La producción discursiva en la traducción de textos pragmáticos francés/castellano : Estudio traductológico a través de los enunciados elípticos con anomalías

Esta tesis doctoral se inscribe dentro de la Traductología, interdisciplina que estudia tanto los procesos implicados en el complejo fenómeno de la traducción como los productos discursivos en la lengua hacia la cual se traduce. Su objetivo general consiste en contribuir a la investigación sobre el macroproceso de traducción en el par de lenguas francés/español, y en especial sobre la producción discursiva puesto que la literatura especializada coincide en destacar que ésta es la fase menos conocida [Lederer, 2005, 126; Toury, 2004, 244, 245]. Nuestro trabajo explora la producción discursiva, limitándola a traducciones absolutas [Gouadec, 1989: 21-30] de textos pragmáticos [Delisle, 1984: 22], cuya función esencial es el pasaje integral de la información. Dentro de dos corpora del campo de la Bioética constituidos por textos originales en francés y sus traducciones al castellano, hemos considerado como hipótesis general que los productos discursivos resultantes de la traducción absoluta de textos pragmáticos francés/castellano, presentan transferencias sintáctico-discursivas gobernadas por el universal de interferencia. Es decir que el planteo rector es que la memoria lingüístico-discursiva en la fase de reexpresión está atravesada por el mecanismo de interferencia. Las hipótesis específicas que se desgranan de la principal indican que la producción discursiva resultante de la traducción de textos pragmáticos francés/castellano exhibe enunciados elípticos anómalos gobernados por el universal de interferencia del discurso de partida [francés] o del sistema de la lengua materna del traductor [castellano]. Nuestra investigación parte entonces de la lectura del texto traducido [TT] y lo compara con el texto original [TO]; esta comparación es parcial puesto que indaga sobre las anomalías de producción; es indirecta pues observa la relación cohesión-coherencia-sentido en el discurso de llegada a través de las anomalías, especialmente de los enunciados elípticos; por último, analiza las anomalías dentro de la teoría de la interferencia y de la teoría de la elipsis [Toury, 2004: 121-124]. Sobre estas bases, hemos generado un instrumento que estudia los binomios textuales seleccionados según las siguientes aproximaciones: la sintaxis de la lengua meta [tipo de elipsis, elemento elidido, construcción de la elipsis, recuperabilidad]; la sintaxis del discurso meta [cohesión-coherencia], la comparación del binomio TT-TO [análisis de la producción del segmento problema en TO; el análisis de la producción del segmento solución en TT; posible extensión de las consecuencias de la anomalía microestructural; verificación del principio traducir toda la información]; los mecanismos de producción [elevación de la frecuencia de uso de recursos o elementos; control lingüístico de la lengua-cultura meta; control lingüístico-discursivo]; el resultado [visibilidad de interferencia; fenómeno sintáctico visible; alcance discursivo; producción palimpséstica; entropía informativa]. La elaboración de este andamiaje analítico aplicado a nuestros corpora nos ha permitido avanzar en el conocimiento de los mecanismos que participan en la producción discursiva en traducción y creemos que puede aplicarse, con las modificaciones de cada caso, para la descripción y quizás explicación de otros factores lingüístico-discursivos presentes en los textos traducidos

Compaction curves and sediment characteristics of ODP Leg 165 and Leg 130 sites

Compaction curves for 11 samples from the mixed sediments and calcareous chalk with clay from the Caribbean Sites 999 and 1001 are discussed with reference to compaction curves for calcareous ooze and chalk of the Ontong Java Plateau (Leg 130). The burial history is discussed from preconsolidation data and present burial conditions and suggests a removal of ~400 m of sediment at the hiatus 166 meters below seafloor (mbsf) at Site 1001. This interpretation predicts a previous burial to >500 mbsf for depth intervals containing microstylolites, which corresponds to observations at Sites 999 and 807 (Ontong Java Plateau). Thus, data from three sites from two widely separate regions indicate that microstylolites in carbonates form at minimum burial depths deeper than 500 m. No direct link between formation of microstylolites and cementation was found, suggesting that dissolution and precipitation are not necessarily related. Porosity rebound during core retrieval could not be detected for soft sediments, whereas a porosity rebound of ~2% was deduced for deeper, cemented intervals. Comparing the compaction curves, two distinct rates of porosity loss are noted: (1) samples dominated by clay (>45% insoluble residue) compact at a higher rate than samples dominated by fine-grained carbonate and (2) fine-grained carbonate supported samples (with <45% insoluble residue) compact at the same rate irrespective of the content of nonsupporting microfossils or pore-filling clay.

Spores and pollen at DSDP Holes 36-330 and 71-511

Samples from Upper Jurassic and Lower Cretaceous sediments at Site 511 were analyzed for palynomorphs. Three palynological assemblages were identified: Upper Jurassic (presumably Tithonian), Neocomian-Aptian, and lower Albian. These were correlated to synchronous assemblages in Argentina, South Africa, and Australia and were compared with Jurassic palynoassemblages from Hole 330, Leg 36.

Geochemical data from pore water and solids from cores GS08-153-91GC12 and GS08-153-53-GC6, Arctic Mid-Ocean Ridge

Microbial communities and their associated metabolic activity in marine sediments have a profound impact on global biogeochemical cycles. Their composition and structure are attributed to geochemical and physical factors, but finding direct correlations has remained a challenge. Here we show a significant statistical relationship between variation in geochemical composition and prokaryotic community structure within deep-sea sediments. We obtained comprehensive geochemical data from two gravity cores near the hydrothermal vent field Loki's Castle at the Arctic Mid-Ocean Ridge, in the Norwegian-Greenland Sea. Geochemical properties in the rift valley sediments exhibited strong centimeter-scale stratigraphic variability. Microbial populations were profiled by pyrosequencing from 15 sediment horizons (59,364 16S rRNA gene tags), quantitatively assessed by qPCR, and phylogenetically analyzed. Although the same taxa were generally present in all samples, their relative abundances varied substantially among horizons and fluctuated between Bacteria- and Archaea-dominated communities. By independently summarizing covariance structures of the relative abundance data and geochemical data, using principal components analysis, we found a significant correlation between changes in geochemical composition and changes in community structure. Differences in organic carbon and mineralogy shaped the relative abundance of microbial taxa. We used correlations to build hypotheses about energy metabolisms, particularly of the Deep Sea Archaeal Group, specific Deltaproteobacteria, and sediment lineages of potentially anaerobic Marine Group I Archaea. We demonstrate that total prokaryotic community structure can be directly correlated to geochemistry within these sediments, thus enhancing our understanding of biogeochemical cycling and our ability to predict metabolisms of uncultured microbes in deep-sea sediments.

Geochemistry and stable isotope record of carbonate oozes and chalks of ODP Hole 130-807B

Light greenish gray and pale purple color bands are common in the ooze and chalk of the Ontong Java Plateau. Analyses of Pleistocene and Pliocene ooze samples that contain abundant bands indicate that the purple bands are colored by finely disseminated iron sulfide, whereas the green bands are colored by finely disseminated Fe- and Al-bearing silicates (probably clays). No local contrasts in the total organic carbon contents, carbon and oxygen isotopic compositions, and grain sizes were found. Band abundances, counted from core photographs of all Leg 130 holes, can be correlated from hole to hole on the basis of age rather than depth. The temporal distribution of these color bands is also comparable with that of the green bands described from the Lord Howe Rise, which were previously interpreted as products of altered volcanic glass. This may indicate that the green and purple bands on the Ontong Java Plateau originate from the early alteration of volcanic ash. The crosscutting relationships between the green and purple bands and original structures in the host sediment indicate that the bands have been locally altered by redox conditions in the sediments after the bands were formed.