Verbal comprehension of university students

En este trabajo se comunican los resultados preliminares de una investigación más amplia sobre desempeño y autopercepción en lectura y escritura de alumnos universitarios. Se trata en este caso de los resultados en comprensión verbal, dadas las relaciones que guarda con la comprensión lectora. Esta última constituye un aspecto crítico, particularmente en la construcción del modelo de situación , que se logra vía integración de la información proporcionada por el texto con el conocimiento previo relevante. Para su estudio se seleccionó una muestra piloto aleatoria de 60 alumnos de tercer año, de ambos sexos, de 23 años de edad promedio, a los que se les aplicó colectivamente las pruebas Vocabulario, Información y Analogías del WAIS III. Los resultados en el Índice de Comprensión Verbal muestran medidas de tendencia central semejantes a los de la muestra de tipificación y una dispersión menor, con casos particulares con puntuaciones en el límite inferior del promedio. Se hacen observaciones respecto del desempeño en población universitaria y sobre algunas particularidades acerca del tipo de errores en las respuestas proporcionadas, que merecen consideraciones adicionales. En principio indican ausencia e insuficiencia de información, confusiones conceptuales en algunos términos de uso relativamente frecuente y dificultades en la formación de conceptos, situación a ser atendida por sus implicaciones en el aprendizaje exitoso a partir de los textos.

Comprensión verbal en alumnos universitarios

En este trabajo se comunican los resultados preliminares de una investigación más amplia sobre desempeño y autopercepción en lectura y escritura de alumnos universitarios. Se trata en este caso de los resultados en comprensión verbal, dadas las relaciones que guarda con la comprensión lectora. Esta última constituye un aspecto crítico, particularmente en la construcción del modelo de situación , que se logra vía integración de la información proporcionada por el texto con el conocimiento previo relevante. Para su estudio se seleccionó una muestra piloto aleatoria de 60 alumnos de tercer año, de ambos sexos, de 23 años de edad promedio, a los que se les aplicó colectivamente las pruebas Vocabulario, Información y Analogías del WAIS III. Los resultados en el Índice de Comprensión Verbal muestran medidas de tendencia central semejantes a los de la muestra de tipificación y una dispersión menor, con casos particulares con puntuaciones en el límite inferior del promedio. Se hacen observaciones respecto del desempeño en población universitaria y sobre algunas particularidades acerca del tipo de errores en las respuestas proporcionadas, que merecen consideraciones adicionales. En principio indican ausencia e insuficiencia de información, confusiones conceptuales en algunos términos de uso relativamente frecuente y dificultades en la formación de conceptos, situación a ser atendida por sus implicaciones en el aprendizaje exitoso a partir de los textos

Benthic foraminifera across the Cretaceous/Paleogene boundary in the Southern Ocean

The impact of an asteroid at the Cretaceous/Paleogene (K/Pg) boundary triggered dramatic biotic, biogeochemical and sedimentological changes in the oceans that have been intensively studied. Paleo-biogeographical differences in the biotic response to the impact and its environmental consequences, however, have been less well documented. We present a high-resolution analysis of benthic foraminiferal assemblages at Southern Ocean ODP Site 690 (Maud Rise, Weddell Sea, Antarctica). At this high latitude site, late Maastrichtian environmental variability was high, but benthic foraminiferal assemblages were not less diverse than at lower latitudes, in contrast to those of planktic calcifiers. Also in contrast to planktic calcifiers, benthic foraminifera did not suffer significant extinction at the K/Pg boundary, but show transient assemblage changes and decreased diversity. At Site 690, the extinction rate was even lower (~3%) than at other sites. The benthic foraminiferal accumulation rate varied little across the K/Pg boundary, indicating that food supply to the sea floor was affected to a lesser extent than at lower latitude sites. Compared to Maastrichtian assemblages, Danian assemblages have a lower diversity and greater relative abundance of heavily calcified taxa such as Stensioeina beccariiformis and Paralabamina lunata. This change in benthic foraminiferal assemblages could reflect post-extinction proliferation of different photosynthesizers (thus food for the benthos) than those dominant during the Late Cretaceous, therefore changes in the nature rather than in the amount of the organic matter supplied to the seafloor. However, severe extinction of pelagic calcifiers caused carbonate supersaturation in the oceans, thus might have given competitive advantage to species with large, heavily calcified tests. This indirect effect of the K/Pg impact thus may have influenced the deep-sea dwellers, documenting the complexity of the effects of major environmental disturbance.

Response of nannoplankton to major changes in sea-surface temperature at the South Chatham Rise, southeastern New Zealand

A high-resolution history of paleoceanographic changes in the subpolar waters of the southern margin of the Subtropical Convergence Zone during the last 130 kyr, is present in foraminiferal assemblages of DSDP Site 594. The foraminifera indicate that sea-surface temperatures during the Last Interglacial Climax were warmer than today, and that between substage 5d through to the end of isotope stage 2, temperatures were mostly cooler than Holocene temperatures. The paleotemperatures suggest that (1) the Subtropical Convergence was located over the site during substage 5e, later moving further north, then moving southwards to near the site during the Holocene, and (2) the Polar Front was positioned over the Site during glacial stages 6, 4, 2 and possibly parts of stage 3. Several major events are indicated by the nannofloral assemblages during these large changes in sea-surface temperature and associated reorganization of ocean circulation. First, the time-progressive trends between E. huxleyi and medium to large Gephyrocupsa are unique to this site, with E. huxleyi dominating over medium Gephyrocupsa during stages 5c-a, middle part of stage 4 and after the middle point of stage 3. This unusual trend may (at least partly) be caused by the shift of the Polar Front across the site. Second, upwelling flora (E. huxleyi and small placoliths) increase in abundance during stages 1, 3 and 5, suggesting that upwelling or disturbance of water stratification took place during the interglacials. Thirdly, there are no significant differences between the distribution patterns of the various morphotypes of medium to large Gephyrocupsu, and the combined value of all medium Gephyrocupsu increases in abundance during glacials (stages 2 and 4 and the end of stage 6), similar to the abundance trends in benthic foraminifera. Finally, subordinate nannofossil taxa also show distinctive climatic trends during the last glacial cycle: (1) Syrucosphaera spp. are present in increased abundance during warmer extremes in climate (substages 5e, 5a, and stage 1); (2) Coccolithus pelagicus and Culcidiscus leptoporus dominate the subordinate nannofossil taxa, and their relative proportions seem to provide a useful paleoceanographic index, with C. pelagicus dominating when the Polar Front Zone is over the site (stages 6, 4 and 2), whilst C. leptoporus is relatively more abundant when the STC is positioned over the site (stages 1 and 5e). Increased abundance of C. pelagicus also can indicate intensified coastal upwelling.

Southern Ocean CO2 uptake and buffer factor from model run 2012-2100, with links to model results

The Southern Ocean is a key region for global carbon uptake and is characterised by a strong seasonality with the annual CO2 uptake being mediated by biological carbon draw-down in summer. Here, we show that the contribution of biology to CO2 uptake will become even more important until 2100. This is the case even if biological production remains unaltered and can be explained by the decreasing buffer capacity of the ocean as its carbon content increases. The same amount of biological carbon draw-down leads to a more than twice as large reduction in CO2 (aq) concentration and hence to a larger CO2 gradient between ocean and atmosphere that drives the gas-exchange. While the winter uptake south of 44°S changes little, the summer uptake increases largely and is responsible for the annual mean response. The combination of decreasing buffer capacity and strong seasonality of biological carbon draw-down introduces a strong and increasing seasonality in the anthropogenic carbon uptake.

Impact of CO2-driven acidification on the development of the sea cucumber Apostichopus japonicus (Selenka) (Echinodermata: Holothuroidea)

We evaluated the impact of ocean acidification on the early development of sea cucumber Apostichopus japonicus. The effect of pH-levels (pH 8.04, 7.85, 7.70 and 7.42) were tested on post-fertilization success, developmental (stage duration) and growth rates. Post-fertilization success decreased linearly with pH leading to a 6% decrease at pH 7.42 as compared to pH 8.1. The impact of pH on developmental time was stage-dependent: (1) stage duration increased linearly with decreasing pH in early-auricularia stage; (2) decreased linearly with decreasing pH in the mid-auricularia stage; but (3) pH decline had no effect on the late-auricularia stage. At the end of the experiment, the size of doliolaria larvae linearly increased with decreasing pH. In conclusion, a 0.62 unit decrease in pH had relatively small effects on A. japonicus early life-history compared to other echinoderms, leading to a maximum of 6% decrease in post-fertilization success and subtle effects on growth and development.

Politics of the 1945 Constitution:Democratization and Its Impact on Political Institutions in Indonesia

Introduction : Before 1998, no one could think about the amendment of the 1945 Constitution. The 1945 Constitution was a product of nationalist who had hard fought for independence from the Dutch colonization. This historical background made it the symbol of independence of the Indonesian nation. Thus, it has been considered as forbidden to touch contents of the 1945 Constitution whereas political leaders have legitimized their authoritarian rulership by utilizing a symbolic character of the Constitution. With the largest political turmoil since its independence, that is, a breakdown of authoritarian regime and democratic transformation in 1998-1999, however, a myth of the "sacred and inviolable" constitution has disappeared. A new theme has then aroused: how can the 1945 Constitution be adapted for a new democratic regime in Indonesia? 　　　The Indonesian modern state has applied the 1945 Constitution as the basic law since its independence in 1945, except for around 10 years in the 1950s. In the period of independence struggle, contrary to the constitutional provision that a kind of presidential system is employed, a cabinet responsible for the Central National Committee was installed. Politics under this institution was in practice a parliamentary system of government. After the Dutch transferred sovereignty to Indonesia in 1949, West European constitutionalism and party politics under a parliamentary system was fully adopted with the introduction of two new constitutions: the 1949 Constitution of Federal Republic of Indonesia and the 1950 Provisional Constitution of Republic of Indonesia. Since a return from the 1950 Constitution to the 1945 Constitution was decided with the Presidential Decree in 1959, the 1945 Constitution had supported two authoritarian regimes of Soekarno's "Guided Democracy" and Soeharto's "New Order" as a legal base. When the 32-year Soeharto's government fell down and democratization started in 1998, the 1945 Constitution was not replaced with a new one, as seen in many other democratizing countries, but successively reformed to adapt itself to a new democratic regime. In the result of four constitutional amendments in 1999-2002, political institutions in Indonesia are experiencing a transformation from an authoritative structure, in which the executive branch monopolized power along with incompetent legislative and judicial branches, to a modern democratic structure, in which the legislative branch can maintain predominance over the executive. However, as observed that President Abdurrahman Wahid, the first president ever elected democratically in Indonesian history, was impeached after one and a half years in office, democratic politics under a new political institution has never been stable. 　　　Under the 1945 Constitution, how did authoritarian regimes maintain stability? Why can a democratic regime not achieve its stability? What did the two constitutional amendments in the process of democratization change? In the first place, how did the political institutions stipulated by the 1945 Constitution come out? Through answering the above questions, this chapter intends to survey the historical continuity and change of political institutions in Indonesia along with the 1945 Constitutions and to analyze impact of regime transformation on political institutions. First, we examine political institutions stipulated by the original 1945 Constitution as well as historical and philosophical origins of the constitution. Second, we search constitutional foundations in the 1945 Constitution that made it possible for Soekarno and Soeharto to establish and maintain authoritarian regimes. Third, we examine contents of constitutional amendments in the process of democratization since 1998. Fourth, we analyze new political dynamics caused by constitutional changes, looking at the impeachment process of President Abdurrahman Wahid. Finally, we consider tasks faced by Indonesia that seeks to establish a stable democracy.

Accession clause of TPP : Is it really open?

One of the most important policy questions relating to the future impact of the Trans-Pacific Partnership on the global and regional economy is whether other countries in the region, particularly China, will join the partnership. While several commentators have made some observations regarding the future prospects of TPP expansion, little scholarly analysis has been conducted. To go beyond the speculation of a certain country's accession to TPP, we first attempt to generalize the issue before moving on to a specific question. We conduct a comparative analysis of a large number of regional trade agreements for a better understanding of the parameters of RTAs that are critical for membership expansion. This general framework enables us to conduct a systematic examination of specific membership expansion cases, such as China's membership in TPP. The paper also proposes a necessary "accession practice" that truly facilitates new members' participation.

An Experimental and Numerical Study of Ballistic Impacts on a Turbine Casing Material at Varying Temperatures

An experimental and numerical study of ballistic impacts on steel plates at various temperatures (700ºC, 400ºC and room temperature) has been carried out. The motivation for this work is the blade‐off event that may occur inside a jet engine turbine. However, as a first attempt to understand this complex loading process, a somewhat simpler approach is carried out in the present work. The material used in this study is the FV535 martensitic stainless steel, which is one of the most commonly used materials for turbine casings. Based on material test data, a Modified Johnson‐Cook (MJC) model was calibrated for numerical simulations using the LS‐DYNA explicit finite element code (see Figure 1). To check the mesh size sensitivity, 2D axisymmetric finite element models with three different mesh sizes and configurations were used for the various temperatures. Two fixed meshes with 64 and 128 elements over the 2mm thick plate and one mesh with 32 elements over the thickness with adaptive remeshing were used in the simulations. The formation of adiabatic shear bands in the perforation process has been found critical in order to achieve good results. Adiabatic shear bands are formed by the temperature rise due to the accumulation of plastic strain during impact (see Figure 2). The influence of the thermal softening in the plastic model has hence been analyzed for the room temperature impact tests, where the temperature gradient is highest