Guidance and counseling in Latin America : General considerations about the criteria of coherence, cooperation and quality

La Orientación en América Latina, como campo de formación profesional y en comparación con Europa y Estados Unidos, es una actividad de reciente aceptación en los medios académicos. La misma se ha caracterizado por una constante evolución en su afán de adaptarse a los nuevos cambios y transformaciones sociales, políticas y económicas que se suceden en el continente latinoamericano. En esta ponencia se presenta un panorama general acerca de la Orientación en América Latina. Las principales consideraciones formuladas se relacionan con cuatro dimensiones: a) la dimensión política pública, donde se presentan la situación actual y las propuestas al respecto; b) la dimensión contextual que hace referencia a la formación del orientador y los diferentes escenarios de acción; c) la dimensión organizacional que se relaciona con la provisión de este servicio, y d) la dimensión metodológica donde se desarrollan los principales aspectos relacionados con la práctica de la Orientación.

Guidance and counseling in Latin America : General considerations about the criteria of coherence, cooperation and quality

La Orientación en América Latina, como campo de formación profesional y en comparación con Europa y Estados Unidos, es una actividad de reciente aceptación en los medios académicos. La misma se ha caracterizado por una constante evolución en su afán de adaptarse a los nuevos cambios y transformaciones sociales, políticas y económicas que se suceden en el continente latinoamericano. En esta ponencia se presenta un panorama general acerca de la Orientación en América Latina. Las principales consideraciones formuladas se relacionan con cuatro dimensiones: a) la dimensión política pública, donde se presentan la situación actual y las propuestas al respecto; b) la dimensión contextual que hace referencia a la formación del orientador y los diferentes escenarios de acción; c) la dimensión organizacional que se relaciona con la provisión de este servicio, y d) la dimensión metodológica donde se desarrollan los principales aspectos relacionados con la práctica de la Orientación.

Guidance and counseling in Latin America : General considerations about the criteria of coherence, cooperation and quality

La Orientación en América Latina, como campo de formación profesional y en comparación con Europa y Estados Unidos, es una actividad de reciente aceptación en los medios académicos. La misma se ha caracterizado por una constante evolución en su afán de adaptarse a los nuevos cambios y transformaciones sociales, políticas y económicas que se suceden en el continente latinoamericano. En esta ponencia se presenta un panorama general acerca de la Orientación en América Latina. Las principales consideraciones formuladas se relacionan con cuatro dimensiones: a) la dimensión política pública, donde se presentan la situación actual y las propuestas al respecto; b) la dimensión contextual que hace referencia a la formación del orientador y los diferentes escenarios de acción; c) la dimensión organizacional que se relaciona con la provisión de este servicio, y d) la dimensión metodológica donde se desarrollan los principales aspectos relacionados con la práctica de la Orientación.

Geochemistry and degree of organic carbon preservation in non-bioturbated, shaly sediments

Based on 13 published porewater H2S and sulphate profiles the amount of H2S escaping from non-bioturbated shales varies between some few % to 45% of the amount of bacterially generated H2S. This finding permits calculation of the original organic carbon (TOCor) content of immature nonbioturbated shales using TOC and sulphur content data. In two immature non-bioturbated sequences from Hungary (Toarcian and Oligocene) the first-order correlation between HI and TOC/TOCor was found to be stronger than that between HI and TOC, indicating that sulphate reduction was the leading process both in decrease in TOC content and degradation of kerogen source potential.

Spectral reflectance of ODP Leg 178 holes

The routine use of spectrophotometry on the sediment surfaces of archive halves of each section during the onboard sedimentological core description process is a great stride toward development of real-time noninvasive characterization of deep-sea sediments. Spectral reflectance data have been used so far for mineral composition studies as well as for lithostratigraphic correlation between sites (Balsam and Deaton, 1991; Balsam et al., 1997; Mix et al., 1995; Ortiz et al., 1999). Their results demonstrate that spectrophotometry can estimate CaCO3 content by using the 4.65-, 5.25-, and 5.55-µm wavelength spectrums. A detailed overview of various other noninvasive methods is given in Ortiz and Rack (1999). The purpose of this study is to test whether spectrophotometry in the visible band can be used as a tool to gather further information about grain-size variation, sorting, compaction, and porosity, which are directly linked to the sedimentation process. From remote sensing data analyses, it is known that diffuse spectral reflectance data in the visible band in the wavelength window of 7.0-6.5 µm are sensitive to grain-size variations. It appears that a relationship between grain size and signal absorption exists only in this wavelength window. (e.g., Clark, 1999; Gaffey, 1986; Gaffey et al., 1993). Variations in grain size during a sedimentation process are linked to depositional energy, which affects sorting, compaction, and porosity of sediment deposits. As an example, we study here the spectrophotometric data of the sedimentary sequence of Hole 1098C, which was deposited under widely varying environmental conditions. Alternating turbidite and finely laminated sediments were recovered from Hole 1098C. The turbidites are related to a high depositional energy environment; the finely laminated sediments are related to a low depositional energy environment. Data from Hole 1098C were therefore used to test whether the spectral reflectance data can provide a proxy for these different depositional environments.

(Table 1) Sulfur isotopes, total sulfur, and degree of oxidation of basalt samples from DSDP Holes 69-504B and 70-504B

Whole-rock basalt samples from the upper half of Deep Sea Drilling Project Hole 504B have oxygen-isotope compositions typical of mid-ocean-ridge basalts which have experienced a moderate degree of low-temperature alteration by sea water. By contrast, d18O values in the lower half of the hole correspond to basalts which have experienced almost no detectable oxygen-isotope alteration. These observations suggest that the overall water/rock ratio was lower in the lower half of the drilled crust. A correlation between d18O values and 87Sr/86Sr ratios suggests that the water/rock ratio, rather than temperature variation, was the main factor determining basalt d18O values. Hydrogen-isotope data appear to be consistent with a low water/rock ratio in the lower part of the crust.

(Table 1) B content, d11B, d18O, degree of alteration, and lithology of basalts from ODP Hole 504B

Boron contents and boron isotopic compositions were determined for the uppermost 1.3 km section of typical 6.2 Ma oceanic crust from DSDP/ODP Hole 504B, Costa Rica Rift, Galapagos Spreading Center. Both the boron content and the d11B value in the oceanic crust are controlled by two types of alteration: 1. (1) low-temperature alteration (0 to 60°C; Zones I and II) and 2. (2) high-temperature hydrothermal alteration (200 to 400°C; Zones III and IV). Basalts subjected to the low-temperature alteration are characterized by their relatively high boron contents (0.69 to 19.3 ppm) and high d11B values (+2.2 to +10.6?), indicating uptake of boron into secondary phases in equilibrium with seawater or evolved seawater. Hydrothermally altered basalts contain less abundant boron (0.17 to 0.52 ppm) and relatively constant d11B values (?0.1 to +1.0?). Although basalts from the upper part of these hydrothermal zones (<1300 mbsf) show equilibrated boron content and d11B value with aqueous fluid, effective leaching of boron from basalt is predominant in the lower part (>1300 mbsf). Original boron content and d11B value of the Hole 504B MORB were 0.35 ppm and +0.2?, respectively. The present data provide fundamental information in understanding of the distribution of boron and boron isotopes in the oceanic crust.