7 resultados para Théorie du noyau central
Resumo:
THÈSE pour l’obtention du grade de DOCTEUR
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A land tortoise from a new locality at Naia, Tondela, is described. It is to be reported either to an advanced form of the genus Hadrianus or to an archaic representative of Cheirogaster; it may be included in the comprehensive genus Geochelone s.l., excluding however Ergilemys and its descendants. There is a strong possibility in favour of Cheirogaster. Testudo must also be excluded. It is not possible to classify this specimen at species'level. Our specimen does agree best with Upper Eocene Testudinidae and with some Lower Oligocene ones. Its age is certainly not Upper Oligocene or later, nor Lower and Middle Eocene. This datation is not opposed to the age of the fossiliferous clays of Naia as supposed by correlation with another locality - Côja, about 30 km to the South - which yielded an assemblage of mammals whose Ludian (Upper Bartonian s.l.) age seems well established. Naia and Côja's fossil-bearing clays must be nearly synchronous; their origin is well in place among the phenomena related to the surrection of iberian Central Chain during paroxysmal phase of pyrenean orogenesis.
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The facies distribution along the Jurassic stages in an already well established stratigraphic frame is defined for the three portuguese basins: North of Tagus, Santiago de Cacém and Algarve. The deposits are organized in two sedimentary cycles. The first one from the Liassic to Calovian shows, in the Tagus Basin, a transgression from NW which did not surpass the Meseta present limits. The iniatilly brackish deposits only changed to marine by the end of Lotharingian. The sedimentation, mainly marly during the Liassic became more calcareous since the Aalenian. During the Dogger the basin differentiated into platform deposits towards East and South and open sea zone towards West. This zone underwent a progressive reduction and, during the Callovian, two small basins were individualized: Cabo Mondego basin in the North and Serra de El-Rei-Montejunto in the South. It is from the latter that the second sedimentary cycle (Middle Oxfordian-Portlandian) developed with open sea deposits along the Sintra–Torres Vedras axis surrounded by platform and litoral brackish formations. During the first sedimentary cycle only litoral platform deposits are known in Santiago de Cacém and Algarve basins. During the second sedimentary cycle temporary sea open deposits are known in Santiago de Cacém and Central Algarve.
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Some outcrops in the western part of Leiria's diapir yielded continental fossils in five points near Amor village (mammals, other vertebrata, and gastropoda). This is most significant as it is the first locality where miocene age could undoubtedly been ascribed to formations northwards the Iberian Central Chain and Nazare's accident. Mammalian fauna comprises 18 taxa. A new cricetid species, Fahlbuschia freudenthali n. sp. is described. This fauna allows to date fossil-bearing units from Upper Orleanian, MN5 mammal zone, that may be correlated to Upper Langhian marine stage. As the fauna is quite varied, it is possible to recognize the main characters of environment and of climatic conditions. It may probably be assumed that at the time the climate was of mediterranean type, generally warmer than today.
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Improved bromoform concentration as developped at CEPUNL allowed better recovery of small mammals'teeth. At Universidade Católica and Avenida do Uruguay 19 taxa (and a further one with doubt) were recognized. Some are new for the level and for Tagus basin: Lagopsis cadeoti and Melissiodon dominans (1st reference for the genus); Glirudinus modestus (formerly under another name); Armantomys (1st reference for this level); Peridyromys murinus (referred before under another name); Microdyromys legidensis (1st ref. of gen. and sp. for this level); and Heteroxerus rubricati, formerly reported to other species of the same genus. Both localities share the same position viz marine levels under and above. This allows us to correlate them with NS or N6 Blow's zones. Both are distinctly younger-than glauconite in underlying beds about 21 MY old (K-Ar). Small mammals point out to MN3a Neogene subunit. Fauna is much alike Lower Burdigalian ones in Spain, France, Germany and Austria. Terrestrial, maybe steppe forms predominate. Land environment was open, with scant plant cover but not devoid of trees. Peridyromys murinus numerical importance and other data suggest a not so warm climate in correspondance to a minimum temperature event. This is corroborated by associated marine fish fauna entirely without warm water stenotherm species, and by paleobotanical/palynological data. Results are in close agreement with Central Northern Spain. The localities studied here are even more interesting as direct correlations between marine and continental stratigraphical scales are possible.
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Ce texte essaie d’interpréter les relations qui s’établissent entre les processus de construction/négociation des identités culturelles et les processus de touristification de l’espace des villes. Les dynamiques culturelles associées au tourisme intègrent des représentations dont la forme convoque, très souvent, les concepts d’authenticité et d’hyperréalité. L’espace des villes devenues des pôles touristiques est lui aussi souvent marqué par ces deux formes culturelles. C’est, comme ce texte essaie de le montrer, le cas de Macao : le Centre Historique (« Patrimoine Mondial »), un réseau de musées (une vingtaine) et un réseau de casinos (une trentaine) constituent les éléments soumis à cette logique de production de l’espace urbain. Les formes culturelles en question – formulées, dans la théorie, comme deux formes indépendantes (et même incompatibles) – coexistent ici dans une réalité culturelle et urbaine complexe et très instable. Son interprétation exige des formes d’abordages nouvelles qui convoquent – en même temps - plusieurs échelles spatiales.
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En 1871, Edward Tylor rejeta fermement les récits de son temps qui niaient l'existence de croyances religieuses chez certains peuples alors considérés comme sauvages. C'était le cas, tout particulièrement, de l'explorateur victorien Samuel Baker, dont l'autorité ethnographique fut mise en cause à travers la citation de quelques voyageurs étrangers, dont deux français, qui avaient également observé les peuples nilotiques. Contrairement à d'autres sources de Primitive Culture, la qualité de ces ethnographies oubliées était, hélas, tout à fait médiocre ; mais elles permirent à Tylor de faire l'une des affirmations les plus décisives de son œuvre, celle de l'universalité de l'animisme. Ce passage capital - concernant des peuples qui deviendront célèbres dans l'histoire de l'anthropologie, à commencer par les Nuer - recèle par ailleurs une dimension additionnelle. Tylor voulait élargir à tout être spirituel les critères d'identification d'une religion, sauf que les ethnographes du Nil Blanc suggéraient que ces rudes populations croyaient bel et bien en un être suprême. Le dossier du monothéisme était comme anticipé par la force de ces données ; mais il ne faut pas y voir une contradiction de la part de Tylor. Au contraire, cette dialectique imprévue entre l'ethnographie et la théorie permet de mieux saisir la portée du concept d'animisme dont il fut le créateur.