TIC nas aulas de educação física: para ensinar basquetebol

Coordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES)

Formação inicial docente para a educação sexual: revelando realidades de licenciaturas em Ciências Biológicas

Coordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES)

A relação entre a álgebra acadêmica e a álgebra escolar em um curso de licenciatura em matemática: concepções de alunos e professores

Pós-graduação em Educação - FCT

Matemática e estatística aplicadas a gestão da qualidadade nos cursos de Engenharia de Produção no Brasil: um contraponto entre a formação e o mercado de trabalho

Pós-graduação em Educação Matemática - IGCE

Matemática e estatística aplicadas a gestão da qualidadade nos cursos de Engenharia de Produção no Brasil: um contraponto entre a formação e o mercado de trabalho

Pós-graduação em Educação Matemática - IGCE

Untersuchungen zum Einfluss des HMG-CoA-Reduktase-Inhibitors Lovastatin auf die Toxizität ionisierender Strahlung sowie des Anthrazyklinderivats Doxorubicin im Mausmodell

Hintergund: HMG-CoA-Reduktase-Inhibitoren (Statine) sind klinisch etablierte Cholesterinsenker. Über die Inhibition der intrinsischen Cholesterinbiosynthese hinaus zeigen sie sogenannte pleiotrope biologische Effekte. Ein Großteil dieser Wirkungen wird auf die Inhibition kleiner Ras homologer GTPasen (Rho GTPasen) zurückgeführt. In vitro schützt das Statinderivat Lovastatin (Lova) primäre humane Endothelzellen vor der Zytotoxizität von ionisierender Strahlung (IR) und dem Krebsmedikament Doxorubicin (Doxo). Zielsetzung: Die Relevanz dieser Befunde für ein in vivo Mausmodell sollte in der vorliegenden Arbeit überprüft werden. Dafür wurden BALB/c-Mäuse mit IR oder Doxo behandelt und der Einfluss einer Kobehandlung mit Lova auf verschiedene Toxizitätsendpunkte untersucht (24 h nach einer einzelnen hohen Dosis IR (i), 14 Tage nach zwei geringen Dosen IR (ii), 48 h nach einer einzelnen hohen Dosis Doxo (iii), sowie 8 Tage nach drei niedrigen Dosen Doxo (iv)). Eine mögliche gleichzeitige Protektion von Tumorzellen durch die Statingabe wurde in einem Xenotransplantationsexperiment überprüft (v), in dem das gleiche Behandlungsschema wie bei iv angewendet wurde. Ergebnisse: Es konnte gezeigt werden, dass eine Statinbehandlung Normalgewebe vor Doxo- und IR-induzierter Toxizität schützt, ohne gleichzeitig protektiv auf transformierte Zellen zu wirken. Dieser Effekt ist wahrscheinlich von einer Inhibition der kleinen GTPasen Rac1 und RhoA abhängig und einer daraus folgenden Modifizierung der DNA-Schadensantwort. i: Die Statinvorbehandlung der Mäuse hatte keinen Einfluss auf die Bildung von initialen IR-induzierten DNA-Doppelstrangbrüchen (DSB) in der Leber. Die Lova-Behandlung wirkte sich jedoch auf IR-induzierte Stressantworten aus, was sich in einer Minderung der Expression von Inflammations- und Fibrosesurrogatmarkern in Leber und Darm widerspiegelte. ii: In der Lunge der Tiere wurde ein Anstieg von molekularen Inflammations- und Fibrosesurrogatmarkern detektiert, der bei Statinkobehandlung ausblieb. Zudem verhinderte die Kobehandlung mit Lova eine IR-induzierte Abnahme der Thrombozytenzahl, ohne sich auf die durch IR verringerte Leukozytenzahl im Blut auszuwirken. iii: Die Verabreichung einer hohen Dosis Doxo induzierte DSB-Formation in der Leber. Die Statinvorbehandlung reduzierte deren Menge um ca. 50 %. Dieser genoprotektive Effekt war unabhängig von der Entstehung reaktiver Sauerstoffspezies sowie einer Änderung des Doxo-Imports oder Exports. Die Expression von proinflammatorischen und profibrotischen Genen fiel besonders in der Leber und im Herzen durch die Lova-Kobehandlung geringer aus, als in der nur mit Doxo behandelten Gruppe. Zudem verringerte Lova die durch Doxo induzierte Hochregulation von für den AP1-Komplex kodierenden Genen sowie von Zellzykluskontrollfaktoren. Die Lova-Vorbehandlung führte darüber hinaus im Herzen zu einem reduzierten mRNA-Spiegel der Topoisomerasen II α und β. iv: Es konnten schwere Herz- und Leberschäden detektiert werden (gemessen an Gldh-, Gpt- sowie cTn-I-Serumkonzentrationen), die bei einer Kobehandlung mit dem Statin nicht auftraten. Die Lova-Kobehandlung verhinderte außerdem eine durch die Doxo-Behandlung verringerte Leukozytenzahl. Molekulare Marker für frühe fibrotische Ereignisse, sowie für Inflammation und Hypertrophie waren in der Leber und im Herzen nach der Doxo-Behandlung erhöht. Das Statin war auch hier in der Lage, diese toxischen Wirkungen des Anthrazyklins zu mindern. Auch die Doxo-induzierte Expression von Surrogatmarkern für Zellantworten auf oxidativen Stress wurde in der Leber abgeschwächt. In der Leber und im Herzen wiesen die mit Doxo behandelten Tiere höhere mRNA Spiegel von an Zellzykluskontrolle beteiligten Faktoren sowie von DNA-Reparatur und Fremdstoffmetabolismus assoziierten Genen auf. Am stärksten wurde die Expression von Topoisomerase II alpha - ein molekularer Marker für Zellproliferation und bedeutsame Zielstruktur von Doxo - in der Leber hochreguliert. Die Statin-Kobehandlung verhinderte all diese Doxo-induzierten Expressionsänderungen. Im Gegensatz zur Leber wurde die Top2a-mRNA Menge im Herzen durch die Doxo-Applikation reduziert. Auch hier bewirkte die Kobehandlung mit dem Statin, dass die Expression nahe dem Kontrollniveau blieb. v: Die Kobehandlung mit Lova führte zu keinem Schutz der Tumorzellen vor Doxo, sondern erhöhte sogar dessen antineoplastisches Potential.rnFazit: Die Erkenntnisse aus vorhergegangenen in vitro Versuchen konnten zum großen Teil auf die in vivo Situation im Mausmodell übertragen werden. Sie stehen im Einklang mit Ergebnissen anderer Gruppen, welche die Inhibition kleiner GTPasen mit einer geringeren, durch zytotoxische Substanzen induzierten, Inflammation und Fibrose korrelieren konnten. Eine Kobehandlung mit Lova während einer Krebstherapie erscheint somit als vielversprechende Möglichkeit Doxo- oder IR-induzierte Nebenwirkungen auf Normalgewebe zu mildern.

Complementary mass spectrometric techniques for the characterization of the organic fraction in atmospheric aerosols

Aerosol particles are strongly related to climate, air quality, visibility and human health issues. They contribute the largest uncertainty in the assessment of the Earth´s radiative budget, directly by scattering or absorbing solar radiation or indirectly by nucleating cloud droplets. The influence of aerosol particles on cloud related climatic effects essentially depends upon their number concentration, size and chemical composition. A major part of submicron aerosol consists of secondary organic aerosol (SOA) that is formed in the atmosphere by the oxidation of volatile organic compounds. SOA can comprise a highly diverse spectrum of compounds that undergo continuous chemical transformations in the atmosphere.rnThe aim of this work was to obtain insights into the complexity of ambient SOA by the application of advanced mass spectrometric techniques. Therefore, an atmospheric pressure chemical ionization ion trap mass spectrometer (APCI-IT-MS) was applied in the field, facilitating the measurement of ions of the intact molecular organic species. Furthermore, the high measurement frequency provided insights into SOA composition and chemical transformation processes on a high temporal resolution. Within different comprehensive field campaigns, online measurements of particular biogenic organic acids were achieved by combining an online aerosol concentrator with the APCI-IT-MS. A holistic picture of the ambient organic aerosol was obtained through the co-located application of other complementary MS techniques, such as aerosol mass spectrometry (AMS) or filter sampling for the analysis by liquid chromatography / ultrahigh resolution mass spectrometry (LC/UHRMS).rnIn particular, during a summertime field study at the pristine boreal forest station in Hyytiälä, Finland, the partitioning of organic acids between gas and particle phase was quantified, based on the online APCI-IT-MS and AMS measurements. It was found that low volatile compounds reside to a large extent in the gas phase. This observation can be interpreted as a consequence of large aerosol equilibration timescales, which build up due to the continuous production of low volatile compounds in the gas phase and/or a semi-solid phase state of the ambient aerosol. Furthermore, in-situ structural informations of particular compounds were achieved by using the MS/MS mode of the ion trap. The comparison to MS/MS spectra from laboratory generated SOA of specific monoterpene precursors indicated that laboratory SOA barely depicts the complexity of ambient SOA. Moreover, it was shown that the mass spectra of the laboratory SOA more closely resemble the ambient gas phase composition, indicating that the oxidation state of the ambient organic compounds in the particle phase is underestimated by the comparison to laboratory ozonolysis. These observations suggest that the micro-scale processes, such as the chemistry of aerosol aging or the gas-to-particle partitioning, need to be better understood in order to predict SOA concentrations more reliably.rnDuring a field study at the Mt. Kleiner Feldberg, Germany, a slightly different aerosol concentrator / APCI-IT-MS setup made the online analysis of new particle formation possible. During a particular nucleation event, the online mass spectra indicated that organic compounds of approximately 300 Da are main constituents of the bulk aerosol during ambient new particle formation. Co-located filter analysis by LC/UHRMS analysis supported these findings and furthermore allowed to determine the molecular formulas of the involved organic compounds. The unambiguous identification of several oxidized C 15 compounds indicated that oxidation products of sesquiterpenes can be important compounds for the initial formation and subsequent growth of atmospheric nanoparticles.rnThe LC/UHRMS analysis furthermore revealed that considerable amounts of organosulfates and nitrooxy organosulfates were detected on the filter samples. Indeed, it was found that several nitrooxy organosulfate related APCI-IT-MS mass traces were simultaneously enhanced. Concurrent particle phase ion chromatography and AMS measurements indicated a strong bias between inorganic sulfate and total sulfate concentrations, supporting the assumption that substantial amounts of sulfate was bonded to organic molecules.rnFinally, the comprehensive chemical analysis of the aerosol composition was compared to the hygroscopicity parameter kappa, which was derived from cloud condensation nuclei (CCN) measurements. Simultaneously, organic aerosol aging was observed by the evolution of a ratio between a second and a first generation biogenic oxidation product. It was found that this aging proxy positively correlates with increasing hygroscopicity. Moreover, it was observed that the bonding of sulfate to organic molecules leads to a significant reduction of kappa, compared to an internal mixture of the same mass fractions of purely inorganic sulfate and organic molecules. Concluding, it has been shown within this thesis that the application of modern mass spectrometric techniques allows for detailed insights into chemical and physico-chemical processes of atmospheric aerosols.rn

Vascular endothelial cell-specific phosphotyrosine phosphatase (VE-PTP) activity is required for blood vessel development

VE-PTP, a receptor-type phosphotyrosine phosphatase, associates with the tyrosine kinase receptor Tie-2 and VE-cadherin and enhances the adhesive function of the latter. Here, VE-PTP was found to be restricted to endothelial cells, with a preference for arterial endothelium. Mutant mice expressing a truncated, secreted form of VE-PTP lacking the cytoplasmic and transmembrane domains and the most membrane-proximal extracellular fibronectin type III repeat, showed severe vascular malformations causing lethality at 10 days of gestation. Although blood vessels were initially formed, the intraembryonic vascular system soon deteriorated. Blood vessels in the yolk sac developed into dramatically enlarged cavities. In explant cultures of mutant allantoides, endothelial cells were found next to vessel structures growing as cell layers. No signs for enhanced endothelial apoptosis or proliferation were observed. Thus, the activity of VE-PTP is not required for the initial formation of blood vessels, yet it is essential for their maintenance and remodeling.

Grain size distribution in surface sediments samples of the continental shelf and slope of southeast Greenland

During "Meteor" Cruise 6/1966 in the northwest Atlantic a systematic survey of the bottom topography of the southeast Greenland continental margin was undertaken. Eighty-seven profiles transverse to the shelf edge at distances of 3-4 nautical miles and two longitudinal profiles parallel to the coast were carried out with the ELAC Narrow Beam Echo-Sounder giving a reliable record of even steep slopes. On the basis of the echo soundings the topography and morphology of the continental shelf and slope are evaluated. A detailed bathymetric chart and a serial profile chart were designed as working material for the morphological research. These maps along with the original echograms are morphometrically evaluated. The analysis of the sea bottom features is the basis of a subsequent morphogenetical interpretation, verified and extended by means of interpretation of magnetic data and sediment analysis (grain size, roundness, lithology). The results of the research are expressed in a geomorphological map. The primary findings can be summarized as follows: 1) The southeast Greenland shelf by its bottom topography can be clearly designated as a glacially formed area. The glacial features of the shelf can be classified into two zones nearly parallel to the coast: glacial erosion forms on the inner shelf and glacial accumulation forms on the outer shelf. The inner shelf is characterized by the rugged and hummocky topography of ice scoured plains with clear west/east slope asymmetry. On the outer shelf three types of glacial accumulation forms can be recognized: ice margin deposits with clearly expressed terminal moraines, glacial till plains and glaciomarine outwash fans. Both zones of the shelf can be subdivided into two levels of relief. The ice scoured plains, with average depths of 240 meters (m), are dissected to a maximum depth of 1060 m (Gyldenloves Trough) by trough valleys, which are the prolongations of the Greenland fjords. The banks of the outer shelf, with an average depth of 180 m, surround glacial basins with a maximum depth of 670 meters. 2) The sediments of the continental shelf can be classified as glacial due to their grain size distribution and the degree of roundness of the gravel particles. The ice margin deposits on the outer shelf can be recognized by their high percentage of gravels. On the inner shelf a rock surface is suggested, intermittently covered by glacial deposits. In the shelf troughs fine-grained sediments occur mixed with gravels. 3) Topography and sediments show that the southeast Greenland shelf was covered by an ice sheet resting on the sea floor during the Pleistocene ice-age. The large end moraines along the shelf edge probably indicate the maximum extent of the Wurm shelf ice resting on the sea floor. The breakthroughs of the end moraines in front of the glacial basins suggest that the shelf ice has floated further seaward over the increasing depths. 4) Petrographically the shelf sediments consist of gneisses, granites and basalts. While gneisses and granites occire on the nearby coast, basalt is not known to exist here. Either this material has been drifted by icebergs from the basalt province to the north or exists on the southeast Greenland shelf itself. The last interpretation is supported bythe high portion of basalt contained in the sediment samples taken and the strong magnetic anomalies probably caused by basaltic intrusions. 5) A magnetic profile allows the recognition of two magnetically differing areas which approximately coincide with the glacial erosion and accumulation zones. The inner shelf shows a strong and variable magnetic field because the glacially eroded basement forms the sea floor. The outer shelf is characterized by a weak and homogenous magnetic field, as the magnetized basement lies at greater depthy, buried by a thick cover of glacial sediments. The strong magnetic anomalies of the inner shelf are probably caused by dike swarms, similar to those observed further to the north in the Kangerdlugssuaq Fjord region. This interpretation is supported by the high basalt content of the sediment samples and the rough topography of the ice scoured plains which correlates in general with the magnetic fluctuations. The dike structures of the basement have been differentially eroded by the shelf ice. 6) The continental slope, extending from the shelf break at 313 m to a depth of 1270 m with an average slope of 11°, is characterized by delta-shaped projections in front of the shelf basins, by marginal plateaus, ridges and hills, by canyons and slumping features. The projections could be identified as glaciomarine sediment fans. This conclusion is supported by the strong decrease of magnetic field intensity. The deep sea hills and ridges with their greater magnetic intensities have to be regarded as basement outcrops projecting through the glaciomarine sediment cover. The upper continental rise, sloping seaward at about 2°, is composed of wide sediment fans and slump material. A marginal depression on the continental rise running parallel to the shelf edge has been identified. In this depression bottom currents capable of erosion have been recorded. South of Cape Farvel the depression extends to the accumulation zone of the "Eirik" sedimentary ridge. 7) By means of a study of the recent marine processes, postglacial modification of the ice-formed relief can be postulated. The retention effect of the fjord troughs and the high velocity of the East Greenland stream prevents the glacial features from being buried by sediments. Bottom currents capable of active erosion have only been found in the marginal depression on the continental rise. In addition, at the time of the lowest glacio-eustatic sea level, the shelf bottom was not situated in the zone of wave erosion. Only on the continental slope and rise bottom currents, sediment slumps and turbidity currents have led to significant recent modifications. Considering these results, the geomorphological development of the southeast Greenland continental terrace can be suggested as follows: 1. initial formation of a "peneplain", 2. fluvial incision, 3. submergence, and finally 4. glacial modification.

(Table 1) Mineralogy of veins in basalts at DSDP Hole 61-462A

Numerous veins are present in basalts recovered from Hole 462A, Leg 61 of the Deep Sea Drilling Project. Three mineral assemblages are recognized and stratigraphically controlled. These assemblages are (1) a zeolite-bearing, quartz-poor assemblage which occurs from Core 44 to the bottom of the hole and contains smectite, clinoptilolite, calcite, pyrite, ± chabazite, ± analcime, ± quartz, ± apophyllite, ± talc (?); (2) a quartz-rich, pyrite-bearing assemblage, found between Cores 19 and 29, which contains smectite, calcite, quartz, and pyrite; and (3) a quartz-rich, celadonite-bearing assemblage which occurs from Cores 14 through 17 and contains smectite, calcite, quartz, celadonite, and Fe oxide. These data are interpreted to represent two episodes of vein mineral formation with an oxidative overprint on the more recent. The first episode followed the outpourings of basaltic lavas onto the sea floor. Zeolite-bearing veins were formed at elevated temperatures under low PCO2 while the thermal gradient was high and before a cover of calcareous sediments had formed. The second mineralization episode followed injection of basalt and microdiabase sills into a thick layer of sediments, and produced all the vein minerals now occurring between Cores 14 and 29. These veins formed at lower temperature and higher PCO2 than zeolite-bearing veins. The presence of pyrite indicates a nonoxidative environment. After the initial formation of these veins, oxygenated seawater diffused through the sedimentary cover and oxidized the pyrite and smectite, forming celadonite and Fe oxides.

Geochemistry of ODP Leg 125 peridotites

Trace element analyses (first-series transition elements, Ti, Rb, Sr, Zr, Y, Nb, and REE) were carried out on whole rocks and minerals from 10 peridotite samples from both Conical Seamount in the Mariana forearc and Torishima Forearc Seamount in the Izu-Bonin forearc using a combination of XRF, ID-MS, ICP-MS, and ion microprobe. The concentrations of incompatible trace elements are generally low, reflecting the highly residual nature of the peridotites and their low clinopyroxene content (<2%). Chondrite-normalized REE patterns show extreme U shapes with (La/Sm)n ratios in the range of 5.03-250.0 and (Sm/Yb)n ratios in the range of 0.05-0.25; several samples show possible small positive Eu anomalies. LREE enrichment is common to both seamounts, although the peridotites from Conical Seamount have higher (La/Ce)n ratios on extended chondrite-normalized plots, in which both REEs and other trace elements are organized according to their incompatibility with respect to a harzburgitic mantle. Comparison with abyssal peridotite patterns suggests that the LREEs, Rb, Nb, Sr, Sm, and Eu are all enriched in the Leg 125 peridotites, but Ti and the HREEs exhibit no obvious enrichment. The peridotites also give positive anomalies for Zr and Sr relative to their neighboring REEs. Covariation diagrams based on clinopyroxene data show that Ti and the HREEs plot on an extension of an abyssal peridotite trend to more residual compositions. However, the LREEs, Rb, Sr, Sm, and Eu are displaced off this trend toward higher values, suggesting that these elements were introduced during an enrichment event. The axis of dispersion on these plots further suggests that enrichment took place during or after melting and thus was not a characteristic of the lithosphere before subduction. Compared with boninites sampled from the Izu-Bonin-Mariana forearc, the peridotites are significantly more enriched in LREEs. Modeling of the melting process indicates that if they represent the most depleted residues of the melting events that generated forearc boninites they must have experienced subsolidus enrichment in these elements, as well as in Rb, Sr, Zr, Nb, Sm, and Eu. The lack of any correlation with the degree of serpentinization suggests that low-temperature fluids were not the prime cause of enrichment. The enrichment in the high-field-strength elements also suggests that at least some of this enrichment may have involved melts rather than aqueous fluids. Moreover, the presence of the hydrous minerals magnesio-hornblende and tremolite and the common resorption of orthopyroxene indicate that this high-temperature peridotite-fluid interaction may have taken place in a water-rich environment in the forearc following the melting event that produced the boninites. The peridotites from Leg 125 may therefore contain a record of an important flux of elements into the mantle wedge during the initial formation of forearc lithosphere. Ophiolitic peridotites with these characteristics have not yet been reported, perhaps because the precise equivalents to the serpentinite seamounts have not been analyzed.

Aprender a enseñar juegos motores con otros : De saber jugar a intervenir como profesor de Educación Física

Durante la formación inicial, los estudiantes del profesorado de Educación Física construyen conocimientos teóricos y prácticos alrededor de prácticas corporales ya conocidas y vivenciadas. Aprenden sobre lo aprendido. Redefinen conocimientos prácticos en un nivel mayor de complejidad y abstracción asignándoles valor educativo que fundamentará su intervención profesional. Cuando le enseñan a proponer 'juegos no juegos' (actividades o deportes que presenta como juegos aunque no todos pueden jugar) el estudiante de Educación Física dispone de elementos teóricos que fundamentan el uso del juego como un recurso pedagógico (ya sea, como contenido de otros ejes, o como estrategia metodológica para la enseñanza de deportes o habilidades motoras). Sin embargo, cuando le enseñan a proponer juegos populares para divertirse, encuentra dificultad para planificar y justificar su futura intervención. Los resultados finales de una investigación cualitativa, presentada como tesis de maestría, muestran que en Educación Física se enseñan múltiples formas de juego motor con otros pero un solo modo de jugarlos: el no lúdico. Se enseña a subordinar el modo de jugar a la forma de los juegos propuestos por el profesor. Se enseña a moverse en el marco de lo permitido por las reglas del juego, a poner el cuerpo al servicio del juego

Aprender a enseñar juegos motores con otros : De saber jugar a intervenir como profesor de Educación Física

Durante la formación inicial, los estudiantes del profesorado de Educación Física construyen conocimientos teóricos y prácticos alrededor de prácticas corporales ya conocidas y vivenciadas. Aprenden sobre lo aprendido. Redefinen conocimientos prácticos en un nivel mayor de complejidad y abstracción asignándoles valor educativo que fundamentará su intervención profesional. Cuando le enseñan a proponer 'juegos no juegos' (actividades o deportes que presenta como juegos aunque no todos pueden jugar) el estudiante de Educación Física dispone de elementos teóricos que fundamentan el uso del juego como un recurso pedagógico (ya sea, como contenido de otros ejes, o como estrategia metodológica para la enseñanza de deportes o habilidades motoras). Sin embargo, cuando le enseñan a proponer juegos populares para divertirse, encuentra dificultad para planificar y justificar su futura intervención. Los resultados finales de una investigación cualitativa, presentada como tesis de maestría, muestran que en Educación Física se enseñan múltiples formas de juego motor con otros pero un solo modo de jugarlos: el no lúdico. Se enseña a subordinar el modo de jugar a la forma de los juegos propuestos por el profesor. Se enseña a moverse en el marco de lo permitido por las reglas del juego, a poner el cuerpo al servicio del juego

Neogene and Quaternary paleoenvironmental history at DSDP Leg 71 Holes

The Neogene and Quaternary sedimentary record of Leg 71 and previously drilled sequences from the Southern Ocean reveal evidence of a major late Miocene change of oceanic and glacial conditions in the southern high latitudes during paleomagnetic Chron 9. The characteristics of late Miocene sedimentation and in particular the study of erosional patterns and ice-rafted debris suggest the following conclusions. 1) In the late Miocene, the Polar Front first migrated to the northern latitudes of the Southern Ocean and surface water temperatures became similar to those of today. 2) Extensive ice shelves or ice tongues were not present along the Antarctic margin until late Chron 9 (about 9.0 Ma). 3) Before Chron 9, West Antarctica was occupied by an archipelago and the West Antarctic Sea. 4) Extensive ice shelves formed in the West Antarctic region, eventually coalescing and thickening to form the grounded West Antarctic ice sheet by Chron 9. 5) The newly formed West Antarctic ice sheet was probably unstable and frequently became an ungrounded ice shelf, thus accounting for the scarcity of late Miocene ice-rafted debris. 6) Extensive erosion or nondeposition of sediment was probably the result of increased Antarctic Bottom Water (AABW) formation in the West Antarctic region during the initial formation of extensive West Antarctic ice shelves and during periods when the West Antarctic ice sheet was ungrounded. 7) In the Southwest Atlantic, AABW velocity waned during the latest Miocene. During the late Gilbert Chron a major and permanent change occurred in the pattern of ice-rafting to the South Atlantic, and after 4.35 Ma the increased IRD accumulation rate and frequency of major episodes of IRD accumulation suggest increased stability of the West Antarctic ice sheet. In addition, radiolarian faunas of Hole 514 record at least eight migrations of the Polar Front to the north of the site during the past 4.07 m.y. An apparent increase in the frequency of Polar Front migrations occurred about 2.7-2.6 Ma, possibly in response to oceanic change induced by fluctuations in glacial conditions of the Northern Hemisphere.

Aprender a enseñar juegos motores con otros : De saber jugar a intervenir como profesor de Educación Física

Durante la formación inicial, los estudiantes del profesorado de Educación Física construyen conocimientos teóricos y prácticos alrededor de prácticas corporales ya conocidas y vivenciadas. Aprenden sobre lo aprendido. Redefinen conocimientos prácticos en un nivel mayor de complejidad y abstracción asignándoles valor educativo que fundamentará su intervención profesional. Cuando le enseñan a proponer 'juegos no juegos' (actividades o deportes que presenta como juegos aunque no todos pueden jugar) el estudiante de Educación Física dispone de elementos teóricos que fundamentan el uso del juego como un recurso pedagógico (ya sea, como contenido de otros ejes, o como estrategia metodológica para la enseñanza de deportes o habilidades motoras). Sin embargo, cuando le enseñan a proponer juegos populares para divertirse, encuentra dificultad para planificar y justificar su futura intervención. Los resultados finales de una investigación cualitativa, presentada como tesis de maestría, muestran que en Educación Física se enseñan múltiples formas de juego motor con otros pero un solo modo de jugarlos: el no lúdico. Se enseña a subordinar el modo de jugar a la forma de los juegos propuestos por el profesor. Se enseña a moverse en el marco de lo permitido por las reglas del juego, a poner el cuerpo al servicio del juego