Formation of aluminosilicate-bearing quartz veins in the Simano nappe (Central Alps): structural, thermobarometric and oxygen isotope constraints

We combined structural analysis, thermobarometry and oxygen isotope geochemistry to constrain the evolution of kyanite and/or andalusite-bearing quartz veins from the amphibolite facies metapelites of the Simano nappe, in the Central Alps of Switzerland. The Simano nappe records a complex polyphase tectonic evolution associated with nappe stacking during Tertiary Alpine collision (D1). The second regional deformation phase (132) is responsible for the main penetrative schistosity and mineral lineation, and formed during top-to-the-north thrusting. During the next stage of deformation (D3) the aluminosilicate-bearing veins formed by crystallization in tension gashes, in tectonic shadows of boudins, as well as along shear bands associated with top-to-the-north shearing. D2 and D3 are coeval with the Early Miocene metamorphic peak, characterised by kyanite + staurolite + garnet + biotite assemblages in metapelites. The peak pressure (P) and temperature (T) conditions recorded are constrained by multiple-equilibrium thermobarometry at 630 +/- 20 degrees C and 8.5 +/- 1 kbar (similar to 27 km depth), which is in agreement with oxygen isotope thermometry indicating isotopic equilibration of quartz-kyanite pairs at 670 +/- 50 degrees C. Quartz-kyanite pairs from the aluminosilicate-bearing quartz veins yield equilibration temperatures of 645 +/- 20 degrees C, confirming that the veins formed under conditions near metamorphic peak. Quartz and kyanite from veins and the surrounding metapelites have comparable isotopic compositions. Local intergranular diffusion in the border of the veins controls the mass-transfer and the growth of the product assemblage, inducing local mobilization of SiO2 and Al2O3. Andalusite is absent from the host rocks, but it is common in quartz veins, where it often pseudomorphs kyanite. For andalusite to be stable at T-max, the pressure in the veins must have been substantially lower than lithostatic. An alternative explanation consistent with structural observations would be inheritance by andalusite of the kyanite isotopic signature during polymorphic transformation after the metamorphic peak.

Total lipid and fatty acid accumulation during basidiospore formation in the ectomycorrhizal fungus Pisolithus sp.

The basidiospores of Pisolithus sp. contain large amounts of lipids, indicating provision for future germination in the host rhizosphere. However, the accumulation, composition, and mobilization of lipids during formation and germination of these spores are largely unknown. In this study, lipid storage and fatty acid composition during basidiosporogenesis were analyzed in fresh basidiocarps using bright-field microscopy and gas chromatography. Abundant lipid bodies are found in the hyphae, basidia, and basidiospores of fungal basidiocarps. This evidences a considerable C transport in the basidiocarp to meet the C demand during basidiospore formation. Fatty acid composition analysis revealed the presence of 24 compounds with chains of 9 to 18 C atoms, either saturated or insaturated, with one or two insaturations. The fatty acid composition and content varied according to the developmental stage of the peridioles. In free basidiospores, the predominant compounds were 16:0, 16:1w5c, 18:1w9c, and 18:2w6,9c/18:0ante, at concentrations of 76, 46, 192, and 51 µg g-1 dry matter, respectively. Our results indicate that oleic acid is the major constituent of lipid reserves in Pisolithus sp. basidiospores. Further studies are being conducted to determine the factors that induce lipid mobilization during spore germination.

Physicians' estimates of the 10-year cardiovascular risk in hypertensive patients

RESUME L'objectif de cette étude est d'évaluer comment de jeunes médecins en formation perçoivent le risque cardiovasculaire de leurs patients hypertendus en se basant sur les recommandations médicales (« guidelines ») et sur leur jugement clinique. Il s'agit d'une étude transversale observationnelle effectuée à la Policlinique Médicale Universitaire de Lausanne (PMU). 200 patients hypertendus ont été inclus dans l'étude ainsi qu'un groupe contrôle de 50 patients non hypertendus présentant au moins un facteur de risque cardiovasculaire. Nous avons comparé le risque cardiovasculaire à 10 ans calculé par un programme informatique basé sur l'équation de Framingham. L'équation a été adaptée pour les médecins par l'OMS-ISH au risque perçu, estimé cliniquement par les médecins. Les résultats de notre étude ont montrés que les médecins sous-estiment le risque cardiovasculaire à 10 ans de leurs patients, comparé au risque calculé selon l'équation de Framingham. La concordance entre les deux méthodes était de 39% pour les patients hypertendus et de 30% pour le groupe contrôle de patients non hypertendus. La sous-estimation du risque. cardiovasculaire pour les patients hypertendus était corrélée au fait qu'ils avaient une tension artérielle systolique stabilisée inférieure a 140 mmHg (OR=2.1 [1.1 ;4.1]). En conclusion, les résultats de cette étude montrent que les jeunes médecins en formation ont souvent une perception incorrecte du risque cardiovasculaire de leurs patients, avec une tendance à sous-estimer ce risque. Toutefois le risque calculé pourrait aussi être légèrement surestimé lorsqu'on applique l'équation de Framingham à la population suisse. Pour mettre en pratique une évaluation systématique des facteurs de risque en médecine de premier recours, un accent plus grand devrait être mis sur l'enseignement de l'évaluation du risque cardiovasculaire ainsi que sur la mise en oeuvre de programme pour l'amélioration de la qualité.

Mort subite cardiaque dans la famille : quel bilan chez les proches ?

La mort subite est fréquemment d'origine génétique, en particulier lorsqu'elle touche les sujets jeunes. Il existe dans ces situations un risque accru pour les proches, qui devraient bénéficier d'un bilan cardiologique et d'un conseil génétique, dans la mesure où des mesures thérapeutiques et/ou préventives sont disponibles. Les analyses génétiques post-mortem, ou autopsie moléculaire, permettent de préciser le diagnostic dans un certain nombre de cas. Ces nouvelles possibilités sont susceptibles d'améliorer le dépistage des sujets à risque, même si leur mise en oeuvre suscite nombre de questions éthiques, majorées par des cicronstances psychologiques difficiles. Des protocoles spécifiques d'évaluation et une information des professionnels doivent être développés.

Ophiolite-related ultramafic rocks (Serpentinites) in the Caribbean region: a review of their occurrence, composition, origin, emplacements and Ni-Laterite soil formation

Ultramafic rocks, mainly serpentinized peridotites of mantle origin, are mostly associated with the ophiolites of Mesozoic age that occur in belts along three of the margins of the Caribbean plate. The most extensive exposures are in Cuba. The ultramafic-mafic association (ophiolites) were formed and emplaced in several different tectonic environments. Mineralogical studies of the ultramafic rocks and the chemistry of the associated mafic rocks indicate that most of the ultramafic-mafic associations in both the northern and southern margins of the plate were formed in arc-related environments. There is little mantle peridotite exposed in the ophiolitic associations of the west coast of Central America, in the south Caribbean in Curacao and in the Andean belts in Colombia. In these occurrences the chemistry and age of the mafic rocks indicates that this association is mainly part of the 89 Ma Caribbean plateau province. The age of the mantle peridotites and associated ophiolites is probably mainly late Jurassic or Early Cretaceous. Emplacement of the ophiolites possibly began in the Early Cretaceous in Hispaniola and Puerto Rico, but most emplacement took place in the Late Cretaceous to Eocene (e.g. Cuba). Along the northern South America plate margin, in the Caribbean mountain belt, emplacement was by major thrusting and probably was not completed until the Oligocene or even the early Miocene. Caribbean mantle peridotites, before serpentinization, were mainly harzburgites, but dunites and lherzolites are also present. In detail, the mineralogical and chemical composition varies even within one ultramafic body, reflecting melting processes and peridotite/melt interaction in the upper mantle. At least for the northern Caribbean, uplift (postemplacement tectonics) exposed the ultramafic massifs as a land surface to effective laterization in the beginning of the Miocene. Tectonic factors, determining the uplift, exposing the peridotites to weathering varied. In the northern Caribbean, in Guatemala, Jamaica, and Hispaniola, uplift occurred as a result of transpresional movement along pre-existing major faults. In Cuba, uplift occurred on a regional scale, determined by isostatic adjustment. In the south Caribbean, uplift of the Cordillera de la Costa and Serrania del Interior exposing the peridotites, also appears to be related to strike-slip movement along the El Pilar fault system. In the Caribbean, Ni-laterite deposits are currently being mined in the central Dominican Republic, eastern Cuba, northern Venezuela and northwest Colombia. Although apparently formed over ultramafic rocks of similar composition and under similar climatic conditions, the composition of the lateritic soils varies. Factors that probably determined these differences in laterite composition are geomorphology, topography, drainage and tectonics. According to the mineralogy of principal ore-bearing phases, Dominican Ni-laterite deposits are classified as the hydrous silicate-type. The main Ni-bearing minerals are hydrated Mg-Ni silicates (serpentine and ¿garnierite¿) occurring deeper in the profile (saprolite horizon). In contrast, in the deposits of eastern Cuba, the Ni and Cooccurs mainly in the limonite zone composed of Fe hydroxides and oxides as the dominant mineralogy in the upper part of the profile, and are classified as the oxide-type.

Linking microtubules to the activation of CDC42 in fission yeast

Cell polarity is an essential property of most cell types and relies on a dynamic cytoskeleton of actin filaments and microtubules. In rod-shaped S. pombe cells microtubules are organized along the length of the cell and transport polarity factors to cell tips to regulate cell polarity. An important cell polarity factor is the protein Tea4, which is responsible for correct cell morphogenesis and bipolar growth. During my research I confirmed the known transport mechanism of Tea4 and I also showed alternative localization and anchoring mechanisms at the cell ends. Tea4 contains a conserved SH3 domain, the function of which was unknown and my results show that the SH3 domain of Tea4 is essential for Tea4 function in vivo. First, cells with tea4SH3 mutations show aberrant cell shapes and monopolar growth patterns similar to tea4A and in addition SH3 domain is important for proper localization of multiple cell polarity proteins. Second, I showed that Tea4 associates with Type 1 Phosphatase Dis2 through both its SH3 domain and an RVxF motif. Tea4 also binds the DYRK kinase Pomi through its SH3 domain. In addition Tea4 is proposed to promote the local dephosphorylation of Pomi by Dis2 to induce the formation of a cortical gradient from cell ends essential for cell size homeostasis. Polarized growth is also controlled by cell tip-localized Cdc42. This Rho- family GTPase is activated by the Guanine Exchange Factors Gef1 and Scd1 and inactivated by the Rho GTPase Activating Protein Rga4. In this study, I investigated the mechanisms of how Tea4 promotes Cdc42 activation. My work suggests that Tea4 promotes the local exclusion of Rga4, which in turn allows the accumulation of active Cdc42, which may result in growth. Exclusion of Rga4 by Tea4 is likely to be mediated by Dis2-dependent dephosphorylation. These results suggest a molecular pathway that links the microtubule- associated factor Tea4 with Cdc42 to promote cell polarization and morphogenesis. - La polarité cellulaire est une propriété essentielle de la plupart des types cellulaires et s'appuie sur une dynamique des cytosquelettes d'actine et de microtubules. Dans les cellules en forme de bâtonnet de S. pombe les microtubules sont alignés selon l'axe longitudinal de la cellule et les facteurs de polarité transportés aux extrémité cellulaires afin de réguler la polarité cellulaire. Un facteur important de polarité cellulaire est la protéine Tea4, qui est responsable de la morphogenèse des cellules et leur croissance bipolaire. Au cours de mes recherches, j'ai confirmé les mécanismes connus de transport de Tea4 et j'ai aussi mis en évidence d'autres mechanismes de localisation et d'ancrage de Tea4 aux extrémités cellulaires. Tea4 contient un domaine SH3 conservé, dont la fonction était inconnue et mes résultats montrent que le domaine SH3 est essentiel pour la fonction de Tea4 in vivo. Tout d'abord, les cellules avec des mutations tea4sm ont des formes aberrantes et leur croissance est monopolaire de manière similaire au mutant tea4A. De plus ce domaine SH3 est important pour la localisation correcte de plusieurs protéines de polarité cellulaire. Deuxièmement, j'ai montré que Tea4 s'associe avec la Phosphatase de Type-1 Dis2 par son domaine SH3 et un motif RVxF. Tea4 se lie également la kinase DYRK Pomi par son domaine SH3. De plus, Tea4 pourrait favoriser la déphosphorylation locale de Pomi par Dis2 afin d'induire la formation d'un gradient cortical de Pomi essentiel pour l'homéostasie de la longueur des cellules. La croissance polarisée est également contrôlée par la protéine Cdc42 localisée aux extrémités cellulaires. Cette GTPase de la famille de Rho GTPase est activée par les facteurs échange de guanine Gef1 et Scd1 et inactivée par la protéine "Rho GTPase activating" Rga4. Dans cette étude, j'ai étudié les mécanismes d' activation de Cdc42 par Tea4. Mes résultats suggèrent que Tea4 favorise l'exclusion locale de Rga4, ce qui permet l'accumulation de Cdc42 active, nécessaire à la croissance. L' exclusion de Rga4 par Tea4 est vraisemblablement médiée par une déphosphorylation Dis2- dépendente. Ces résultats suggèrent une voie moléculaire qui lie le facteur associé aux microtubules Tea4 à Cdc42 pour promouvoir la polarisation cellulaire et la morphogenèse. - Cell polarity is important for several essential biological functions such as generation of distinct cell fates during development and function of differentiated cells. Defective cell polarity has been related to uncontrolled cell division and subsequently to cancer initiation. Cell polarity depends on a functional cytoskeleton that consists of actin filaments and microtubules, which maintains cell shape, helps cellular motion, enables intracellular protein transport and plays a vital role in cell division. A component of cytoskeleton is microtubules that regulate cell polarization in diverse cell types. During my research, I worked with Schizosaccharomyces pombe, also named fission yeast, a powerful unicellular model organism that allows combination of genetic, biochemical and microscopic analysis for the proper study of cell polarity. Microtubule-associated protein Tea4 is transported to cell tips where it is thought to organize polarized growth. I showed that Tea4 and its evolutionarily conserved SH3 domain play an important role for maintenance of fission yeast cells shape and growth. Furthermore, Tea4 is responsible for the proper localization of multiple polarity proteins and acts as a mediator to control the local activity of an essential polarity regulator called Cdc42. Thus, my results provide a better understanding of the molecular mechanisms that regulate cell polarity. - La polarité cellulaire est importante pour plusieurs fonctions biologiques essentielles telles que la différenciation cellulaires au cours du développement et de la fonction de cellules différenciées. Les défauts de la polarité cellulaire ont été liés à des divisions cellulaires incontrôlées et à l'initiation de tumeur. La polarité cellulaire dépend d'un cytosquelette fonctionnel, qui maintient la forme des cellules, aide à la migration cellulaire, permet le transport intracellulaire des protéines et joue un rôle essentiel dans la division cellulaire. Un composant du cytosquelette est constitué de microtubules qui régissent la polarisation cellulaire dans divers types cellulaires. Au cours de mes recherches, j'ai travaillé avec Schizosaccharomyces pombe, appelé également levure fissipare, un modèle unicellulare puissant qui permet la combinaison de différentes d'approches expérimentales: génétiques, biochimiques et microscopiques pour l'étude de la polarité cellulaire. La protéine Tea4 associée aux microtubules est transportée aux extrémités cellulaires où elle organise la croissance polarisée. J'ai montré que Tea4 et son domaine conservé SH3 jouent un rôle important pour le maintien de la forme des cellules de levure et leur croissance. De plus, Tea4 est responsable de la localisation correcte de multiples facteurs de polarité et agit comme un médiateur pour contrôler l'activité locale d'un régulateur de polarité essentiel appelé Cdc42. Ainsi, mes résultats permettent de mieux comprendre les mécanismes moléculaires qui régulent la polarité cellulaire.

Influence of the (111) twinning on the formation of diamond cubic/diamond hexagonal heterostructures in Cu-catalyzed Si nanowires

The occurrence of heterostructures of cubic silicon/hexagonal silicon as disks defined along the nanowire (111) growth direction is reviewed in detail for Si nanowires obtained using Cu as catalyst. Detailed measurements on the structural properties of both semiconductor phases and their interface are presented. We observe that during growth, lamellar twinning on the cubic phase along the (111) direction is generated. Consecutive presence of twins along the (111) growth direction was found to be correlated with the origin of the local formation of the hexagonal Si segments along the nanowires, which define quantum wells of hexagonal Si diamond. Finally, we evaluate and comment on the consequences of the twins and wurtzite in the final electronic properties of the wires with the help of the predicted energy band diagram.