As téchnai da cidade e a competência do filósofo

El propósito de esta comunicación es examinar la competencia del filósofo en el texto que hoy conocemos como Primer Alcibíades o Alcibíades Mayor. El trabajo propone la lectura del diálogo como un texto de filosofía política. La hipótesis sostenida es que el diálogo fue escrito con la intención de explicar la filosofía como una forma de intervenir políticamente basada en la exégesis filosófica de la sentencia apolínea "Conócete a ti mismo". Se argumenta que la perspectiva del texto se fundamenta en el principio de que la frase lleva consigo una exhortación a ejercer la política de manera recta. El diálogo, pues, no sólo contiene un análisis filosófico sobre la competencia adecuada para el ejercicio del poder, sino que también analiza cómo esta competencia se relaciona con la política, lo que pone a la filosofía en conflicto con las téchnai practicadas en la ciudad

Territorialidades, espacios vividos y sentidos de lugar en tiempos de avance de la frontera productiva

En pleno proceso de corrimiento de la frontera productiva y emergente disputa por el uso y apropiación de los recursos, la intervención de distintos sujetos sociales en el oeste de La Pampa está redefiniendo las prácticas productivas-reproductivas de los crianceros campesinos y, en consecuencia, la construcción social del espacio. Desde la finalización de las campañas militares contra las sociedades indígenas diferentes agentes, mediante el ejercicio de poder, construyeron determinadas representaciones territoriales y pusieron en acción prácticas tendientes a articular el oeste pampeano con la economía nacional. Sin embargo la escasa valorización de este espacio posibilitó el desarrollo de cierta autonomía en las formas de organización socio-productivas y simbólicas. Ante la expansión de la frontera ganadera, el impuso hidrocarburífero en la región y creciente presencia de nuevas lógicas territoriales crecen las confrontaciones por el desigual acceso a los recursos naturales, por la apropiación del espacio y la construcción de territorialidades. En este marco, el artículo focaliza la mirada en la organización interna de los asentamientos rurales y en los usos sociales de los espacios a través del tiempo, en dos áreas del "extremo" oeste: La Humada y Chos Malal. De este modo se pretende establecer cómo se organizaron diacrónicamente los espacios doméstico, peridoméstico y monte y qué sentidos expresan los sujetos en torno a los espacios de vida y lugares en tiempos de expansión de la frontera productiva. El nuevo campo social generado producto del avance del capitalismo sobre las unidades campesinas se expresa, no sólo en las modificaciones en las formas de manejo del ganado, organización de la producción y construcción social del espacio, sino también en las formas de sociabilidad y estrategias de resistencia colectivas. Este proceso, que se está gestando en la región, tiene un desarrollo similar en otros espacios donde el avance productivo se ha generado con anterioridad o a un ritmo más acelerado. Para la realización de la investigación se articulan diferentes estrategias de metodología cualitativa que combinan el estudio de caso con historias de vida, entrevistas en profundidad y análisis de fuentes documentales.

El subdesarrollo del macrosistema eléctrico en la costa atlántica de la Provincia de Buenos Aires

El macrosistema eléctrico de la costa atlántica bonaerense muestra un desarrollo divergente respecto de las tracciones y expectativas del proceso productivo global y de las condiciones generales de la reproducción social que puede ser calificado como subdesarrollo. Desde 2003, al producirse el sostenido repunte del consumo eléctrico, la problemática del abastecimiento de electricidad se agravó y el territorio local comenzó a atravesar un estado de emergencia energética. El trabajo analiza los principales factores explicativos de dicha situación: la reestructuración capitalista del sector eléctrico llevada a cabo durante los noventa y los funcionamientos impuestos por el marco regulatorio, los cambios político-económicos de la Posconvertibilidad, la aplicación de una estrategia anticrisis basada en medidas paliativas y la marcada estacionalidad de la demanda eléctrica local inducida por la enorme afluencia turística de la zona

Mariano Moreno, el Contrato Social y el mercado de impresos en el comienzo de la América Independiente

En un mundo colonial que se acercaba a su fin, a medio camino entre el Ancien Régime y lo que vendría después, Mariano Moreno escribió su obra a la vez que era protagonista de los eventos políticos que sacudieron Buenos Aires en 1810. Tomando a este personaje como puerta de entrada al Río de la Plata decimonónico, aquí se intenta reconstruir las ideas y el lenguaje de la época. Un punto de especial interés para el trabajo es la cultura impresa, con la cual Moreno tuvo una relación activa, fundando y dirigiendo el primer boletín oficial y editando una versión del Contrato Social de Rousseau. La pregunta que recorre el texto es la siguiente ¿Qué tan "moderno" fue Moreno y qué tanto lo era el mundo en que vivía?

As téchnai da cidade e a competência do filósofo

El propósito de esta comunicación es examinar la competencia del filósofo en el texto que hoy conocemos como Primer Alcibíades o Alcibíades Mayor. El trabajo propone la lectura del diálogo como un texto de filosofía política. La hipótesis sostenida es que el diálogo fue escrito con la intención de explicar la filosofía como una forma de intervenir políticamente basada en la exégesis filosófica de la sentencia apolínea "Conócete a ti mismo". Se argumenta que la perspectiva del texto se fundamenta en el principio de que la frase lleva consigo una exhortación a ejercer la política de manera recta. El diálogo, pues, no sólo contiene un análisis filosófico sobre la competencia adecuada para el ejercicio del poder, sino que también analiza cómo esta competencia se relaciona con la política, lo que pone a la filosofía en conflicto con las téchnai practicadas en la ciudad

Thomas Hobbes : Sobre el miedo

Este trabajo pretende echar cierta luz sobre el papel del miedo en el pensamiento político de Hobbes. Sabido es que esta pasión subyace al contrato social, en el sentido de que impulsa al hombre a abandonar el estado de naturaleza a fin de encontrar seguridad y de deshacerse de la amenaza de la muerte violenta. Teniendo en cuenta que el miedo y la muerte son inseparables en la filosofía de Hobbes, surge una pregunta fundamental: ¿hasta qué punto podemos decir que el miedo desaparece completamente después del contrato social? En Hobbes, el miedo parecería ser una característica intrínseca del hombre.

Cacao trees in tropical agroforestry landscapes of the Napu Valley in Central Sulawesi, Indonesia

All sample sites were situated at the northern tip of Napu Valley in Central Sulawesi, Indonesia. After an initial mapping of the study area, we selected 15 smallholder cacao plantations as sites for bird and bat exclosure experiments in March 2010. On each study site, we established 4 treatments for these exclosure experiments (bird exclosure - closed during daytime and open during night; bat exclosure - closed overnight and opened during daytime; full exclosure of both birds and bats - always closed and unmanipulated/open control treatments - always open). In each treatment, there were 2 cacao trees (total of 8 cacao trees per study site), surrounded by nylon filament (2x2 cm mesh size) that was opened and closed according to the activity period of day and night active flying vertebrates (05:00-06:00 am and 17:00-18:00 pm) on a daily basis. The mean tree height and diameter at breast height (dbh) result from two measures of all study trees at the beginning of the exclosure experiment (June 2010) and 6 months later (February 2011).

Southern Ocean CO2 uptake and buffer factor from model run 2012-2100, with links to model results

The Southern Ocean is a key region for global carbon uptake and is characterised by a strong seasonality with the annual CO2 uptake being mediated by biological carbon draw-down in summer. Here, we show that the contribution of biology to CO2 uptake will become even more important until 2100. This is the case even if biological production remains unaltered and can be explained by the decreasing buffer capacity of the ocean as its carbon content increases. The same amount of biological carbon draw-down leads to a more than twice as large reduction in CO2 (aq) concentration and hence to a larger CO2 gradient between ocean and atmosphere that drives the gas-exchange. While the winter uptake south of 44°S changes little, the summer uptake increases largely and is responsible for the annual mean response. The combination of decreasing buffer capacity and strong seasonality of biological carbon draw-down introduces a strong and increasing seasonality in the anthropogenic carbon uptake.

Avian species identity and predation success in tropical cacao agroforestry of the Napu Valley in Central Sulawesi, Indonesia

Avian ecosystem services such as the suppression of pests are considered being of high ecological and economic importance in a range of ecosystems, especially in tropical agroforestry. But how bird predation success is related to the diversity and composition of the bird community, as well as local and landscape factors, is poorly understood. The author quantified arthropod predation in relation to the identity and diversity of insectivorous birds, using experimental exposure of artificial, caterpillar-like prey on smallholder cacao agroforestry systems, differing in local shade management and distance to primary forest. The bird community was assessed using both mist netting (targeting on active understory insectivores) and point count (higher completeness of species inventories) sampling. The study was conducted in a land use dominated area in Central Sulawesi, Indonesia, adjacent to the Lore Lindu National Park. We selected 15 smallholder cacao plantations as sites for bird and bat exclosure experiments in March 2010. Until July 2011, we recorded several data in this study area, including the bird community data, cacao tree data and bird predation experiments that are presented here. We found that avian predation success can be driven by single and abundant insectivorous species, rather than by overall bird species richness. Forest proximity was important for enhancing the density of this key species, but did also promote bird species richness. The availability of local shade trees had no effects on the local bird community or avian predation success. Our findings are both of economical as well as ecological interest because the conservation of nearby forest remnants will likely benefit human needs and biodiversity conservation alike.

Bird observation and sampling in tropical agroforestry landscapes of the Napu Valley in Central Sulawesi, Indonesia

We investigated the local bird community in Central Sulawesi (Indonesia), with focus on insectivorous species in the agroforestry landscapes adjacent to the Lore Lindu National Park. All study sites were situated at the northern tip of Napu Valley in Central Sulawesi, Indonesia. After an initial mapping of the study area, we selected 15 smallholder cacao plantations as sites for our study in March 2010. These sides were mainly used for bird and bat exclosure experiments. All sited were situated along a local gradient (shade availability on each plantation) and a landscape gradient (distance to primary forest), which were independent from each other. In September 2010 and from February until June 2011, we assessed the bird community on our 15 study sites using monthly point count and mist netting sampling. Point count (20 minutes between 07 am and 10 am and in between the net checking hours) and mist netting surveys (12 hours, between 05:30 am and 17:30 pm) were conducted simultaneously but only once per month on each study site, to avoid habituation of the local bird community to our surveys. Further, point counts were conducted at least 100 m apart from the mist netting sites, to avoid potential disturbance between the two methods. We discarded all observations beyond 50 m (including those individuals that flew over the canopy) from the statistical analysis, as well as recaptures of individuals within identical mist netting rounds.

Pore pressure measurements on IODP Exp308 sites

Overpressures measured with pore pressure penetrometers during Integrated Ocean Drilling Program (IODP) Expedition 308 reach 70% and 60% of the hydrostatic effective stress (View the MathML source) in the first 200 meters below sea floor (mbsf) at Sites U1322 and U1324, respectively, in the deepwater Gulf of Mexico, offshore Louisiana. High overpressures are present within low permeability mudstones where there have been multiple, very large, submarine landslides during the Pleistocene. Beneath 200 mbsf at Site U1324, pore pressures drop significantly: there are no submarine landslides in this mixture of mudstone, siltstone, and sandstone. The penetrometer measurements did not reach the in situ pressure at the end of the deployment. We used a soil model to determine that an extrapolation approach based on the inverse of square route of time (View the MathML source) requires much less decay time to achieve a desirable accuracy than an inverse time (1/t) extrapolation. Expedition 308 examined how rapid and asymmetric sedimentation above a permeable aquifer drives lateral fluid flow, extreme pore pressures, and submarine landslides. We interpret that the high overpressures observed are driven by rapid sedimentation of low permeability material from the ancestral Mississippi River. Reduced overpressure at depth at Site U1324 suggests lateral flow (drainage) whereas high overpressure at Site U1322 requires inflow from below: lateral flow in the underlying permeable aquifer provides one mechanism for these observations. High overpressure near the seafloor reduces slope stability and provides a mechanism for the large submarine landslides and low regional gradient (2°) offshore from the Mississippi delta.

Benthic foraminiferal stable isotope stratigraphy of ODP Site 138-846 in the tropical Pacific Ocean

A stable-isotope stratigraphy at Site 846 (tropical Pacific, 3°06'S, 90°49'W, 3307 m water depth), based on the benthic foraminifers Cibicides wuellerstorfi and Uvigerina peregrina, yields a high-resolution record of deep-sea delta18O and delta13C over the past 1.8 Ma, with an average sampling interval of 3 k.y. Variance in the delta18O and delta13C records is concentrated in the well-known orbital periods of 100, 41, and 23 k.y. In the 100-k.y. band, both isotopic signals grow from relatively low amplitudes prior to 1.2 Ma, to high amplitudes in the late Quaternary since 0.7 Ma. The amplitude of delta18O and especially of delta13C decreases in the 41-k.y. band as it grows in the 100-k.y. band, consistent with a transfer of energy into an orbitally-paced internal oscillation. A weak 30-k.y. rhythm, present in both delta18O and delta13C, may reflect nonlinear interaction between the 41-k.y. and 100-k.y. bands in the evolving climate system. In the 23-k.y. and 19-k.y. bands associated with orbital precession, delta18O and delta13C are not coherent with each other on long time scales, and do not evolve like the 100-k.y. and 41-k.y. bands. This suggests that the source of the growing 100-k.y. oscillation is not a nonlinear response to precession, in contrast to predictions of some climate models. Sedimentation rates at this site also vary with a strong 100-k.y. cycle. Unlike the isotope records, the amplitude of 100-k.y. variations in sedimentation rate is relatively constant over the past 1.8 Ma, ranging from about 15 to 70 m/m.y. Prior to 0.9 Ma, sedimentation rates co-vary with orbital eccentricity, rather than with global climate as reflected by delta18O or delta13C. A source of this 100-k.y. cycle of sedimentation rate in the absence of similar ice volume fluctuations may be precessional heating of equatorial land masses, which in an energy balance climate model drives variations of monsoonal climates with a 100-k.y. rhythm. For the interval younger than 0.9 Ma, high sedimentation rates in the 100-k.y. band are consistently associated with glacial stages. This change of pattern suggests that when the amplitude of glacial cycles become large enough, their global effects overpower a local monsoon-driven variation in sedimentation rate at Site 846.

Coral-algae metabolism and diurnal changes in the CO2-carbonate system of bulk sea water

Precise measurements were conducted in continuous flow seawater mesocosms located in full sunlight that compared metabolic response of coral, coral-macroalgae and macroalgae systems over a diurnal cycle. Irradiance controlled net photosynthesis (Pnet), which in turn drove net calcification (Gnet), and altered pH. Pnet exerted the dominant control on [CO3]2- and aragonite saturation state (Omega arag) over the diel cycle. Dark calcification rate decreased after sunset, reaching zero near midnight followed by an increasing rate that peaked at 03:00 h. Changes in Omega arag and pH lagged behind Gnet throughout the daily cycle by two or more hours. The flux rate Pnet was the primary driver of calcification. Daytime coral metabolism rapidly removes dissolved inorganic carbon (DIC) from the bulk seawater and photosynthesis provides the energy that drives Gnet while increasing the bulk water pH. These relationships result in a correlation between Gnet and Omega arag, with Omega arag as the dependent variable. High rates of H+ efflux continued for several hours following mid-day peak Gnet suggesting that corals have difficulty in shedding waste protons as described by the Proton Flux Hypothesis. DIC flux (uptake) followed Pnet and Gnet and dropped off rapidly following peak Pnet and peak Gnet indicating that corals can cope more effectively with the problem of limited DIC supply compared to the problem of eliminating H+. Over a 24 h period the plot of total alkalinity (AT) versus DIC as well as the plot of Gnet versus Omega arag revealed a circular hysteresis pattern over the diel cycle in the coral and coral-algae mesocosms, but not the macroalgae mesocosm. Presence of macroalgae did not change Gnet of the corals, but altered the relationship between Omega arag and Gnet. Predictive models of how future global changes will effect coral growth that are based on oceanic Omega arag must include the influence of future localized Pnet on Gnet and changes in rate of reef carbonate dissolution. The correlation between Omega arag and Gnet over the diel cycle is simply the response of the CO2-carbonate system to increased pH as photosynthesis shifts the equilibria and increases the [CO3]2- relative to the other DIC components of [HCO3]- and [CO2]. Therefore Omega arag closely tracked pH as an effect of changes in Pnet, which also drove changes in Gnet. Measurements of DIC flux and H+ flux are far more useful than concentrations in describing coral metabolism dynamics. Coral reefs are systems that exist in constant disequilibrium with the water column.