135 resultados para Sedimentary structures
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Dopaminergic, serotonergic and noradrenergic nuclei form the trimonoamine modulating system (TMMS). This system modulates emotional/motivational activities mediated by the limbic circuitry, where glutamate is the major excitatory neurotransmitter. Two main concepts are the basis of this review. First, since 1950 and the discovery of the antipsychotic activity of the dopamine D2 receptor antagonist chlorpromazine, it appears that drugs that can modulate the TMMS possess therapeutic psychiatric properties. Second, the concept of glutamate/trimonoamine imbalance in the cortico-striato-thalamo-cortical loop that has been so successful in explaining the pathophysiology of Parkinson disease has been applied in the pathophysiology of schizophrenia. This review will focus on the complex interactions between the fast synaptic glutamatergic transmission and the TMMS in specific parts of the limbic lobe and we will try to link these interactions to some psychiatric disorders, mainly depression, schizophrenia and drug addiction.
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The formation and structural evolution of the jungrau syncline is described, based on excellent outcrops occurring in the lotschental, in the central alps of switzerland. the quality of the outcrops allows us to demonstrate that the external massifs of the swiss alps have developed due to internal folding. The jungfrau suncline, which separates the autochtonous gastern dome from the aar massif basement gneiss folds, is composed of slivers of basement rocks with their mesozoic sedimentary cover. in the inner faflertal, a side valley of the lotschental, the 200 m thick syncline cp, roses fpir imots, the gastern massif with a reduced mesozoic sedimentary cover in a normal stratigraphic succession, two units of overturned basement rocks with their mesozoic sedimentary cover, and the overturned lower limn of the tschingelhorn gneiss fold of the aar massif with lenses of its sedimentary cover. stratigraphy shows that the lower units, related to the gastern massis, are condensed and that the upper units, deposited farther away from a gastern paleo-high, form a more complete sequence, linked to the doldenhorn meso-cneozoic basin fill. the integration of these local observations with published regional data leads to the following model. on the northern margin of the doldenhorn hbasin, at the northern fringe of the alpine tethuys, the pre-triassic crystalline basement and its mesozoic sedimentary cover were folded by ductile deformation at temperatures above 300 degrees C and in the presence of high fluid pressures, as the helveti c and penninic nappes were overthrusted towards the northwest during the main alpine deformation phase, the visosity contrast between the basement gneisses and the sediments caused the formation of large basement anticlines and tight sedimentary sunclines (mullion-type structures). The edges of basement blocks bounded buy pre-cursor se-dipping normal faults at the northwestern border of the doldenhorn basin were deformed bu simple shear, creating overturned slices of crystalline rocks with their sedimentary cover in what now forms the hungfrau syncline. the localisation of ductile deformation in the vicinity of pre-existing se-dipping faults is thought to have been helped by the circulation of fluids along the faults; these fluids would have been released from the mesozoic sediments by metamorphic dehydration reactions accompanied by creep and dynamic recrystallisation of quartz at temperatures above 300 degrees C. Quantification of the deformation suggests an strain ellipsoid with a ratio (1 + e(1)/+ e(3)) of approximately 1000. The jungfrau suncline was deformed bu more brittle nw-directed shear creating well-developed shear band cleavages at a late stage, after cooling by uplift and erosion. It is suggested that the external massifs of the apls are basement gneiss folds created at temperatures of 300 degrees C by detachment through ductile deformation of the upper crust of the european plate as it was underthrusted below the adriatic plate.
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1. Little is known on the occurrence and magnitude of faster than normal (catch-up) growth in response to periods of undernutrition in the wild, and the extent to which different body structures compensate and over what timescales is poorly understood. 2. We investigated catch-up growth in nestling Alpine Swifts, Apus melba, by comparing nestling growth trajectories in response to a naturally occurring 1-week period of inclement weather and undernutrition with growth of nestlings reared in a good year. 3. In response to undernutrition, nestlings exhibited a hierarchy of tissues preservation and compensation, with body mass being restored quickly after the end of the period of undernutrition, acceleration of skeletal growth occurring later in development, and compensation in wing length occurring mostly due to a prolongation of growth and delayed fledging. 4. The effect of undernutrition and subsequent catch-up growth was age-dependent, with older nestlings being more resilient to undernutrition, and in turn having less need to compensate later in the development. 5. This shows that young in a free-living bird population can compensate in body mass and body size for a naturally occurring period of undernutrition, and that the timing and extent of compensation varies with age and between body structures.
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With the dramatic increase in the volume of experimental results in every domain of life sciences, assembling pertinent data and combining information from different fields has become a challenge. Information is dispersed over numerous specialized databases and is presented in many different formats. Rapid access to experiment-based information about well-characterized proteins helps predict the function of uncharacterized proteins identified by large-scale sequencing. In this context, universal knowledgebases play essential roles in providing access to data from complementary types of experiments and serving as hubs with cross-references to many specialized databases. This review outlines how the value of experimental data is optimized by combining high-quality protein sequences with complementary experimental results, including information derived from protein 3D-structures, using as an example the UniProt knowledgebase (UniProtKB) and the tools and links provided on its website ( http://www.uniprot.org/ ). It also evokes precautions that are necessary for successful predictions and extrapolations.
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An understanding of details of the interaction mechanisms of bacterial endotoxins (lipopolysaccharide, LPS) with the oxygen transport protein hemoglobin is still lacking, despite its high biological relevance. Here, a biophysical investigation into the endotoxin:hemoglobin interaction is presented which comprises the use of various rough mutant LPS as well as free lipid A; in addition to the complete hemoglobin molecule from fetal sheep extract, also the partial structure alpha-chain and the heme-free sample are studied. The investigations comprise the determination of the gel-to-liquid crystalline phase behaviour of the acyl chains of LPS, the ultrastructure (type of aggregate structure and morphology) of the endotoxins, and the incorporation of the hemoglobins into artificial immune cell membranes and into LPS. Our data suggest a model for the interaction between Hb and LPS in which hemoglobins do not react strongly with the hydrophilic or with the hydrophobic moiety of LPS, but with the complete endotoxin aggregate. Hb is able to incorporate into LPS with the longitudinal direction parallel to the lipid A double-layer. Although this does not lead to a strong disturbance of the LPS acyl chain packing, the change of the curvature leads to a slightly conical molecular shape with a change of the three-dimensional arrangement from unilamellar into cubic LPS aggregates. Our previous results show that cubic LPS structures exhibit strong endotoxic activity. The property of Hb on the physical state of LPS described here may explain the observation of an increase in LPS-mediating endotoxicity due to the action of Hb.
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[Table des matières] 1. Méthodes d'évaluation. 2. Le Passage et le Point d'eau. 2.1. Historique et objectifs. 2.2. Etapes de la mise en route. 3.1. Professionnels salariés. 3.2. Bénévoles professionnels. 3.3. Bénévoles d'accueil. 4.1. Activités de la structure. 4.2. Accueil (animations, repas, collations). 4.3. L'offre socio-éducative. 4.4. L'offre sanitaire. 4.5. La distribution du matériel stérile. 5.1. Prestations d'hygiène. 5.2. Soins somatiques. 5.3. Activité sportive. 6.1. Profil des usagers. 6.2. Indicateurs socio-démographiques et d'intégration sociale. 6.3. Etat de santé perçu. 6.4. Fréquentation du réseau (dispositif bas seuil et autre) et de Point d'eau. 7. Consommation de drogues illégales. 8. Fréquentation de la structure. 9.1. Méthodes d'évaluation utilisées. 9.2. Evaluation du Passage et du Point d'eau.
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Depuis quelque temps, de plus en plus de spécialistes de la politique sociale préconisent une stratégie d'investissement social dans laquelle les crèches joueraient un rôle majeur. Cette stratégie vise à prévenir les exclusions sociales par la promotion de l'égalité des chances et de l'accès à l'emploi en vue d'un allègement des dépenses de protection sociale passive. Outre qu'elles permettent aux familles d'avoir deux revenus, les crèches ont en effet l'avantage de réduire les écarts au niveau des compétences cognitives et linguistiques entre les enfants venant de différents milieux sociaux. Mais le succès d'une telle stratégie présuppose que certains publics cibles recourent effectivement aux crèches, à savoir les ménages disposant d'un faible revenu ou/et de niveau de formation, ainsi que les familles issues de l'immigration. Or, des analyses statistiques sur la base de l'Enquête suisse sur la population active (ESPA) de 2008 montrent que, pour les familles en Suisse, les chances d'utiliser une crèche augmentent avec le niveau de formation des parents. Concernant plus particulièrement le niveau de formation des mères, ce phénomène n'est d'ailleurs que partiellement conditionné par le taux d'activité supérieur de celles ayant accompli une formation de degré tertiaire. En outre, certaines populations d'immigrés dont l'intégration dans la société suisse est réputée difficile sont peu disposées à recourir aux crèches. Les immigrés de première génération de quasiment toutes les origines fortement représentées en Suisse ont en revanche plus de chances que les parents d'origine suisse de faire appel au service d'une crèche à raison d'au moins 4 jours/semaine, ce qui peut influer négativement sur le comportement de l'enfant. Ce dernier résultat semble paradoxal mais montre qu'une migration rend plus difficile l'organisation d'une garde informelle comme solution complémentaire à la crèche. En synthèse, la présente étude attire l'attention sur le fait que les atouts pédagogiques et socialisants des crèches reviennent avant tout aux enfants de parents d'origine suisse ou venant de pays culturellement proches et ayant un niveau de formation supérieur. Telle que conçue actuellement, l'offre de crèches en Suisse ne semble guère opérer comme un instrument efficace de l'investissement social. Immer mehr Experten der Sozialpolitik empfehlen eine ,,Strategie der sozialen Investitionen", die den Kindertagesstätten (bzw. Kinderkrippen) eine wichtige Rolle zuschreibt. Ziel dieser Strategie ist es, durch Förderung von Chancengleichheit und Arbeitsmarktpartizipation sozialen Ausgrenzungen vorzubeugen, um Einsparungen im Bereich der passiven Sozialleistungen zu ermöglichen. Krippen haben einerseits den Vorteil, dass sie es den Familien ermöglichen, zwei Einkommen zu erzielen. Andererseits tragen sie zur Minderung von kognitiven und sprachlichen Fähigkeitsunterschieden zwischen Vorschulkindern aus verschiedenen sozialen Milieus bei. Der Erfolg dieser Strategie setzt jedoch voraus, dass gewisse Zielgruppen tatsächlich Krippen nutzen, nämlich bezüglich Einkommen und/oder Bildung benachteiligte Haushalte sowie Familien mit Migrationshintergrund. Die vorliegenden statistischen Analysen aufgrund der SAKE-Daten von 2008 (Schweizerische Arbeitskräfteerhebung) ergeben jedoch für die Schweiz, dass die Wahrscheinlichkeit, eine Krippe zu nutzen, mit dem Bildungsniveau der Eltern steigt. Was das Bildungsniveau der Mütter im Besonderen anbelangt, ist dieses Phänomen nur teilweise bedingt durch den tendenziell höheren Beschäftigungsgrad der besser Ausgebildeten. Zudem haben einige Migrantengruppen, deren Integration in die Schweizer Gesellschaft als besonders schwierig betrachtet wird, eine bedeutend tiefere Benützungswahrscheinlichkeit als Eltern Schweizer Herkunft. Für fast alle in der Schweiz stark vertretenen Migranten erster Generation ist dennoch das statistische Risiko grösser, die Krippe während mindestens 4 Tagen/Woche zu nutzen, was einen negativen Einfluss auf das Verhalten des Kindes haben kann. Dieses scheinbar paradoxe Ergebnis ist darauf zurückzuführen, dass ein Migrationshintergrund das Organisieren von krippenergänzenden Betreuungslösungen informeller Art meist erschwert. Gesamthaft zeigt die vorliegende Studie auf, dass die positiven pädagogischen und sozialisierenden Effekte der Krippen in erster Linie Kindern zugutekommen, deren Eltern eine höhere Ausbildung haben, Schweizer Herkunft sind oder aus einem kulturell nahestehenden Land kommen. So wie es gegenwärtig eingerichtet ist, scheint das Krippenangebot in der Schweiz kaum als effizientes Instrument sozialer Investitionen zu wirken.
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Surface geological mapping, laboratory measurements of rock properties, and seismic reflection data are integrated through three-dimensional seismic modeling to determine the likely cause of upper crustal reflections and to elucidate the deep structure of the Penninic Alps in eastern Switzerland. Results indicate that the principal upper crustal reflections recorded on the south end of Swiss seismic line NFP20-EAST can be explained by the subsurface geometry of stacked basement nappes. In addition, modeling results provide improvements to structural maps based solely on surface trends and suggest the presence of previously unrecognized rock units in the subsurface. Construction of the initial model is based upon extrapolation of plunging surface. structures; velocities and densities are established by laboratory measurements of corresponding rock units. Iterative modification produces a best fit model that refines the definition of the subsurface geometry of major structures. We conclude that most reflections from the upper 20 km can be ascribed to the presence of sedimentary cover rocks (especially carbonates) and ophiolites juxtaposed against crystalline basement nappes. Thus, in this area, reflections appear to be principally due to first-order lithologic contrasts. This study also demonstrates not only the importance of three-dimensional effects (sideswipe) in interpreting seismic data, but also that these effects can be considered quantitatively through three-dimensional modeling.