998 resultados para Dámaso I, Papa, Santo, 305-384


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In this paper, I present preliminary findings of the first-large scale, systematic study of English Latino vowels in Miami. Sociolinguistic interviews were conducted with 25 Miami-born participants: 10 Anglo Whites and 15 Latinos with varying degrees of Spanish fluency. Here I focus on the vowel quality (/i, ɪ, ai, æ, ɔ, u /) in the speech of the 2nd and 3rd generations to examine the nature of influence of Spanish on English in Miami over the past 60 years. I conduct an in-depth analysis of the vowel productions of two female speakers, Maria & Blaze, to show the range of vowel productions in Miami Latino English. The vocalic analysis is comprised of a minimum of 15 non-repeating tokens of each vowel. These vowels were extracted from interview data and analyzed for F1, F2, and F3 values using PRAAT. Two allophones of /æ/ were considered: pre-nasal and pre-non-nasal, since Latinos in other regions have shown to resist pre-nasal /æ/ raising (Thomas 2001).

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Surface samples, mostly from abyssal sediments of the South Atlantic, from parts of the equatorial Atlantic, and of the Antarctic Ocean, were investigated for clay content and clay mineral composition. Maps of relative clay mineral content were compiled, which improve previous maps by showing more details, especially at high latitudes. Large-scale relations regarding the origin and transport paths of detrital clay are revealed. High smectite concentrations are observed in abyssal regions, primarily derived from southernmost South America and from minor sources in Southwest Africa. Near submarine volcanoes of the Antarctic Ocean (South Sandwich, Bouvet Island) smectite contents exhibit distinct maxima, which is ascribed to the weathering of altered basalts and volcanic glasses. The illite distribution can be subdivided into five major zones including two maxima revealing both South African and Antarctic sources. A particularly high amount of Mg- and Fe-rich illites are observed close to East Antarctica. They are derived from biotite-bearing crystalline rocks and transported to the west by the East Antarctic Coastal Current. Chiorite and well-crystallized dioctaedral illite are typical minerals enriched within the Subantarctic and Polarfrontal-Zone but of minor importance off East Antarctica. Kaolinite dominates the clay mineral assemblage at low latitudes, where the continental source rocks (West Africa, Brazil) are mainly affected by intensive chemical weathering. Surprisingly, a slight increase of kaolinite is observed in the Enderby Basin and near the Filchner-Ronne Ice shelf. The investigated area can be subdivided into ten, large-scale clay facies zones with characteristic possible source regions and transport paths. Clay mineral assemblages of the largest part of the South Atlantic, especially of the western basins are dominated by chlorite and illite derived from the Antarctic Peninsula and southernmost South America and supported by advection within the Circumantarctic Deep Water flow. In contrast, the East Antarctic provinces are relatively small. Assemblages of the eastern basins north of 30°S are strongly influenced by African sources, controlled by weathering regimes on land and by a complex interaction of wind, river and deep ocean transport. The strong gradient in clay mineral composition at the Brazilian slope indicate a relatively low contribution of tropically derived assemblages to the western basins.

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We analyzed 214 new core-top samples for their CaCO3 content from shelves all around Antarctica in order to understand their distribution and contribution to the marine carbon cycle. The distribution of sedimentary CaCO3 on the Antarctic shelves is connected to environmental parameters where we considered water depth, width of the shelf, sea-ice coverage and primary production. While CaCO3 contents of surface sediments are usually low, high(> 15%) CaCO3 contents occur at shallow water depths (150-200 m) on narrow shelves of the eastern Weddell Sea and at a depth range of 600-900 m on the broader and deeper shelves of the Amundsen, Bellingshausen and western Weddell Seas. Regions with high primary production, such as the Ross Sea and the western Antarctic Peninsula region, have generally low CaCO3 contents in the surface sediments. The predominant mineral phase of CaCO3 on the Antarctic shelves is low-magnesium calcite. With respect to ocean acidification, our findings suggest that dissolution of carbonates in Antarctic shelf sediments may be an important negative feedback only after the onset of calcite undersaturation on the Antarctic shelves. Macrozoobenthic CaCO3 standing stocks do not increase the CaCO3 budget significantly as they are two orders of magnitude lower than the budget of the sediments. This first circumpolar compilation of Antarctic shelf carbonate data does not claim to be complete. Future studies are encouraged and needed to fill data gaps especially in the under-sampled southwest Pacific and Indian Ocean sectors of the Southern Ocean.

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Previous studies about the strength of the lithosphere in the Iberia centre fail to resolve the depth of earthquakes because of the rheological uncertainties. Therefore, new contributions are considered (the crustal structure from a density model) and several parameters (tectonic regime, mantle rheology, strain rate) are checked in this paper to properly examine the role of lithospheric strength in the intraplate seismicity and the Cenozoic evolution. The strength distribution with depth, the integrated strength, the effective elastic thickness and the seismogenic thickness have been calculated by a finite element modelling of the lithosphere across the Central System mountain range and the bordering Duero and Madrid sedimentary basins. Only a dry mantle under strike-slip/extension and a strain rate of 10-15 s-1, or under extension and 10-16 s-1, causes a strong lithosphere. The integrated strength and the elastic thickness are lower in the mountain chain than in the basins. These anisotropies have been maintained since the Cenozoic and determine the mountain uplift and the biharmonic folding of the Iberian lithosphere during the Alpine deformations. The seismogenic thickness bounds the seismic activity in the upper–middle crust, and the decreasing crustal strength from the Duero Basin towards the Madrid Basin is related to a parallel increase in Plio–Quaternary deformations and seismicity. However, elasto–plastic modelling shows that current African–Eurasian convergence is resolved elastically or ductilely, which accounts for the low seismicity recorded in this region.

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Juniperus navicularis Gand. is a dioecious endemic conifer that constitutes the understory of seaside pine forests in Portugal, areas currently threatened by increasing urban expansion. The aim of this study is to assess the conservation status of previously known populations of this species located on its core area of distribution. The study was performed in south-west coast of Portugal. Three populations varying in size and pine density were analyzed. Number of individuals, population density, spatial distribution and individual characteristics of junipers were estimated. Female cone, seed characteristics and seed viability were also evaluated. Results suggest that J. navicularis populations are vulnerable because seminal recruitment is scarce, what may lead to a reduction of genetic variability due solely to vegetative propagation. This vulnerability seems to be strongly determined by climatic constraints toward increasing aridity. Ratio between male and female shrubs did not differ from 1:1 in any population. Deviations from 1:1 between mature and non-mature plants were found in all populations, denoting population ageing. Very low seed viability was observed. A major part of described Juniperus navicularis populations have disappeared through direct habitat loss to urban development, loss of fitness in drier and warmer locations and low seed viability. This study is the first to address J. navicularis conservation, and represents a valuable first step toward this species preservation. 

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Este trabajo estudia las distintas interpretaciones del inicio del capítulo 22 centrándose en la segunda frase. Se propone una nueva interpretación basada en la construcción sintáctica del participio πυνθανόμενος.

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A partir de un abordaje retórico-literario, nuestro objetivo es indagar las representaciones discursivas de los elementos supersticiosos en la biografía de Nicias y en la de Dión. Tomaremos como ejemplo el eclipse de luna narrado en Nicias 23 y reiterado en Dión 24, para demostrar que mediante la repetición del ejemplo en dos contextos distintos Plutarco nos invita a reflexionar sobre la superstición de un modo más atractivo que la mera exposición teórica de doctrinas filosóficas.

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We aspire to shape the Constantine’s personality in particular by analyzing his loving relationship, first with Minervina and then with Fausta, and not forgetting the bond with his mother Helena, hence the reference to uxor, mater and concubina in our title. We will analyze if these women exercised any influence on the composition of his production rules and, if so, to what extent they were able to determine the historical development of the following decades. From this point of view we must consider in general the emperor had to combine their political claims and government with these relationships, showing great skill in handling times and ways, always putting the first to the second.

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What is the human being? Which is its origin and its end? What is the influence of the nature in the man and what is his impact on nature? Forthe animalists, men are like other animals; freedom and rationality are not signs of superiority, nor having rights over the animals. For the ecohumanists, human beings are part of nature, but is qualitatively different and superior to animals; and is the creator of the civilization. We analyze these two ecological looks. A special point is the contribution ofecohumanists -from the first half of the Renaissance, who dealt in extenso the dignity and freedom of the human being-, of Michelangelo and finally, of Mozart, through his four insurmountable operas, which display the difficulty of physical ecology to engender so much beauty, so much wealth, so much love for the creatures and so much variety.

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La presente investigación científica es de naturaleza cualitativa, con abordaje fenomenológico, como objeto de estudio las experiencias de las enfermeras en el cuidado post operatorio inmediato, el objetivo que guió la investigación fue describir, analizar y comprender estas experiencias. La presente investigación se justifico porque hoy en día los cuidados de las enfermeras a nivel mundial, nacional y local requiere que desarrollen competencias necesarias para brindar un cuidado humanizado, más aún a las personas que se encuentran en el post operatorio inmediato; por lo que es conveniente profundizar y conocer la forma cómo viven, enfrentan y expresan sus experiencias frente al cuidado, y así ofrecer la oportunidad de mejorar en el día a día la práctica del cuidado de enfermería. Esta investigación se sustentó en los conceptos de experiencia de Wojtyla (2005), cuidado por Waldow (2008), post operatorio inmediato según Almeida (2005). Se tuvieron como sujetos de estudio a 7 enfermeras que laboran en la unidad de cuidados post anestésicos del Hospital I Naylamp, la muestra se determinó por saturación; los datos se recolectaron mediante la entrevista a profundidad no estructurada y se trataron mediante el análisis fenomenológico. Se tuvo en cuenta los criterios de rigor ético según Sgreccia y rigor científico según Hernández. Obteniéndose las siguientes proposiciones: Proposición A: Entre la satisfacción e insatisfacción al brindar cuidados post operatorios, Proposición B: Brindando un cuidado integral a la persona post operada, Proposición C: Responsabilidad vs Temor e impotencia frente a las complicaciones post operatorias.