Hibridismo e conflitos morais em 'Narrativas Militares' (1878), do Visconde de Taunay

Coordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES)

Estudo estrutural dos precursores, intermediários e colóides derivados do acetato de zinco e propriedades elétricas, óticas e estruturais dos filmes de óxido de zinco dopados com índio

Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)

O discurso literário e cinematográfico: simetrias e assimetrias em O Leopardo, Guisseppe Tomasi di Lampedusa X Luchino Visconti

Este trabalho trata de duas artes, Literatura e Cinema. Embora autônomas e específicas, traduzem-se em textos distintos, relações de identificação e ao mesmo tempo afastamento de uma obra em relação à outra. Nossa abordagem tem, como ponto de partida, o texto literário "O Leopardo", do escritor italiano Giuseppe Tomasi di Lampedusa e, como ponto de chegada, a obra cinematográfica homônima do cineasta, também italiano, Luchino Visconti. Lampedusa produziu uma obra que só ganharia reconhecimento postumamente. Nela, criou um discurso narrativo através do qual põe em destaque a História e a representação da sociedade. Apesar de ter nos legado uma obra pequena, caracteriza-se por apresentar um estilo próprio, marcado por requintes de liberdade e recriação da palavra. Luchino Visconti, o mais requintado criador da sétima arte de seu tempo, transpôs, com rigor, para a tela, importantes obras de renomados escritores. Seus filmes traduzem uma precisa visão histórica e aristocrática. A narrativa cinematográfica mescla ousadia e criatividade, desafiando a escritura ao arquitetá-la em magníficas imagens, cumprindo com o (quase) intuito da fidelidade a abstração da imagem literária.

Matrizes híbridas siloxano-poliéter para liberação controlada de fármacos

Pós-graduação em Química - IQ

Investigação de plantas africanas: Viviane Raïssa Sipowo Tala.-

Pós-graduação em Química - IQ

Provenienza dei sedimenti arenitici nel bacino di Tracia (eo-oligocene, Turchia nord-occidentale e Grecia nord-orientale)

The Thrace Basin is the largest and thickest Tertiary sedimentary basin of the eastern Balkans region and constitutes an important hydrocarbon province. It is located between the Rhodope-Strandja Massif to the north and west, the Marmara Sea and Biga Peninsula to the south, and the Black Sea to the est. It consists of a complex system of depocenters and uplifts with very articulate paleotopography indicated by abrupt lateral facies variations. Its southeastern margin is widely deformed by the Ganos Fault, a segment of the North Anatolian strike-slip fault system . Most of the Thrace Basin fill ranges from the Eocene to the Late Oligocene. Maximum total thickness, including the Neogene-Quaternary succession, reaches 9.000 meters in a few narrow depocenters. This sedimentary succession consists mainly of basin plain turbiditic deposits with a significant volcaniclastic component which evolves upwards to shelf deposits and continental facies, with deltaic bodies prograding towards the basin center in the Oligocene. This work deals with the provenance of Eocene-Oligocene clastic sediments of the southern and western part of Thrace Basin in Turkey and Greece. Sandstone compositional data (78 gross composition analyses and 40 heavy minerals analyses) were used to understand the change in detrital modes which reflects the provenance and geodinamic evolution of the basin. Samples were collected at six localities, which are from west to est: Gökçeada, Gallipoli and South-Ganos (south of Ganos Fault), Alexandroupolis, Korudağ and North-Ganos (north of Ganos Fault). Petrologic (framework composition and heavy-mineral analyses) and stratigraphic-sedimentologic data, (analysis of sedimentologic facies associations along representative stratigraphic sections, paleocurrents) allowed discrimination of six petrofacies; for each petrofacies the sediment dispersal system was delineated. The Thrace Basin fill is made mainly of lithic arkoses and arkosic litharenites with variable amount of low-grade metamorphic lithics (also ophiolitic), neovolcanic lithics, and carbonate grains (mainly extrabasinal). Picotite is the most widespread heavy mineral in all petrofacies. Petrological data on analyzed successions show a complex sediment dispersal pattern and evolution of the basin, indicating one principal detrital input from a source area located to the south, along both the İzmir-Ankara and Intra-Pontide suture lines, and a possible secondary source area, represented by the Rhodope Massif to the west. A significant portion of the Thrace Basin sediments in the study area were derived from ophiolitic source rocks and from their oceanic cover, whereas epimetamorphic detrital components came from a low-grade crystalline basement. An important penecontemporaneous volcanic component is widespread in late Eocene-Oligocene times, indicating widespread post-collisional (collapse?) volcanism following the closure of the Vardar ocean. Large-scale sediment mass wasting from south to north along the southern margin of the Thrace Basin is indicated (i) in late Eocene time by large olistoliths of ophiolites and penecontemporaneous carbonates, and (ii) in the mid-Oligocene by large volcaniclastic olistoliths. The late Oligocene paleogeographic scenario was characterized by large deltaic bodies prograding northward (Osmancik Formation). This clearly indicates that the southern margin of the basin acted as a major sediment source area throughout its Eocene-Oligocene history. Another major sediment source area is represented by the Rhodope Massif, in particolar the Circum-Rhodopic belt, especially for plutonic and metamorphic rocks. Considering preexisting data on the petrologic composition of Thrace Basin, silicilastic sediments in Greece and Bulgaria (Caracciolo, 2009), a Rhodopian provenance could be considered mostly for areas of the Thrace Basin outside our study area, particularly in the northern-central portions of the basin. In summary, the most important source area for the sediment of Thrace Basin in the study area was represented by the exhumed subduction-accretion complex along the southern margin of the basin (Biga Peninsula and western-central Marmara Sea region). Most measured paleocurrent indicators show an eastward paleoflow but this is most likely the result of gravity flow deflection. This is possible considered a strong control due to the east-west-trending synsedimentary transcurrent faults which cuts the Thrace Basin, generating a series of depocenters and uplifts which deeply influenced sediment dispersal and the areal distribution of paleoenvironments. The Thrace Basin was long interpreted as a forearc basin between a magmatic arc to the north and a subduction-accretion complex to the south, developed in a context of northward subduction. This interpretation was challenged by more recent data emphasizing the lack of a coeval magmatic arc in the north and the interpretation of the chaotic deposit which outcrop south of Ganos Fault as olistoliths and large submarine slumps, derived from the erosion and sedimentary reworking of an older mélange unit located to the south (not as tectonic mélange formed in an accretionary prism). The present study corroborates instead the hypothesis of a post-collisional origin of the Thrace Basin, due to a phase of orogenic collapse, which generated a series of mid-Eocene depocenters all along the İzmir-Ankara suture (following closure of the Vardar-İzmir-Ankara ocean and the ensuing collision); then the slab roll-back of the remnant Pindos ocean played an important role in enhancing subsidence and creating additional accommodation space for sediment deposition.

Geochemistry, petrogenesis and tectonic setting of ophiolites and mafic-ultramafic complexes in the Northeastern Aegean Region

In this study two ophiolites and a mafic-ultramafic complexes of the northeastern Aegean Sea, Greece, have been investigated to re-evaluate their petrogenetic evolution and tectonic setting. These complexes are: the mafic-ultramafic complex of Lesvos Island and the ophiolites of Samothraki Island and the Evros area. In order to examine these complexes in detail whole-rock major- and trace-elements as well as Sr and Nd isotopes, and minerals were analysed and U-Pb SHRIMP ages on zircons were determined. The mafic-ultramafic complex of Lesvos Island consists of mantle peridotite thrusted over a tectonic mélange containing metasediments, metabasalts and a few metagabbros. This succession had previously been interpreted as an ophiolite of Late Jurassic age. The new field and geochemical data allow a reinterpretation of this complex as representing an incipient continental rift setting that led to the subsequent formation of the Meliata-Maliac-Vardar branches of Neotethys in Upper Permian times (253 ± 6 Ma) and the term “Lesvos ophiolite” should be abandoned. With proceeding subduction and closure of the Maliac Ocean in Late Jurassic times (155 Ma) the Lesvos mafic-ultramafic complex was obducted. Zircon ages of 777, 539 and 338 Ma from a gabbro strongly suggest inheritance from the intruded basement and correspond to ages of distinct terranes recently recognized in the Hellenides (e.g. Florina terrane). Geochemical similar complexes which contain rift associations with Permo-Triassic ages can be found elsewhere in Greece and Turkey, namely the Teke Dere Thrust Sheet below the Lycian Nappes (SW Turkey), the Pindos subophiolitic mélange (W Greece), the Volcanosedimentary Complex on Central Evia Island (Greece) and the Karakaya Complex (NW Turkey). This infers that the rift-related rocks from Lesvos belong to an important Permo-Triassic rifting episode in the eastern Mediterranean. The ‘in-situ’ ophiolite of Samothraki Island comprises gabbros, sparse dykes and basalt flows as well as pillows cut by late dolerite dykes and had conventionally been interpreted as having formed in an ensialic back-arc basin. The results of this study revealed that none of the basalts and dolerites resemble mid-ocean ridge or back-arc basin basalts thus suggesting that the Samothraki ophiolite cannot represent mature back-arc basin crust. The age of the complex is regarded to be 160 ± 5 Ma (i.e. Oxfordian; early Upper Jurassic), which precludes any correlation with the Lesvos mafic-ultramafic complex further south (253 ± 6 Ma; Upper Permian). Restoration of the block configuration in NE Greece, before extensional collapse of the Hellenic hinterland and exhumation of the Rhodope Metamorphic Core Complex (mid-Eocene to mid-Miocene), results in a continuous ophiolite belt from Guevgueli in the NW to Samothraki in the SE, thus assigning the latter to the Innermost Hellenic Ophiolite Belt. In view of the data of this study, the Samothraki ophiolite represents a rift propagation of the Sithonia ophiolite spreading ridge into the Chortiatis calc-alkaline arc. The ophiolite of the Evros area consists of a plutonic sequence comprising cumulate and non-cumulate gabbros with plagiogranite veins, and an extrusive sequence of basalt dykes, massive and pillow lavas as well as pyroclastic rocks. Furthermore, in the Rhodope Massif tectonic lenses of harzburgites and dunites can be found. All rocks are spatially separated. The analytical results of this study revealed an intra-oceanic island arc setting for the Evros ophiolitic rocks. During late Middle Jurassic times (169 ± 2 Ma) an intra-oceanic arc has developed above a northwards directed intra-oceanic subduction zone of the Vardar Ocean in front of the Rhodope Massif. The boninitic, island arc tholeiitic and calc-alkaline rocks reflect the evolution of the Evros island arc. The obduction of the ophiolitic rocks onto the Rhodope basement margin took place during closure of the Vardar ocean basins. The harzburgites and dunites of the Rhodope Massif are strongly depleted and resemble harzburgites from recent oceanic island arcs. After melt extraction they underwent enrichment processes by percolating melts and fluids from the subducted slab. The relationship of the peridotites and the Evros ophiolite is still ambiguous, but the stratigraphic positions of the peridotites and the ophiolitic rocks indicate separated origin. The harzburgites and dunites most probably represent remnants of the mantle wedge of the island arc of the Rhodope terrane formed above subducted slab of the Nestos Ocean in late Middle Jurassic times. During collision of the Thracia terrane with the Rhodope terrane thrusting of the Rhodope terrane onto the Thracia terrane took place, whereas the harzburgites and dunites were pushed between the two terranes now cropping out on top of the Thracia terrane of the Rhodope Massif.

UHP metamorphic rocks of the Eastern Rhodope Massif, NE Greece: new constraints from petrology, geochemistry and zircon ages

In this PhD thesis, a multidisciplinary study has been carried out on metagranitoids and paragneisses from the Eastern Rhodope Massif, northern Greece, to decipher the pre-Alpine magmatic and geodynamic evolution of the Rhodope Massif and to correlate the eastern part with the western/central parts of the orogen. The Rhodope Massif, which occupies the major part of NE Greece and S Bulgaria, represents the easternmost part of the Internal Hellenides. It is regarded as a nappe stack of high-grade units, which is classically subdivided into an upper unit and a lower unit, separated by a SSE-NNW trending thrust plane, the Nestos thrust. Recent research in the central Greek Rhodope Massif revealed that the two units correspond to two distinct terranes of different age, the Permo-Carboniferous Thracia Terrane, which was overthrusted by the Late Jurassic/Early Cretaceous Rhodope Terrane. These terranes are separated by the Nestos suture, a composite zone comprising metapelites, metabasites, metagranitoids and marbles, which record high-pressure and even ultrahigh-pressure metamorphism in places. Similar characteristic rock associations were investigated during this study along several well-constrained cross sections in vincity to the Ada, Sidiro and Kimi villages in the Greek Eastern Rhodope Massif. Field evidence revealed that the contact zone of the two terranes in the Eastern Rhodope Massif is characterized by a mélange of metapelites, migmatitic amphibolites/eclogites, strongly sheared orthogneisses and marbles. The systematical occurrence of this characteristic rock association between the terranes implies that the Nestos suture is a continuous belt throughout the Greek Rhodope Massif. In this study, a new UHP locality could be established and for the first time in the Greek Rhodope, metamorphic microdiamonds were identified in situ in their host zircons using Laser-Raman spectroscopy. The presence of the diamonds as well as element distribution patterns of the zircons, obtained by TOF-SIMS, indicate metamorphic conditions of T > 1000 °C and P > 4 GPa. The high-pressure and ultrahigh-pressure rocks of the mélange zone are considered to have formed during the subduction of the Nestos Ocean in Jurassic times at ~150 Ma. Melting of metapelitic rocks at UHP conditions facilitated the exhumation to lower crustal levels. To identify major crust forming events, basement granitoids were dated by LA-SF-ICPMS and SHRIMP-II U-Pb analyses of zircons. The geochronological results revealed that the Eastern Rhodope Massif consists of two crustal units, a structurally lower Permo-Carboniferous unit corresponding to the Thracia Terrane and a structurally upper Late Jurassic/Early Cretaceous unit corresponding to the Rhodope Terrane, like it was documented for the Central Rhodope Massif. Inherited zircons in the orthogneisses from the Thracia Terrane of the Eastern Rhodope Massif indicate the presence of a pre-existing Neoproterozoic and Ordovician-Silurian basement in this region. Triassic magmatism is witnessed by the zircons of few orthogneisses from the easternmost Rhodope Massif and is interpreted to be related to rifting processes. Whole-rock major and trace element analyses indicate that the metagranitoids from both terranes originated in a subduction-related magmatic-arc environment. The Sr-Nd isotope data for both terranes of the Eastern and Central Rhodope Massif suggest a mixed crust-mantle source with variable contributions of older crustal material as already indicated by the presence of inherited zircons. Geochemical and isotopic similarity of the basement of the Thracia Terrane and the Pelagonian Zone implies that the Thracia Terrane is a fragment of a formerly unique Permo-Carboniferous basement, separated by rifting and opening of the Meliata-Maliac ocean system in Triassic times. A branch of the Meliata-Maliac ocean system, the Nestos Ocean, subducted northwards in Late Jurassic times leading to the formation of the Late Jurassic/Early Cretaceous Rhodope magmatic arc on remnants of the Thracia Terrane as suggested by inherited Permo-Carboniferous zircons. The ~150 Ma zircon ages of the orthogneisses from the Rhodope Terrane indicate that subduction-related magmatism and HP/UHP metamorphism occurred during the same subduction phase. Subduction ceased due to the closure of the Nestos Ocean in the Late Jurassic/Early Cretaceous. The post-Jurassic evolution of the Rhodope Massif is characterized by the exhumation of the Rhodope core complex in the course of extensional tectonics associated with late granite intrusions in Eocene to Miocene times.

Low-temperature thermochronological evolution of the Menderes and Alanya massifs (Turkey)

The application of two low-temperature thermochronometers [fission-track analysis and (U-Th)/He analyses, both on apatite] to various tectonostratigraphic units of the Menderes and Alanya Massifs of Turkey has provided significant new constraints to the understanding of their structural evolution. The Menderes Massif of western Anatolia is one of the largest metamorphic core complexes on Earth. The integration of the geochronometric dataset presented in this dissertation with preexisting ones from the literature delineates three groups of samples within the Menderes Massif. In the northern and southern region the massif experienced a Late Oligocene-Early Miocene tectonic denudation and surface uplift; whereas data from the central region are younger, with most ages ranging between the Middle-Late Miocene. The results of this study are consistent with the interpretation for a symmetric exhumation of the Menderes Massif. The Alanya Massif of SW Anatolia presents a typical nappe pile consisting of thrust sheets with contrasting metamorphic histories. Petrological and geochronological data clearly indicate that the tectonometamorphic evolution Alanya started from Late Cretaceous with the northward subduction of an ‘Alanya ocean’ under the Tauride plate. As an effect of the closure of the İzmir–Ankara–Erzincan ocean, northward backthrusting during the Paleocene-Early Eocene created the present stacking order. Apatite fission-track ages from this study range from 31.8 to 26.8 Ma (Late Rupelian-Early Chattian) and point to a previously unrecognized mid-Oligocene cooling/exhumation episode. (U-Th)/He analysis on zircon crystals obtained from the island of Cyprus evidentiate that the Late Cretaceous trondhjemites of the Troodos Massif not recorded a significant cooling event. Instead results for the Late Triassic turbiditic sandstones of the Vlambouros Formation show that the Mamonia mélange was never buried enough to reach the closure temperature of the ZHe radiometric system (ca. 200°C), thus retaining the Paleozoic signature of a previous sedimentary cycle.

Creativite langagiere et contact de langues: Le cas du langage sms et chat chez les jeunes camerounais

Résumé L’apparition de l’internet au Cameroun offre une réelle occasion d’échange, surtout pour les jeunes. Les innovations de la toile sont à considérer à plusieurs niveaux, les linguistes sous tous les cieux ont actuellement à débattre du langage SMS et CHAT, qui est, d’après (Dejond ,2002) « un mélange d’anglicisme, d’abréviation, de sigles et de rebus d’écriture phonétique. On écrit comme on parle. » Cette forme d’écriture facile à transcrire est éloignée des normes orthographiques et grammaticales du français standard. En effet, le langage SMS et CHAT des jeunes camerounais n’obéit qu’à la norme dictée par l’imagination de ses adeptes. Il se caractérise par des phénomènes comme la troncation, l’élision vocalique et consonantique ou l’agglutination à l’intérieur des mots. L’un des phénomènes les plus marquants est l’introduction des chiffres allant de 1 à 9 dans la graphie de certains mots. Ces écritures simplifiées nécessitent souvent l’intuition ou la compétence linguistique des lecteurs pour décrypter le message, le but étant l’interprétation du contenu. De plus, le type de message est strictement communicatif ou expressif et non normatif. Ainsi, l’essentiel est de faire passer un message. Les règles, les principes ou les contraintes qui gouvernent la transcription orthographique d’un mot français sont relégués au second plan. L’écriture texto employé par les jeunes camerounais cherche parcimonieusement à en dire le plus avec un minimum de caractère. Pour cela, on chatte entre amis, parents ou avec des connaissances éparpillée de part le monde qui naissent de ces rencontres virtuelles.

Manejo de suelo mediante coberturas vegetales establecidas

El objetivo de esta investigación fue determinar los efectos de las coberturas vegetales en el microclima de la planta de vid. Se compararon cinco coberturas de diferente ciclo vegetativo con respecto al manejo de suelo sin labranza mediante aplicación de herbicidas. El estudio se desarrolló en un viñedo cv. Malbec conducido en espaldera alta, situado en Agrelo, Luján de Cuyo, Mendoza, Argentina. Se determinaron parámetros microclimáticos, temperatura, humedad relativa y radiación a nivel de racimos, temperatura del suelo, cantidad y calidad de la radiación reflejada por la cobertura. También se midió la expresión vegetativa y de uvas y el potencial enológico. Se verificó una significativa disminución de la radiación fotosintéticamente activa (RFA) reflejada por las coberturas con una menor relación “Rojo/Rojo lejano" comparada con el suelo descubierto. Sin embargo, el efecto no se percibió dentro de la canopia debido a que las coberturas permanentes de trébol rojo (Trifolium pratensis) y agropiro alargado (Agropyron elongatum) restringieron el vigor de las cepas, disminuyendo el crecimiento de brotes y el tamaño de hojas, lo cual se tradujo en una mayor recepción directa de la RFA a nivel de racimos. No hubo una significativa variación en cuanto a temperatura máxima, mínima y amplitud térmica a nivel de racimos. No obstante ello, los tratamientos con mayor cobertura de suelo tendieron a reducir levemente la temperatura mínima a nivel de racimos. La humedad relativa en la canopia no fue significativamente afectada. El trébol rojo, el agropiro alargado, la mezcla centeno-cebadilla (Secale cereale-Bromus catharticus) y el sorgo del Sudán (Sorghum sudanensis) redujeron notablemente la amplitud térmica del suelo. El efecto fue determinado principalmente por la disminución de la temperatura máxima. Las coberturas vegetales con alguna dificultad para desarrollarse durante su ciclo vegetativo tuvieron un comportamiento intermedio o uno muy similar al de un suelo descubierto. La introducción de una cobertura permanente con buena invasión del sitio interfilar permitió modificar indirectamente las características microclimáticas de la canopia, a través del control del crecimiento vegetativo y de los rendimientos de la planta de vid, modificando el equilibrio vigor / producción del viñedo, y por lo tanto la composición de las uvas y del vino elaborado.

Preliminary data on horse mackerel (Trachurus spp) landings from Mauritanian waters

European fishery off Mauritania (one of the most productive and most intensively exploited regions in the world) targeted to small pelagic fish accounts for 30% of the total catches in the area. The Instituto Español de Oceanografía (IEO), through its Centro Oceanográfico de Canarias, follows up the activity of these vessels that land at Spanish port (Las Palmas de Gran Canaria, Spain), under the European Project Data Collection (Regulation (EC) 1543/2000). One of the target groups in this fishery is Trachurus spp, commercially named “JAX”. During 2008 and 2009, several samples of this group from these landings were analysed, and Caranx rhonchus was the second species of importance. The mixture of these species in the landings of this UE fleet should be determined to improve the data provided to the international Working Groups responsible for assessment of those resources.

Interactions métaboliques entre le bisphénol A et le naproxène dans un modèle de foie de rat isolé et perfusé

L'exposition aux mélanges de contaminants (environnementaux, alimentaires ou thérapeutiques) soulève de nombreuses interrogations et inquiétudes vis-à-vis des probabilités d'interactions toxicocinétiques et toxicodynamiques. Une telle coexposition peut influencer le mode d’action des composants du cocktail et donc de leur toxicité, suite à un accroissement de leurs concentrations internes. Le bisphénol A (4 dihydroxy-2,2-diphenylpropane) est un contaminant chimique répandu de manière ubiquitaire dans notre environnement, largement utilisé dans la fabrication des plastiques avec l’un des plus grands volumes de production à l’échelle mondiale. Il est un perturbateur endocrinien par excellence de type œstrogèno-mimétique. Cette molécule est biotransformée en métabolites non toxiques par un processus de glucuronidation. L'exposition concomitante à plusieurs xénobiotiques peut induire à la baisse le taux de glucuronidation du polluant chimique d'intérêt, entre autres la co-exposition avec des médicaments. Puisque la consommation de produits thérapeutiques est un phénomène grandissant dans la population, la possibilité d’une exposition simultanée est d’autant plus grande et forte. Sachant que l'inhibition métabolique est le mécanisme d'interaction le plus plausible pouvant aboutir à une hausse des niveaux internes ainsi qu’à une modulation de la toxicité prévue, la présente étude visait d'abord à confirmer et caractériser ce type d'interactions métaboliques entre le bisphénol A et le naproxène, qui est un anti-inflammatoire non stéroïdiennes (AINS), sur l'ensemble d'un organe intact en utilisant le système de foie de rat isolé et perfusé (IPRL). Elle visait ensuite à déterminer la cinétique enzymatique de chacune de ces deux substances, seule puis en mélange binaire. Dans un second temps, nous avons évalué aussi l’influence de la présence d'albumine sur la cinétique métabolique et le comportement de ces deux substances étudiées en suivant le même modèle de perfusion in vivo au niveau du foie de rat. Les constantes métaboliques ont été déterminées par régression non linéaire. Les métabolismes du BPA et du NAP seuls ont montré une cinétique saturable avec une vélocité maximale (Vmax) de 8.9 nmol/min/ mg prot de foie et une constante d'affinité de l'enzyme pour le substrat (Km) de 51.6 μM pour le BPA et de 3 nmol/min/mg prot de foie et 149.2 μM pour le NAP. L'analyse des expositions combinées suggère une inhibition compétitive partielle du métabolisme du BPA par le NAP avec une valeur de Ki estimée à 0.3542 μM. Les résultats obtenus montrent que l’analyse de risque pour les polluants environnementaux doit donc prendre en considération la consommation des produits pharmaceutiques comme facteur pouvant accroitre le niveau interne lors d’une exposition donnée. Ces données in vivo sur les interactions métaboliques pourraient être intégrées dans un modèle pharmacocinétique à base physiologique (PBPK) pour prédire les conséquences toxicococinétique (TK) de l'exposition d'un individu à ces mélanges chimiques.

Le processus de construction de l'identité collective du mouvement queer montréalais : perspectives militantes francophones

Ce mémoire vise à analyser le processus de construction de l'identité collective du mouvement queer à Montréal dans un contexte francophone. Bien que plusieurs travaux portent en partie sur les groupes militants queers québécois, aucune recherche ne s'est employée à comprendre comment les militant.es queers à Montréal se constituent comme un collectif qui développe une identité. Pour analyser le processus de construction de l'identité collective du mouvement queer montréalais, je m'appuie sur la théorie de Melucci (1985; 1996), qui définit l'identité collective d'un mouvement selon plusieurs axes : les champs d'action, les moyens employés et les fins visées, ainsi que le mode d'organisation. Afin de répondre à cette question de recherche, j'ai effectué une recherche documentaire ainsi que sept entrevues avec des militant.es queers montréalais.es francophones. L'analyse des données a été faite grâce à divers travaux qui portent sur les champs d'action, les valeurs, les fins et moyens, le mode d'organisation de mouvements contemporains anti-autoritaires et anti-oppressifs, ainsi qu'en fonction de trois dimensions élaborées par Melucci (1985) : le conflit, la solidarité et les limites du système. Je conclus que l'identité collective comme processus s'articule autour de plusieurs enjeux : premièrement, la diversité des champs d'action, les valeurs anti-oppressives, les relations d'affinités, le mode de vie alternatif et le mode d'organisation anti-oppressif des militant.es queers permettent au mouvement de créer une solidarité interne, d'affirmer une position anti-autoritaire qui brise les limites du système dominant et de se différencier du mouvement LGBT mainstream. Par ailleurs, les actions militantes concrètes qui réalisent le changement dans l'ici et maintenant participent à créer une solidarité et une reconnaissance entre militant.es, ainsi qu'à mettre en lumière un conflit avec le système dominant oppressif. Enfin, les perspectives francophones sur le mouvement queer ne semblent pas donner au bilinguisme du mouvement un rôle fondamental dans la construction de son identité collective. Cependant, l'intérêt marqué des militant.es francophones comparativement aux militant.es anglophones pour la politique institutionnelle fait émerger de nouvelles interrogations sur l'impact que pourrait avoir le mélange des cultures francophone et anglophone à Montréal sur la culture politique et l'identité du mouvement.

Interactions métaboliques entre le bisphénol A et le naproxène dans un modèle de foie de rat isolé et perfusé

L'exposition aux mélanges de contaminants (environnementaux, alimentaires ou thérapeutiques) soulève de nombreuses interrogations et inquiétudes vis-à-vis des probabilités d'interactions toxicocinétiques et toxicodynamiques. Une telle coexposition peut influencer le mode d’action des composants du cocktail et donc de leur toxicité, suite à un accroissement de leurs concentrations internes. Le bisphénol A (4 dihydroxy-2,2-diphenylpropane) est un contaminant chimique répandu de manière ubiquitaire dans notre environnement, largement utilisé dans la fabrication des plastiques avec l’un des plus grands volumes de production à l’échelle mondiale. Il est un perturbateur endocrinien par excellence de type œstrogèno-mimétique. Cette molécule est biotransformée en métabolites non toxiques par un processus de glucuronidation. L'exposition concomitante à plusieurs xénobiotiques peut induire à la baisse le taux de glucuronidation du polluant chimique d'intérêt, entre autres la co-exposition avec des médicaments. Puisque la consommation de produits thérapeutiques est un phénomène grandissant dans la population, la possibilité d’une exposition simultanée est d’autant plus grande et forte. Sachant que l'inhibition métabolique est le mécanisme d'interaction le plus plausible pouvant aboutir à une hausse des niveaux internes ainsi qu’à une modulation de la toxicité prévue, la présente étude visait d'abord à confirmer et caractériser ce type d'interactions métaboliques entre le bisphénol A et le naproxène, qui est un anti-inflammatoire non stéroïdiennes (AINS), sur l'ensemble d'un organe intact en utilisant le système de foie de rat isolé et perfusé (IPRL). Elle visait ensuite à déterminer la cinétique enzymatique de chacune de ces deux substances, seule puis en mélange binaire. Dans un second temps, nous avons évalué aussi l’influence de la présence d'albumine sur la cinétique métabolique et le comportement de ces deux substances étudiées en suivant le même modèle de perfusion in vivo au niveau du foie de rat. Les constantes métaboliques ont été déterminées par régression non linéaire. Les métabolismes du BPA et du NAP seuls ont montré une cinétique saturable avec une vélocité maximale (Vmax) de 8.9 nmol/min/ mg prot de foie et une constante d'affinité de l'enzyme pour le substrat (Km) de 51.6 μM pour le BPA et de 3 nmol/min/mg prot de foie et 149.2 μM pour le NAP. L'analyse des expositions combinées suggère une inhibition compétitive partielle du métabolisme du BPA par le NAP avec une valeur de Ki estimée à 0.3542 μM. Les résultats obtenus montrent que l’analyse de risque pour les polluants environnementaux doit donc prendre en considération la consommation des produits pharmaceutiques comme facteur pouvant accroitre le niveau interne lors d’une exposition donnée. Ces données in vivo sur les interactions métaboliques pourraient être intégrées dans un modèle pharmacocinétique à base physiologique (PBPK) pour prédire les conséquences toxicococinétique (TK) de l'exposition d'un individu à ces mélanges chimiques.