID-TIMS (sur grain entier) et LA-ICPMS (in-situ) et une analyse texturale (MEB) approfondie nous montrons que cette supposition est trop simpliste et que le rutile est repartie en sous-domaines. Chacun de ces domaines a ça propre longueur ou chemin de diffusion spécifique. Nous proposons donc une nouvelle approche plus cohérente pour l'interprétation des âges U-Pb sur rutile.

Fluctuation-Driven Neural Dynamics Reproduce Drosophila Locomotor Patterns.

The neural mechanisms determining the timing of even simple actions, such as when to walk or rest, are largely mysterious. One intriguing, but untested, hypothesis posits a role for ongoing activity fluctuations in neurons of central action selection circuits that drive animal behavior from moment to moment. To examine how fluctuating activity can contribute to action timing, we paired high-resolution measurements of freely walking Drosophila melanogaster with data-driven neural network modeling and dynamical systems analysis. We generated fluctuation-driven network models whose outputs-locomotor bouts-matched those measured from sensory-deprived Drosophila. From these models, we identified those that could also reproduce a second, unrelated dataset: the complex time-course of odor-evoked walking for genetically diverse Drosophila strains. Dynamical models that best reproduced both Drosophila basal and odor-evoked locomotor patterns exhibited specific characteristics. First, ongoing fluctuations were required. In a stochastic resonance-like manner, these fluctuations allowed neural activity to escape stable equilibria and to exceed a threshold for locomotion. Second, odor-induced shifts of equilibria in these models caused a depression in locomotor frequency following olfactory stimulation. Our models predict that activity fluctuations in action selection circuits cause behavioral output to more closely match sensory drive and may therefore enhance navigation in complex sensory environments. Together these data reveal how simple neural dynamics, when coupled with activity fluctuations, can give rise to complex patterns of animal behavior.

Severe pneumonia due to Parachlamydia acanthamoebae following intranasal inoculation: a mice model.

Parachlamydia acanthamoebae is an obligate intracellular bacterium naturally infecting free-living amoebae. The role of this bacterium as an agent of pneumonia is suggested by sero-epidemiological studies and molecular surveys. Furthermore, P. acanthamoebae may escape macrophages microbicidal effectors. Recently, we demonstrated that intratracheal inoculation of P. acanthamoebae induced pneumonia in 100% of infected mice. However, the intratracheal route of infection is not the natural way of infection and we therefore developed an intranasal murine model. Mice inoculated with P. acanthamoebae by intranasal inoculation lost 18% of their weight up to 8 days post-inoculation. All mice presented histological signs of pneumonia at day 2, 4, 7, and 10 post-inoculation, whereas no control mice harboured signs of pneumonia. A 5-fold increase in bacterial load was observed from day 0 to day 4 post-inoculation. Lungs of inoculated mice were positive by Parachlamydia-specific immunohistochemistry 4 days post-inoculation, and P. acanthamoebae were localized within macrophages. Thus, we demonstrated that P. acanthamoebae induce a severe pneumonia in mice. This animal model (i) further supports the role of P. acanthamoebae as an agent of pneumonia, confirming the third Koch postulate, and (ii) identified alveolar macrophages as one of the initial cells where P. acanthamoebae is localized following infection.

Role of Munc18c in SNARE-mediated exocytosis

Background: The SNARE (Soluble N-ethylmaleimide-sensitive factor Attachment protein Receptors) and SM (Sec1/Munc18) family of proteins form the core machinery that drives the fusion of vesicles in different membrane trafficking steps. They are highly conserved, implying a similar mode of binding and function. In vertebrates, Munc18a is essential for neuronal exocytosis. It binds to its partner syntaxin1a (Syx1a) at both its N-peptide and closed conformation, and thereby inhibits SNARE complex formation in vitro. By contrast, its close homolog Munc18c is thought to interact with only the N-peptide of its partner Syx4. Moreover, different effects of Munc18c on SNARE complex formation have been reported, suggesting that the two Munc18/Syx pairs act differently. Objective: The aim of the present study was to investigate whether the mechanism of action of Munc18c indeed deviates from that of Munc18a by using sensitive biochemical and biophysical methods. Results: I found that Munc18c does have a similar binding mode as Munc18a and interacts tightly with Syx4 at both the N-peptide and closed conformation. Moreover, I established, through a novel assay, that Munc18c inhibits SNARE complex assembly, with both the binding sites contributing to inhibition, similar to Munc18a. However, there were several subtle differences between the two Munc18/Syx pairs. Munc18a exerted stronger inhibition than Munc18c. Also their respective Syx partners were found to differ in the rate of binding to SNAP25, suggesting that the equilibrium of their open and closed conformations is different. Moreover, Munc18a was found to interact with Syx 1, 2, 3 but not 4, while Munc18c bound to Syx 2, 4 and 1 but not 3. By comparing the kinetics of interaction of Syx with either Munc18 or SNAP25, I found that the block of SNARE complex assembly by Munc18 is effective on a shorter time scale, but SNAP25 eventually binds to Syx resulting in SNARE complex formation. Nevertheless, these findings do not explain how Syx can escape the tight grip of Munc18, suggesting that other proteins or mechanisms are needed for this step. I also discovered that Munc18 is able to bind on the surface of the SNARE core complex; however, this observation needs to be tested more rigorously. Conclusion: Munc18c was found to be similar to Munc18a in its mode of binding to Syx and inhibition of SNARE complex assembly. However, differences in kinetics and interaction specificities were observed between the different Munc18/Syx pairs. -- Contexte : Les familles des protéines SNARE (Soluble N-ethylmaleimide-sensitive factor At- tachment protein Receptors) et SM (Sec1/Munc18) forment le coeur de la machinerie chargée de la fusion vésiculaire au cours des différentes étapes du trafic intracellulaire. Elles sont très conservées, suggérant un mode d'interaction et des fonctions semblables. Chez les Verté- brés, Munc18a est essentielle à l'exocytose neuronale. Elle se lie à sa partenaire d'interaction syntaxin1a (Syx1a) à la fois via un peptide N-terminal et la conformation fermée de celle-ci, inhibant ainsi la formation du complexe SNARE in vitro. Son homologue proche Munc18c au contraire, est supposée interagir seulement avec le peptide N-terminal de sa partenaire Syx4. En outre, différents effets de Munc18c sur la formation du complexe SNARE ont été décrits, suggérant que les deux paires Munc18/Syx fonctionnent différemment. Objectif : Le but de cette étude est de tester si les mécanismes de fonctionnement de Munc18c diffèrent vraiment de ceux de Munc18a par le biais de méthodes biochimiques et biophysiques très précises. Résultats : J'ai pu démontrer que Munc18c se comporte en effet de façon semblable à Munc18a, et interagit étroitement avec Syx4 à ses deux sites de liaison. J'ai pu de surcroît montrer par une nouvelle méthode que Munc18c inhibe l'assemblage du complexe SNARE en impliquant ces deux sites de liaison, comme le fait Munc18a. il existe cependant de subtiles différences entre les deux paires Munc18/Syx : Munc18a exerce une inhibition plus forte que Munc18c ; leurs Syx partenaires diffèrent également dans leur degré de liaison à SNAP25, ce qui suggère un équilibre different de leurs conformations ouverte et fermée. De plus, Munc18a interagit avec Syx 1, 2 et 3 mais pas Syx 4, alors que Munc18c se lie à Syx 2, 4 et 1 mais pas Syx 3. En comparant les cinétiques d'interaction de Syx avec Munc18 ou SNAP25, j'ai découvert que le blocage par Munc18 de l'assemblage du complexe SNARE est effectif de façon brève, bien que SNAP25 finisse par se lier à Syx et aboutir ainsi à la formation du complexe SNARE. Ces découvertes n'expliquent cependant pas comment Syx parvient à échapper à la solide emprise de Munc18, et suggèrent ainsi l'intervention nécessaire d'autres protéines ou mécanismes à cette étape. J'ai également découvert que Munc18 peut se lier à la surface de la partie centrale du complexe SNARE - cette observation reste à être testée de façon plus stringente. Conclusion : Il a pu être établi que Munc18c est semblable à Munc18a quant à son mode de liaison à Syx et d'inhibition de l'assemblage du complexe SNARE. Des différences de cinétique et de spécificité d'interaction entre les diverses paires Munc18/Syx ont cependant été identifiées.

Predator or prey? Chlamydophila abortus infections of a free-living amoebae, Acanthamoeba castellani 9GU.

Limited evidence exists to suggest that the ability to invade and escape protozoan host cell bactericidal activity extends to members of the Chlamydiaceae, intracellular pathogens of humans and animals and evolutionary descendants of amoeba-resisting Chlamydia-like organisms. PCR and microscopic analyses of Chlamydophila abortus infections of Acanthamoeba castellani revealed uptake of this chlamydial pathogen but, unlike the well-described inhabitant of A. castellani, Parachlamydia acanthamoebae, Cp. abortus did not appear to propagate and is likely digested by its amoebal host. These data raise doubts about the ability of free-living amoebae to serve as hosts and vectors of pathogenic members of the Chlamydiaceae but reveal opportunities, via comparative genomics, to understand virulence mechanisms used by Chlamydia-like organisms to avoid amoebal digestion.

Immediate ecotoxicological effects of short-lived oil spills on marine biota.

Marine environments are frequently exposed to oil spills as a result of transportation, oil drilling or fuel usage. Whereas large oil spills and their effects have been widely documented, more common and recurrent small spills typically escape attention. To fill this important gap in the assessment of oil-spill effects, we performed two independent supervised full sea releases of 5 m(3) of crude oil, complemented by on-board mesocosm studies and sampling of accidentally encountered slicks. Using rapid on-board biological assays, we detect high bioavailability and toxicity of dissolved and dispersed oil within 24 h after the spills, occurring fairly deep (8 m) below the slicks. Selective decline of marine plankton is observed, equally relevant for early stages of larger spills. Our results demonstrate that, contrary to common thinking, even small spills have immediate adverse biological effects and their recurrent nature is likely to affect marine ecosystem functioning.