Ocupaçâo, valorizaçâo e comércio de terras no norte do Rio Grande do Sul - séculos 19 e 20

This article focuses on some aspects of the agrarian history of Soledade, a town in the north of the state of Rio Grande do Sul, southern Brazil. Our aim is to understand how this area was in many ways affected by the Land Law of 1850, particularly in economic and social terms. Population growth, arrival of European immigrants and increasing privatization of the commons contributed for the increasing of land prices in the region during the second half of the 19 th century. Understanding this situation as a great opportunity to make money, some landowners, directly or through a colonization company, allotted and sold the land they had previously acquired through the Land Law of 1850

El bienestar social durante el peronismo clásico. La expansión de los servicios de salud hacia las áreas rurales de los municipios de la provincia de Mendoza (1946-1955)

Con la llegada del peronismo al gobierno se produjeron reformas en relación a la organización y funcionamiento del sistema de salud pública. Pero más allá de sus éxitos o fracasos, el cuidado y la preservación de la salud de la población, incluyendo la de las zonas más apartadas y atrasadas del interior del país, fue una de las metas principales del gobierno de Juan Domingo Perón. A partir de esto, nuestro objetivo central es estudiar las políticas sanitarias en los municipios de la provincia de Mendoza durante el período 1946-1955, atendiendo a dos aspectos: el primero de ellos, relacionado con el rol del gobierno nacional y provincial en la ejecución de esta política pública, y el segundo, con los resultados, logros y efectos de la misma en los departamentos mendocinos. Este estudio empírico, en el cual se cotejan programas con resultados, permitirá conocer entonces el real cumplimiento de los objetivos establecidos por el peronismo.

Conflicto en el Territorio Nacional del Chaco : Las Cooperativas agrícolas frente al Estatuto del Peón Rural

La llegada a la presidencia de Juan Perón en 1946, significó para el agro argentino la continuidad de algunas políticas desarrolladas antes de la Revolución de 1943 y profundizadas por ésta. A esas decisiones de carácter productivo y de comercialización se sumaron aquellas orientadas a la mejora de la clase trabajadora rural, sector descuidado hasta el momento. La aplicación del Estatuto del Peón Rural (1947) en un territorio de frontera productiva y ocupacional como el Chaco, en un contexto local desfavorable, despertó uno de los más agitados enfrentamientos entre las entidades Cooperativas agrícolas-en representación de sus asociados- y la Administración local encargada de su aplicación. Es objetivo de este trabajo estudiar, desde la documentación que produjeron las cooperativas y los medios gráficos locales, el conflicto que se despertó en el Chaco al momento de implementarse el Estatuto del Peón

Memória e resistência na migraçao para a Amazônia : O caso de Nova Londrina em Ji-Paraná, estado de Rondônia, Brasil

The occupation of Rondônia, from the 1970s, occurred in a disorganized way, since it attracted an amount of migrants which was much bigger than the settling projects could sustain. The aim of this research was to analyze the circumstances in which the district of Nova Londrina was settled, utilizing for this reason a bibliographic survey, as well as the Oral History method. The arrival in Nova Londrina, Ji-Paraná, was highlighted by conflicts between the settlers and the settling company Calama S/A. In spite of the company's violence, the colonists resisted until there was an intervention from INCRA, through a land regularization program. In this context, the Urban Center for Rural Support (NUAR) was implanted, intending to support the agricultural workers

Conflictividad y resistencias en los márgenes de La Pampa (1990-2012)

Las formas de producción de territorios materiales e inmateriales entran en tensión y se yuxtaponen cuando espacios dominados por la territorialidad campesina son revalorizados por el capital y buscan imponer su espacialidad. En el extremo oeste pampeano, en el período 1990-2012, además de las nuevas racionalidades y prácticas de los campesinos, avanzaron el proceso de mercantilización y el accionar de productores-empresarios extralocales. En este contexto, emergieron los conflictos por el uso y la apropiación de los recursos, el modo de vida y la construcción social del espacio. La organización de las familias que ejercen actos posesorios para conservar la forma de manejo de los "campos abiertos" y el control del territorio dio origen a la conformación de estrategias de lucha colectivas. Ante los conflictos generados por el uso del monte y el achicamiento de los campos de los últimos diez años por la llegada de nuevos agentes que cercan las propiedades y desarticulan los circuitos de pastoreo, muchas familias del paraje comenzaron a organizarse con el apoyo de organizaciones urbanas para denunciar la reducción del espacio de pastoreo compartido. Con la finalidad de analizar los cambios y reconstruir las estrategias de organización campesinas, utilizamos distintos materiales empíricos en los que se combinan el análisis de estadísticas con entrevistas en profundidad e interpretación de diversos documentos

El elefante : Un caso paradigmático en la historia del contacto entre las culturas de la India, Grecia y Roma

La historia del conocimiento que el mundo mediterráneo, primero Grecia y luego Roma, tuvo de la India, comienza en forma paulatina con la llegada, por ejemplo, de objetos de marfil. A partir de la expedición de Alejandro, tiempo en el que ya circulaban fantasiosas historias, vinieron las cosas reales, como el elefante, que no dejaron menos pasmados a los occidentales. Un seguimiento de las actitudes de ambas culturas en relación con el elefante ayuda a comprender la mentalidad de una y otra, y también la situación histórica en que experimentaron el contacto

Las prácticas profesionales de formación como experiencias de pasaje y tránsito identitario

El presente artículo tiene por objeto compartir algunas ideas sobre las prácticas profesionales de formación a partir de relatos de estudiantes y referencias teóricas que replantean algunos supuestos generalizados en el campo de la formación profesional. Con la intención de interrogar la imagen que muchas veces se plantea de las prácticas como ámbitos de integración y aplicación de saberes teóricos y procedimentales, los relatos e itinerarios teóricos propuestos en el texto, las muestran como tiempos de formación que suponen el abandono de una posición identitaria conocida -la de ser estudiante- para arriesgar allí otro rostro, otra palabra -la del profesional que quiere llegarse a ser-. En este tránsito se asoma algo del recién llegado, del extranjero, de aquel que emigra por primera vez de la propia casa para explorar otros mundos y dejarse sorprender en la difícil tarea de descubrirse a 'sí mismo' siendo 'otro'. En esta perspectiva, el artículo pretende aportar una mirada que abona la reflexión sobre los procesos de socialización y transmisión cultural que se desarrollan en las prácticas y sobre los efectos que esta experiencia genera en el plano identitario. Como corolario de este desarrollo plantea algunas consideraciones sobre la alternancia como estrategias de formación para el trabajo de claro potencial formativo y de alta complejidad en el plano organizativo y pedagógico

Apuntes en torno a la renovación de la educación inicial a mediados del siglo XX

El presente trabajo tiene por objeto explorar los acontecimientos centrales que habilitaron la renovación de la educación inicial en Argentina a mediados del siglo XX. A partir del trabajo con fuentes analizo la construcción de un discurso que posibilitó la renovación de las prácticas en las salas de los jardines de infantes cuyos rasgos centrales perduran hasta nuestros días. En ese sentido, se analizan los modos en que la educación inicial se hace presente en las políticas educativas del peronismo y se recorren algunos de los textos significativos de aquel período. Luego, se indagan los efectos de la recepción del discurso psicológico en las familias y en las salas hasta la llegada de la última dictadura. En cuanto, a las fuentes se seleccionaron las que forman parte del corpus teórico de referencia para la segunda mitad del siglo pasado.

Los radicalizados del sector rural. Los dirigentes del Movimiento Agrario Misionero y Montoneros (1971- 1976)

En este artículo analizaremos la trayectoria de un grupo de agricultores que fundó en el interior de la provincia de Misiones el Movimiento Agrario Misionero (MAM). Al principio, igual que en las demás provincias del Nordeste, los agricultores participaron juntos en las movilizaciones de protesta y fueron apoyados por el obispo católico del lugar. Los dirigentes se vincularon tempranamente con los líderes de la Tendencia de nivel nacional - creada por Montoneros- y de la capital provincial, y construyeron un discurso adonde afirmaban que el MAM debía representar, tanto a los medianos y pequeños propietarios como a la "clase trabajadora" del sector rural, lo que generó un creciente malestar entre sus filas. Con la llegada del peronismo al poder, se abrió otra etapa adonde quedaron expuestas las diferencias al interior del Movimiento. En 1974 se produjeron dos grandes rupturas: a principios de ese año, un grupo de agricultores formó la Asociación Misionera de Agricultores (AMA) y a mediados, otro sector decidió expulsar a los agricultores que integraban la conducción del MAM. Los expulsados formaron las Ligas Agrarias Misioneras (LAM) y en el medio de la escalada de la violencia armada y el pase a la clandestinidad de Montoneros, crearon junto a los dirigentes capitalinos, el Partido Descamisado primero y el Partido Auténtico después. Participaron de las elecciones de abril de 1975, ganaron dos bancas y en la Cámara Legislativa siguieron defendiendo los intereses de los "obreros rurales" y la instauración de la "patria socialista". Esta historia se vio violentamente interrumpida con la llegada del golpe militar del 24 de marzo de 1976, cuando los militantes del MAM, las LAM y del Partido Auténtico fueron el blanco de la represión en la provincia, aunque ésta se había iniciado unos meses antes. Pretendemos mostrar, a partir del microanálisis, cómo se fue organizando y consolidando desde 1972, este grupo de militantes locales provenientes de la capital provincial y del interior, que pretendió encuadrar al MAM en la Tendencia y fue perdiendo apoyos avanzada la década. Aún después de la expulsión, veremos de qué manera continuaron considerándose la "vanguardia" de los "agricultores" y de la "clase trabajadora rural". Todo esto en un clima adonde la cúpula de Montoneros ordenaba el pase a la clandestinidad y privilegiaba la lucha armada. En suma, trataremos de rescatar la complejidad que envolvió a estos grupos y que fue característica de esos años.

Decade Wind and Wave Data for NW Iberia, Cabo Sillerio

Seafloor sediment mobilization on the inner Northwest Iberian continental shelf is caused largely by ocean surface waves. The temporal and spatial variability in the wave height, wave period, and wave direction has a profound effect on local sediment mobilization, leading to distinct sediment mobilization scenarios. Six grain-size specific sediment mobilization scenarios, representing seasonal average and storm conditions, were simulated with a physics-based numerical model. Model inputs included meteorological and oceanographic data in conjunction with seafloor grain-size and the shelf bathymetric data. The results show distinct seasonal variations, most importantly in wave height, leading to sediment mobilization, specifically on the inner shelf shallower than 30 m water depth where up to 49% of the shelf area is mobilized. Medium to severe storm events are modeled to mobilize up to 89% of the shelf area above 150 m water depth. The frequency of each of these seasonal and storm-related sediment mobilization scenarios is addressed using a decade of meteorological and oceanographic data. The temporal and spatial patterns of the modeled sediment mobilization scenarios are discussed in the context of existing geological and environmental processes and conditions to assist scientific, industrial and environmental efforts that are directly affected by sediment mobilization. Examples, where sediment mobilization plays a vital role, include seafloor nutrient advection, recurrent arrival of oil from oil-spill-laden seafloor sediment, and bottom trawling impacts.

Coccolithosphores and fossil organic compounds of sediment core MD01-2444

This study analyzes coccolithophore abundance fluctuations (e.g., Emiliania huxleyi, Gephyrocapsa specimens, and Florisphaera profunda) in core MD01-2444 sediment strata retrieved at the Iberian Margin, northeastern Atlantic Ocean. Coccolithophores are calcareous nannofossils, a major component of the oceanic phytoplankton, which provide information about past ecological and climatological variability. Results are supported by data on fossil organic compounds (sea surface temperatures, alkenones, and n-hexacosan-1-ol index) and geochemical analyses (benthic d13Ccc and planktonic d18Occ isotopes). Three scenarios are taken into account for this location at centennial-scale resolution over the last 70,000 years: the Holocene and the stadial and interstadial modes. The different alternatives are described by means of elements such as nutrients; upwelling phenomena; temperatures at surface and subsurface level; or the arrival of surface turbid, fresh, and cold waters due to icebergs, low sea level, increased aridity, and dust. During the Holocene, moderate primary productivity was observed (mainly concentrated in E. huxleyi specimens); surface temperatures were at maxima while the water column was highly ventilated by northern-sourced polar deep waters and warmer subsurface, nutrient-poor subtropical waters. Over most of the last glacial stadials, surface productivity weakened (higher F. profunda and reworked specimen percentages and lower diunsaturated and triunsaturated C37 alkenones); the arrival of cold Arctic surface waters traced by tetraunsaturated C37 peaks and large E. huxleyi, together with powerful ventilated southern-sourced polar deep waters, disturbed, in all likelihood, the delicate vertical equilibrium while preventing significant upwelling mixing. Finally, during the last glacial interstadials (lower F. profunda percentages, nonreworked material, and higher diunsaturated and triunsaturated C37 alkenones) a combined signal is observed: warm surface temperatures were concurrent with generally low oxygenation of the deep-sea floor, moderate arrival of northern-sourced deep waters, and subsurface cold, nutrient-rich, recently upwelled waters, probably of polar origin; these particular conditions may have promoted vertical mixing while enhancing surface primary productivity (mainly of Gephyrocapsa specimens).

Geochemistry of North Atlantic Igneous Province basalts

New Sr-Nd-Pb-Hf data require the existence of at least four mantle components in the genesis of basalts from the the North Atlantic Igneous Province (NAIP): (1) one (or more likely a small range of) enriched component(s) within the Iceland plume, (2) a depleted component within the Iceland plume (distinct from the shallow N-MORB source), (3) a depleted sheath surrounding the plume and (4) shallow N-MORB source mantle. These components have been available since the major phase of igneous activity associated with plume head impact during Paleogene times. In Hf-Nd isotope space, samples from Iceland, DSDP Leg 49 (Sites 407, 408 and 409), ODP Legs 152 and 163 (southeast Greenland margin), the Reykjanes Ridge, Kolbeinsey Ridge and DSDP Leg 38 (Site 348) define fields that are oblique to the main ocean island basalt array and extend toward a component with higher 176Hf/177Hf than the N-MORB source available prior to arrival of the plume, as indicated by the compositions of Cretaceous basalts from Goban Spur (~95 Ma). Aside from Goban Spur, only basalts from Hatton Bank on the oceanward side of the Rockall Plateau (DSDP Leg 81) lie consistently within the field of N-MORB, which indicates that the compositional influence of the plume did not reach this far south and east ~55 Ma ago. Thus, Hf-Nd isotope systematics are consistent with previous studies which indicate that shallow MORB-source mantle does not represent the depleted component within the Iceland plume (Thirlwall, J. Geol. Soc. London 152 (1995) 991-996; Hards et al., J. Geol. Soc. London 152 (1995) 1003-1009; Fitton et al., 1997 doi:10.1016/S0012-821X(97)00170-2). They also indicate that the depleted component is a long-lived and intrinsic feature of the Iceland plume, generated during an ancient melting event in which a mineral (such as garnet) with a high Lu/Hf was a residual phase. Collectively, these data suggest a model for the Iceland plume in which a heterogeneous core, derived from the lower mantle, consists of 'enriched' streaks or blobs dispersed in a more depleted matrix. A distinguishing feature of both the enriched and depleted components is high Nb/Y for a given Zr/Y (i.e. positive DeltaNb), but the enriched component has higher Sr and Pb isotope ratios, combined with lower epsilon-Nd and epsilon-Hf. This heterogeneous core is surrounded by a sheath of depleted material, similar to the depleted component of the Iceland plume in its epsilon-Nd and epsilon-Hf, but with lower 87Sr/86Sr, 208Pb/204Pb and negative DeltaNb; this material was probably entrained from near the 670 km discontinuity when the plume stalled at the boundary between the upper and lower mantle. The plume sheath displaced more normal MORB asthenosphere (distinguished by its lower epsilon-Hf for a given epsilon-Nd or Zr/Nb ratio), which existed in the North Atlantic prior to plume impact. Preliminary data on MORBs from near the Azores plume suggest that much of the North Atlantic may be 'polluted' not only by enriched plume material but also by depleted material similar to the Iceland plume sheath. If this hypothesis is correct, it may provide a general explanation for some of the compositional diversity and variations in inferred depth of melting (Klein and Langmuir, 1987 doi:10.1029/JB092iB08p08089) along the MAR in the North Atlantic.

Bird count in Mastbos forest (Breda, Netherlands) in the years 1950 to 1981

Notes from Henrik de Nie: The project started as a phenological study in cooperation with the (Dutch) meteorological institute (KNMI) to register the time of arrival of Fitis and Tjiftaf. During 1951 to 1969 he went every day to the wood (except 1966, in this year his wife died). Thereafter he went no more daily, but because he knew the wood very well and he was free to choice the day on which he did a survey, therefore he choose days with relatively good weather. He did not observe very common bird species, maybe because they are dependent on nest boxes and he did not want to be dependent on the management of the nest box-people (in fact I forgot precisely his arguments, and now I cannot ask him this): Common Starling; Eurasian Tree Sparrow (not common); Great Tit; Eurasian Blue Tit Pieter mentioned 14 species that scored many zero values or only one observation: Stock Dove; Common Cuckoo; Lesser Spotted Woodpecker; Eurasian Golden Oriole; Eurasian Nuthatch; Short-toed Treecreeper; Common Nightingale; Marsh Warbler; Lesser Whitethroat; Goldcrest; Common Firecrest (after 1970 he had difficulties in hearing these two species); Spotted Flycatcher; Eurasian Bullfinch; Black Woodpecker He also mentioned species that he found much fewer as: European Greenfinch; European Pied Flycatcher; Long-eared Owl; Red Crossbill; Sedge Warbler; Icterine Warbler; Eurasian Woodcock; Eurasian Siskin; European Green Woodpecker; Great Spotted Woodpecker; Eurasian Hobby; Western Barn Owl; Woodlark; Common Wood Pigeon; Little Owl; European Crested Tit; Hawfinch. But for these species I think that observations are strongly dependent on the number of visits to the wood. Also here, many zeros and few 1 x during the whole series of visits.

Jurassic sedimentation history at DSDP Hole 76-534A

Site 534 reflects a complex interplay of global, basinal, and local influences on sedimentation during the Callovian and Late Jurassic. Rifting and rapid subsidence of the continental margins of the North Atlantic-Tethys seaway occurred during the late Early Jurassic (Sinemurian-Pliensbachian), but rapid spreading between the North American margin (Blake Spur Ridge and magnetic lineation) and the northwest African margin did not commence until the Bathonian or earliest Callovian. Site 534, drilled on marine magnetic anomaly "M-28" of Bryan et al. (1980), was initially about 150 km from either continental margin. The ?middle Callovian basal sediments are dusky red silty marl. Callovian transgression led to active carbonate platforms on the margin, recorded at Site 534 as a rise in the CCD (carbonate compensation depth), then arrival of lime-rich turbidites from the Blake Plateau platform across the Blake Spur Ridge. The host pelagic sediment is greenish black, organic-rich, radiolarian-rich, silty claystone. Hydrothermal activity on the nearby spreading ridge enriched this lower unit in metals. In the Oxfordian, the input of terrestrial silt rapidly diminished; radiolarians or other bioclasts were not preserved. The dark variegated claystone has fine-grained marl and reddish claystone turbidite beds. The late Callovian-Oxfordian Western Tethys has radiolarian chert deposition, marine hiatuses, or organic-rich sediments. The Kimmeridgian and Tithonian had a stable or receding sea level. Near the end of the Jurassic many of the carbonate platforms of the margins were buried beneath prograding fan or alluvial deposits. Carbonate deposition shifted to the deep sea. Site 534 records the deepening of the CCD and ACD (aragonite compensation depth) during the Kimmeridgian and early Tithonian, then a rise of the ACD in the middle Tithonian. Similar trends occurred throughout the Western Tethys-Atlantic. High nannofossil productivity of the seaway led to deposition of very widespread white micritic limestone in the late Tithonian-Berriasian. The underlying sediment had a slower deposition rate of carbonate, therefore its higher clay and associated Fe content produced a red marl. A short sea-level incursion occurred on the Atlantic margins during the Kimmeridgian and is reflected in the Site 534 greenish gray marl unit by numerous turbidite beds of shallow-water carbonates.

Isotopic composition of modern ice wedges and winter precipitation in the Laptev Sea region (Table 2)

The first step for the application of stable isotope analyses of ice wedges for the correct paleoclimatic reconstruction supposes the study of the isotopic composition of modern ice wedges and their relationship with the isotopic composition of modern precipitation. The purpose of this research is to present, to analyze and to discuss new data on isotopic composition (d18O, dD, 3H) of modern ice wedges obtained in the Laptev Sea region in 1998-99. Investigations were carried out at two sites: on Bykovsky Peninsula in 1998 and on Bol'shoy Lyakhovsky Island in 1999 and were based on the combined application of both tritium CH) and stable isotope (d18O, dD) analyses. Tritium analyses of the atmospheric precipitation collected during two field seasons show seasonal variations: high tritium concentration in snow (to a maximum of 207 TU) and low values of tritium concentration (<20 TU) in rain. High tritium concentrations are also observed in the surface water, in suprapermafrost ground waters, and in the upper part of permafrost. High tritium concentrations range between 30-40 TU and 750 TU in the studied modern ice wedges (active ice wedges), which let us believe that they are of modern growth. Such high tritium concentrations in ice wedges can not be associated with old thermonuclear tritium because of the radioactive decay. High tritium concentrations found in the snow cover in 1998/99, in the active layer and in the upper part of permafrost give evidence of modern (probably the last decade) technogenic tritium arrival from the atmosphere on to the Earth surface in the region. The comparison of the isotopic composition (d18O, dD and d-excess) of active ice wedges and modern winter precipitation in both sites shows: 1) the isotopic composition of snow correlates linearly with a slope close to 8.0 and parallel to the GMWL at both sites; 2) the mean isotopic composition of active ice wedges on Bykovsky Peninsula is in good agreement with the mean isotopic composition of modern snow; 3) the isotopic composition of active ice wedges and snow on Bol'shoy Lyakhovsky Island are considerably different. There are low values of d-excess in all studied active ice wedges (mean value is about 4.8 per mil), while in snow, the mean value of d-excess is about 9.5 per mil. Possible reasons for this gap are the following: 1) the modification of the isotopic composition in snow during the spring period; 2) changes in the isotopic composition of ice wedges due to the process of ice sublimation in open frost cracks during the cold period; 3) mixing of snowmelt water with different types of surface water during the spring period; 4) different moisture source regions.