Barroco y modernidad : De Maravall a Lezama Lima

En las décadas de 1960 y 1970 convergen varias de las líneas que, desde principios del siglo XX, habían centrado las discusiones en torno del Barroco. Tanto en Europa como en América, y desde diversas disciplinas -filología, ensayo literario, retórica, historia, filosofía, psicoanálisis- el Barroco es visto como un punto de partida de la cultura moderna. En 1975 José Antonio Maravall publica La cultura del Barroco, definida como un concepto histórico, en oposición a la teoría de los eones y las constantes desarrollada por Eugenio d'Ors. Para Maravall el Barroco vincula a España con el surgimiento de la modernidad. Años antes, el cubano José Lezama Lima ve en el Barroco el puente que establece la continuidad entre la cultura española y la americana, lanzándola hacia el futuro. Y en el París de la década de 1970, Severo Sarduy introduce el barroco y neobarroco entre los conceptos que circulan en el intenso intercambio intelectual del momento. Proponemos un abordaje de la cuestión en el cruce de esas líneas diversas

Traducción de poesía: forma, repetición y fantasma en el estudio comparado de traducciones de Emily Dickinson (Silvina Ocampo, Amelia Rosselli)

Este trabajo se inscribe en el proyecto de fundación de una Escuela de Traducción Poética, en la que nos proponemos pensar y practicar nuevos criterios específicos para traducir poesía. Las premisas teóricas de Walter Benjamin y Giorgio Agamben nos sirven para pensar nuestra tarea como una Nueva Filología. Será fundamental en ella el estudio interdisciplinario en el que confluyen filosofía, historia, psicoanálisis, estética y teoría literaria. Una filología absorta en la facticidad y la devoción mágica por los particulares, por el detalle, que Agamben destaca como fundamentales en Benjamin.

Descripción de colecciones de manuscritos : Una propuesta articulada desde la bibliotecología y la archivística

Los documentos manuscritos constituyen fuentes de información primaria, tanto para estudios históricos como para estudios literarios del área de la filología y la crítica genética. La descripción y difusión de este patrimonio constituye una prioridad para las bibliotecas que son depositarias del mismo, dado el creciente interés observado por este tipo de documentos. En pos de contribuir a este objetivo, se brinda un panorama de la normativa vigente aplicable a la descripción de manuscritos. Se enfatizan los beneficios de la descripción normalizada y del empleo de esquemas de metadatos específicos para la difusión de este tipo de material en Internet y se propone su integración a las prácticas bibliotecológicas corrientes

Los objetos escénicos y su funcionalidad en Caballeros de Aristófanes

Nos proponemos estudiar, a partir de un análisis filológico-literario, la comedia Caballeros de Aristófanes, que se puso en escena y obtuvo el primer premio en las Leneas del año 424 a. C. La composición de esta obra es consecuencia directa de los acontecimientos ocurridos en Pilos durante el séptimo año de la Guerra del Peloponeso y resulta una sátira de carácter político en la cual constantemente se ataca a Cleón y se exponen abiertamente los vicios de la administración en Atenas. El objetivo de esta investigación es detectar e indagar los objetos presentes en el universo ficcional para dilucidar la funcionalidad de los mismos en relación con las distintas partes de la obra. Nos centraremos en aquellos que aparecen mencionados en el texto dramático atendiendo a los distintos sentidos que asumen a lo largo de la obra porque los consideramos elementos propulsores del desarrollo de la trama, caracterizadores de personajes, generadores de malos entendidos y poseedores de sentido simbólico

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

La sintaxis griega hoy

Este artículo presenta una discusión sobre algunas nociones que emplea la sintaxis actual del griego clásico. En primer lugar, expone el ámbito que ocupa la sintaxis en el marco de la lingüística y la filología. En segundo y tercer lugar, expone el concepto de enunciado y de sintagma aplicados a la sintaxis del griego clásico. En cuarto lugar, expone brevemente algunos criterios distribucionales empleados para identificar las funciones desempeñadas por los complementos en la oración. A continuación, se exponen los conceptos de papel semántico, noción relacional, función semántica, función sintáctica y función pragmática. La sección 7 resume la estructura de la oración y defiende la idea de que hay que distinguir una serie de niveles o capas en los que se alojan los complementos. El parágrafo final contiene una breve conclusión. El artículo se cierra con una lista de libros sobre sintaxis griega publicados desde 1991 hasta 2003.

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.

Occurrence of tethyan radiolarian species in early Cretaceous sediments of ODP Hole 123-765C in the Northeast Indian Ocean (Fig. 4)

During ODP Leg 123, abundant and well-preserved Neocomian radiolarians were recovered at Site 765 (Argo Abyssal Plain) and Site 766 (lower Exmouth Plateau). Assemblages are characterized by the numerical dominance of a small number of non-tethyan forms and by the scarcity of tethyan taxa. Remarkable contrasts exist between radiolarian assemblages extracted from claystones of Site 765 and reexamined DSDP Site 261, and faunas recovered from radiolarian sand layers, only found at Site 765. Clay faunas are unusual in their low diversity of apparently ecologically tolerant (or solution resistant?), ubiquist species, whereas sand faunas are dominated by non-tethyan taxa. Comparisons with Sites 766 and 261, as well as sedimentological observations, lead to the conclusion that this faunal contrast resulted from a difference in provenance, rather than from hydraulic sorting or selective dissolution. The ranges of 27 tethyan taxa from Site 765 were compared to the tethyan radiolarian zonation by Jud ( 1992 ) by means of the Unitary Associations Method. This calculation allows to directly date the Site 765 assemblages and to estimate the amount of truncation of ranges for tethyan taxa. Over 70% of the already few tethyan species of Site 765, have truncated ranges during the Valanginian-Hauterivian. Radiolarian assemblages recovered from claystones at Sites 765 and 261 in the Argo Basin apparently reflect restricted oceanic conditions during the latest Jurassic-Barremian. Neither sedimentary facies nor faunal associations bear any resemblance to what we know from typical tethyan sequences. We conclude that the Argo Basin was paleoceanographically separated from the Tethys during the Late Jurassic and part of the Early Cretaceous by its position at higher paleolatitudes and/or by enclosing land masses. Assemblages recovered from radiolarian sand layers are dominated by non-tethyan species that are interpreted as circumantarctic. Their first appearance in the late Berriasian-early Valanginian predates the oceanization of the Indo-Australian breakup (M11, late Valanginian), but coincides with a sharp increase in margin-derived pelagic turbidites. The Indo-Australian rift zone and the adjacent margins must have been submerged deeply enough to allow an intermittent influx of circumantarctic cold water into the Argo Basin, creating increased bottom current activity. Cold-water radiolarians carried into the Argo Basin upwelled along the margin, died, and accumulated in radiolarite layers due to winnowing by bottom currents. High rates of faunal change and the sharp increase of bottom current activity are thought to be synchronous with possible pronounced late Berriasian-early Valanginian lowstands in sea level. Hypothetically, both phenomena might have been caused by a tendency to glaciation on the Antarctic-Australian continent, which was for the first time isolated from the rest of Gondwana by oceanic seaways as a result of Jurassic-Early Cretaceous sea-floor spreading. The absence of most typical tethyan radiolarian species during the Valanginian-Hauterivian is interpreted as reflecting a time of strong influx of circumantarctic cold water following oceanization (M 11) and rapid spreading between Southeast India and West Australia. The reappearance and gradual abundance/diversity increase of tethyan taxa, along with the still dominant circumantarctic species are thought to result from overall more equitable climatic conditions during the Barremian-early Aptian and from the establishment of an oceanic connection with the Tethys Ocean during the early Aptian.

Lithogeochemical and isotope (Rb-Sr, Sm-Nd, Pb-Pb whole rock and Lu-Hf zircon) composition of samples from the Shackleton Range, East Antarctica

Three distinct, spatially separated crustal terranes have been recognised in the Shackleton Range, East Antarctica: the Southern, Eastern and Northern Terranes. Mafic gneisses from the Southern Terrane provide geochemical evidence for a within-plate, probably back-arc origin of their protoliths. A plume-distal ridge origin in an incipient ocean basin is the favoured interpretation for the emplacement site of these rocks at c. 1850 Ma, which, together with a few ocean island basalts, were subsequently incorporated into an accretionary continental arc/supra-subduction zone tectonic setting. Magmatic underplating resulted in partial melting of the lower crust, which caused high-temperature granulite-facies metamorphism in the Southern Terrane at c. 1710-1680 Ma. Mafic and felsic gneisses there are characterised by isotopically depleted, positive Nd and Hf initials and model ages between 2100 and 2000 Ma. They may be explained as juvenile additions to the crust towards the end of the Palaeoproterozoic. These juvenile rocks occur in a narrow, c. 150 km long E-W trending belt, inferred to trace a suture that is associated with a large Palaeoproterozoic accretionary orogenic system. The Southern Terrane contains many features that are similar to the Australo-Antarctic Mawson Continent and may be its furthermost extension into East Antarctica. The Eastern Terrane is characterised by metagranitoids that formed in a continental volcanic arc setting during a late Mesoproterozoic orogeny at c. 1060 Ma. Subsequently, the rocks experienced high-temperature metamorphism during Pan-African collisional tectonics at 600 Ma. Isotopically depleted zircon grains yielded Hf model ages of 1600-1400 Ma, which are identical to Nd model ages obtained from juvenile metagranitoids. Most likely, these rocks trace the suture related to the amalgamation of the Indo-Antarctic and West Gondwana continental blocks at ~600 Ma. The Eastern Terrane is interpreted as the southernmost extension of the Pan-African Mozambique/Maud Belt in East Antarctica and, based on Hf isotope data, may also represent a link to the Ellsworth-Whitmore Mountains block in West Antarctica and the Namaqua-Natal Province of southern Africa. Geochemical evidence indicates that the majority of the protoliths of the mafic gneisses in the Northern Terrane formed as oceanic island basalts in a within-plate setting. Subsequently the rocks were incorporated into a subduction zone environment and, finally, accreted to a continental margin during Pan-African collisional tectonics. Felsic gneisses there provide evidence for a within-plate and volcanic arc/collisional origin. Emplacement of granitoids occurred at c. 530 Ma and high-temperature, high-pressure metamorphism took place at 510-500 Ma. Enriched Hf and Nd initials and Palaeoproterozoic model ages for most samples indicate that no juvenile material was added to the crust of the Northern Terrane during the Pan-African Orogeny but recycling of older crust or mixing of crustal components of different age must have occurred. Isotopically depleted mafic gneisses, which are spatially associated with eclogite-facies pyroxenites, yielded late Mesoproterozoic Nd model ages. These rocks occur in a narrow, at least 100 km long, E-W trending belt that separates alkaline ocean island metabasalts and within-plate metagranitoids from volcanic arc metabasalts and volcanic arc/syn-collisional metagranitoids in the Northern Terrane. This belt is interpreted to trace the late Neoproterozoic/early Cambrian Pan-African collisional suture between the Australo-Antarctic and the combined Indo-Antarctic/West Gondwana continental blocks that formed during the final amalgamation of Gondwana.