1000 resultados para Éoliennes, Îles


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The study of new abundant coral crops and a systematic revision of the historie collections allow us to extend significantly the data about the Upper Oligocene and Miocene Scleractinia of the French atlantic basins. The SW and W-NW France faunas have been considered, and complete lists of the different defined taxa are presented. The general lines of the evolution of this group are specified, and linked to the paleoclimatic and paleobiogeographic changes.

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The Aquitaine Basin (southwestem France) is known since long ago for its richness in marine miocene deposits ofvarious facies. A few stratotypes concerning this period have bccn described in the investigated area. The stratigraphical framework has becn recently revised and the study of new exposures completes our knowledge on these levels. In the present work, the authors produce a biostratigraphical distribution of about 160 species (Iarger and smaller foraminifera), found in the surface exposures of Aquitaine, from the topmost Oligocene (Chattian) through to Middle Miocene (including Serravallian). As a rule, the common species without significant ranges have not bcen mentioned. The microfaunas of several exposures have been thoroughly revised, which has allowcd to precise the distribution of many species and induced a few modifications of the results previously produced. Synonymy problems and new taxonomical revisions have been taken into account. Of course, this work will be probably submitted to some changes according to new research on the already known exposures or other more recently discovered.

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Proceedings of the I" R.C.A.N.S. Congress, Lisboa, October 1992

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The Quaternary fluvial formations of the Doukkala plain are, until now, slightly studied. Our study has allowed to precise that the fluvial terraces of the oued "the Ourn Rbia oued", are clearly distinguished from the secondary oueds terraces by the dynamic deposit of the alluvial materials. Moreover, the mammal fossils recolted from some of these terraces allow to review the ages attributed by Gigout (1951).

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New data led us to revise Miocene Perissodactyla from Lisbon. Equids (Anchitherium) have been decribed by Alberdi & González (1999); we fully agree with their conclusions. On the other hand, the only Chalicotheriid cannot be clearly reported to any genus. It therefore will be left in open nomenclature Schizorheriinae ind.). The Rhinocerotids have been described in detail (1983). We could recognize now that: Protaceratherium sagicum is a synonym of P. minutum; Plesiaceratherium platyodon and Plesiaceratherium lumiarense should be ascribed to the genus Plesiaceratherium and not to Aceratherium; there are no reasons for name changes as far as the forms previously referred as Diaceratherium aurelianensis, Prosantorhinus germanicus and Hispanotherium matritensis are concerned; as the genera Dicerorhinus and Lartetotherium are distinct, Dicerorhinus (Lartetotherium) sansaniensis has to be named Lartetotherium sansaniensis; as Gaindatherium (Ïberotherium) rexmanueli cannot be reported to Gaindatherium, we therefore upgrade the subgenus Iberotherium to the genus'rank - hence the names of the concerned taxa become Iberotherium rexmanueli rexmanueli and I. rexmanueli zbyszewski; Chilotherium ibericus is but a dental variation of I. rexmanueli zbyszewski. The stratigraphic distribution and age of the Miocene Perissodactyla so far known in the Lower Tagus basin / Lisbon region are presented.

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Les années quatre-vingt signalent un point de bascule dans et une mutation majeure dans les caractéristiques narratives de la littérature française. D’une certaine façon, elles entament la contemporanéité littéraire telle que nous la connaissons du point de vue critique. Nous insisterons sur le rôle des revues et des éditoriaux dans ce processus. Ils manifestent quelques hésitations de la critique par rapport à la littérature naissante.

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Congresso Internacional de História da Medicina (ISHM); 39º - p.217-218

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The geological sections studied at the São Gião sector (Cantanhede region) have allowed the establishment of a clear succession of ammonite associations during the Middle and Upper Toarcian (“Margas calcárias de São Gião” and “Calcários margosos de Póvoa da Lomba” Formations). The fossil collections were gathered over the last 40 years and, in spite of the apparent facies monotony, come from a thick and fossiliferous marly-limestone unit. The ammonite succession allows the establishment and/or verification of a certain number of biostratigraphical elements, of which are worthy of mention: – the tethyan character of the fauna from the Gradata to the Meneghinii Zones; this differentiation starts with the occurrence of Collina, Crassiceras and Furloceras of the Gradata Zone; – the succession of Osperleioceras, with the connection between the “caussenardes”(O. reynesi, O. authelini) forms and those from Algeria (O. nadorense, O. matteii), which is placed at the beginning of the Aalensis Zone; – the succession of Hammatoceratinae: H. roubanense (Gradata Z.), H. bonarellii (Bonarellii Z.), H. speciosum (Speciosum Sub-zone), followed by Crestaites meneghinii (Reynesi Sub-zone and Meneghinii Z.); Pseudaptetoceras appear next (Aalensis Zone). The dynamic evolution of the sector is characterized by the persistence of marly sedimentation during the Meneghinii Zone, in probable relation to the paleostructural play of the Arunca-Montemor meridian axis.

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Comunicação apresentada no Congresso Internacional do IIAS, realizado em Lausanne, Suiça, de 4 a 8 de Julho de 2011.

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La présente thèse doctorale propose l’étude de l’activité théâtrale développée dans les théâtres permanents construits en Amérique Portugaise au long du XVIIIe et dans la première décennie du XIXe siècle, en mettant l’accent sur les idéalisateurs des Casas da Ópera et les moyens de financement utilisés dans l’édification et l’entretien de celles-ci, le répertoire mis en scène, les artistes composant les compagnies théâtrales, les spectateurs et les possibilités de sociabilité établies dans l’espace théâtrale et les modèles architectoniques qui ont inspiré la construction des bâtiments théâtraux au cours de la période mentionnée. Ces cinq axes principaux soulignent l’approche interdisciplinaire qui a orienté nos études, dans un souci de contribution à une plus complète compréhension de notre sujet de recherche. Mots clés : Théâtres, Amérique Portugaise, Comédiens Mulâtres, Théâtre Éphémère, Comédies Portugaises, Architecture théâtrale luso-américaine, Casa da Ópera de Vila Rica/Ouro Preto.

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pp. 15-28

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Dans cet article, nous mettrons en évidence le rapport étroit tissé par Xenakis entre les œuvres La légende d’Eer et Jonchaies notamment au niveau de la structure formelle et des sonorités. // In this paper, we will show some evident examples about the close rapports between La légende d’Eer and Jonchaies by Xenakis, especially in terms of formal structure and sonorities.

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Tese de doutoramento em Línguas e Literaturas Românicas, Literatura Românica Comparada