94 resultados para island exploration


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Freud defined the drive as "a concept on the frontier between the mental and the somatic". Today this view that was based on clinical observations interpreted within the psychoanalytical framework, can be revisited in light of the current neuroscientific notions of neuronal plasticity and somatic states. Indeed, through the mechanisms of plasticity experience leaves a trace that forms the neural basis of a representation of the experience. Such a representation R is associated with a somatic state S in the sense taken from the "somatic marker" model of Damasio. Thus, the internal reality of the subject, particularly the unconscious one, is constituted by such connected R's and S's. In the model that we discuss, the posterior insula represents the primary interoceptive cortex where information about somatic states S converges, while in the anterior insula the connection between R and S can take place and establish a neurobiological correlate for the notion of drive. We posit that the re-representations of S associated with R in the anterior insula may correspond to the Vorstellungsrepräsentanz postulated by Freud. We further propose that the tension between R and S established in the anterior insula is discharged according to the notion of drive through the motor arm of the limbic system, namely the anterior cingulate cortex which is heavily connected with the anterior insula.

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Quels rapports entretiennent travail et santé et quel type de recherche faut-il entreprendre pourétudier cette relation? Cet article vise à présenter les transformations de la recherche au niveau de l'interface travail/santé et essaye, à partir de là, de déterminer en quoi consiste aujourd'hui la recherche en santé au travail.

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High-precision isotope dilution - thermal ionization mass spectrometry (ID-TIMS) U-Pb zircon and baddeleyite ages from the PX1 vertically layered mafic intrusion Fuerteventura, Canary Islands, indicate initiation of magma crystallization at 22.10 +/- 0.07 Ma. The magmatic activity lasted a minimum of 0.52 Ma. Ar-40/Ar-39 amphibole dating yielded ages from 21.9 +/- 0.6 to 21.8 +/- 0.3, identical within errors to the U-Pb ages, despite the expected 1% theoretical bias between Ar-40/Ar-39 and U-Pb dates. This overlap could result from (i) rapid cooling of the intrusion (i. e., less than the 0.3 to 0.6 Ma 40Ar/39Ar age uncertainties) from closure temperatures (T-c) of zircon (699-988 degrees C) to amphibole (500-600 degrees C); (ii) lead loss affecting the youngest zircons; or (iii) excess argon shifting the plateau ages towards older values. The combination of the Ar-40/Ar-39 and U/Pb datasets implies that the maximum amount of time PX1 intrusion took to cool below amphibole T-c is 0.8 Ma, suggesting PX1 lifetime of 520 000 to 800 000 Ma. Age disparities among coexisting baddeleyite and zircon (22.10 +/- 0.07/0.08/0.15 Ma and 21.58 +/- 0.15/0.16/0.31 Ma) in a gabbro sample from the pluton margin suggest complex genetic relationships between phases. Baddeleyite is found preserved in plagioclase cores and crystallized early from low silica activity magma. Zircon crystallized later in a higher silica activity environment and is found in secondary scapolite and is found close to calcite veins, in secondary scapolite that recrystallised from plagioclase. close to calcite veins. Oxygen isotope delta O-18 values of altered plagioclase are high (+7.7), indicating interaction with fluids derived from host-rock carbonatites. The coexistence of baddeleyite and zircon is ascribed to interaction of the PX1 gabbro with CO2-rich carbonatite-derived fluids released during contact metamorphism.

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While studies on triggers and outcomes of Psychological Momentum (PM) exist, little is known about the dynamics by which PM emerges and develops over time. Based on video-assisted recalls of PM experiences in table tennis and swimming competitions, this research qualitatively explored the triggering processes, contents, and the development of PM over time. PM was found to be triggered by mechanisms of dissonance, consonance, or fear of not winning. During the PM experience, participants reported a variety of perceptions, affects and emotions, cognitions, and behaviors, and PM was found to develop through processes of amplification that sometimes ended with a reduction of efforts when the victory or defeat was perceived as certain. These findings are discussed in light of theories on self-regulation and reactance-helplessness. From a practical standpoint, achievement goal-based strategies are suggested, since mastery-approach goals were found to be endorsed to maintain positive PM and overcome negative PM

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This naturalistic cross-sectional study explores how and to what extent cannabis dependence was associated with intrapersonal aspects (anxiety, coping styles) and interpersonal aspects of adolescent functioning (school status, family relationships, peer relationships, social life). A convenience sample of 110 adolescents (aged 12 to 19) was recruited and subdivided into two groups (38 with a cannabis dependence and 72 nondependent) according to DSM-IV-TR criteria for cannabis dependence. Participants completed the State-Trait Anxiety Inventory (STAI-Y), the Coping Across Situations Questionnaire (CASQ), and the Adolescent Drug Abuse Diagnosis (ADAD) interview investigating psychosocial and interpersonal problems in an adolescent's life. Factors associated with cannabis dependence were explored with logistic regression analyses. The results indicated that severity of problems in social life and peer relationships (OR = 1.68, 95% CI = 1.21 - 2.33) and avoidant coping (OR = 4.22, 95% CI = 1.01 - 17.73) were the only discriminatory factors for cannabis dependence. This model correctly classified 84.5% of the adolescents. These findings are partially consistent with the "self-medication hypothesis" and underlined the importance of peer relationships and dysfunctional coping strategies in cannabis dependence in adolescence. Limitations of the study and implications for clinical work with adolescents are discussed.

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We launched a cryptoendolithic habitat, made of a gneissic impactite inoculated with Chroococcidiopsis sp., into Earth orbit. After orbiting the Earth for 16 days, the rock entered the Earth's atmosphere and was recovered in Kazakhstan. The heat of entry ablated and heated the rock to a temperature well above the upper temperature limit for life to below the depth at which light levels are insufficient for photosynthetic organisms ( approximately 5 mm), thus killing all of its photosynthetic inhabitants. This experiment shows that atmospheric transit acts as a strong biogeographical dispersal filter to the interplanetary transfer of photosynthesis. Following atmospheric entry we found that a transparent, glassy fusion crust had formed on the outside of the rock. Re-inoculated Chroococcidiopsis grew preferentially under the fusion crust in the relatively unaltered gneiss beneath. Organisms under the fusion grew approximately twice as fast as the organisms on the control rock. Thus, the biologically destructive effects of atmospheric transit can generate entirely novel and improved endolithic habitats for organisms on the destination planetary body that survive the dispersal filter. The experiment advances our understanding of how island biogeography works on the interplanetary scale.

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Genomic islands (GEIs) are large DNA segments, present in most bacterial genomes, that are most likely acquired via horizontal gene transfer. Here, we study the self-transfer system of the integrative and conjugative element ICEclc of Pseudomonas knackmussii B13, which stands model for a larger group of ICE/GEI with syntenic core gene organization. Functional screening revealed that unlike conjugative plasmids and other ICEs ICEclc carries two separate origins of transfer, with different sequence context but containing a similar repeat motif. Conjugation experiments with GFP-labelled ICEclc variants showed that both oriTs are used for transfer and with indistinguishable efficiencies, but that having two oriTs results in an estimated fourfold increase of ICEclc transfer rates in a population compared with having a single oriT. A gene for a relaxase essential for ICEclc transfer was also identified, but in vivo strand exchange assays suggested that the relaxase processes both oriTs in a different manner. This unique dual origin of transfer system might have provided an evolutionary advantage for distribution of ICE, a hypothesis that is supported by the fact that both oriT regions are conserved in several GEIs related to ICEclc.

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Messages à retenir: Connaître la pharmacocinétique du produit de contraste hépato spécifique Gd-EOB-DTPA.Apprendre la valeur diagnostique supplémentaire du Gd-EOB-DTPA comparée à celle des produits de contraste purement intravasculaires pour l'exploration destumeurs hépatiques.Connaître les situations cliniques typiques dans lesquelles l 'utilisation du Gd-EOB-DTPA est recommandée. Résumé: Le produit de contraste Gd-EOB-DTPA, un sel de l'acide gadoxétique, est un agent de contraste intra vasculaire et hépato-spécifique. Environ 50% de la doseinjectée par voie intraveineuse (IV) sont captés par les hépatocytes en phase veineuse, suivie d'une excrétion biliaire à environ 20 minutes après l'injection IV enbolus. En phase tardive, il en résulte donc un renforcement de contraste entre le parenchyme hépatique et toutes les lésions intra-hépatiques focales qui sontcomposées d'autres cellules que d'hépatocytes sains. La détection de métastases hépatiques est ainsi rendue plus facile, notamment celles de petite taille,même infra-centimétrique, en permettant de connaître exactement leur nombre total, ce qui est essentiel en cas de bilan pré-opératoire. La caractérisation destumeurs bénignes, telle que de l'hyperplasie nodulaire focale et de l'adénome hépatique, est également améliorée, en raison de leur contenu cellulaire différent.En cas de remaniement fibrotique ou cirrhotique sous-jacent, le Gd-EOB-DTPA s'est révélé supérieur que d'autres agents de contraste hépato-spécifiques enraison d'une meilleure imprégnation du parenchyme hépatique.

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Cette thèse présente les résultats d'une démarche comparatiste en histoire des religions. Elle poursuit un double but, à la fois thématique et méthodologique, en explorant une variété de représentations des transactions entre des figures féminines et des dieux. Elle en fait ressortir la diversité à partir d'un certain nombre de dossiers tirés de corpus de sources sélectionnés et constitués dans ce but. L'un de ces corpus est formé du Padavali (traduit sur la base de l'édition de P. Caturvedï), une collection de chants-poèmes dévotionnels krishnaïtes attribués à Mïràbàï (composés principalement entre le 16e et le 18e siècle en Inde du nord). L'autre corpus consiste en une sélection d'extraits de la littérature grecque d'auteurs et de styles différents. Au sein de cette sélection, la tragédie attique (5ème siècle avant l'ère commune), en particulier celle d'Euripide, et plusieurs traités de Plutarque (1er siècle de l'ère commune) figurent parmi les sources les plus importantes. La catégorie de « figure féminine » permet de prendre en considération des figures de statuts différents (mythologique, hagiographique ou historique) et de se focaliser sur les représentations des transactions avec des dieux, sans se restreindre à l'étude des pratiques historiquement attestées ou à leur reconstitution. Mirabai, en tant que figure hagiographique et emblématique du mouvement dévotionnel de la bhakti, les gopis et d'autres figures de la mythologie ou de l'hagiographie hindoue comptent parmi les figures féminines considérées sur la base du corpus indien de cette recherche ; les dossiers grecs incluent des sources variées mettant en scène les bacchantes, Ariane, la pythie, Cassandre, Créouse et d'autres figures féminines dans leur rapports avec des dieux, principalement Dionysos, Apollon et Hadès. Pensée comme une traversée des différences plutôt que comme une construction d'universaux, l'exploration thématique met en relief la grande variété des modalités des transactions de figures féminines avec des dieux et la mise en jeu du corps avant, pendant ou après celles-ci. Cinq axes thématiques transversaux, compris comme des faisceaux de questions, forment les comparables de cette recherche. Ils portent principalement sur (1) l'ajout au corps (ou le corps marqué, paré et équipé), (2) le retrait au corps (ou le corps dépouillé et dénudé), (3) la mise à disposition du corps féminin pour le dieu et ses conséquences, notamment en termes d'emprise attribuée au dieu, (4) la violence contre la figure féminine dans le cadre de sa relation au dieu et (5) les dissolutions, transformations, disparitions et dispersions du corps féminin. En plus du travail préalable de traduction et de contextualisation des sources, la mise en regard comparatiste de certains éléments des dossiers permet de dégager des axes de questionnement qui se veulent valables à plus large échelle pour une histoire des religions s'intéressant à la question des représentations du corps en intégrant une perspective de genre. La démonstration méthodologique consiste en une évaluation sur la base d'un exercice concret des limites et des apports d'une démarche de comparaison différentielle. Celle-ci comporte certes quelques défis dans sa mise en oeuvre et sa restitution, mais elle rend possible un processus de recherche souple et créatif qui permet d'envisager des dossiers connus sous de nouveaux angles ainsi qu'une redéfinition ou une création de catégories de recherche dynamiques et flexibles en histoire des religions.

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The aim of this study is to contribute to a better understanding of the risk factors associated with school burnout, which has recently been described as a syndrome of emotional exhaustion due to school demands, cynical and detached attitude towards school and feelings of inadequacy as a student (Salmela-Aro, Kiuru, Pietikainen & Jokela, 2008a). The research focuses on students in the last years of compulsory schooling, period in which burnout has not received much attention yet. A total of 342 adolescents (Mean age = 14.84) were asked to complete questionnaires about school burnout, school-related stress and background variables. The results showed differences in school burnout by gender, grade level and school track, with girls, last grade of compulsory school and high-track classes, showing the highest scores. No difference was observed with respect to grade retention. Several types of school stress were identified, with stress type Success related to pressures to succeed and concerns about the academic future being the highest. Finally, stress and burnout were strongly and positively correlated, and the type of stress Success was the best predictor of overall Burnout, Exhaustion and Inadequacy dimension scores. The results are discussed in relation to their theoretical relevance and implications for the prevention of school burnout in adolescents.

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In the Sverdrup Basin (Canadian Arctic), the Lower Triassic Blind Fiord Formation, comprising siltstone and shale, overlies various Middle to Late Permian (post-Wordian) sedimentary units. This formation is subdivided into three members: the Confederation Point, Smith Creek and Svartfjeld members of, respectively, Griesbachian-Dienerian, Smithian-Spathian and Spathian ages. Lower Triassic bryozoan beds are known from many sections of Ellesmere Island, but have never been studied in detail. During the Early Triassic biotic recovery interval, immediately following the Permian/Triassic extinction event, only one new bryozoan genus evolved in the Boreal region: Arcticopora. The first lower Triassic bryozoan bed appears in the upper part of the Confederation Point Member, and is dated as late Dienerian. Succeeding bryozoan levels occur in the upper Smith Creek Member, and are late Smithian-early Spathian in age. Bryozoan beds occupy a similar stratigraphic position in Spitsbergen. There, they occur scattered in silt to coarse sandstone beds, but also in bryozoan-dominated packstone beds resembling the packstone units in the uppermost part of the Confederation Point Member of Ellesmere Island. Previously, bryozoan-rich beds of Triassic age have not been reported, and the present work fills an important time gap in the bryozoan carbonate database