Reseña de: Ezcurra, A.M. (2011). Igualdad en Educación Superior : Un desafío mundial. Los Polvorines: Universidad Nacional de General Sarmiento - IEC/CONADU, 108 pp.

Fil: Marchese, Elisa. Universidad Nacional de La Plata. Facultad de Humanidades y Ciencias de la Educación; Argentina.

Procedimientos servianos de lectura acerca de los certámenes fúnebres en Eneida V : La naumaquia (vv. 104-285)

La figura de Servio y su comentario a la obra virgiliana constituye la summa opera de la tradición escolar tardoantigua; su importancia reside porque es el resultado de numerosas estratificaciones que recogen diversos abordajes exegéticos. Al tratarse de un comentario ?continuo?, los Commentarii servianos comprenden un conjunto de saberes que examinan la obra literaria desde la perspectiva histórica y de todo aquello que se relacionaba con esta. A partir de esta mirada lectora, la comunicación se centrará en el análisis que Servio realiza sobre la naumaquia del libro V de la Eneida (vv. 104-285), donde el texto base expone una secuencia narrativa caracterizada por epicismos homéricos y pos-homéricos que el gramático desarticula, privilegiando aspectos como el lingüístico, retórico, fabuloso y histórico-arqueológico. Asimismo, se comprobará que el certamen virgiliano constituye un pretexto para instalar un nuevo contexto que garantice la continuidad del sistema burocrático imperial

Procedimientos servianos de lectura acerca de los certámenes fúnebres en Eneida V : La naumaquia (vv. 104-285)

La figura de Servio y su comentario a la obra virgiliana constituye la summa opera de la tradición escolar tardoantigua; su importancia reside porque es el resultado de numerosas estratificaciones que recogen diversos abordajes exegéticos. Al tratarse de un comentario ?continuo?, los Commentarii servianos comprenden un conjunto de saberes que examinan la obra literaria desde la perspectiva histórica y de todo aquello que se relacionaba con esta. A partir de esta mirada lectora, la comunicación se centrará en el análisis que Servio realiza sobre la naumaquia del libro V de la Eneida (vv. 104-285), donde el texto base expone una secuencia narrativa caracterizada por epicismos homéricos y pos-homéricos que el gramático desarticula, privilegiando aspectos como el lingüístico, retórico, fabuloso y histórico-arqueológico. Asimismo, se comprobará que el certamen virgiliano constituye un pretexto para instalar un nuevo contexto que garantice la continuidad del sistema burocrático imperial

Cenozoic ostracoda of ODP Leg 104 holes

Ostracodes are less common than might be normally expected at Sites 642, 643, and 644, perhaps pointing to the fact that the marine habitat below the overlying Pleistocene ice covers was a severe environment. This explanation, however, would not apply to the Pliocene and Miocene deposits from which ostracodes are just as poorly represented. In the latter case the Iceland-Faeroe Ridge might still have acted as a submerged barrier that did not allow an open ocean circulation of bottom waters. Thus the barrier presumably prevented an exchange of cold subarctic bottom water with that of the open Atlantic and therefore benthic deep-sea migration from the south was impeded. Some Quaternary species are, for the first time, recorded to extend to the Pliocene and/or Miocene.

Neogene magneto- and biostratigraphy of ODP Leg 104 holes

Silicoflagellate assemblages of ODP Leg 104 Neogene sequences are the basis of an interpretation of changes in the Neogene paleoenvironment of the Norwegian Sea. Fluctuations in the percentages of temperature and nutrient-sensitive taxonomic groups document major changes in sea-surface conditions. A brief, but distinct, cooling event occurred at 18.0-17.5 Ma which resulted in the disappearance of Naviculopsis. Following this early Miocene cooling a long period of increasing surface-water temperature occurred, leading up to a thermal high in the early middle Miocene (14.0 Ma). The early late Miocene (10.0-9.0 Ma) was distinctly cooler than the middle Miocene, but warmer than the remainder of the Neogene. Conditions between 13.0 and 10.0 Ma are unrecorded because of a regional hiatus, which is the earliest evidence for an end to the more temperate and stable conditions of the early to middle middle Miocene. A major plunge in temperatures occurred between 8.5 and 7.4 Ma and during the remainder of the late Miocene and Pliocene; from 7.4 to 2.65 Ma subpolar conditions prevailed. Silicoflagellates disappeared, except for sporadic occurrences, at 2.64 Ma with the beginning of dominant glacial sedimentation. Biogenic opal is absent in sediments younger than 0.76 Ma, indicating the dominance of glacial conditions with extensive sea ice.

Dinoflagellates of ODP Leg 104 holes

Dinoflagellate cysts, pollen, and spores were studied from 78 samples of the Eocene to Miocene section of ODP Site 643 at the outer Wring Plateau. Dinoflagellate cysts ranging from less than 1,000 to rarely over 30,000 per gram of sediment in the Paleogene, and generally between 50,000 and 100,000 in the Miocene were present. The shift to conspicuously higher cyst frequencies takes place in the lowermost Miocene section and appears to reflect increased cyst recruitment rather than a change in sedimentation rate. Of the 179 dinoflagellate cyst forms whose ranges were recorded, 129 are known species. Fifteen assemblage zones have been recognized, although the upper Eocene is missing and no substantial lower Eocene was recorded at Site 643. Norwegian Sea and Rockall Plateau zonations were compared with this study. Detailed correlation with existing onshore section zonations was difficult because key zonal species are inadequately represented; however, the middle to upper Miocene zonation established for Denmark is applicable. Pollen and spores occur with relatively low frequencies, and palynodebris is generally absent, in contrast to the observations from DSDP Leg 38. Thirty-nine samples from Eocene to Miocene sediments at Site 642 were studied and correlated with Site 643. A lower Eocene cyst assemblage present in Hole 642D is older than the questionably lower Eocene assemblage from Site 643. Site 642 has a lower Eocene to lower Miocene hiatus.

Ice-rafted debris of Late Cenozoic sediments from ODP Leg 104 holes

The abundance and composition of the upper Cenozoic terrigenous coarse-sand fraction (250 µm-2 mm) at ODP Sites 642, 643, and 644 were investigated to date the onset of significant ice-rafting in the Norwegian Sea, establish the regional chronology of ice-rafting, and determine the relative importance of global vs. regional controls on ice-rafting in this area. The first input of ice-rafted debris (IRD) occurs at approximately 2.9 Ma, with significant ice-rafting beginning at about 2.5 Ma. IRD abundances increase significantly in sediments younger than 0.9 Ma at all three holes, indicating climatic deterioration in the late Pleistocene. Differences in the timing of this IRD increase between holes result from regional patterns of IRD supply and surface circulation. Variations in IRD sources and dispersal patterns may also explain the slightly higher background level of IRD abundance at Hole 642B, a seaward site. Major peaks in the generalized IRD records from the Norwegian Sea are tentatively correlated to glacial stages or glacial-to-interglacial transitions in the globally defined oxygen isotope record. This correlation indicates the effect of global conditions on the regional climate of the Norwegian Sea, although the detailed IRD records at these sites are also affected by local/regional processes (e.g., circulation patterns and source area differences).