982 resultados para Epica filosófica


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Coordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES)

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The relationship between humans and non-human animals dates back to the Prehistoric Era, when groups of humans migrated from the nomadic and extractive stage to sedentariness, starting to develop agriculture and animal husbandry. Ancient Greek philosophy, notably the Aristotelian school of philosophy, posited that nature has not done anything for nothing, and all things have a purpose: plants were created for the sake of animals, and these for the good of men, while the Bible preaches the view that the world was created for the good of men and other species were subordinated to their wants and needs. During the Renaissance, centuries XIV to XVI, anthropocentrism was established as the main philosophical concept. However, in relation to the treatment of animals, Renaissance did not differ substantially from medieval scholasticism, considering animals like machines, devoid of pain and immortal soul. In this context, scientific knowledge about plants, non-human animals and nature in general, is built on anthropocentric values, thus influencing the construction of school education in the disciplines of Science and Biology. Nowadays, at São Paulo state schools, specifically in the Ensino Fundamental II (6th to 9th grade), the program of the discipline Ciências da Natureza e suas Tecnologias is set by the Currículo Oficial do Estado de São Paulo, via the São Paulo Faz Escola Program, implemented by the Secretaria Estadual de Educação in 2010. This documentary research used the methodology of Content Analysis and aimed to analyze the presentation of non-human animals in Caderno do Professor and Caderno do Aluno, from 6th to 9th grades of the discipline Ciências da Natureza e suas Tecnologias. The analysis of the courseware revealed that its contents were influenced by the anthropocentric view, in both implicitly and explicitly ways, conveying anthropomorphic, utilitarian, stereotyped and derogatory statements towards...

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The relationship between humans and non-human animals dates back to the Prehistoric Era, when groups of humans migrated from the nomadic and extractive stage to sedentariness, starting to develop agriculture and animal husbandry. Ancient Greek philosophy, notably the Aristotelian school of philosophy, posited that nature has not done anything for nothing, and all things have a purpose: plants were created for the sake of animals, and these for the good of men, while the Bible preaches the view that the world was created for the good of men and other species were subordinated to their wants and needs. During the Renaissance, centuries XIV to XVI, anthropocentrism was established as the main philosophical concept. However, in relation to the treatment of animals, Renaissance did not differ substantially from medieval scholasticism, considering animals like machines, devoid of pain and immortal soul. In this context, scientific knowledge about plants, non-human animals and nature in general, is built on anthropocentric values, thus influencing the construction of school education in the disciplines of Science and Biology. Nowadays, at São Paulo state schools, specifically in the Ensino Fundamental II (6th to 9th grade), the program of the discipline Ciências da Natureza e suas Tecnologias is set by the Currículo Oficial do Estado de São Paulo, via the São Paulo Faz Escola Program, implemented by the Secretaria Estadual de Educação in 2010. This documentary research used the methodology of Content Analysis and aimed to analyze the presentation of non-human animals in Caderno do Professor and Caderno do Aluno, from 6th to 9th grades of the discipline Ciências da Natureza e suas Tecnologias. The analysis of the courseware revealed that its contents were influenced by the anthropocentric view, in both implicitly and explicitly ways, conveying anthropomorphic, utilitarian, stereotyped and derogatory statements towards...

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Estudo reflexivo com o objetivo de apresentar, na perspectiva da hermenêutica filosófica, elementos relevantes para o seguimento da saúde da criança em atenção primária à saúde. A assistência à saúde da criança tem como eixo norteador o processo de crescimento e desenvolvimento na infância, sendo fundamental conhecer as escolhas e tomadas de decisão das famílias, estimular a produção de narrativas, fortalecer virtudes e experiências cotidianas, contribuindo para enriquecer o cuidado e apreendê-lo numa perspectiva integradora, contingencial, longitudinal e suficientemente boa. O seguimento da criança pode ser tomado como uma tecnologia de cuidado em saúde que não pressupõe um saber a priori, mas remete a uma reconstrução de saberes e práticas com novas dimensões para a produção de cuidados.

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Políticas públicas de educação ambiental no Brasil estimulam o envolvimento de educadores em processos de políticas públicas mediados pelo diálogo. Isso demanda o desvelamento do conceito de diálogo, objetivo deste trabalho. Os resultados do levantamento bibliográfico estabelecem a relação entre o diálogo, as políticas públicas de educação ambiental e seus pressupostos epistemológicos, trazem a fundamentação filosófica e abordam a teoria operacional para o diálogo. Por fim, indicam obstáculos a sua ocorrência e sugerem a formação de espaços de diálogo para contorná-los.

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Este trabalho relata a experiência de avaliação do acolhimento em saúde mental na cidade de São Paulo-SP, utilizando entrevistas com trabalhadores de um Centro de Atenção Psicossocial (CAPS) e duas Unidades Básicas de Saúde (UBS). Objetivou entender o acolhimento, considerando a percepção dos trabalhadores e identificando o vínculo e a articulação da rede nesse processo. Utilizou-se como método a hermenêutica filosófica, para identificar que elementos participantes do processo de acolhimento poderiam ser destacados. Procedeu-se à análise das narrativas a partir de três linhas de argumentação: vínculo, acolhimento e articulação da rede - resultando em quatro categorias: sensação de ausência; mistura de modelos; primazia em tecnologias duras; e ineficiência quanto à integralidade. A discussão apontou uma imbricação dessas categorias, colocando o investimento em tecnologias leves como centro do debate para a superação da sensação de ausência, da mistura dos modelos e para construção da integralidade do cuidado.

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Nella mia tesi di dottorato mi propongo di indagare la metamorfosi del romanzo nella letteratura italiana contemporanea attraverso il lavoro di Paolo Volponi, che può essere descritto come un’«opera mondo», in accordo con la formula critica coniata da Franco Moretti. Volponi intende superare il divario fra l’io e il mondo e ricomporre il corpo come una mediazione umanistica di ragione e sensi. La sua opera può essere definita ‘epica’ perché recupera la tradizione del romanzo cavalleresco e la parodia esercitata su questa tradizione letteraria da Cervantes nel Don Chisciotte. Ma, come l’Ulysses di Joyce, è un’epica «moderna» perché fondata su una totalità disgiunta e sul conflitto dialogico, in una linea che accomuna la moltiplicazione dei punti di vista, propria del romanzo polifonico secondo Bachtin, alla pluralità di prospettive del discorso scientifico. Dopo un primo capitolo teorico, nel secondo e nel terzo capitolo della tesi i romanzi di Volponi vengono studiati in rapporto al filone dell’«epica moderna» e al genere satirico, che ha un suo modello fondativo nell’opera di Giacomo Leopardi. Il quarto capitolo si focalizza sulle ultime raccolte poetiche, che mostrano la tendenza a recuperare il linguaggio formulare e la matrice orale della poesia delle origini, servendosene per rappresentare in funzione contrappuntistica l’universo globale dell’età contemporanea.

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Este estudio se propone indagar el problema de la relación entre individuo, multitud y libertad en la obra de Spinoza, problema que, es nuestra hipótesis, permite echar luz sobre las alternativas fundamentales que se pusieron en juego en el debate teórico-político de la primera modernidad, y consecuentemente, en la formación de los órdenes políticos secularizados contemporáneos. ¿Cómo es posible la fundación y la conservación de un orden político en estas condiciones de incertidumbre? Más aún: ¿cómo hacer de esta incertidumbre no ya una amenaza, sino la fuerza motriz de un orden político? Estas son algunas de las preguntas que Spinoza responde a partir de una política y una filosofía de la inmanencia y que presentan, para nosotros, el doble interés de una interrogación “histórica” que busca en los orígenes de la modernidad sus posibilidades no transitadas, y “teórico política” en tanto busca en la ontología política spinoziana una forma de interrogar, desde las posibilidades inscriptas en su origen, las encrucijadas de la política moderna. Para llevar adelante esta investigación tomaremos como punto de partida la noción spinoziana de individualidad, buscando comprender sus determinaciones, su especificidad y el modo en que, a partir de ella, resulta posible pensar la "naturaleza humana" y las condiciones de la vida en común. Esta noción de individualidad, sostendremos, implica una crítica moderna de las categorías centrales del proyecto moderno, cuya clave se encuentra justamente en una crítica radical de la concepción moderna de la subjetividad (ya sea en su dimensión individual, como concepción del hombre, o en su dimensión política, como concepción del sujeto soberano). A partir de este desarrollo, daremos tratamiento a la concepción spinoziana de la política, y del que se revela en sus últimos escritos como su actor fundamental: la multitud. Para ello, hemos pretendido poner de relieve la distancia de Spinoza respecto del paradigma de la soberanía estatal desarrollado por Hobbes (y continuado en toda la tradición filosófica del derecho natural, pasando por Locke, Rousseau y Kant) y las consecuencias históricas, políticas e institucionales de tal distancia, así como las posibilidades abiertas a un pensamiento político a partir del registro conceptual abierto por Spinoza.

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The present dissertation focuses on the dual number in Ancient Greek in a diachronical lapse stretching from the Mycenaean age to the Attic Drama and Comedy of the 5th century BC. In the first chapter morphological issues are addressed, chiefly in a comparative perspective. The Indo European evidence on the dual is hence gathered in order to sketch patterns of grammaticalisation and paradigmatisation of specific grams, growing increasingly functional within the Greek domain. In the second chapter syntactical problems are tackled. After a survey of scholarly literature on the Greek dual, we engage in a functional and typological approach, in order to disentangle some biased assessments on the dual, namely its alleged lack of regularity and intermittent agreement. Some recent frameworks in General Linguistics provide useful grounds for casting new light on the subject. Internal Reconstruction, for instance, supports the facultativity of the dual in each and every stage of its development; Typology and the Animacy Hierarcy add precious cross linguistical insight on the behaviour of the dual toward agreement. Glaring differences also arise as to the adoption — or avoidance — of the dual by different authors. Idiolectal varieties prove in fact conditioned by stylistical and register necessity. By means of a comparison among Epics, Tragedy and Comedy it is possible to enhance differences in the evaluation of the dual, which led sometimes to forms of ‘censure’ — thus triggering the onset of competing strategies to express duality. The last two chapters delve into the tantalising variety of the Homeric evidence, first of all in an account of the notorious issue of the Embassy of Iliad IX, and last in a commentary of all significant Homeric duals — mostly represented by archaisms, formulae, and ad hoc coinages.

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Since its discovery in Greenland ice cores, the millennial scale climatic variability of the last glacial period has been increasingly documented at all latitudes with studies focusing mainly on Marine Isotopic Stage 3 (MIS 3; 28–60 thousand of years before present, hereafter ka) and characterized by short Dansgaard-Oeschger (DO) events. Recent and new results obtained on the EPICA and NorthGRIP ice cores now precisely describe the rapid variations of Antarctic and Greenland temperature during MIS 5 (73.5–123 ka), a time period corresponding to relatively high sea level. The results display a succession of abrupt events associated with long Greenland InterStadial phases (GIS) enabling us to highlight a sub-millennial scale climatic variability depicted by (i) short-lived and abrupt warming events preceding some GIS (precursor-type events) and (ii) abrupt warming events at the end of some GIS (rebound-type events). The occurrence of these sub-millennial scale events is suggested to be driven by the insolation at high northern latitudes together with the internal forcing of ice sheets. Thanks to a recent NorthGRIP-EPICA Dronning Maud Land (EDML) common timescale over MIS 5, the bipolar sequence of climatic events can be established at millennial to sub-millennial timescale. This shows that for extraordinary long stadial durations the accompanying Antarctic warming amplitude cannot be described by a simple linear relationship between the two as expected from the bipolar seesaw concept. We also show that when ice sheets are extensive, Antarctica does not necessarily warm during the whole GS as the thermal bipolar seesaw model would predict, questioning the Greenland ice core temperature records as a proxy for AMOC changes throughout the glacial period.

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Millennial variability is a robust feature of many paleoclimate records, at least throughout the last several glacial cycles. Here we use the mean signal from Antarctic climate events 1 to 4 to probe the EPICA Dome C temperature proxy reconstruction through the last 500 ka for similar millennial-scale events. We find that clusters of millennial events occurred in a regular fashion over half of the time during this with a mean recurrence interval of 21 kyr. We find that there is no consistent link between ice-rafted debris deposition and millennial variability. Instead we speculate that changes in the zonality of atmospheric circulation over the North Atlantic form a viable alternative to freshwater release from icebergs as a trigger for millennial variability. We suggest that millennial changes in the zonality of atmospheric circulation over the North Atlantic are linked to precession via sea-ice feedbacks and that this relationship is modified by the presence of the large, Northern Hemisphere ice sheets during glacial periods.

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We measured δ17O and δ18O in two Antarctic ice cores at EPICA Dome C (EDC) and TALDICE (TD), respectively and computed 17O-excess with respect to VSMOW. The comparison of our 17O-excess data with the previous record obtained at Vostok (Landais et al., 2008) revealed differences up to 35 ppm in 17O-excess mean level and evolution for the three sites. Our data showed that the large increase depicted at Vostok (20 ppm) during the last deglaciation, is a regional and not a general pattern in the temporal distribution of 17O-excess in East Antarctica. The EDC data display an increase of 13 ppm, whereas the TD data show no significant variation from the Last Glacial Maximum (LGM) to the Early Holocene (EH). Lagrangian moisture source diagnostic revealed very different source regions for Vostok and EDC compared to TD. These findings combined with the results of a sensitivity analysis, using a Rayleigh-type isotopic model, suggest that relative humidity (RH) at the oceanic source region (OSR) are a determining factor for the spatial differences of 17O-excess in East Antarctica. However, 17O-excess in remote sites of continental Antarctica (e.g. Vostok) may be highly sensitive to local effects. Hence, we consider 17O-excess in coastal East Antarctic ice cores (TD) to be more reliable as a proxy for RH at the OSR.

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We measured δ17O and δ18O in two Antarctic ice cores at EPICA Dome C (EDC) and TALDICE (TD), respectively, and computed 17O-excess with respect to VSMOW. The comparison of our 17O-excess data with the previous record obtained at Vostok (Landais et al., 2008a) revealed differences up to 35 ppm in 17O-excess mean level and evolution for the three sites. Our data show that the large increase depicted at Vostok (20 ppm) during the last deglaciation is a regional and not a general pattern in the temporal distribution of 17O-excess in East Antarctica. The EDC data display an increase of 12 ppm, whereas the TD data show no significant variation from the Last Glacial Maximum (LGM) to the Early Holocene (EH). A Lagrangian moisture source diagnostic revealed very different source regions for Vostok and EDC compared to TD. These findings combined with the results of a sensitivity analysis, using a Rayleigh-type isotopic model, suggest that normalized relative humidity (RHn) at the oceanic source region (OSR) is a determining factor for the spatial differences of 17O-excess in East Antarctica. However, 17O-excess in remote sites of continental Antarctica (e.g. Vostok) may be highly sensitive to local effects. Hence, we consider 17O-excess in coastal East Antarctic ice cores (TD) to be more reliable as a proxy for RHn at the OSR.

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High-resolution measurements of chemical impurities and methane concentrations in Greenland ice core samples from the early glacial period allow the extension of annual-layer counted chronologies and the improvement of gas age-ice age difference (Δage) essential to the synchronization of ice core records. We report high-resolution measurements of a 50 m section of the NorthGRIP ice core and corresponding annual layer thicknesses in order to constrain the duration of the Greenland Stadial 22 (GS-22) between Greenland Interstadials (GIs) 21 and 22, for which inconsistent durations and ages have been reported from Greenland and Antarctic ice core records as well as European speleothems. Depending on the chronology used, GS-22 occurred between approximately 89 (end of GI-22) and 83 kyr b2k (onset of GI-21). From annual layer counting, we find that GS-22 lasted between 2696 and 3092 years and was followed by a GI-21 pre-cursor event lasting between 331 and 369 yr. Our layer-based counting agrees with the duration of stadial 22 as determined from the NALPS speleothem record (3250 ± 526 yr) but not with that of the GICC05modelext chronology (2620 yr) or an alternative chronology based on gas-marker synchronization to EPICA Dronning Maud Land ice core. These results show that GICC05modelext overestimates accumulation and/or underestimates thinning in this early part of the last glacial period. We also revise the possible ranges of NorthGRIP Δdepth (5.49 to 5.85 m) and Δage (498 to 601 yr) at the warming onset of GI-21 as well as the Δage range at the onset of the GI-21 precursor warming (523 to 654 yr), observing that temperature (represented by the δ15N proxy) increases before CH4 concentration by no more than a few decades.

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We present a Rare Earth Elements (REE) record determined on the EPICA ice core drilled at Dronning Maud Land (EDML) in the Atlantic sector of the East Antarctic Plateau. The record covers the transition from the last glacial stage (LGS) to the early Holocene (26 600–7500 yr BP) at decadal to centennial resolution. Additionally, samples from potential source areas (PSAs) for Antarctic dust were analyzed for their REE characteristics. The dust provenance is discussed by comparing the REE fingerprints in the ice core and the PSA samples. We find a shift in variability in REE composition at ~15 000 yr BP in the ice core samples. Before 15 000 yr BP, the dust composition is very uniform and its provenance was most certainly dominated by a South American source. After 15 000 yr BP, multiple sources such as Australia and New Zealand become relatively more important, although South America remains the major dust source. A similar change in the dust characteristics was observed in the EPICA Dome C ice core at around ~15 000 yr BP, accompanied by a shift in the REE composition, thus suggesting a change of atmospheric circulation in the Southern Hemisphere.