Panorama general 1970 al 2005 de la matrícula y el egreso universitarios en México como indicadores de la tensión en el mercado laboral

En este trabajo se presentan algunos avances de un proyecto sobre empleo profesional de egresados de universidades públicas y privadas en México. Concretamente se describen los resultados de la fase de indagación cuantitativa de las características de la matrícula y el egreso de nivel universitario por área de estudio, carrera y régimen, de 1970 al 2005, para la población total a nivel nacional, así como algunas características de la participación laboral de nivel profesional. El trabajo se centra en la población de instituciones públicas y privadas por la presencia creciente de estas últimas en la atención de la demanda y para comprender un mercado laboral que parece cada vez más competido y diferenciado por origen institucional. Partimos del supuesto de que la exploración cuantitativa de la dinámica de la educación superior en México en los últimos 35 años, ofrece elementos para conocer algunas de las características de los mercados laborales de nivel profesional y sus niveles de tensión por saturación. En este sentido, la indagación cuantitativa del estudio es una dimensión, entre otras, que contribuye en cierta medida a la comprensión del papel de la educación en el mercado laboral y, en general, de la función social de la educación, dos de los objetivos más amplios del proyecto en el que se enmarca lo que aquí se expone

La dinámica de crecimiento de la matrícula universitaria de Artes : La creación del IUNA y su impacto en el sistema universitario

La ponencia 'La dinámica de crecimiento de la matrícula universitaria de Artes: la creación del IUNA y su impacto en el sistema universitario' se inscribe en el proyecto de investigación sobre "Areas y factores de cambio en la organización del Instituto Universitario Nacional del Arte (IUNA), desde su inicio hasta la actualidad", cuyo objetivo general es describir y caracterizar las principales dinámicas de cambio en el IUNA. Dada la particular experiencia del origen de esta institución universitaria, en el sentido que articula en su proyecto institucional a centenarias escuelas terciarias con nuevas unidades académicas y nuevas ofertas de carreras de arte, enmarcadas en un nuevo escenario de nivel universitario; este trabajo presenta un primer acercamiento hacia el análisis de las dinámicas de cambio en el IUNA, contextualizando su surgimiento, explicitando sus condiciones de desarrollo y presentando su estado de situación actual; todo ello, observando, particularmente, la dinámica de la demanda de estudios universitarios en arte, tanto en relación con la evolución de la matrícula en el conjunto de las universidades nacionales, como al interior de la universidad misma, entre las distintas ofertas de carreras de arte

(Figure 1) Stratigraphic distribution of taxa at DSDP Hole 79-547B

Twenty-five samples from selected cored intervals of problematic Triassic-Jurassic age from Sites 545, 546, and Hole 547B have been analyzed palynologically to aid age determination. Section 545-73-1 yielded a marine palynoflora of Sinemurian-Bajocian age. A palynoflora of nonmarine origin and assigned a Rhaetian-Hettangian age was recovered from halite in Section 546-18-2. Marine palynofloras of Hettangian-early Pliensbachian age were recovered from Sample 547B-24-CC to Section 547B-14-2. Sections 547B-28-1 to 547B-25-3 yielded impoverished nonmarine palynofloras to which only a general Rhaetian-Hettangian age could be given.

Properties of water masses, taxa abundance, and isotopic ratios of samples obtained around Svalbard archipelago

The feeding strategies of Calanus hyperboreus, C. glacialis, and C. finmarchicus were investigated in the high-Arctic Svalbard region (77-81 °N) in May, August, and December, including seasons with algal blooms, late- to post-bloom situations, and unproductive winter periods. Stable isotope and fatty acid trophic marker (FATM) techniques were employed together to assess trophic level (TL), carbon sources (phytoplankton vs. ice algae), and diet of the three Calanus species. In addition, population development, distribution, and nutritional state (i.e. storage lipids) were examined to estimate their population status at the time of sampling. In May and August, the vertical distribution of the three Calanus species usually coincided with the maximum algal biomass. Their stable isotope and fatty acid (FA) composition indicated that they all were essentially herbivores in May, when the algal biomass was highest. Their FA composition, however, revealed different food preferences. C. hyperboreus had high proportions of 18:4n3, suggesting that it fed mainly on Phaeocystis, whereas C. glacialis and C. finmarchicus had high proportions of 16:4n1, 16:1n7, and 20:5n3, suggesting diatoms as their major food source. Carbon sources (i.e. phytoplankton vs. ice algae) were not possible to determine solely from FATM techniques since ice-diatoms and pelagic-diatoms were characterised by the same FA. However, the enriched d13C values of C. glacialis and C. finmarchicus in May indicated that they fed both on pelagic- and ice-diatoms. Patterns in absolute FA and fatty alcohol composition revealed that diatoms were the most important food for C. hyperboreus and C. glacialis, followed by Phaeocystis, whereas diatoms, Phaeocystis and other small autotrophic flagellates were equally important food for C. finmarchicus. During periods of lower algal biomass, only C. glacialis exhibited evidence of significant dietary switch, with a TL indicative of omnivory (mean TL=2.4). Large spatial variability was observed in population development, distribution, and lipid store sizes in August. At the northernmost station at the southern margin of the Arctic Ocean, the three Calanus species had similarly low lipid stores as they had in May, suggesting that they ascended later in the year. In December, relatively lipid-rich specimens had TL similar to those during the peak productive season (TL~2.0), suggesting that they were hibernating and not feeding on the available refractory material available at that time of the year. In contrast, lipid-poor specimens in December had substantially high TL (TL=2.5), suggesting that they were active and possibly were feeding.

Biostratigraphy of selected taxa and radiolarian events in ODP Hole 183-1138A sediments

Well-preserved radiolarian assemblages of late middle Miocene to early Pliocene age are found in Ocean Drilling Program (ODP) Hole 1138A (Cores 183-1138A-12R to 20R), which was rotary drilled into the Central Kerguelen Plateau. The faunas are typical for Antarctic assemblages of this time interval, and the site appears to have been south of the Polar Front during the time period studied. Despite only moderate drilling recovery of the section, most late middle to early Pliocene radiolarian zones are present, although at the sample resolution used, subzones could not be identified. A significant discontinuity in the section is present at the boundary between lithologic Units I and II (between Cores 183-1138A-12R and 13R), corresponding to an interval from at least 4.6 to 6.1 Ma. Mixed late Miocene-early Pliocene assemblages are seen in the base of Core 183-1138A-12R (Sample 183-1138A-12R-3, 20 cm), and the overlying basal Pliocene Tau Zone appears to be absent. It cannot be determined if the discontinuity is due to incomplete recovery of the section and drilling disturbance or if it reflects a primary sedimentary structure - a hiatus or interval of condensed sedimentation.