Quema de libros y antitotalitarismo : Manuel Rivas Los libros arden mal y Ray Bradbury Fahrenheit 451

El presente artículo se propone comparar dos novelas cuyo común denominador es el compromiso antitotalitario con motivo de la quema de libros considerada como el culmen de la barbarie anticultural, a saber Los libros arden mal (2006) de Manuel Rivas y Fahrenheit 451 (1953) de Ray Bradbury. Partiendo de las reflexiones de Fernando Rodríguez de la Flor en torno al biblioclasmo (2004), el paralelo se centra en los siguientes aspectos: la descripción zoo- y antropomorfizada de los libros en llamas; el biblioclasmo como expresión del totalitarismo, denotando asimismo una relación ambivalente y dialéctica entre cultura y barbarie; los movimientos subversivos dedicados a mantener el culto al libro y la tradición filosófico-literaria; la intertextualidad y el papel destacado de la Biblia en cuanto Libro de los libros. En conclusión se podrá constatar que, a pesar de numerosos puntos en común, en particular su compromiso antitotalitario, ambos autores se distinguen en concreto por su orientación política y el enfoque de su crítica cultural.

(Table, page 13-59), Annotated record of the detailed examination of Mn deposits from Amphitrite Expedition stations

The cores described in this report were taken on AMPHITRITE Expedition in Decenber 1963 - February 1964 by Scripps Institution of Oceanography from, the R/V Argo. A total of 148 cores were recovered and are available at Scripps for sampling and study. The coring sites, all in the tropical central Pacific. The AMPHITRITE cores are here briefly described to identify visually distinct units based on lithology, color, texture, or other characteristic unique to an interval of sediment. For determination of lithology, the slides prepared from samples of the cores were examined microscopically in conjuction with the visual examination.

Data compilation of ESOP

The work in this sub-project of ESOP focuses on the advective and convective transforma-tion of water masses in the Greenland Sea and its neighbouring areas. It includes observational work on the sub-mesoscale and analysis of hydrographic data up to the gyre-scale. Observations of active convective plumes were made with a towed chain equipped with up to 80 CTD sensors, giving a horizontal and vertical resolution of the hydrographic fields of a few metres. The observed scales of the penetrative convective plumes compare well with those given by theory. On the mesoscale the structure of homogeneous eddies formed as a result of deep convection was observed and the associated mixing and renewal of the intermediate layers quantified. The relative importance and efficiency of thermal and haline penetrative convection in relation to the surface boundary conditions (heat and salt fluxes and ice cover) and the ambient stratification are studied using the multi year time series of hydro-graphic data in the central Greenland Sea. The modification of the water column of the Greenland Sea gyre through advection from and mixing with water at its rim is assessed on longer time scales. The relative contributions are quantified using modern water mass analysis methods based on inverse techniques. Likewise the convective renewal and the spreading of the Arctic Intermediate Water from its formation area is quantified. The aim is to budget the heat and salt content of the water column, in particular of the low salinity surface layer, and to relate its seasonal and interannual variability to the lateral fluxes and the fluxes at the air-sea-ice interface. This will allow to estimate residence times for the different layers of the Greenland Sea gyre, a quantity important for the description of the Polar Ocean carbon cycle.