La figura de Orestes como "Semilla de la Salvación" en Coéforas de Esquilo

En el presente trabajo llevaremos a cabo el análisis de la figura de Orestes como "Semilla de la Salvación" a lo largo de toda la obra desde la perspectiva suministrada por la mirada de Electra y por las palabras del coro. Ya que el personaje de Orestes brinda nombre a la trilogía nos proponemos demostrar que es en la tragedia intermedia, Coéforas, en donde es presentado como un "salvador impulsado por la divinidad". Para tal fin, analizaremos especialmente cómo esta figura resulta comparada con distintos personajes míticos como Altea y Escila (vv. 605), Hermes (vv. 811) y Perseo (vv. 831)

Cuerpo y envejecimiento en el profesor en educación física

En esta exposición haremos referencia a un proyecto de tesina que se está gestando en el marco de la Licenciatura en Educación Física, radicado en el Departamento de Educación Física de la Facultad de Humanidades y Ciencias de la Educación de la Universidad Nacional de La Plata. El envejecimiento y la vejez es una temática que viene siendo estudiada por numerosos campos académicos y profesionales. Al respecto, la Educación Física ha realizado numerosos y valiosos aportes. Sin embargo, en la mayoría de los casos estos estudios se centran en los beneficios biológicos de la práctica de ejercicio físico en la vejez, dejando de lado otras posibles vías de investigación. En consecuencia, en este proyecto de investigación pretendemos indagar en los sentidos y significados que le otorgan a su propio proceso de envejecimiento los Profesores en Educación Física que se desempeñan con adultos mayores. Partimos de una serie de interrogantes: ¿Cómo vivencian los Profesores en Educación Física el propio envejecimiento corporal? ¿Qué piensan sobre el envejecimiento los Profesores en Educación Física que se desempeñan con adultos mayores? ¿Cómo perciben el envejecimiento a medida que transcurre el tiempo de desempeño profesional? ¿Qué pensamos acerca del envejecimiento? ¿Cuáles son las estrategias de cuidados que utilizamos? En ese sentido, vamos a abordar algunos estudios que han realizado una primera aproximación a la temática y nos dieron el sustento teórico para encauzarnos en este tema. Retomando lo descripto en párrafos precedentes, con esta investigación de corte cualitativo, intentaremos definir y problematizar los conceptos de cuerpo, envejecimiento y vejez, en especial referencia a los Profesores en Educación Física que se desempeñan en prácticas corporales con adultos mayores. En esta ponencia, sólo realizaremos una exposición del proyecto de Tesina antes mencionado, ya que se encuentra en la etapa intermedia de conformación

Late Albian foraminiferal carbon and oxygen isotope data and biostratigraphic datums from ODP holes 171-1050C and 171-1052E

A late Albian-early Cenomanian record (~103.3 to 99.0 Ma), including organic-rich deposits and a d13C increase associated with oceanic anoxic event 1d (OAE 1d), is described from Ocean Drilling Program sites 1050 and 1052 in the subtropical Atlantic. Foraminifera are well preserved at these sites. Paleotemperatures estimated from benthic d18O values average ~14°C for middle bathyal Site 1050 and ~17°C for upper bathyal Site 1052, whereas surface temperatures are estimated to have ranged from 26°C to 31°C at both sites. Among planktonic foraminifera, there is a steady balance of speciation and extinction with no discrete time of major faunal turnover. OAE 1d is recognized on the basis of a 1.2 per mill d13C increase (~100.0-99.6 Ma), which is similar in age and magnitude to d13C excursions documented in the North Atlantic and western Tethys. Organic-rich "black shales" are present throughout the studied interval at both sites. However, deposition of individual black shale beds was not synchronous between sites, and most of the black shale was deposited before the OAE 1d d13C increase. A similar pattern is observed at the other sites where OAE 1d has been recognized indicating that the site(s) of excess organic carbon burial that could have caused the d13C increase has (have) yet to be found. Our findings add weight to the view that OAEs should be chemostratigraphically (d13C) rather than lithostratigraphically defined.

Ni surrealistas ni concretos. Tensiones vanguardistas en el invencionismo

¿Por qué el invencionismo poético, a pesar de haber recepcionado el arte concreto unos años antes que Brasil, no tuvo la natural deriva hacia la poesía visual, que en Argentina no terminó de imponerse sino hasta las primeras publicaciones de Antonio Vigo -un artista plástico- a mediados de la década de 1960? Aunque el movimiento recibió una fuerte influencia surrealista, la respuesta sin duda no se agota en esa vía. El origen conjunto y el vínculo posterior del invencionismo con el arte concreto argentino explican muchas de las derivas estéticas, que lo llevaron a experimentar con las materias fónica y semántica, centrando su ataque en la metáfora -y no el verso-, porque consideraban que era esta figura la que mantenía la función representativa del lenguaje y sostenía el ideal poético instituido. Ese enfoque de la experimentación los acercó a ciertos aspectos del surrealismo, sin soslayar la base concreta que había originado el movimiento. Este trabajo procura dar cuenta de estas tensiones, como una forma de dar entidad al invencionismo y pensarlo en una zona intermedia entre los dos movimientos contrapuestos

La escala local, desde la periferia. Análisis de la industria de maquinaria agrícola en Las Parejas (provincia de Santa Fe, Argentina) relacionada con su contexto dentro de la economía argentina

El trabajo analiza las posibilidades que tienen las estrategias de desarrollo local, inspiradas en realidades como la europea, de ser aplicadas del mismo modo en países de la periferia como la Argentina. En esta descripción se diferencian el contexto global-nacional y local. Se realiza el análisis a partir de los discursos geográficos y también sociológicos y económicos que, a partir de la experiencia italiana, francesa, etc., relativizan la escala nacional como eje del análisis y se enfocan en el surgimiento de lo local como escala de referencia. Se utiliza el ejemplo de las empresas de maquinaria agrícola de la ciudad argentina de Las Parejas, provincia de Santa Fe, para graficar cómo una ciudad intermedia puede generar proyectos asociativos que ayudan a los actores a enfrentar el contexto, pero que éste sigue siendo una variable determinante de la performance empresaria y de la vida de los tejidos productivos locales.

El rol del amante anónimo en el discurso de Sócrates-Diotima

La posición intermedia del éros en el Banquete organiza los dos polos de la relación erótica (amante-amado) en función de la falta que moviliza al amante (erastés). El filósofo interroga en virtud de su deseo por alcanzar la sabiduría (philosohía), aquel otro polo ocupado por el objeto de deseo (erómenos): la idea de Belleza. En el marco del discurso que Sócrates pone en boca de Diotima aparece un amante anónimo (tis) que también interroga sobre el éros (204d, 204e). En nuestro trabajo nos ocupamos de analizar el rol del amante anónimo en el discurso de Sócrates-Diotima

Diatoms in Paleocene sediments of the southwestern South Atlantic

The taxonomy and stratigraphy of pelagic Paleocene diatoms from ODP Sites 698, 700, and 702 and DSDP Site 524 in the South Atlantic and DSDP Site 214 in the Indian Ocean are presented, as well as paleogeographic and paleoecologic implications. Eleven new species and one new variety are described and one new combination is proposed: Coscinodiscus cruxii sp. nov. Grunowiella palaeocaenica var. alternans var. nov. Hemiaulusl beatus sp. nov. Hemiaulusl ciesielskii sp. nov. Hemiaulusl conicus sp. nov. Hemiaulus kristoffersenii sp. nov. Hemiaulus nocchiae sp. nov. Hemiaulusl oonkii sp. nov. Hemiaulusl velatus sp. nov. Triceratium gombosii sp. nov. Trochosira gracillima comb. nov. Trochosira marginata sp. nov. Trochosira radiata sp. nov. Hole 700B provides one of the most continuous diatomaceous Paleocene profiles known. Stratigraphic ranges of diatom species from this and other Southern Hemisphere sites are calibrated against calcareous microfossil zones. The first-appearance datums of Triceratium gombosii, Hemiaulus incurvus, and Triceratium mirabile in Paleocene deep-sea sediments are useful for regional stratigraphic correlations. Quantitative analysis of the biosiliceous microfossil groups (diatoms, silicoflagellates, radiolarians, and archaeomonadaceae) shows that preservation of diatoms is confined primarily to the upper Paleocene (planktonic foraminifer Zones P3 and P4 and calcareous nannofossil Zones upper NP5 to lower NP9). In the lower Paleocene only short intervals in Hole 700B are diatomaceous. A correlation between the degree of silica diagenesis and the calcium carbonate content of the sediment is not obvious. Diatom species analysis reflects changes in the paleoenvironment between island-related upwelling conditions with highly diverse and well-preserved diatom assemblages and less productive periods resulting in less wellpreserved diatom assemblages with a higher content of robust neritic diatoms.

Macrobenthos from the Novaya Zemlya Trough, Kara Sea

During Cruise 54 of R/V Akademik Mstislav Keldysh macrobenthos of the Novaya Zemlya Trough was studied with use of a Sigsby trawl along a submeridional transect near 75°30'N at depth range from 68 to 362 m. In total 140 species of bottom animals were found. Relative role of taxons was assessed using three parameters: abundance, biomass, and energy flow. Similarity of the parameters was used for comparison of samples. New material greatly contributes to data on composition of fauna and structure of communities of the studied region. It was revealed that small scyphozoid polyps and sipunculoids play an important role in the trough's community. Presence of a community dominated by Ophiocten sericeum (with important role of small bivalves) was revealed for the first time not only at the eastern by also at the western slope of the Novaya Zemlya Trough. The sharpest changes in composition and structure of the bottom community were confined to a zone of transition from the trough floor to the slope. These changes are determined by specificity of the macrorelief (of the floor and slope), composition of ground (soft brown silts abound in rhizopods and dense gray silts with admixture of pebbles), and possibly by hydrodynamic processes near the bottom.

Palynology on sediment profile Tso Kar in Ladakh

Palynological investigation of a 410 cm long core section from Tso Kar (33°10'N, 78°E, 4527 m a.s.l.), an alpine lake situated in the arid Ladakh area of NW India at the limit of the present-day Indian summer monsoon, was performed in order to reconstruct post-glacial regional vegetation and climate dynamics. The area was covered with alpine desert vegetation from ca. 15.2 to 14 kyr BP (1 kyr=1000 cal. years), reflecting dry and cold conditions. High influx values of long-distance transported Pinus sylvestris type pollen suggest prevailing air flow from the west and northwest. The spread of alpine meadow communities and local aquatic vegetation is a weak sign of climate amelioration after ca. 14 kyr BP. Pollen data (e.g. influx values of Pinus roxburghii type and Quercus) suggest that this was due to a strengthening of the summer monsoon and the reduced activity of westerly winds. The further spread of Artemisia and species-rich meadows occurred in response to improved moisture conditions between ca. 12.9 and 12.5 kyr BP. The subsequent change towards drier desert-steppe vegetation likely indicates more frequent westerly disturbances and associated snowfalls, which favoured the persistence of alpine meadows on edaphically moist sites. The spread of Chenopodiaceae-dominated vegetation associated with an extremely weak monsoon occurred at ca. 12.2-11.8 kyr BP during the Younger Dryas interstadial. A major increase in humidity is inferred from the development of Artemisia-dominated steppe and wet alpine meadows with Gentianaceae after the late glacial/early Holocene transition in response to the strengthening of the summer monsoon. Monsoonal influence reached maximum activity in the Tso Kar region between ca. 10.9 and 9.2 kyr BP. The subsequent development of the alpine meadow, steppe and desert-steppe vegetation points to a moderate reduction in the moisture supply, which can be linked to the weaker summer monsoon and the accompanying enhancement of the winter westerly flow from ca. 9.2 to 4.8 kyr BP. The highest water levels of Tso Kar around 8 kyr BP probably reflect combined effect of both monsoonal and westerly influence in the region. An abrupt shift towards aridity in the Tso Kar region occurred after ca. 4.8 kyr BP, as evidenced by an expansion of Chenopodiaceae-dominated desert-steppe. Low pollen influx values registered ca. 2.8-1.3 kyr BP suggest scarce vegetation cover and unfavourable growing conditions likely associated with a further weakening of the Indian Monsoon.

Abundance and biomass of the benthic infauna of the North Sea

In 1986 participants of the Benthos Ecology Working Group of ICES conducted a synoptic mapping of the infauna of the southern and central North Sea. Together with a mapping of the infauna of the northern North Sea by Eleftheriou and Basford (1989, doi:10.1017/S0025315400049158) this provides the database for the description of the benthic infauna of the whole North Sea in this paper. Division of the infauna into assemblages by TWINSPAN analysis separated northern assemblages from southern assemblages along the 70 m depth contour. Assemblages were further separated by the 30, 50 m and 100 m depth contour as well as by the sediment type. In addition to widely distributed species, cold water species do not occur further south than the northern edge of the Dogger Bank, which corresponds to the 50 m depth contour. Warm water species were not found north of the 100 m depth contour. Some species occur on all types of sediment but most are restricted to a special sediment and therefore these species are limited in their distribution. The factors structuring species distributions and assemblages seem to be temperature, the influence of different water masses, e.g. Atlantic water, the type of sediment and the food supply to the benthos.

List of plant species found on Victoria Island

While engaged in geoecological field work on Victoria Island, 277 new plants could be recorded for the vicinities of Holman, Cambridge Bay, Wellington Bay, Mt. Pelly, Richardson Islands, Hadley Bay, and Minto lnlet; 8 of them were new for Victoria Island, 6 for the western Canadian arctic archipelago.

Calcareous nannofossil biostratigraphy of the central East Pacific Rise

During Leg 92 of the Deep Sea Drilling Project, sediments containing calcareous nannofossils of latest Oligocene to Holocene age were recovered from 14 holes at six sites (597 to 602) along the East Pacific Rise. The combined sections yield a virtually complete record for the region, with a compressed upper Miocene to Pleistocene interval. The nannofossil content of 14 U.S.N.S. Eltanin piston cores from the study area were also examined in order to supplement data generated during Leg 92. Two taxonomically new combinations are presented: Sphenolithus umbellus and Pontosphaera segmenta. Assemblages of calcareous nannofossils juxtaposed in reversed stratigraphic order within the upper Miocene provide strong evidence for downslope transport of sediments along the East Pacific Rise during the Messinian. Narrow bands of dark metalliferous sediment of coccolith Zone CN8b alternate with normal light-colored, in situ, pelagic sequences of Zone CN9b. This may indicate more vigorous bottom current activity between 5.40 and 6.70 Ma.

Calcareous nannofossils from the Sumisu Rift and Izu-Bonin Forearc Basin

During Ocean Drilling Program Leg 126, we recovered three expanded Pleistocene sections from the active backarc rift (Sumisu Rift) and three expanded Oligocene-Miocene sections from the forearc basin of the Izu-Bonin volcanic island arc. Quantitative analysis of the Pleistocene nannofossils revealed five major assemblages between 0 and LO Ma: Assemblage 1 (Holocene-0.085 Ma) contains dominant Emiliania huxleyi; Assemblage 2 (ca. 0.085-0.275 Ma) contains dominant small Gephyrocapsa and common E. huxleyi and Gephyrocapsa oceanica; Assemblage 3 (ca. 0.275-0.6 Ma) contains dominant Gephyrocapsa caribbeanica; Assemblage 4 (ca. 0.6-0.9 Ma) contains a peak abundance of small Gephyrocapsa in the middle part, and dominant occurrences of two types of G. caribbeanica in the lower and upper parts; and Assemblage 5 (ca. 0.9-1.0 Ma) contains dominant small Gephyrocapsa and common G. caribbeanica and Reticulofenestra asanoi. These assemblages are largely synchronous with similar assemblages recognized from tropical and subtropical regions, and can be used for finer subdivision of the Pleistocene than that based on standard Pleistocene nannofossil datums. The Oligocene-Miocene sections contain several hiatuses: up to 3 m.y. may be missing from the uppermost Oligocene (Zone CP19) at Sites 792 and 793; all of Zone CN2 is missing at Sites 792 and 793; part of Zone CN3 and all of Zone CN4 are missing at Site 792. Biochronology of several nannofossil datums at Leg 126 sites indicate that Sphenolithus distentus, Sphenolithus ciperoensis, Cyclicargolithus floridanus, and Discoaster kugleri have diachronous occurrences compared with other sites in the western Pacific Ocean and Philippine Sea.