Savitri y Orfeo : La argumentación en la lógica india y en la retórica clásica

Los mitos de Savitri (Mahabharata 3.293-299) y Orfeo (Ovidio. Metamorfosis 10.1-85), pertenecientes al ámbito cultural indoeur opeo, presentan algunos puntos en común: narran la historia del amante que rescata a su ser amado de la muerte, y combinan el encuentro con los dioses de la muerte y el discurso mediante el poder de la palabra. En esta propuesta, se analizan los discursos de los protagonistas a partir de las convenciones propias de cada contexto de enunciación. Para el caso indio, se sigue el modelo lógico de la escuela Nyaya; para el greco-latino, el de la retórica clásica. De este modo, sobre la base de la estructura argumentativa del silogismo aristotélico, se plantean dos variaciones, respectivamente, el silogismo hindú y el silogismo retórico. Se trata de dos aproximaciones argumentativas con métodos distintos pero con un mismo fin: (con)vencer al oponente

Breve nota sobre a etimologia de Dioniso

This article aims chiefly to discuss the status quaestionis regarding the etymology of Dionysus. The main theories thereon are analyzed and a new connection is put forward between the name of the god and one of his characteristic activities -dancing. In view of this, some passages of the Rig Veda are pointed out which might strengthen the bond already suggested between Dionysus and the god Indra within the Indo-European tradition

Isotopic composition of terrestrial plant waxes (dD and d13C of n-alkanes) of sediment core SO188_342 from the Northern Bay of Bengal for the last 18 ka

The Indian Summer Monsoon (ISM) is a major global climatic phenomenon. Long-term precipitation proxy records of the ISM, however, are often fragmented and discontinuous, impeding an estimation of the magnitude of precipitation variability from the Last Glacial to the present. To improve our understanding of past ISM variability, we provide a continuous reconstructed record of precipitation and continental vegetation changes from the lower Ganges-Brahmaputra-Meghna catchment and the Indo-Burman ranges over the last 18,000 years (18 ka). The records derive from a marine sediment core from the northern Bay of Bengal (NBoB), and are complemented by numerical model results of spatial moisture transport and precipitation distribution over the Bengal region. The isotopic composition of terrestrial plant waxes (dD and d13C of n-alkanes) are compared to results from an isotope-enabled general atmospheric circulation model (IsoCAM) for selected time slices (pre-industrial, mid-Holocene and Heinrich Stadial 1). Comparison of proxy and model results indicate that past changes in the dD of precipitation and plant waxes were mainly driven by the amount effect, and strongly influenced by ISM rainfall. Maximum precipitation is detected for the Early Holocene Climatic Optimum (EHCO; 10.5-6 ka BP), whereas minimum precipitation occurred during the Heinrich Stadial 1 (HS1; 16.9-15.4 ka BP). The IsoCAM model results support the hypothesis of a constant moisture source (i.e. the NBoB) throughout the study period. Relative to the pre-industrial period the model reconstructions show 20% more rain during the mid-Holocene (6 ka BP) and 20% less rain during the Heinrich Stadial 1 (HS1), respectively. A shift from C4-plant dominated ecosystems during the glacial to subsequent C3/C4-mixed ones during the interglacial took place. Vegetation changes were predominantly driven by precipitation variability, as evidenced by the significant correlation between the dD and d13C alkane records. When compared to other records across the ISM domain, precipitation and vegetation changes inferred from our records and the numerical model results provide evidence for a coherent regional variability of the ISM from the Last Glacial to the present.

Breve nota sobre a etimologia de Dioniso

This article aims chiefly to discuss the status quaestionis regarding the etymology of Dionysus. The main theories thereon are analyzed and a new connection is put forward between the name of the god and one of his characteristic activities -dancing. In view of this, some passages of the Rig Veda are pointed out which might strengthen the bond already suggested between Dionysus and the god Indra within the Indo-European tradition

Planktic foraminiferal Mg/Ca and oxygen isotopes, plus estimated d18Oseawater and ice volume corrected d18Oseawater for the past 35000 years of sediment core GeoB10069-3

Evidence from geologic archives suggests that there were large changes in the tropical hydrologic cycle associated with the two prominent northern hemisphere deglacial cooling events, Heinrich Stadial 1 (HS1; ~19 to 15 kyr BP; kyr BP = 1000 yr before present) and the Younger Dryas (~12.9 to 11.7 kyr BP). These hydrologic shifts have been alternatively attributed to high and low latitude origin. Here, we present a new record of hydrologic variability based on planktic foraminifera-derived d18O of seawater (d18Osw) estimates from a sediment core from the tropical Eastern Indian Ocean, and using 12 additional d18Osw records, construct a single record of the dominant mode of tropical Eastern Equatorial Pacific and Indo-Pacific Warm Pool (IPWP) hydrologic variability. We show that deglacial hydrologic shifts parallel variations in the reconstructed interhemispheric temperature gradient, suggesting a strong response to variations in the Atlantic Meridional Overturning Circulation and the attendant heat redistribution. A transient model simulation of the last deglaciation suggests that hydrologic changes, including a southward shift in the Intertropical Convergence Zone (ITCZ) which likely occurred during these northern hemisphere cold events, coupled with oceanic advection and mixing, resulted in increased salinity in the Indonesian region of the IPWP and the eastern tropical Pacific, which is recorded by the d18Osw proxy. Based on our observations and modeling results we suggest the interhemispheric temperature gradient directly controls the tropical hydrologic cycle on these time scales, which in turn mediates poleward atmospheric heat transport.

A oralidade e a transcriçao em joe sacco

Hoy día, llama la atención los variados temas y la osadía de las formas de narra una historieta. El foco de este artículo es la obra de Joe Sacco, que ha publicado narraciones sobre los conflictos de la Palestina en el inicio de los años 1990 y sobre la Guerra de la Bosnia, que ha terminado en 1995. Indo a las ubicaciones sobre las cuales escribe, Sacco entrevista personas y oye sus narraciones, que transcribe, en el formato de historietas, juntamente con sus propias experiencias como viajante. Esa abordaje permite la análisis comparada del narrador en Joe Sacco con el narrador de Benjamin (1934) y también con el narrador pos-moderno

Savitri y Orfeo : La argumentación en la lógica india y en la retórica clásica

Los mitos de Savitri (Mahabharata 3.293-299) y Orfeo (Ovidio. Metamorfosis 10.1-85), pertenecientes al ámbito cultural indoeur opeo, presentan algunos puntos en común: narran la historia del amante que rescata a su ser amado de la muerte, y combinan el encuentro con los dioses de la muerte y el discurso mediante el poder de la palabra. En esta propuesta, se analizan los discursos de los protagonistas a partir de las convenciones propias de cada contexto de enunciación. Para el caso indio, se sigue el modelo lógico de la escuela Nyaya; para el greco-latino, el de la retórica clásica. De este modo, sobre la base de la estructura argumentativa del silogismo aristotélico, se plantean dos variaciones, respectivamente, el silogismo hindú y el silogismo retórico. Se trata de dos aproximaciones argumentativas con métodos distintos pero con un mismo fin: (con)vencer al oponente

A oralidade e a transcriçao em joe sacco

Hoy día, llama la atención los variados temas y la osadía de las formas de narra una historieta. El foco de este artículo es la obra de Joe Sacco, que ha publicado narraciones sobre los conflictos de la Palestina en el inicio de los años 1990 y sobre la Guerra de la Bosnia, que ha terminado en 1995. Indo a las ubicaciones sobre las cuales escribe, Sacco entrevista personas y oye sus narraciones, que transcribe, en el formato de historietas, juntamente con sus propias experiencias como viajante. Esa abordaje permite la análisis comparada del narrador en Joe Sacco con el narrador de Benjamin (1934) y también con el narrador pos-moderno

Savitri y Orfeo : La argumentación en la lógica india y en la retórica clásica

Los mitos de Savitri (Mahabharata 3.293-299) y Orfeo (Ovidio. Metamorfosis 10.1-85), pertenecientes al ámbito cultural indoeur opeo, presentan algunos puntos en común: narran la historia del amante que rescata a su ser amado de la muerte, y combinan el encuentro con los dioses de la muerte y el discurso mediante el poder de la palabra. En esta propuesta, se analizan los discursos de los protagonistas a partir de las convenciones propias de cada contexto de enunciación. Para el caso indio, se sigue el modelo lógico de la escuela Nyaya; para el greco-latino, el de la retórica clásica. De este modo, sobre la base de la estructura argumentativa del silogismo aristotélico, se plantean dos variaciones, respectivamente, el silogismo hindú y el silogismo retórico. Se trata de dos aproximaciones argumentativas con métodos distintos pero con un mismo fin: (con)vencer al oponente

Breve nota sobre a etimologia de Dioniso

This article aims chiefly to discuss the status quaestionis regarding the etymology of Dionysus. The main theories thereon are analyzed and a new connection is put forward between the name of the god and one of his characteristic activities -dancing. In view of this, some passages of the Rig Veda are pointed out which might strengthen the bond already suggested between Dionysus and the god Indra within the Indo-European tradition

Diatom studies in surface and downcore sediments off southern Sumatra and Java

A wealth of sedimentary records aimed at reconstructing late Quaternary changes in productivity and temperature have been devoted to understanding linkages between the Indo-Pacific Warm Pool (IPWP) and other distant oceanic areas. Most of these reconstructions are based, however, on biogeochemical and sedimentological proxies, with comparatively less attention devoted to microfossils. A high-resolution (<1 ka) study of diatom concentrations and the community at site GeoB10038-4, recovered off southern Sumatra (ca. 6°S, 103°E), closely tracks the variations of diatom concentrations in the westernmost IPWP during the last glacial-interglacial cycle. The diatom record provides evidence that diatom paleoproductivity was highest during interglacials, primarily due to the input of lithogenics and nutrients following the rise in sea level after full glacials. In addition, the co-variation of total diatom concentration and Northern Hemisphere forcing for Marine Isotope Stage 5 suggests a direct response of diatom productivity and upwelling intensity to boreal summer insolation. Temporal shifts of the diverse diatom community at site GeoB10038-4 correspond well with the present-day seasonal monsoon pattern and the strengthening and weakening phases of upwelling along the southern coast of Sumatra. Resting spores of Chaetoceros, typical of nutrient-rich waters, were dominant during periods of highest diatom paleoproductivity and responded to the strengthening of the SE monsoon, while diatoms of oligotrophic to mesotrophic waters characterized intermonsoon periods. The close correspondence between the dominance of upwelling diatoms and the boreal summer insolation resembles the present-day dynamics of diatom production. The observed interglacial highs and glacial lows of diatom productivity at site GeoB10038-4 is a unique pattern in the late Quaternary tropics.

Strontium isotope data from DSDP Sites 32-305 and 62-463 and ODP Sites 113-689 and 113-690

Fluctuations in oxygen (d18O) and carbon (d13C) isotope values of benthic foraminiferal calcite from the tropical Pacific and Southern Oceans indicate rapid reversals in the dominant mode and direction of the thermohaline circulation during a 1 m.y. interval (71-70 Ma) in the Maastrichtian. At the onset of this change, benthic foraminiferal d18O values increased and were highest in low-latitude Pacific Ocean waters, whereas benthic and planktic foraminiferal d13C values decreased and benthic values were lowest in the Southern Ocean. Subsequently, benthic foraminiferal d18O values in the Indo-Pacific decreased, and benthic and planktic d13C values increased globally. These isotopic patterns suggest that cool intermediate-depth waters, derived from high-latitude regions, penetrated temporarily to the tropics. The low benthic d13C values at the Southern Ocean sites, however, suggest that these cool waters may have been derived from high northern rather than high southern latitudes. Correlation with eustatic sea-level curves suggests that sea-level change was the most likely mechanism to change the circulation and/or source(s) of intermediate-depth waters. We thus propose that oceanic circulation during the latest Cretaceous was vigorous and that competing sources of intermediate- and deep-water formation, linked to changes in climate and sea level, may have alternated in importance.

Distribution of the planktonic foraminifer genus Streptochilus in Neogene sediments

Study of four species of the biserial planktonic foraminifer Streptochitus from Deep Sea Drilling Project cores of the Eauripik Rise, western equatorial Pacific, and Ninety-east Ridge, Indian Ocean, shows that both the stratigraphic distribution of species and their frequency patterns (though not actual frequencies or abundances) are correlative in the two areas, supporting their use as stratigraphic and paleoecologic index fossils. Their distributional trends are linked to eustatic sea level changes and to changes in the mixing of surface waters; low frequencies and species turnovers occur during regressive phases when strong circulation of oxygenated waters could lead to the subsequent decline of their oxygen-minimum habitat. The species S. subglobigerum. S. latum. S. globigerum, and S. globulosum succeed one another at intervals averaging 2,5 my from late middle Miocene Zone N15 through Quaternary Zone N23. The new species, Streptochilus suhglobigerum, is described for what was formerly thought to be a stratiraphically lower, disjunct part of the range of S. globigerum. These four species most likely belong to a single phylogenetic lineage as evidenced by some transitional morphologies.

Sediment geochemical evidence for an early-middle Gilbert (early Pliocene) productivity peak in the North Pacific Red Clay Province

Current attempts to understand climatic variability during the early to middle Pliocene require paleoceanographic information from the Pacific and Indian Oceans that may serve to test and/or constrain future circulation models. Ocean Drilling Program (ODP) Sites 885/886 are located in the central subarctic North Pacific at water depths exceeding 5700 m. Recent studies of rock magnetic properties suggest that the fine-grained Fe oxide component in sediment at Sites 885/886 experienced reductive dissolution during the early-middle Gilbert. Because such an interval in the North Pacific Red Clay Province suggests a maximum in the sedimentary flux of organic carbon and/or a minimum in bottom water dissolved O2 concentrations (and hence, a peak change in North Pacific oceanographic conditions), a geochemical investigation was conducted to test the hypothesis. Quaternary sediment at Hole 886B was subjected to an oxyhydroxide removal procedure, and chemical analyses indicate that bulk sediment concentrations of Fe and the Fe/Sc ratio decrease significantly upon reductive dissolution. Downcore chemical analyses of untreated sediment at Hole 886B demonstrate that similar depletions also occur across the proposed interval of reduced sediment. Downcore chemical analyses also indicate that a pronounced increase in the Ba/Sc ratio occurs across the interval. These results are consistent with an interpretation that abyssal sediment of the North Pacific experienced a decrease in redox conditions during the early-middle Gilbert, and that this change in oxidation state was related to a peak in paleoproductivity. If the zenith of late Miocene to middle Pliocene enhanced productivity observed at other Indo-Pacific divergence regions similarly can be constrained to the early-middle Gilbert, there exists an oceanographic boundary condition in which to test future models concerning Pliocene warmth.