497 resultados para Marche récréative


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During Oceanic Anoxic Event 1a (OAE 1a, 120 Ma; Li et al., 2008), organic carbon-rich layers were deposited in marine environments under anoxic conditions on a global scale. In this study, palaeoenvironmental conditions leading to this event are characterised by studying the Upper Barremian to the Lower Aptian succession of the Gorgo a Cerbara section (central Italy). For this, an integrated multi-proxy approach (δ13Ccarb; δ13Corg; δ18O; phosphorus; Total Organic Carbon, TOC; bulk-rock mineralogy, as well as redox-sensitive trace elements — RSTEs) has been applied. During the LateBarremian, thin organic-rich layers occur episodically, and associated Corg:Ptot ratios indicate the presence of intermittent dysoxic to anoxic conditions. Coarse correlations are observed between TOC, P and biogenic silica contents, indicating links between P availability, productivity, and TOC preservation. However, the corresponding δ13Ccarb and δ18O records remain quite stable, indicating that these brief periods of enhanced TOC preservation did not have sufficient impact on the marine carbon reservoir to deviate δ13C records. Around the Barremian–Aptian boundary, TOC-enriched layers become more frequent. These layers correlate with negative excursions in the δ13Ccarb and δ13Corg records, possibly due to a warming period as indicated by the δ18O record. During the earliest Aptian, this warming trend is reverted into a cooling trend, which is then followed by an important warming step near the onset of Oceanic Anoxic Event 1a (OAE 1a). During this time period, organic-rich intervals occur, which are characterised by the progressive increase in RSTE. The warming step prior the onset of OAE 1a is associated with the well-known negative spike in δ13Ccarb and δ13Corg records, an important peak in P accumulation, RSTE enrichments and Corg:Ptot ratios indicating the prevalence of anoxic conditions. The Selli Level itself may document a cooling phase. RSTE enrichments and Corg:Ptot ratios confirm the importance of anoxic conditions during OAE 1a at this site. The Gorgo a Cerbara section is interpreted to reflect the progressive impact of palaeoenvironmental change related to the formation of the Ontong-Java plate-basalt plateau, which started already around the Barremian–Aptian boundary and culminated into OAE 1a.

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Cette dissertation propose l analyse des Mémoires de Olivier de La Marche, homme de la cour qui a vécu comme serviteur des maisons de Bourgogne et d Autriche de l année 1439 jusqu à 1502. Nous avons compris sa littérature comme particulière pour l époque, car elle est née motivé par les questions personnelles de l auteur. C est pourquoi qu elle s est éloignée des genres littéraires liés à la fonction de servir aux propos du prince, particulièrement les chroniques. Nous avons cru que ces intentions particulières ont eu l origine dans la tradition de la mémoire médiévale, qui a répandu de l oral pour l écrit pendant la fin de la Moyen Âge. Cette écriture de la mémoire, réglementée à l expérience de qui écrivait, a promu la naissance de l individu quand il a cherché assumer les lieux du personnage et du témoin des événements dans l espace du texte . Telle affirmation nous avons conduit jusqu à la fonction des discours qui ont créé des espaces dans l oeuvre. Motivé par la vision spécialisée comme maître d hôtel, tels discours ont produit un espace de la cour idéal, capable de justifier la personnalité de l auteur et de lui consacrer comme le maître de la pratique de la courtoisie

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Progetto e costruzione di una casa tradizionale con telaio di legno nelle Marche.

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Analisi tecnico ambientale delle biomasse a fini energetici: il caso della regione marche

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Signatur des Originals: S 36/F03355

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par Joachim Raff