983 resultados para Le Roy, Louis


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"Escrita originariament en provençal o en llatí, aquesta producció degué veures transformada devers 1453 en la narració francesa que avuy coneixèm si hem de donar fe a lo qu'es declarat en una de les més antigues edicions en dita llengue, o sía la que donà a llum l'estamper de Lyó, Guillaume Le Roy; edició qui, per altra part, no té data, suposàntsela seta poch abans de 1483." -- p. [vii]

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At head of title: C. de Varigny.

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Thesis (doctoral)--Hoogeschool te Leiden.

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Mode of access: Internet.

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Includes German translation and Latin text of "Quaestio medica ... An praecipua valetudinis tutela exercitatio?" for which Andry was praeses and L. J. Le Thieullier, respondent.

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Durante el siglo XIII se produjo una sucesión de revueltas que supuso la desaparición del Imperio almohade y su sustitución por poderes regionales en al-Andalus, el Magreb y el Magreb al-Aqsà. La historiografía ha presentado el surgimiento y pugna entre estos poderes como un fenómeno social, político e, incluso, cultural y religioso, con el que se ha podido explicar su aniquilación o marginalización. Este trabajo pretende contextualizar los hechos desde una perspectiva medioambiental, de forma que la desintegración del califato almohade, el surgimiento de aquellos poderes y la progresión de los reinos cristianos en la península ibérica puedan entenderse desde una visión global de cambio climático y una posible crisis agrícola.

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Los niños con parálisis cerebral (PC) tienen mayor riesgo de deficiencia de vitamina D (VD). Aunque existen bastantes estudios sobre VD en PC, hay limitada información sobre suplementación con VD en estos pacientes. El objetivo de este artículo es evaluar el efecto de la suplementación con VD en monodosis en las concentraciones plasmáticas de 25-hidroxi-vitamina-D (25OHD) en niños con PC.

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The Mediterranean Sea constitutes a unique environment to study cold-seep ecosystems due to the presence of different geodynamic settings, from an active margin along the Mediterranean Ridge (MR) to a passive margin in the Nile Deep-Sea Fan (NDSF). We attempted to identify the structure of benthic communities associated with the Napoli and Amsterdam mud volcanoes (MVs) located on the MR and to establish the links between faunal distribution and environmental conditions at different spatial scales. Comparison between the 2 MVs revealed that the faunal distribution seemed to be mainly controlled by the characteristics of the microhabitats. On both geological structures, the variability between the different microhabitats was higher than the variability observed between replicates of the same microhabitat, and the distribution of macro-fauna was apparently linked to gradients in physico-chemical conditions. The peripheral sites from Napoli were generally more oxygenated and harboured lower species richness than the active sites. The reduced sediment microhabitat from Amsterdam presented the highest methane concentrations and was mainly colonised by symbiont-bearing vesicomyid bivalves and heterotrophic dorvilleid polychaetes. Overall, a higher taxonomic diversity was observed on Napoli. Sub-stratum type was hypothesised to be the second factor influencing faunal distribution. The results of this study highlight the high heterogeneity of faunal communities associated with seep ecosystems within this region and the need to pursue investigations at various spatial and temporal scales.

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Isolated carbonate platforms occur throughout the geologic record, from Archean to present. Although the respective roles of tectonics, sediment supply and sea-level changes in the stratigraphical architecture of these systems are relatively well constrained, the details of the nature and controls on the variability of sedimentological patterns between and within individual geomorphologic units on platforms have been barely investigated. This study aims at describing and comparing geomorphological and sedimentological features of surficial sediments and fossil reefs from three isolated carbonate platforms located in the SW Indian Ocean (Glorieuses, Juan de Nova and Europa). These carbonate platforms are relatively small and lack continuous reef margins, which have developed only on windward sides. Field observations, petrographic characterization and grain-size analyses are used to illustrate the spatial patterns of sediment accumulation on these platforms. The internal parts of both Glorieuses and Juan de Nova platforms are blanketed by sand dunes with medium to coarse sands with numerous reef pinnacles. Skeletal components including coral, green algae, and benthic foraminifera fragments prevail in these sediments. Europa platform exhibits a similar skeletal assemblage dominated by coral fragments, with the absence of wave-driven sedimentary bodies. Fossil reefs from the Last interglacial (125,000 years BP) occur on the three platforms. At Glorieuses, a succession of drowned terraces detected on seismic lines is interpreted as reflecting the last deglacial sea-level rise initiated 20,000 years ago. These findings highlight the high potential of these platforms to study past sea-level changes and the related reef response, which remain poorly documented in the SW Indian Ocean.

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The study of modern carbonate systems is commonly helps in improving facies interpretation in fossil reefs and in providing analogues of sediment distribution depending on the specific platform configuration (i.e. rimmed shelves and isolated carbonate platforms). This paper deals with a geomorphological and sedimentological study of the Glorieuses Archipelago, an isolated carbonate platform located between the northern tip of Madagascar and Mayotte. The dataset consists of Digital Terrain Model, satellite imagery, and box-sediment samples. Analyses of grain-size and composition of carbonate grains are used to characterize the distribution and heterogeneity of sediment accumulated on the isolated platform. Main results show that the Glorieuses Archipelago is organized in distinctive morphological units, including a reef flat developed along the windward side, an apron, and a semi-enclosed (< 12 m water depth) to open lagoon (> 12 m and up to 15 m water depth). The lack of carbonate mud in sediments deposited on the archipelago can be explained by the direct connection between the lagoon and the open ocean. The main carbonate grains include Halimeda segments, coral fragments, large benthic foraminifers, red algae, and molluscs. According to the shape and the position of intertidal sandwaves, the current arrangement of moderately sorted fine to medium sands appears to be strongly influenced by tidal currents. The in-situ sediment production, accumulation and transport on the platform finally contribute to carbonate sand export to distinct deep marine areas depending on wind regimes and currents.

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Comets harbor the most pristine material in our solar system in the form of ice, dust, silicates, and refractory organic material with some interstellar heritage. The evolved gas analyzer Cometary Sampling and Composition (COSAC) experiment aboard Rosetta's Philae lander was designed for in situ analysis of organic molecules on comet 67P/Churyumov-Gerasimenko. Twenty-five minutes after Philae's initial comet touchdown, the COSAC mass spectrometer took a spectrum in sniffing mode, which displayed a suite of 16 organic compounds, including many nitrogen-bearing species but no sulfur-bearing species, and four compounds-methyl isocyanate, acetone, propionaldehyde, and acetamide-that had not previously been reported in comets.

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El precio de la tierra en Colombia ha sido cuestionado durante mucho tiempo principalmente por las compras que el estado ha venido realizando durante los últimos años. Como es sabido, el estado ha sido de los pocos compradores sino el único de terrenos en Colombia durante este tiempo, para dar paso a sus programas y proyectos enmarcados principalmente dentro de la Reforma Agraria, dentro de los cuales se han hecho cuestionamientos del valor de adquisición de los terrenos

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Contient : « Traicté entre le Grand-Seigneur et les consuls des Catelans et François, pour le faict du commerce », 1528 ; Traités entre la Turquie et Venise, 1530 ; Traité de paix entre la France et la Turquie, 1535 ; Traité entre Charles-Quint et le roi de Tunis, 1535 (f. 35), — et pièces concernant les relations de l'Empire et de la Turquie au XVIe siècle (f. 42) ; « Meubles envoyez à dom Jehan d'Austriche par sultan Sélim » ; « Traicté entre sultan Sélim... et Charles IX..., 1569 » ; Confirmation des traités entre la France et la Turquie, 1581 ; « Sommaire de la vie de Sélim second..., 1566-1574 » ; « Déclaration de guerre... envoyée au roy de Pologne par... Mahometh III » ; « Sommaire de la vie de Soliman..., 1520-1566 » ; « Traductio litterarum Suleyman Beg, gabellarii quondam Constantino politani, quas scribit ad mortem domini quondam oratoris Franciae domini Johannis de Dolu, propter debita facta, 1565 » ; « Zizimi, ou la relation des aventures du prince Zizimi... ; ce que j'ay trouvé à propos d'insérer icy, à cause qu'il y a plusieurs particularitez qui n'ont point esté mises dans son histoire imprimée » ; «Relatione del viaggio delle galere di Fiorenza..., 1599 » ; « Capitulation d'entre Henry-le-Grand et sultan Achmet » ; « Lettre escrite au roy... Henry IV par Mr de L'Isle », Madrid, 1608 ; « Capitulation et traicté accordés entre sultan Acmat..., d'une part, et... les Estats-Généraux des ... Provinces-Unies des Pays-Bas, d'autre part », juillet 1612 ; « Traicté de paix et d'accommodement, du 21 mars 1619, faict entre monsieur de Guise et les Marseillois, d'une part, et les députez du bâcha et divan d'Alger, d'autre » ; « Lettre du grand roy de Sumatra à Jacques premier, roy d'Angleterre » ; « Advis donné au Roy Très chrestien par Raymond Merigon, de Marseille, pour la conqueste des royaumes d'Alger et Thunis » ; Courte relation du « voyage du Père Pacifique de Provins, capucin, faict en Perse, l'an 1628 » ; Lettre du roi de Perse Cha Abbas à Louis XIII ; « Relation du royaume de Marroque et des villes qui en dépendent » ; Pièces concernant les relations de la France avec Alger, notamment pendant la mission de « Sanson Napolon », 1628-1629 ; Traités avec Alger, 1628 (f. 294), — et 1629 (f. 317 v) ; Traités avec le Maroc, 1630 (f. 324 v), — 1631 (f. 330, etc.), — 1632 (f. 339 v), — et 1635 (f. 341, etc.) ; « Compendio delle varie sette che si trovano fra gli Turchi, authore Mehemet Emin, figliuolo di Sadredin, tradotto di lingua turquesca in vulgare italiano per Yahacob Romano, haebreo Constantinopolitano » ; « Mémorial de l'Estat d'Égipte, en l'an 1634 »