Analyse des processus de traduction : Considérations épistémologiques et pedagogiques

Analyse des processus de traduction considérations épistémologiques et pedagogiques Le présent article se propose, après avoir situé les études empiriques en traduction dans un cadre large, intégrant la linguistique et la terminologie, d'apprécier la valeur épistémologique et pratique de ces études, notamment de celles qui utilisent le protocole de verbalisation (en anglais, think-aloud protocol, TAP)

El proceso de implementación de la enseñanza de español en la ciudad de Cabo de Santo Agostinho (Pernambuco, Brasil)

La provincia de Pernambuco es un importante escenario de la educación del Nordeste de Brasil. En lo que se refiere a la enseñanza de la Lengua Española, en la Enseñanza Fundamental y Media, se destaca la ciudad de Cabo de Santo Agostinho por ser pionera en la implementación del español en la Red Municipal. La discusión sobre la influencia hispánica en la ciudad empezó cuando algunos expertos, a través de estudios académicos, concluyeron que el navegador español Vicente Yáñez Pinzón arribó a tierras cabenses tresmeses antes que el portugués Pedro Álvares Cabral. Debido a eso, y a la importancia de Brasil en MERCOSUR, el Ayuntamiento de Cabo, a través de un proyecto de Ley, implementó el español como segunda lengua extranjera. Por esta razón, los docentes tuvieron formación continua ofrecida por La Facultad de Formación de Profesores de Olinda. Actualmente, la Coordinación de Lenguas de Cabo de Santo Agostinho realizó el I Encuentro Hispanoamérica de Cabo, el I Congreso Pernambucano de Profesores de Español y el I Simposio de Formación de Profesores de Español en Conmemoración a los veinte años de la Asociación de Profesores de Español de Pernambuco.

El proceso de implementación de la enseñanza de español en la ciudad de Cabo de Santo Agostinho (Pernambuco, Brasil)

La provincia de Pernambuco es un importante escenario de la educación del Nordeste de Brasil. En lo que se refiere a la enseñanza de la Lengua Española, en la Enseñanza Fundamental y Media, se destaca la ciudad de Cabo de Santo Agostinho por ser pionera en la implementación del español en la Red Municipal. La discusión sobre la influencia hispánica en la ciudad empezó cuando algunos expertos, a través de estudios académicos, concluyeron que el navegador español Vicente Yáñez Pinzón arribó a tierras cabenses tresmeses antes que el portugués Pedro Álvares Cabral. Debido a eso, y a la importancia de Brasil en MERCOSUR, el Ayuntamiento de Cabo, a través de un proyecto de Ley, implementó el español como segunda lengua extranjera. Por esta razón, los docentes tuvieron formación continua ofrecida por La Facultad de Formación de Profesores de Olinda. Actualmente, la Coordinación de Lenguas de Cabo de Santo Agostinho realizó el I Encuentro Hispanoamérica de Cabo, el I Congreso Pernambucano de Profesores de Español y el I Simposio de Formación de Profesores de Español en Conmemoración a los veinte años de la Asociación de Profesores de Español de Pernambuco.

Per-field land use and land cover data set of the Haean catchment, South Korea

Detailed data on land use and land cover constitute important information for Earth system models, environmental monitoring and ecosystem services research. Global land cover products are evolving rapidly; however, there is still a lack of information particularly for heterogeneous agricultural landscapes. We censused land use and land cover field by field in the agricultural mosaic catchment Haean in South Korea. We recorded the land cover types with additional information on agricultural practice. In this paper we introduce the data, their collection and the post-processing protocol. Furthermore, because it is important to quantitatively evaluate available land use and land cover products, we compared our data with the MODIS Land Cover Type product (MCD12Q1). During the studied period, a large portion of dry fields was converted to perennial crops. Compared to our data, the forested area was underrepresented and the agricultural area overrepresented in MCD12Q1. In addition, linear landscape elements such as waterbodies were missing in the MODIS product due to its coarse spatial resolution. The data presented here can be useful for earth science and ecosystem services research.

Petrology of ODP Leg 210 and Leg 173, and DSDP Leg 47 sites

Sand detrital modes of Albian-Eocene clastic gravity-flow deposits cored and recovered at Ocean Drilling Program Site 1276 reflect the postrift geologic evolution of the Newfoundland passive continental margin. Cretaceous sandstone compositions (average: Q57F23L20; Ls%Lsc = 35; total%bioclasts = 3) are consistent with a source on Grand Banks such as Avalon Uplift. Their relatively low potassium feldspar (Qm71K8P21) contents distinguish them from Iberian sandstones and appear to preclude an easterly source during the early history of the ocean basin. Isolated volcaniclastic input near the Paleocene/Eocene boundary (~60 Ma) at Site 1276 is also present in Iberian samples of this age, suggesting that magmatism was widespread across the North Atlantic during this time frame; the source(s) of this volcanic debris remains equivocal. In the Eocene, the development of carbonate bank facies on the shelf marks a profound compositional change to calcareous grainstones (average: Q27F11L62; Ls%Lsc = 82; total%bioclasts = 55) in basinal gravity-flow deposits at Site 1276. This calcareous petrofacies is present on the Iberian margin and in the Pyrenees, suggesting that it was a regional event. The production and downslope redistribution of carbonate debris, including bioclastic and lithic fragments, was likely eustatically controlled. The Newfoundland (Site 1276 and Jeanne d'Arc Basin) sandstones are mainly quartzolithic. Their composition and the contrast in composition between them and more quartzofeldspathic sandstones from the Iberian margin are likely a product of rifting along a Paleozoic suture zone separating distinct basement terranes. This prerift geologic setting contrasts with that of rifts developed within other cratonic settings with variable amounts of synrift volcanism. When synthesized, the spectrum of synrift and postrift sand compositions produces a general model of passive margin (rift-to-drift) sandstone provenance.

Glacial-interglacial sediment record from the North Atlantic

Studies from the subtropical western and eastern Atlantic Ocean, using the 231Pa/230Th ratio as a kinematic proxy for deep water circulation, provided compelling evidence for a strong link between climate and the rate of meridional overturning circulation (MOC) over the last deglaciation. In this study, we present a compilation of existing and new sedimentary 231Pa/230Th records from North Atlantic cores between 1710 and 4550 m water depth. Comparing sedimentary 231Pa/230Th from different depths provides new insights into the evolution of the geometry and rate of deep water formation in the North Atlantic during the last 20,000 years. The 231Pa/230Th ratio measured in upper Holocene sediments indicates slow water renewal above ?2500 m and rapid flushing below, consistent with our understanding of modern circulation. In contrast, during the Last Glacial Maximum (LGM), Glacial North Atlantic Intermediate Water (GNAIW) drove a rapid overturning circulation to a depth of at least ?3000 m depth. Below ~4000 m, water renewal was much slower than today. At the onset of Heinrich event 1, transport by the overturning circulation declined at all depths. GNAIW shoaled above 3000 m and significantly weakened but did not totally shut down. During the Bølling-Allerød (BA) that followed, water renewal rates further decreased above 2000 m but increased below. Our results suggest for the first time that ocean circulation during that period was quite distinct from the modern circulation mode, with a comparatively higher renewal rate above 3000 m and a lower renewal rate below in a pattern similar to the LGM but less accentuated. MOC during the Younger Dryas appears very similar to BA down to 2000 m and slightly slower below.