¿Mercosur o Alca? : Clase dominante, gobierno e inserción regional en los inicios del Kirchnerismo

El objetivo de este trabajo es analizar la relación entre gobierno, corporaciones empresarias de la clase dominante y los proyectos MERCOSUR y ALCA en los inicios del gobierno de Kirchner. La hipótesis principal es que los cambios en la inserción regional de Argentina desde 2003 (reconstrucción del MERCOSUR y rechazo al ALCA), tuvieron entre una de sus causas a las acciones de corporaciones como la Unión Industrial Argentina (UIA) y la Sociedad Rural Argentina (SRA). Como afirma Katz (2006) aquella reconfiguración regional, además de estar influenciada por las protestas sociales antineoliberales, también respondió a la demanda de una diferente inserción regional por parte de las clases dominantes locales. Mediante el análisis de la prensa escrita y de documentación de las corporaciones, observaremos los posicionamientos sobre el ALCA y el MERCOUSR, el tipo de intervención del gobierno que reclaman y por qué apoyan o rechazan las negociaciones entre 2003 y 2004, en la reunión de la Ronda Doha de Cancún de la Organización mundial de Comercio (OMC) y en las Minicumbres del ALCA de Miami y Puebla, donde quedaron trabadas las negociaciones del ALCA y se produjo la reorientación del MERCOSUR

Educación física Argenmex : Temas y posiciones

Tabla de contenidos: La Educación Física, una polifonía barroca / Román Césaro. Algunas tensiones en el campo de la Educación Física en Argentina / Carlos Carballo. Cuerpo: territorio de impresiones experienciales / Evelyn I. Rodríguez Morrill, Leticia Villarreal Caballero. Rasgos de personalidad en nadadores de la Universidad de Colima / Sara Lidia Pérez Ruvalcaba, Paulina León Govea, Luis Gustavo González Carballido. De los diseños de investigación a una epistemología de la Educación Física / Juan Pablo Villagrán. La pasión por la investigación en Educación Física / Gabriel Cachorro. La Educación Física en México. Rompiendo Paradigmas / Héctor Manuel Icaza Campa. Concepciones de ciencia que construyen los estudiantes de Educación Física y Deporte / Ciria Margarita Salazar C., Emilio Gerzaín Manzo Lozano, Maricela Larios Torres. Etica, estética y cinética. El deporte en tres dimensiones / Martín Scarnatto. Abordajes sobre la práctica del rugby: significados culturales en torno a la construcción de masculinidad / Juan Branz. Fútbol, Sociedad y Política en La Provincia Colimense / Ciria Margarita Salazar C., Emilio Gerzaín Manzo Lozano, Samuel Martínez López. Uso del Tiempo Libre en alumnos de Educación Secundaria / Mayra Puente González, Minerva Liliana Sandoval Jalomo, Rossana Tamara Medina Valencia. Actividad física y salud... prioridades de nuestro tiempo / Osvaldo Ron. Las relaciones entre la Educación Física y Salud / Miriam Marracino. El impacto de la Actividad Física sobre la Resistencia a la Insulina en la Adolescencia / Julio Alejandro Gómez Figueroa, Sergio Hernández López, Alfredo Quintana Rivera. La salud físico-emocional de los profesores de la Universidad de Colima / Jonás Larios Deniz, Maricela Larios Torres, Rodolfo Rangel Alcantar. Cuando la mirada y sus efectos están más allá (o más acá) de la discapacidad / Sandra Katz. La Formación profesional en Educación Física sobre la Discapacidad / Laura Sosa. Barreras para la práctica de actividades físico-deportivas en escolares / Oswaldo Ceballos Gurrola, Rosa Elena Medina Rodríguez, Fernando Ochoa Ahmed. La actuación del profesor de educación física en la integración educativa de alumnos con necesidades educativas especiales asociados a discapacidad motriz / Alma Patricia Cruz Gómez, Isis Cruz Ursúa, Martín Gerardo Vargas Elizondo.

El estado del peso corporal en sujetos con retraso mental en un centro de día

La investigación del peso corporal en sujetos con retraso mental (RM) ha sido emparentada con la obesidad y, en menor medida, con el bajo peso. Con el motivo de determinar el estado del peso corporal y establecer si existen desviaciones respecto al peso normal, es que se realizó un estudio con diseño descriptivo transversal teniendo en cuenta las diferentes variables que afectan a sujetos con retraso mental, tomando como indicadores de evaluación el Índice de Masa Corporal y el IMC para la Edad, recolectándose los datos en concurrentes a un Centro de Día. Según este trabajo, el estado de peso corporal en sujetos con RM varía entre el peso normal y el exceso de peso en forma de sobrepeso y de obesidad, en menor medida el bajo peso. Los grupos de mujeres, individuos mayores de edad, sujetos con capacidad ambulatoria, discapacidad mental, menor grado de retraso mental, poseen mayor riesgo de sobrepeso y obesidad según los porcentuales obtenidos; mientras que los conjuntos de sujetos menores de 20 años, discapacidad motora, mayor grado de retraso mental, parálisis cerebral, individuos cuyo desplazamiento ambulatorio es nulo o casi nulo, y en menor medida varones y personas con discapacidad visual, presentaron tendencia al peso normal y el bajo peso como grupo. En los sujetos que recibían medicación su peso corporal se distribuía en valores proporcionales entre los diferentes estados. Nuevas investigaciones que muestren preocupación por las personas con discapacidad intelectual favorecerán la calidad de vida y el desenvolvimiento de este conjunto en la sociedad

La voz de las minorías culturales y la enseñanza de lenguas extranjeras

En los últimos diez años, la enseñanza de lenguas extranjeras ha experimentado un cambio de paradigma en nuestro país, el cual reconoce los ejes de interculturalidad y ciudadanía como centrales, tanto para la enseñanza de las lenguas extranjeras como para la formación integral de los niños. En relación con estos ejes, en este trabajo, nos proponemos explorar la riqueza lingüística y cultural que ofrecen las manifestaciones artísticas que se originan en el seno de las minorías culturales para la enseñanza de lenguas extranjeras en nuestro ámbito de trabajo. Más específicamente, se otorgará atención a la producción de la poeta chicana Pat Mora y de la artista cinematográfica canadiense de origen judío Sharon Katz y se revisarán las estrategias que pueden elaborarse para implementar el uso de estos materiales innovadores en la clase inglés como lengua extranjera

Bibliotecas accesibles para personas con discapacidad visual : Un estudio de caso en la Universidad Nacional de La Plata

En la actualidad, existen diversas barreras a las cuales se enfrentan las personas con discapacidad visual, no sólo físicas, sino también de acceso a la información, quedando excluidas del sistema educativo. Este trabajo de investigación tiene como objetivo conocer en qué situación se encuentran hoy las bibliotecas universitarias de La Plata para brindar servicios accesibles a personas con discapacidad visual. A tal fin se aplicó una encuesta por e-mail a cada responsable de las unidades de información, con el propósito de realizar un relevamiento y recolectar información que permita analizar en dicha situación. Para complementar la encuesta se realizaron dos entrevistas semi estructuradas en profundidad. La primera a la Licenciada Sandra Katz [Directora de la Comisión sobre Discapacidad], en la que se le preguntó por las políticas universitarias llevadas a cabo por la UNLP para personas con discapacidad visual y su opinión en el plano nacional e internacional acerca de estas cuestiones. La segunda a la Licenciada Ivana Harari [Miembro de Laboratorio de Investigación en Nuevas Tecnologías]. Las preguntas de la entrevista estuvieron orientadas a conocer si los sitios web de las Bibliotecas de las Facultades de la UNLP eran accesibles, cuáles eran las barreras más habituales encontradas en ellos y qué políticas se estaban llevando a cabo con respecto a este tema. Por último, se elaboró una propuesta para la organización de servicios accesibles para personas con discapacidad visual para bibliotecas universitarias

Geochemistry and pyrolysis at DSDP Hole 77-535

There are substantial differences in the character of organic matter contained in the Pleistocene and Cretaceous sedimentary sequences of DSDP Site 535. The argillaceous Pleistocene section contains type III, gas-prone organic matter whereas the calcareous Cretaceous section is dominated by type II, oil-prone organic matter. A more detailed investigation of the Cretaceous section reveals that the finely laminated limestones of Valanginian to Barremian age are of good to excellent source quality. The indigenous organic matter contained within this organically rich section is thermally immature, not having undergone sufficient thermal diagenesis for the generation and expulsion of hydrocarbons. Within this stratigraphic section, however, staining by mature hydrocarbons was detected. These stains are associated with a fractured interval. These fractures may in turn represent potential migration pathways.

Organic geochemical characteristics at DSDP Holes 76-534A and 44-391C

Pyrolysis assay, bitumen analysis, and elemental analysis of kerogen were used to characterize the organic matter of selected core samples from Hole 534A (Leg 76) and Hole 391C (Leg 44) on the Blake-Bahama Plateau. The organic matter throughout the stratigraphic section appears to be principally of a terrestrial origin. The data from several isolated horizons in the Hatteras and Blake-Bahama Formations imply the presence of significant quantities of autochthonous marine organic matter. However, these horizons appear so limited that they cannot be considered potential liquid hydrocarbon source rocks. All the analyzed samples are immature and have not evolved sufficiently to enter into the main stage of hydrocarbon generation. The temporal and spatial restrictions of strata rich in marine organic matter suggest that they do not represent major expansions and contractions of anoxic bottom-water masses, but represent limited occurrences of anoxic conditions.

Cenozoic oxygen isotopic values for benthic foraminifera from DSDP and ODP low and high latitude marine sediment cores

The climate during the Cenozoic era changed in several steps from ice-free poles and warm conditions to ice-covered poles and cold conditions. Since the 1950s, a body of information on ice volume and temperature changes has been built up predominantly on the basis of measurements of the oxygen isotopic composition of shells of benthic foraminifera collected from marine sediment cores. The statistical methodology of time series analysis has also evolved, allowing more information to be extracted from these records. Here we provide a comprehensive view of Cenozoic climate evolution by means of a coherent and systematic application of time series analytical tools to each record from a compilation spanning the interval from 4 to 61 Myr ago. We quantitatively describe several prominent features of the oxygen isotope record, taking into account the various sources of uncertainty (including measurement, proxy noise, and dating errors). The estimated transition times and amplitudes allow us to assess causal climatological-tectonic influences on the following known features of the Cenozoic oxygen isotopic record: Paleocene-Eocene Thermal Maximum, Eocene-Oligocene Transition, Oligocene-Miocene Boundary, and the Middle Miocene Climate Optimum. We further describe and causally interpret the following features: Paleocene-Eocene warming trend, the two-step, long-term Eocene cooling, and the changes within the most recent interval (Miocene-Pliocene). We review the scope and methods of constructing Cenozoic stacks of benthic oxygen isotope records and present two new latitudinal stacks, which capture besides global ice volume also bottom water temperatures at low (less than 30°) and high latitudes. This review concludes with an identification of future directions for data collection, statistical method development, and climate modeling.

Stable carbon and oxygen isotope record of benthic foraminifera from Paleocene-Eocene sediments

A major change in Cenozoic deep-sea benthic foraminifera occurred in the Atlantic, Indian, and Pacific oceans near the Paleocene/Eocene boundary. Benthic foraminiferal abundance changes began at about 61.5 Ma at Pacific Deep Sea Drilling Project (DSDP) Site 577. A major extinction event followed at 58-57 Ma (between Zones P6a and P6b), and a series of first appearances continued until circa 55.5 Ma (Zone P6c). These faunal changes occurred during a 6°C warming of Pacific bottom water and may indicate that the primary cause was changing temperature. Other potential causes of the faunal turnover include global changes in surface ocean productivity and changing bottom water source regions. Comparison of benthic and planktonic delta13C records requires no change in the ratio of oceanic phosphorous to carbon during the late Paleocene to early Eocene, which weakens the case for (but does not disprove) a change in surface ocean productivity at this time. Interbasinal comparisons of benthic foraminiferal delta13C records document that water with high delta13C values filled the Cape Basin during the late Paleocene and possibly the early Eocene (circa 61-57 Ma), but apparently did not extend into the western basins of the Atlantic. This pattern suggests a supply of Antarctic source water for the Cape Basin and possible tectonic isolation of the western Atlantic basins during at least part of the late Paleocene. Carbon isotope comparisons show that bottom water supply to the Cape Basin was reduced in the early Eocene. Eolian grain size data suggest that a decrease in zonal wind intensity occurred at the end of the Paleocene. These late Paleocene climatic changes (bottom water warming and decreased wind intensity) correspond with evidence for an important global tectonic reorganization and extensive subaerial volcanism, which may have contributed to climatic warming through increased supply of CO2.

Benthic foraminiferal biofacies and stable isotopic record of St. Stephens Quarry, Alabama

We integrate upper Eocene-lower Oligocene lithostratigraphic, magnetostratigraphic, biostratigraphic, stable isotopic, benthic foraminiferal faunal, downhole log, and sequence stratigraphic studies from the Alabama St. Stephens Quarry (SSQ) core hole, linking global ice volume, sea level, and temperature changes through the greenhouse to icehouse transition of the Cenozoic. We show that the SSQ succession is dissected by hiatuses associated with sequence boundaries. Three previously reported sequence boundaries are well dated here: North Twistwood Creek-Cocoa (35.4-35.9 Ma), Mint Spring-Red Bluff (33.0 Ma), and Bucatunna-Chickasawhay (the mid-Oligocene fall, ca. 30.2 Ma). In addition, we document three previously undetected or controversial sequences: mid-Pachuta (33.9-35.0 Ma), Shubuta-Bumpnose (lowermost Oligocene, ca. 33.6 Ma), and Byram-Glendon (30.5-31.7 Ma). An ~0.9 per mil d18O increase in the SSQ core hole is correlated to the global earliest Oligocene (Oi1) event using magnetobiostratigraphy; this increase is associated with the Shubuta-Bumpnose contact, an erosional surface, and a biofacies shift in the core hole, providing a first-order correlation between ice growth and a sequence boundary that indicates a sea-level fall. The d18O increase is associated with a eustatic fall of ~55 m, indicating that ~0.4 per mil of the increase at Oi1 time was due to temperature. Maximum d18O values of Oi1 occur above the sequence boundary, requiring that deposition resumed during the lowest eustatic lowstand. A precursor d18O increase of 0.5 per mil (33.8 Ma, midchron C13r) at SSQ correlates with a 0.5 per mil increase in the deep Pacific Ocean; the lack of evidence for a sea-level change with the precursor suggests that this was primarily a cooling event, not an ice-volume event. Eocene-Oligocene shelf water temperatures of ~17-19 °C at SSQ are similar to modern values for 100 m water depth in this region. Our study establishes the relationships among ice volume, d18O, and sequences: a latest Eocene cooling event was followed by an earliest Oligocene ice volume and cooling event that lowered sea level and formed a sequence boundary during the early stages of eustatic fall.

Middle Eocene bulk sediment, benthic and planktic foraminiferal stable isotope values, and relative weight percent CaCO3 content from ODP Site 207-1260

Major ice sheets were permanently established on Antarctica approximately 34 million years ago, close to the Eocene/ Oligocene boundary, at the same time as a permanent deepening of the calcite compensation depth in the world's oceans. Until recently, it was thought that Northern Hemisphere glaciation began much later, between 11 and 5million years ago. This view has been challenged, however, by records of ice rafting at high northern latitudes during the Eocene epoch and by estimates of global ice volume that exceed the storage capacity of Antarctica at the same time as a temporary deepening of the calcite compensation depth 41.6 million years ago. Here we test the hypothesis that large ice sheets were present in both hemispheres 41.6 million years ago using marine sediment records of oxygen and carbon isotope values and of calcium carbonate content from the equatorial Atlantic Ocean. These records allow, at most, an ice budget that can easily be accommodated on Antarctica, indicating that large ice sheets were not present in the Northern Hemisphere. The records also reveal a brief interval shortly before the temporary deepening of the calcite compensation depth during which the calcite compensation depth shoaled, ocean temperatures increased and carbon isotope values decreased in the equatorial Atlantic. The nature of these changes around 41.6 million years ago implies common links, in terms of carbon cycling, with events at the Eocene/Oligocene boundary and with the 'hyperthermals' of the Early Eocene climate optimum. Our findings help to resolve the apparent discrepancy between the geological records of Northern Hemisphere glaciation and model results that indicate that the threshold for continental glaciation was crossed earlier in the Southern Hemisphere than in the Northern Hemisphere.

Total organic carbon content, methane isotopic composition and hydrocarbon characteristics of ODP Leg 180 sites

The organic geochemistry of Sites 1108 and 1109 of the Woodlark Basin, offshore Papua New Guinea, was studied to determine whether thermally mature hydrocarbons were present in the penetrated section and, if present, whether they are genetically related to the penetrated "coaly" interval. Both the organic carbon and pyrolysis data indicate that there is no significant hydrocarbon source-rock potential at Site 1108. The hydrocarbons encountered during drilling appear to be indigenous and not migrated products or contaminants. In contrast, the coaly interval at Site 1109 contains zones with significant hydrocarbon-generation potential. Several independent lines of evidence indicate that the coaly sequence encountered at Site 1109 is thermally immature. The Site 1108 methane stable-carbon isotope composition does not display a clear trend with depth as would be expected if it was solely reflecting a maturation profile. The measured isotopic composition of methane has most probably been altered by fractionation during sample handling and storage. This fractionation would result in isotopically heavier values than would be obtained on free gas. The organic geochemical data gathered indicate that Site 1108 can be safely revisited and that the organic-rich sediments encountered at Site 1109 were not the source of the gas encountered at Site 1108.

Eocene benthic foraminiferal community DSDP of Holes 95-612, 95-613 and 11-108

Benthic foraminiferal biofacies may vary independently of water depth and water mass; however, calibration of biofacies and stratigraphic ranges with independent paleodepth estimates allows reconstruction of age-depth patterns applicable throughout the deep Atlantic (Tjalsma and Lohmann, 1983). We have attempted to test these faunal calibrations in a continental margin setting, reconstructing Eocene benthic foraminiferal distributions along a dip section afforded by the New Jersey Transect (DSDP Sites 612, 108, 613). The following independent estimates of Eocene depths for the transect were obtained by "backtracking," "backstripping," and by assuming increasing depth downdip ("paleoslope"): Site 612, near the middle/lower bathyal boundary (about 1000 m); Site 108, in the middle bathyal zone (about 1600 m); and Site 613, near the lower bathyal/upper abyssal boundary (about 2000 m). Within uncertainties of backtracking (hundreds of meters), these estimates agree with estimates of paleodepth based on comparison of the New Jersey margin biofacies with other backtracked faunas. The stratigraphic ranges of many benthic taxa correspond to those found at other Atlantic DSDP sites. The major biofacies patterns show: (1) a depth dichotomy between an early to middle Eocene Nuttallides truempyidominated biofacies (greater than 2000 m) and a Lenticulina-Osangularia-Alabamina cf. dissonata biofacies (1000- 2000 m); and (2) a difference between a middle and a late Eocene biofacies at Site 612. The faunal boundary at about 2000 m, between bathyal and abyssal zones, occurs not only on the margin, but also throughout the deep Atlantic. The faunal change between the middle and late Eocene at Site 612 was due to a decrease of Lenticulina spp., the local disappearance of N. truempyi, and establishment of a Bulimina alazanensis-Gyroidinoides spp. biofacies. Although this change could be attributed to local paleoceanographic or water-depth changes, we argue that it is the bathyal expression of a global deep-sea benthic foraminiferal change which occurred across the middle/late Eocene boundary.