956 resultados para Hume, Ross
Resumo:
No resulta fácil desentrañar el pensamiento de un escéptico acerca de temas sobre los que prefiere abstenerse de formular juicios. Es el caso de David Hume y la religión.El filósofo escocés nacido en 1711 dejó varios escritos aludiendo al fenómeno, es decir, a la religión tal como existe de hecho, y manifestó su opinión crítica acerca de las distintas posturas intelectuales de su tiempo en torno a cuestiones religiosas. Pero siempre fue ambiguo e irónico cuando le tocó dejar asentado su propio juicio con respecto a este tema. La dificultad principal reside en que, para Hume, a quien podríamos considerar un ?escéptico mitigado?, los juicios correctos son aquellos que se ajustan a la estrecha capacidad del entendimiento humano, que no va más allá de los límites de la experiencia de la vida cotidiana. Muchos aspectos vinculados a la religión ?tales como la posibilidad de conocer de la esencia y los atributos divinos- exceden nuestras limitadas facultades y, si nos aventuramos a argumentar en ese ámbito, corremos el riesgo de caer en el error y la irracionalidad. Nuestra propuesta consiste en examinar cuál es la postura de Hume sobre los distintos problemas que presentan el conocimiento y la práctica vinculados con la religión. Respecto del conocimiento, las dificultades se plantean a la hora de determinar qué estatuto otorgarle a las creencias religiosas, cuál es el origen en nuestra mente de la religiosidad y cómo justificar por medio de argumentos la existencia y atributos de la divinidad. En cuanto a la práctica, Hume formula una serie de críticas a las actitudes e instituciones religiosas tal como se han dado históricamente a partir del análisis de las consecuencias que observa en la sociedad, de las que surge una contradicción entre un conjunto de principios respetables y un sinnúmero de acciones deplorables. Para examinar estas cuestiones es necesario tener en cuenta el punto de vista desde el que efectúa su análisis, que se vincula, como acabamos de mencionar, con el escepticismo mitigado. Finalmente, evaluaremos si es posible proponer alguna forma de religión que tenga el visto bueno de Hume y, en ese caso, qué características debería revestir. Para lograrlo, deberemos abrirnos paso entre su inteligente ironía y su excesiva prudencia.
Resumo:
Por sus propias palabras y por las de la mayoría de sus intérpretes, se ha considerado a Hume un escéptico mitigado. Sin embargo, la distinción hecha por el filósofo entre escepticismo pirrónico y académico no es correcta en absoluto. El objetivo de este trabajo es mostrar que quizá la filosofía escéptico-naturalista de Hume no se halla tan distanciada del pirronismo auténtico como lo afirma su propio autor. En tal sentido, intentaremos desentrañar si el 'mitigado' escepticismo del escocés no esconde cierto pirronismo inconsciente, señalando que la clave puede hallarse en el desenlace del escepticismo humeano: la 'cura de la naturaleza'
Resumo:
Fil: Elgarte, Julieta Magdalena. Universidad Nacional de La Plata. Facultad de Humanidades y Ciencias de la Educación; Argentina.
Resumo:
Dissolved and particulate organic matter was measured during six cruises to the southern Ross Sea. The cruises were conducted during late austral winter to autumn from 1994 to 1997 and included coverage of various stages of the seasonal phytoplankton bloom. The data from the various years are compiled into a representative seasonal cycle in order to assess general patterns of dissolved organic matter (DOM) and particulate organic matter (POM) dynamics in the southern Ross Sea. Dissolved organic carbon (DOC) and particulate organic carbon (POC) were at background concentrations of approximately 42 and 3 µM C, respectively, during the late winter conditions in October. As the spring phytoplankton bloom progressed, organic matter increased, and by January DOC and POC reached as high as 30 and 107 µM C, respectively, in excess of initial wintertime conditions. Stocks and concentrations of DOC and POC returned to near background values by autumn (April). Approximately 90% of the accumulated organic matter was partitioned into POM, with modest net accumulation of DOM stocks despite large net organic matter production and the dominance of Phaeocystis antarctica. Changes in NO3 concentration from wintertime values were used to calculate the equivalent biological drawdown of dissolved inorganic carbon (DICequiv). The fraction of DICequiv drawdown resulting in net DOC production was relatively constant (ca. 11%), despite large temporal and spatial variability in DICequiv drawdown. The C : N (molar ratio) of the seasonally produced DOM had a geometric mean of 6.2 and was nitrogen-rich compared to background DOM. The DOM stocks that accumulate in excess of deep refractory background stocks are often referred to as "semi-labile" DOM. The "semi-labile" pool in the Ross Sea turns over on timescales of about 6 months. As a result of the modest net DOM production and its lability, the role DOM plays in export to the deep sea is small in this region.
Resumo:
Phytoliths (siliceous plant microfossils) have been recovered from Cenozoic sediments (c. 34 to 17 Ma) in the CRP-2/2A and CRP-3 drillholes cored off Cape Roberts, Victoria Land Basin, Antarctica. The phytolith assemblages are sparse, but well-preserved and dominated by spherical forms similar to those of modern trees or shrubs. Rare phytoliths comparable to modern grass forms are also present. However, due to the paucity of phytolith data, any interpretations made are necessarily tentative. The assemblages of CRP-2/2A and the upper c. 250 m of CRP-3 are interpreted as representing a predominantly woody vegetation, including Nothofagus and Libocedrus with local areas of grass in the more exposed locations. A cool climate is interpreted to have prevailed throughout both cores. However, beneath c. 250 metres below sea floor in CRP-3, the dominant woody vegetation is supplemented by pockets of Palmae, ?Proteaceae and 'warm' climate grasses. This association represents vegetation growth in sheltered, moist sites - possibly north-facing mid-slopes or the coastal fringe. It may also represent remnant vegetation that grew in moist, temperate conditions during the Middle to Late Eocene, previously interpreted from the Southern McMurdo Sound erratics and lower part of the CIROS-1 drillhole. The phytolith analysis compares well to the terrestrial palynomorph record from both cores and provides additional independent taxonomic and climatic interpretations.
Resumo:
Fil: Calvente, Sofía Beatriz. Universidad Nacional de La Plata. Facultad de Humanidades y Ciencias de la Educación; Argentina.
Resumo:
The objective of this study was to examine the presence and diversity of Archaea within mineral and ornithogenic soils from 12 locations across the Ross Sea region. Archaea were not abundant but DNA sufficient for producing 16S rRNA gene clone libraries was extracted from 18 of 51 soil samples, from four locations. A total of 1452 clones were analysed by restriction fragment length polymorphism and assigned to 43 operational taxonomic units from which representatives were sequenced. Archaea were primarily restricted to coastal mineral soils which showed a predominance of Crenarchaeota belonging to group 1.1b (>99% of clones). These clones were assigned to six clusters (A through F), based on shared identity to sequences in the GenBank database. Ordination indicated that soil chemistry and water content determined archaeal community structure. This is the first comprehensive study of the archaeal community in Antarctic soils and as such provides a reference point for further investigation of microbial function in this environment.
Resumo:
Fil: Calvente, Sofía Beatriz. Universidad Nacional de La Plata. Facultad de Humanidades y Ciencias de la Educación; Argentina.