La organización territorial del movimiento de trabajadores desocupados Aníbal Verón del barrio Malvinas de la ciudad de La Plata

Este trabajo sintetiza los resultados de un estudio de campo realizado en la Organización Territorial del Movimiento de Trabajadores Desocupados Aníbal Verón del Barrio Malvinas de la ciudad de La Plata, entre el mes de Marzo del año 2003 (momento en el cual la Organización Territorial comienza sus actividades en el barrio y se incorpora, paulatinamente, al Movimiento de Trabajadores Desocupados Aníbal Verón) y los primeros meses del año 2005, cuando esta Organización conforma, junto a otras, el Frente Popular Darío Santillán. Los principales temas aquí desarrollados están relacionados, en principio, con la novedosa forma de participación político-comunitaria que insertó esta Organización Territorial en un barrio como Malvinas donde predominaban, desde hacía más de veinte años, formas de participación político-comunitarias de tipo clientelar. Otro de los temas aquí abordados está relacionado con los vínculos existentes entre la Organización Territorial y el Movimiento Regional. En esta trama vincular, se observó un desfasaje entre los criterios y acuerdos propuestos por el movimiento y las prácticas político-comunitarias llevadas adelante por la organización y los vecinos del barrio. Por último, en esta investigación también son centrales los distintos tipos de actores que interpretaban al movimiento de diferente manera. Aquí se observaron diversas formas de actuar, participar y comprometerse. En aquel momento, esto me llevó a proponer el armado de una tipología de participación de la que se desprende que la participación de los integrantes de la Organización Territorial del MTD Aníbal Verón del Barrio Malvinas, entre el año 2003 y 2005 era directa, inestable y complementaria. Lo que hacía que se fuera modificando con el propio devenir de la organización en movimiento. Es un trabajo más bien empírico y se nutrió por un lado, de datos obtenidos de entrevistas y observaciones realizadas para dos proyectos de extensión en los cuales participé y por otro, del trabajo de campo realizado entre el mes de Junio del año 2003 y Marzo del año 2005. El trabajo de campo constó de observaciones participantes y no participantes y, de entrevistas a los integrantes de la organización territorial. Entre el mes de octubre del año 2003 y el mes de enero del año 2004 realicé veinte entrevistas en profundidad. Para su realización se tomaron cuotas por sexo y edad hasta agotar información

Counselors' education in complex contexts with special reference to Latin America

This paper makes reference to the importance lying, at present, on the professional education of counselors. It goes through the history of the different pre-scientific and scientific stages of counseling, and it points out the main representatives in Latin America . It also shows the current state of the specialization, taking as an antecedent some in-depth, widely encompassing research carried out in the European Union in this area. Coincidences and differences are exposed here in terms of professional profiles, university degrees, institutional dependence, up-dating processes and modes of intervention. The current state of postgraduate studies at university is also touched upon, and the different proposals for further education in Latin America are analyzed as well as their dependence upon an undergraduate degree in Psychology, Educational Sciences or Psycho-pedagogy. Finally, this paper places counseling within the complexity and the need to provide all-encompassing and integrative answers which require a wide and deep enough education so as to answer all these issues and problems.

Registro de lectura : Dispositivo pedagógico que acompaña trayectorias formativas universitarias

El siguiente trabajo se enmarca en la línea de investigación sobre formación docente en Educación Física, desarrollada en el Centro Regional Universitario Bariloche de la Universidad Nacional del Comahue (CRUB-UNCo). Los proyectos que la integran, a partir del incremento sostenido del número de estudiantes que abandonan la carrera durante los dos primeros años, procuran interrogar las prácticas pedagógicas universitarias en ese campo, desentrañar sus modos particulares de producción y analizar su impacto en la constitución de los trayectos formativos de los y las estudiantes. En las indagaciones hallamos indicios de un trabajo docente sistemático para mejorar las condiciones de la enseñanza y del aprendizaje e identificamos dispositivos pedagógicos institucionales y áulicos a modo de andamiaje de las trayectorias estudiantiles y modos de recepción a los y las ingresantes. En esta oportunidad describimos y analizamos uno de estos dispositivos, denominado "registro de lectura", generado en la cátedra Pedagogía del 1º año del Profesorado en Educación Física del mencionado centro universitario. Dicho instrumento forma parte de una serie de prácticas pedagógicas deliberadamente planificadas en relación con el ingreso, la permanencia y el egreso del nivel superior, que pretende habilitar mejores escenarios para el desarrollo de los procesos educativos. El dispositivo, construido a modo de andamiaje de las prácticas lectoras de los y las estudiantes, pretende contribuir a la promoción de trayectorias formativas democráticas y procura dar lugar a nuevas explicaciones en tanto anclajes para la transformación y para la construcción de nuevos conocimientos así como lograr mejores intervenciones pedagógicas

Counselors' education in complex contexts with special reference to Latin America

This paper makes reference to the importance lying, at present, on the professional education of counselors. It goes through the history of the different pre-scientific and scientific stages of counseling, and it points out the main representatives in Latin America . It also shows the current state of the specialization, taking as an antecedent some in-depth, widely encompassing research carried out in the European Union in this area. Coincidences and differences are exposed here in terms of professional profiles, university degrees, institutional dependence, up-dating processes and modes of intervention. The current state of postgraduate studies at university is also touched upon, and the different proposals for further education in Latin America are analyzed as well as their dependence upon an undergraduate degree in Psychology, Educational Sciences or Psycho-pedagogy. Finally, this paper places counseling within the complexity and the need to provide all-encompassing and integrative answers which require a wide and deep enough education so as to answer all these issues and problems.

La organización territorial del movimiento de trabajadores desocupados Aníbal Verón del barrio Malvinas de la ciudad de La Plata

Este trabajo sintetiza los resultados de un estudio de campo realizado en la Organización Territorial del Movimiento de Trabajadores Desocupados Aníbal Verón del Barrio Malvinas de la ciudad de La Plata, entre el mes de Marzo del año 2003 (momento en el cual la Organización Territorial comienza sus actividades en el barrio y se incorpora, paulatinamente, al Movimiento de Trabajadores Desocupados Aníbal Verón) y los primeros meses del año 2005, cuando esta Organización conforma, junto a otras, el Frente Popular Darío Santillán. Los principales temas aquí desarrollados están relacionados, en principio, con la novedosa forma de participación político-comunitaria que insertó esta Organización Territorial en un barrio como Malvinas donde predominaban, desde hacía más de veinte años, formas de participación político-comunitarias de tipo clientelar. Otro de los temas aquí abordados está relacionado con los vínculos existentes entre la Organización Territorial y el Movimiento Regional. En esta trama vincular, se observó un desfasaje entre los criterios y acuerdos propuestos por el movimiento y las prácticas político-comunitarias llevadas adelante por la organización y los vecinos del barrio. Por último, en esta investigación también son centrales los distintos tipos de actores que interpretaban al movimiento de diferente manera. Aquí se observaron diversas formas de actuar, participar y comprometerse. En aquel momento, esto me llevó a proponer el armado de una tipología de participación de la que se desprende que la participación de los integrantes de la Organización Territorial del MTD Aníbal Verón del Barrio Malvinas, entre el año 2003 y 2005 era directa, inestable y complementaria. Lo que hacía que se fuera modificando con el propio devenir de la organización en movimiento. Es un trabajo más bien empírico y se nutrió por un lado, de datos obtenidos de entrevistas y observaciones realizadas para dos proyectos de extensión en los cuales participé y por otro, del trabajo de campo realizado entre el mes de Junio del año 2003 y Marzo del año 2005. El trabajo de campo constó de observaciones participantes y no participantes y, de entrevistas a los integrantes de la organización territorial. Entre el mes de octubre del año 2003 y el mes de enero del año 2004 realicé veinte entrevistas en profundidad. Para su realización se tomaron cuotas por sexo y edad hasta agotar información

Registro de lectura : Dispositivo pedagógico que acompaña trayectorias formativas universitarias

El siguiente trabajo se enmarca en la línea de investigación sobre formación docente en Educación Física, desarrollada en el Centro Regional Universitario Bariloche de la Universidad Nacional del Comahue (CRUB-UNCo). Los proyectos que la integran, a partir del incremento sostenido del número de estudiantes que abandonan la carrera durante los dos primeros años, procuran interrogar las prácticas pedagógicas universitarias en ese campo, desentrañar sus modos particulares de producción y analizar su impacto en la constitución de los trayectos formativos de los y las estudiantes. En las indagaciones hallamos indicios de un trabajo docente sistemático para mejorar las condiciones de la enseñanza y del aprendizaje e identificamos dispositivos pedagógicos institucionales y áulicos a modo de andamiaje de las trayectorias estudiantiles y modos de recepción a los y las ingresantes. En esta oportunidad describimos y analizamos uno de estos dispositivos, denominado "registro de lectura", generado en la cátedra Pedagogía del 1º año del Profesorado en Educación Física del mencionado centro universitario. Dicho instrumento forma parte de una serie de prácticas pedagógicas deliberadamente planificadas en relación con el ingreso, la permanencia y el egreso del nivel superior, que pretende habilitar mejores escenarios para el desarrollo de los procesos educativos. El dispositivo, construido a modo de andamiaje de las prácticas lectoras de los y las estudiantes, pretende contribuir a la promoción de trayectorias formativas democráticas y procura dar lugar a nuevas explicaciones en tanto anclajes para la transformación y para la construcción de nuevos conocimientos así como lograr mejores intervenciones pedagógicas

Nitrogen isotopic composition in South China Sea sediments

The d15N of surface and down-core sediments spanning the last 20-200 kyr from the entire South China Sea (SCS) ranges only from ~3.0 to ~6.5 per mil, with no correlation with discernible paleoclimatic/oceanographic changes. Detailed profiles of the uppermost sediment column, including fluff samples, indicate a minor diagenetic overprint of 0.3-1.2 per mil at the sediment-water interface. The absence of any correlation with reconstructed (glacial-interglacial) changes in primary production, terrigenous input, and/or sea level related basin configuration is attributed to a complete consumption of nitrate during primary production in this marginal basin during at least the last 140,000 years. This, in turn, implies that the d15N of the nitrate used during primary production remained approximately constant during the last climatic cycle. The proposed scenario infers an unchanged nitrogen isotopic composition of the western Pacific subsurface nitrate between glacial and interglacial stages as well as during terminations and thus constrains proposed changes in the oceanic N inventory.

Benthic foraminiferal faunas of Miocene to Holocene sediments of ODP Site 184-1143 from the southern South China Sea

Deep-sea benthic foraminiferal assemblages from Ocean Drilling Program (ODP) Site 1143 located in the southern South China Sea (SCS) were investigated to evaluate the relationship between faunal composition patterns and paleoceanographic changes during the last 6 million years (late Miocene to Holocene). We used multivariate statistics (correspondence analysis) to analyze carbon-flux-related changes in assemblage composition of benthic foraminifers. Additional proxies for carbon flux and deep-water ventilation include delta13C records of epifaunal Cibicidoides wuellerstorfi and infaunal Uvigerina peregrina var. dirupta and Melonis pompilioides, benthic foraminiferal accumulation rates (BFARs), diversity indices, and relative abundances of indicator species. We observe three significant benthic faunal changes in the southern South China Sea during the last 6 million years. Strong fluctuations in BFAR and relative abundance of productivity indicator species between glacial and interglacial stages after the mid-Pleistocene revolution (MPR) at approximately 0.9 Ma, indicating stronger seasonal carbon flux fluctuations, are accompanied by the extinction of such species as Stilostomella spp. Increases in carbon flux indicator species are coupled with an overall decrease in benthic foraminifer diversity around 3.0 Ma in the late Pliocene. This may indicate increasing carbon flux in a period of productivity maximum caused by enhanced offshore upwelling from intensified winter monsoon wind strength.

Paleomagneitc of early Cretaceous sediments from the western Central Atlantic

Drilling at Sites 534 and 603 of the Deep Sea Drilling Project recovered thick sections of Berriasian through Aptian white limestones to dark gray marls, interbedded with claystone and clastic turbidites. Progressive thermal demagnetization removed a normal-polarity overprint carried by goethite and/or pyrrhotite. The resulting characteristic magnetization is carried predominantly by magnetite. Directions and reliability of characteristic magnetization of each sample were computed by using least squares line-fits of magnetization vectors. The corrected true mean inclinations of the sites suggest that the western North Atlantic underwent approximately 6° of steady southward motion between the Berriasian and Aptian stages. The patterns of magnetic polarity of the two sites, when plotted on stratigraphic columns of the pelagic sediments without turbidite beds, display a fairly consistent magnetostratigraphy through most of the Hauterivian-Barremian interval, using dinoflagellate and nannofossil events and facies changes in pelagic sediment as controls on the correlations. The composite magnetostratigraphy appears to include most of the features of the M-sequence block model of magnetic anomalies from Ml to Ml ON (Barremian-Hauterivian) and from M16 to M23 (Berriasian-Tithonian). The Valanginian magnetostratigraphy of the sites does not exhibit reversed polarity intervals corresponding to Ml 1 to M13 of the M-sequence model; this may be the result of poor magnetization, of a major unrecognized hiatus in the early to middle Valanginian in the western North Atlantic, or of an error in the standard block model. Based on these tentative polarity-zone correlations, the Hauterivian/Barremian boundary occurs in or near the reversed-polarity Chron M7 or M5, depending upon whether the dinoflagellate or nannofossil zonation, respectively, is used; the Valanginian/Hauterivian boundary, as defined by the dinoflagellate zonation, is near reversed-polarity Chron M10N.

Stable isotope ratios in shells of marine organisms

Oxygen and carbon isotope analyses have been carried out on calcareous skeletons of important recent groups of organisms. Annual temperature ranges and distinct developmental stages can be reconstructed from single shells with the aid of the micro-sampling technique made possible by modern mass-spectrometers. This is in contrast to the results of earlier studies which used bulk sampIes. The skeletons analysed are from Bermuda, the Philippines, the Persian Gulf and the continental margin off Peru. In these environments, seasonal salinity ranges and thus annual variations in the isotopic composition of the water are small. In addition, environmental parameters are weIl documented in these areas. The recognition of seasonal isotopic variations is dependant on the type of calcification. Shells built up by carbonate deposition at the margin, such as molluscs, are suitable for isotopic studies. Analysis is more difficult where chambers are added at the margin of the shell but where older chambers are simultaneously covered by a thin veneer of carbonate e. g. in rotaliid foraminifera. Organisms such as calcareous algae or echinoderms that thicken existing calcareous parts as weIl as growing in length and breadth are the most difficult to analyse. All organisms analysed show temperature related oxygen-isotope fractionation. The most recent groups fractionate oxygen isotopes in accordance with established d18O temperature relationships (Tab. 18, Fig. 42). These groups are deep-sea foraminifera, planktonic foraminifera, serpulids, brachiopods, bryozoa, almost all molluscs, sea urchins, and fish (otoliths). A second group of organisms including the calcareous algae Padina, Acetabularia, and Penicillus, as weIl as barnacles, cause enrichment of the heavy isotope 18O. Finally, the calcareous algae Amphiroa, Cymopolia and Halimeda, the larger foraminifera, corals, starfish, and holothurians cause enrichment of the lighter isotope 16O. Organisms causing non-equilibrium fractionation also record seasonal temperature variations within their skeletons which are reflected in stable-oxygen-isotope patterns. With the exception of the green algae Halimeda and Penicillus, all organisms analysed show lower d13C values than calculated equilibrium values (Tab. 18, Fig. 42). Especially enriched with the lighter isotope 12C are animals such as hermatypic corals and larger foraminifera which exist in symbiosis with other organisms, but also ahermatypic corals, starfish, and holothurians. With increasing age of the organisms, seven different d13C trends were observed within the skeletons. 1) No d13C variations are observed in deep-sea foraminifera presumably due to relatively stable environmental conditions. 2) Lower d13C values occur in miliolid larger foraminifera and are possibly related to increased growth with increasing age of the foraminifera. 3) Higher values are found in planktonic foraminifera and rotaliid larger foraminifera and can be explained by a slowing down of growth with increasing age. 4) A sudden change to lower d13C values at a distinct shell size occurs in molluscs and is possibly caused by the first reproductive event. 5) A low-high-Iow cycle in calcareous algae is possibly caused by variations in the stage of calcification or growth. 6) A positive correlation between d18O and d13C values is found in some hermatypic corals, all ahermatypic corals, in the septa of Nautilus and in the otoliths of fish. In hermatypic corals from tropical areas, this correlation is the result of the inverse relationship between temperature and light caused by summer cloud cover; in other groups it is inferred to be due to metabolic processes. 7) A negative correlation between d18O and d13C values found in hermatypic corals from the subtropics is explained by the sympathetic relationship between temperature and light in these latitudes. These trends show that the carbon isotope fractionation is controlled by the biology of the respective carbonate producing organisms. Thus, the carbon isotope distribution can provide information on the symbiont-host relationship, on metabolic processes and calcification and growth stages during ontogenesis of calcareous marine organisms.

(Table 3) Geochemistry at DSDP Leg 79 Holes

Detailed mineralogical and geochemical studies were performed on samples from selected time intervals recovered during Leg 79 on the Mazagan Plateau. The uppermost Albian and Cenomanian sediments of Sites 545 and 547 can be correlated on the basis of mineralogy and geochemistry; these sediments illustrate differential settling processes and the existence of hot climates with alternating humid and dry seasons in the African coastal zone. The upper Aptian to Albian black shales of Site 545 point to an irregular alternation of tectonic activity and relaxation stages, allowing different behaviors in the reworking of soils, crystalline rocks, and sediments born in peri-marine basins. The barren lower Mesozoic reddish sediments and evaporitic series of Sites 546 and 547 are characterized by a strong physical erosion of sialic landscapes, without clear evidence of post-depositional metamorphic events. At Site 546 strong early diagenetic processes in a confined evaporitic environment affect both the mineralogy and the geochemistry of pre-Miocene rocks.

Anundance of phytoplankton at time series station DYNAPROC

A general study of biogeochemical processes (DYNAPROC cruise) was conducted in May 1995 at a time-series station in the open northwestern Mediterranean Sea where horizontal advection was weak. Short-term variations of the vertical distributions of pico- and nanophytoplankton were investigated over four 36-h cycles, along with parallel determinations of metabolic CO2 production rates and amino acid-containing colloid (AACC) concentrations at the chlorophyll maximum depth. The vertical (0-1000-m depth) distributions of (i) AACC, (ii) suspended particles and (iii) metabolic CO2 production rate were documented during the initial and final stages of these 36-h cycles. This study was concerned with diel vertical migration (DVM) of zooplankton, which provided periodic perturbations. Accordingly, the time scale of the experimental work varied from a few hours to a few days. Although all distributions exhibited a periodic behaviour, AACC distributions were generally not linked to diel vertical migrations. In the subsurface layer, Synechococcus made the most abundant population and large variations in concentration were observed both at day and at night. The corresponding integrated (over the upper 90 m) losses of Synechococcus during one night pointed to a potential source of exported organic matter amounting to 534 mg C/m**2. This study stresses the potential importance of organic matter export from the euphotic zone through the daily grazing activity of vertically migrating organisms, which would not be accounted for by measurements at longer time scales. The metabolic CO2 production exhibited a peak of activity below 500 m that was shifted downward, apparently in a recurrent way and independently of the vertical distributions of AACC or of suspended particulate material. To account for this phenomenon, a 'sustained wave train» hypothesis is proposed that combines the effect of the diel superficial faecal pellet production by swarming migrators and the repackaging activity of the nonmigrating midwater populations. Our results confirm the recent finding that the particulate compartment is not the major source of the observed instantaneous remineralisation rate and shed a new light on the fate of organic matter in the aphotic zone.

Geochemistry of oceanic crust of the North Atlantic

87Sr/a6Sr ratios, Sr, K, Rb and Cs contents and the petrology of basalts and secondary phases recovered from deep basement drilling at DSDP Sites 332B, 417A, 417D and 418A show that the oceanic crust alters in four distinct stages characterized by formation of palagonite, smectite and calcite (Stages I, II and III, respectively). Stage IV represents the final compaction of the crust, including a dehydration of the crust without major chemical changes. Isotopic age determinations by Hart and Staudigel (1978, doi:10.1029/GL005i012p01009) and Richardson et al. (doi:10.1029/JB085iB12p07195), show that, at least for Atlantic-type crustal regimes, Stage I and II last for a maximum of 3 m.y., and Stage III lasts beyond Stage I and II, but is probably completed in significantly less than 10 m.y. Stage IV is long-lived and may still be active at 100 m.y. Stages I and II, the phase of halmyrolysis, include geochemically significant interactions between seawater and basalt for the upper 500 m of layer II and involve volumes of seawater containing a large basaltic component. Stage III solutions show evidence of less seawater-basalt interaction, at least to depths of 500 m; calcites deposited from these solutions have Sr isotopic ratios close to seawater values; but also have very low Sr/Ca ratios indicating a large basalt Ca component in the solutions. Smectite formation is the result of the interaction of seawater and basalt. The initial 87Sr/a6Sr ratios of smectites represent the Sr isotopic composition of the solution when the smectite is being formed. Thereafter, alkalies may be continuously added to interlayer positions in the smectite in order of decreasing hydration energy (Cs is more enriched than Rb, Rb more than K). The later-formed carbonates have very low alkali concentrations, and 87Sr/86Sr ratios identical to contemporaneous seawater. Therefore, since the alkali concentrations in a whole rock sample are affected by different alteration processes, the alkali concentrations alone are not reliable indicators of the degree of alteration.

Seawater carbonate chemistry, the abiotic conditions in the fluid surrounding the embryo, growth, calcification of the cuttlefish Sepia officinalis in a laboratory experiment

This study investigated the effects of seawater pH (i.e., 8.10, 7.85 and 7.60) and temperature (16 and 19 °C) on (a) the abiotic conditions in the fluid surrounding the embryo (viz. the perivitelline fluid), (b) growth, development and (c) cuttlebone calcification of embryonic and juvenile stages of the cephalopod Sepia officinalis. Egg swelling increased in response to acidification or warming, leading to an increase in egg surface while the interactive effects suggested a limited plasticity of the swelling modulation. Embryos experienced elevated pCO2 conditions in the perivitelline fluid (>3-fold higher pCO2 than that of ambient seawater), rendering the medium under-saturated even under ambient conditions. The growth of both embryos and juveniles was unaffected by pH, whereas 45Ca incorporation in cuttlebone increased significantly with decreasing pH at both temperatures. This phenomenon of hypercalcification is limited to only a number of animals but does not guarantee functional performance and calls for better mechanistic understanding of calcification processes.

Effect of increased pCO2 level on early shell development in great scallop (Pecten maximus Lamarck) larvae

As a result of high anthropogenic CO2 emissions, the concentration of CO2 in the oceans has increased, causing a decrease in pH, known as ocean acidification (OA). Numerous studies have shown negative effects on marine invertebrates, and also that the early life stages are the most sensitive to OA. We studied the effects of OA on embryos and unfed larvae of the great scallop (Pecten maximus Lamarck), at pCO(2) levels of 469 (ambient), 807, 1164, and 1599 µatm until seven days after fertilization. To our knowledge, this is the first study on OA effects on larvae of this species. A drop in pCO(2) level the first 12 h was observed in the elevated pCO(2) groups due to a discontinuation in water flow to avoid escape of embryos. When the flow was restarted, pCO(2) level stabilized and was significantly different between all groups. OA affected both survival and shell growth negatively after seven days. Survival was reduced from 45% in the ambient group to 12% in the highest pCO(2) group. Shell length and height were reduced by 8 and 15 %, respectively, when pCO(2) increased from ambient to 1599 µatm. Development of normal hinges was negatively affected by elevated pCO(2) levels in both trochophore larvae after two days and veliger larvae after seven days. After seven days, deformities in the shell hinge were more connected to elevated pCO(2) levels than deformities in the shell edge. Embryos stained with calcein showed fluorescence in the newly formed shell area, indicating calcification of the shell at the early trochophore stage between one and two days after fertilization. Our results show that P. maximus embryos and early larvae may be negatively affected by elevated pCO(2) levels within the range of what is projected towards year 2250, although the initial drop in pCO(2) level may have overestimated the effect of the highest pCO(2) levels. Future work should focus on long-term effects on this species from hatching, throughout the larval stages, and further into the juvenile and adult stages.