Crises of social significances: adolescents and their projects for future work

This is a report on data raised through research, which has already finished, about Identification references in adolescents . Objetives : To analyze and reflect upon the collected data, adolescents' representations about the work field and their projects for future work. To conceptualize about the crises of social significances which produce and order sense and, therefore, organize our perceptions of work through social discourses and practices which have an impact on the subjectivity of adolescents and young adults. Methodology: Brief presentation of the concepts which frame the qualitative research in this area. Reading and analysis of fragments from adolescents' accounts, obtained in focal groups at different state secondary schools. Conclusions: The adolescents researched portray a self-image full of uncertainty and skepticism as regards their future possibilities. The impact produced by the fall of work as an ideal of doing and being is made evident in their accounts. Only some of them link their future project with an invested and valuable activity, even if this is not associated with economic safety and wellbeing. Others present themselves as incapable to modify the state of things, which offers a field connected with consumerist values and with the idea that "you are worth what you have (in material things)".

Las leyes sobre vagancia : Control policial y práctica judicial en el ocaso de la frontera (Tandil 1872-1881)

A fines de la década de 1870, el gobierno provincial, con el objeto de lograr mayor control social sobre la población rural, implementó una reestructuración policial en la campaña bonaerense. La misma tenía por objetivo afianzar la propiedad privada y contribuir al mercado de trabajo, asimismo perseguía un fuerte interés en satisfacer la necesidad del estado de hombres en plena etapa de expansión de la frontera. La presión reclutadora del estado se reflejará en un aumento de detenidos por vagancia, dado que las leyes de represión de la vagancia del Código Rural permitían su penalización al servicio de las armas. El Código Rural sancionado en 1865 estipulaba dos normas procesales a cumplir en los acusados: formación de un sumario y constitución de un jury para su juzgamiento. Disposiciones que raramente se pusieron en práctica por los jueces de paz desde que esta legislación entró en vigencia. Será a fines de la década de 1870 cuando el gobierno exigirá más firmemente no solo la persecución de la vagancia sino también la aplicación de estas normas procesales en los acusados. Aún así, el análisis de la práctica judicial revelará que continuará existiendo una constante manipulación normativa sobre la base de dos valores que se intentaban afianzar, el trabajo y la propiedad. En los perjudiciales que atentaran contra estos dos valores, será en quienes se manipulará la normativa sancionada y se canalizará la presión reclutadora.

Autosuperación del Hombre

Según Nietzsche, a partir de la Revolución Francesa tenemos que estar preparados para 'conmociones fundamentales'; desde entonces se producen acontecimientos que anuncian modificaciones infra y superestructurales para el próximo milenio, con lo cual, el orden social se ajustará al rumbo de las ?nuevas ideas?. En la actualidad, los triunfos y logros de la civilización ponen en peligro el desarrollo mismo de la cultura; son tiempos de procesos políticos extraordinarios o en otras palabras, de grandes luchas por el dominio de la tierra. Es así que se aproxima el 'ocaso de los ídolos', es decir, la ruina de las verdades antiguas pues casi todo lo que hasta el presente se llama verdad es sólo mentira y, cuando la nueva realidad se enfrente a las fabulaciones milenarias, nuestra cosmovisión sufrirá terribles sacudidas; las guerras serán inevitables y todas las instituciones basadas en el engaño y la ilusión caerán ante el asombro de los sobrevivientes. Nietzsche inicia la desacralización o 'desenmascaramiento' de las verdades eternas y la transmutación de todos los valores que son, en definitiva, procesos ineluctables. Asimismo, no hay fenómenos morales sino una 'interpretación moral de los fenómenos' o, en todo caso, una falsa interpretación. Y la moral no es otra cosa que una coacción prolongada. En la medida en que la Humanidad se aleja de la fe, más se acerca a la Ciencia, porque mientras la primera significa no querer saber qué es la verdad, la segunda nos asemeja a Dios. Según Nietzsche, estamos en ese camino. Día tras día el Hombre se perfecciona mediante la investigación de la Naturaleza; forma un cuerpo físico, mental y espiritual cada vez más enaltecido, realiza experimentos para mejorar la nutrición, el modo de vivir, la manera de interpretar los fenómenos de la Naturaleza y la expansión de la conciencia; pero en última instancia, no se trata del Hombre, pues éste tiene que ser superado. En consecuencia con lo dicho, el propósito del presente trabajo consiste en brindar una interpretación de la propuesta nietzscheana de 'Autosuperación del Hombre' en relación con los diferentes períodos de la vida intelectual de Nietzsche; la misma se inscribe en el marco de una teoría política contraria a las doctrinas antes mencionadas: la filosofía de la historia hegeliana, el socialismo, el nacionalismo, el anarquismo, la democracia y el cristianismo

Rewriting the history of the tyrannicides : Thucydides versus Herodotus?

Este trabajo trata sobre la famosa digresión de Tucídides en el libro sexto de su historia acerca de la caída de la tiranía en Atenas (Tuc. 6.54-59) y su relación con el relato de Heródoto. La digresión de Tucídides (y más específicamente su tono polémico) ha provocado controversia entre los comentadores, que han analizado a fondo las narrativas de los dos historiadores tanto desde una perspectiva histórica como historiográfica. Este estudio tiende a contribuir a esta discusión a través de tres sugerencias: la primera, Tucídides se mete no solo con la pequeña sección sobre los tiranicidas de la Historia de Heródoto (esto es Hdt. 5.55-65), sino, más bien, con toda la narrativa de la Historia de Heródoto sobre la liberación de Atenas de la tiranía que se extiende hasta el discurso de Socles (esto es Hdt. 5.55-5.96.2); segunda, las correcciones de Tucídides al relato de Heródoto son menores, tercera, dado que las divergencias de Tucídides con respecto a Heródoto no son decisivas para la versión correcta de los hechos, el tono polémico de Tucídides en su digresión resulta todavía más difícil de explicar. En este trabajo se sugiere tentativamente que la actitud polémica de Tucídides tiene más sentido si es interpretada en el contexto de la rivalidad del historiador con Heródoto

Crises of social significances: adolescents and their projects for future work

This is a report on data raised through research, which has already finished, about Identification references in adolescents . Objetives : To analyze and reflect upon the collected data, adolescents' representations about the work field and their projects for future work. To conceptualize about the crises of social significances which produce and order sense and, therefore, organize our perceptions of work through social discourses and practices which have an impact on the subjectivity of adolescents and young adults. Methodology: Brief presentation of the concepts which frame the qualitative research in this area. Reading and analysis of fragments from adolescents' accounts, obtained in focal groups at different state secondary schools. Conclusions: The adolescents researched portray a self-image full of uncertainty and skepticism as regards their future possibilities. The impact produced by the fall of work as an ideal of doing and being is made evident in their accounts. Only some of them link their future project with an invested and valuable activity, even if this is not associated with economic safety and wellbeing. Others present themselves as incapable to modify the state of things, which offers a field connected with consumerist values and with the idea that "you are worth what you have (in material things)".

Age models of upper Pliocene samples of the North Atlantic

Abundance variations of six Pliocene species of discoasters have been analyzed over the time interval from 1.89 to 2.95 Ma at five contrasting sites in the North Atlantic: Deep Sea Drilling Project Sites 552 (56°N) and 607 (41°N) and Ocean Drilling Program 658 (20°N), 659 (18°N), and 662 (1°S). A sampling interval equivalent to approximately 3 k.y. was used. Total Discoaster abundance showed a reduction with increasing latitude and from the effects of upwelling. This phenomenon is most obvious in Discoaster brouweri, the only species that survived over the entire time interval studied. Prior to 2.38 Ma, Discoaster pentaradiatus and Discoaster surculus are important components of the Discoaster assemblage: Discoaster pentaradiatus increases slightly with latitude up to 41°N, and its abundance relative to D. brouweri increases up to 56°N; D. surculus increases in abundance with latitude and with upwelling conditions relative to both D. brouweri and D. pentaradiatus and is dominant to the latter species at upwelling Site 658 and at the highest latitude sites. Discoaster asymmetricus and Discoaster tamalis appear to increase in abundance with latitude relative to D. brouweri. Many of the abundance changes observed appear to be connected with the initiation of glaciation in the North Atlantic at 2.4 Ma. The long-term trend of decreasing Discoaster abundance probably reflects the fall of sea-surface temperatures. This trend of cooling is overprinted by short-term variations that are probably associated with orbital forcing. Evidence for the astronomical elements of eccentricity and obliquity periodicities were found at all sites; however, only at Sites 607, 659, and 662 were precessional periodicities detected. Furthermore, only at Site 659 was precession found to be dominant to obliquity. Abundance peaks of individual species were found to cross-correlate between sites. The distinct abundance fluctuations observed especially in the tropics suggest that temperature is not the only factor responsible for this variation. This study reveals for the first time the importance of productivity pressure on the suppression of Discoaster abundance.

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.

Tab. 1: Mineralogical composition and chemical analyses of major and trace elements of Ameghino Formation rocks

As a result of a petrographical, mineralogical and geochemical characterization of the Ameghino Formation mudstones (Upper Jurassic- Lower Cretaceous, Antarctic Peninsula), "epiclastic" radiolaria-rich and mixed (radiolaria-rich + tuff) mudstone types were recognized. Contents of clastic material in the mudstones generally increase with younger paleontological age, but local exceptions to this trend have been found. The anoxic environment of the lower part of the sequence changes to more oxidizing conditions towards the top, in transition to the Hauterivian - Barrêmian conglomerates. Element to element correlations show good agreement with the normal differentiation trends of volcanic (andesite-rhyolite) rocks, suggesting that the overall sequence is mainly volcanic in origin with various grade of reworking. For example, the radiolaria-rich mudstone matrix could have been originated from very fine touffaceous suspensions deposited very slowly after the main fall of the tuffs. However, in the upper part of the sequence, some epiclastic supply is revealed by petrographic evidence and illite crystallinity index. The clay mineral association (illite, chlorite and illite-smectite mixed layers) is mainly of diagenetic origin in the stratigraphically lower sections. Low percentages of expandable layers in the illite-smectite mixed layers, as well as the general mineralogical association, suggest a late mesodiagenetic stage, and together with geological evidence, a relatively deep burial (> 1000 m - probably > 2500 m) and temperatures exceeding 100°C.