Perspectives on guidance and social inclusion in a global society

The world is changing rapidly. People today face numerous challenges in achieving a meaningful and fulfilling life. In many countries, there are enormous systemic barriers to address, such as: massive unemployment, HIV/AIDS, social disintegration, and inadequate infrastructure. One job for life is over. For many it never existed. Old metaphors and old models of career development no longer apply. New ways of thinking about careers are necessary, that take into account the context in which people are living, the reality of today's labour market, and the fact people's career-life journey contains many branching paths, barriers, and obstacles, but also allies and sources of assistance. Flexibility is important, as is keeping options open and making sure the journey is meaningful. Guidance professionals need to begin early, working with other professionals and those seeking assistance to develop attitudes that facilitate people taking charge of their own career-life paths. People need a vision for their life that will drive a purposeful approach to career-life planning and avoid floundering. Helping people achieve that direction can be most effectively accomplished when policy makers and practitioners work together to ensure that effective and accessible services are available for those who need them and when a large part of focus in on addressing the context in which marginalized people work and live.

Magnetic properties of ODP Hole 109-670A

Magnetic fabrics of serpentinized peridotites are related to anisomorphic magnetite formed during serpentinization. In the less serpentinized facies they are, however, mainly mimetic of the high temperature deformation prior to serpentinization. In more serpentinized peridotites, the magnetic fabrics, related to magnetite veins which are more developed in this case, are superimposed on mimetic fabrics. Remanent properties, hysteresis loop parameters, and Curie temperatures were measured. Natural remanent magnetizations (NRM) have crystallization remanent magnetic (CRM) origin. Measured magnetic parameters suggest that pseudo-single domain (PSD) grains of magnetite are present in samples with low degree of serpentinization. The samples with high degree of serpentinization contain mainly multi-domain (MD) magnetite grains.

Perspectivas en Orientación e inclusión de lo social en una sociedad globalizada

El mundo cambia rápidamente. Se enfrentan muchos desafíos para acceder a una vida plena y con sentido. Muchos países padecen de graves obstáculos como el desempleo masivo, el SIDA, la desintegración social, una infraestructura inadecuada. Ya no puede pensarse en un trabajo para toda la vida. Para algunos inclusive nunca existió. Los antiguos modelos de carrera ya no están vigentes. Se necesitan entonces nuevos modelos que tengan en cuenta el contexto en el cual la gente vive, la realidad del mercado laboral actual y el hecho de que el viaje que se realiza hacia una ocupación o carrera es un camino con bifurcaciones y obstáculos, pero que también cuenta con aliados y con ayuda disponible. Es importante mantenerse flexible y abierto a opciones para asegurarse así un camino pleno de sentido. La orientación vocacional ocupacional debe empezar en los primeros años de vida, trabajando conjuntamente con otros profesionales para generar actitudes que alienten a que cada uno esté a cargo del camino elegido. Se necesita contar con una visión de la propia vida que conduzca a proponerse una carrera, en lo posible sin tropiezos. Si orientadores, autoridades, políticos y legisladores trabajan en forma conjunta, podrán asegurar un servicio efectivo y accesible para quienes lo necesitan, siempre incluyendo el contexto en el que los marginados viven y trabajan.

Un marco conceptual que demuestra el valor de los servicios de orientación

Tanto profesionales como quienes tienen a su cargo diferentes servicios están de acuerdo en que la evaluación es importante. Sin embargo, los orientadores rara vez evalúan su trabajo de manera de hallar una relación causal entre los servicios que los usuarios reciben y los cambios a los que acceden. Se ha desarrollado un marco teórico para evaluar los cambios en los conocimientos, habilidades, actitudes y creencias del usuario y examinar el impacto que dichos cambios han hecho en su vida y en la sociedad en la que se desenvuelve. El marco incluye también un sistema de seguimiento de las intervenciones realizadas y de los recursos necesarios para poder implementar exitosamente estas acciones. Ha sido empleado en diversas situaciones orientadoras, establecimientos educativos y acciones de orientación vocacional, con el objeto de proporcionar evidencia de que el servicio brindado realmente produce un impacto sobre la vida del usuarioTanto profesionales como quienes tienen a su cargo diferentes servicios están de acuerdo en que la evaluación es importante. Sin embargo, los orientadores rara vez evalúan su trabajo de manera de hallar una relación causal entre los servicios que los usuarios reciben y los cambios a los que acceden. Se ha desarrollado un marco teórico para evaluar los cambios en los conocimientos, habilidades, actitudes y creencias del usuario y examinar el impacto que dichos cambios han hecho en su vida y en la sociedad en la que se desenvuelve. El marco incluye también un sistema de seguimiento de las intervenciones realizadas y de los recursos necesarios para poder implementar exitosamente estas acciones. Ha sido empleado en diversas situaciones orientadoras, establecimientos educativos y acciones de orientación vocacional, con el objeto de proporcionar evidencia de que el servicio brindado realmente produce un impacto sobre la vida del usuario

Chemistry of sulfide deposits from ODP Site 106-649

In Snake Pit massive sulfide fragments and friable, unconsolidated material recovered during ODP Leg 106, isocubanite and pyrite are generally the predominant phases, followed by marcasite, chalcopyrite, sphalerite, and pyrrhotite. Detailed analyses of paragenetic relations of minerals indicate that isocubanite first precipitated together with pyrrhotite. With decreasing temperature, chalcopyrite and sphalerite precipitated, and at the latest stage colloform sphalerite-pyrite (or colloform marcasite) formed. Isocubanite usually has exsolution lamellae of chalcopyrite and less commonly of pyrrhotite. The average bulk chemical composition of the friable, unconsolidated material indicates that it is rich in copper, reflecting the dominance of isocubanite in the specimens, and is characterized by high Co, low Pb, and Ag contents. Sulfur isotope ratios are very uniform, ranging in d34S from +1.2 to +2.8 per mil. The obtained values are apparently low, compared to those for the eastern Pacific sulfide samples, reflecting a smaller contribution of seawater sulfate in the Snake Pit sulfide deposit.

(Table S3) Benthic foraminiferal Mg/Ca, Li/Ca and stable isotope ratios of ODP Site 122-761

The sensitivities of benthic foraminiferal Mg/Ca and Li/Ca to bottom water temperature and carbonate saturation state have recently been assessed. Here we present a new approach that uses paired Mg/Ca and Li/Ca records to calculate simultaneous changes in temperature and saturation state. Using previously published records, we first use this approach to document a cooling of deep ocean waters associated with the establishment of the Antarctic ice sheet at the Eocene-Oligocene climate transition. We then apply this approach to new records of the Middle Miocene Climate Transition from ODP Site 761 to estimate variations in bottom water temperature and the oxygen isotopic composition of seawater. We estimate that the oxygen isotopic composition of seawater varied by ~1 per mil between the deglacial extreme of the Miocene Climatic Optimum and the glacial maximum following the Middle Miocene Climate Transition, indicating large amplitude variations in ice volume. However, the longer-term change between 15.3 and 12.5 Ma is marked by a ~1°C cooling of deep waters, and an increase in the oxygen isotopic composition of seawater of ~0.6 per mil. We find that bottom water saturation state increased in the lead up to the Middle Miocene Climate Transition and decreased shortly after. This supports decreasing pCO2 as a driver for global cooling and ice sheet expansion, in agreement with existing boron isotope and leaf stomatal index CO2 records but in contrast to the published alkenone CO2 records.

Mg/Ca-temperature proxy in benthic foraminifera from the Florida Strait

Over the past decade, the ratio of Mg to Ca in foraminiferal tests has emerged as a valuable paleotemperature proxy. However, large uncertainties remain in the relationships between benthic foraminiferal Mg/Ca and temperature. Mg/Ca was measured in benthic foraminifera from 31 high-quality multicore tops collected in the Florida Straits, spanning a temperature range of 5.8° to 18.6°C. New calibrations are presented for Uvigerina peregrina, Planulina ariminensis, Planulina foveolata, and Hoeglundina elegans. The Mg/Ca values and temperature sensitivities vary among species, but all species exhibit a positive correlation that decreases in slope at higher temperatures. The decrease in the sensitivity of Mg/Ca to temperature may potentially be explained by Mg/Ca suppression at high carbonate ion concentrations. It is suggested that a carbonate ion influence on Mg/Ca may be adjusted for by dividing Mg/Ca by Li/Ca. The Mg/Li ratio displays stronger correlations to temperature, with up to 90% of variance explained, than Mg/Ca alone. These new calibrations are tested on several Last Glacial Maximum (LGM) samples from the Florida Straits. LGM temperatures reconstructed from Mg/Ca and Mg/Li are generally more scattered than core top measurements and may be contaminated by high-Mg overgrowths. The potential for Mg/Ca and Mg/Li as temperature proxies warrants further testing.

Magnetic properties of ODP Hole 109-648B

Seventeen samples from pillow or massive "zero age" fresh basalts from ODP Legs 106 and 109 were studied in order to examine their magnetic properties and oxidation degree. Thermomagnetic analyses of studied samples show Curie temperatures from 127°C to 220°C with reversible heating and cooling curves. Hysteresis parameters indicate the contribution of large Pseudo-Single Domain (PSD) grain of titanomagnetites with saturation magnetization between 0.4 and 0.7 emu/g which is almost twice that those of other recent mid-oceanic dredged basalts (e.g., FAMOUS and CYAMEX-RISE). The large grain sizes and higher magnetic mineral concentration may suggest a slower cooling of these basalts compared to those previously studied. Electron microprobe analyses of titanomagnetite grains combined with Curie point determinations give z = 0.3 for the degree of low temperature oxidation, which is close to the other values reported for low temperature oxidation of mid-oceanic ridge basalts.