A time-slice study in Heinrich Stadial 1 and Mid Holocene sediment cores off northern Senegal

Sediment dynamics in limnic, fluvial and marine environments can be assessed by granulometric and rock-magnetic methodologies. While classical grain-size analysis by sieving or settling mainly bears information on composition and transport, the magnetic mineral assemblages reflect to a larger extent the petrology and weathering conditions in the sediment source areas. Here, we combine both methods to investigate Late Quaternary marine sediments from five cores along a transect across the continental slope off Senegal. This region near the modern summer Intertropical Convergence Zone is particularly sensitive to climate change and receives sediments from several aeolian, fluvial and marine sources. From each of the investigated five GeoB sediment cores (494-2956 m water depth) two time slices were processed which represent contrasting climatic conditions: the arid Heinrich Stadial 1 (~ 15 kyr BP) and the humid Mid Holocene (~ 6 kyr BP). Each sediment sample was split into 16 grain-size fractions ranging from 1.6 to 500 µm. Concentration and grain-size indicative magnetic parameters (susceptibility, SIRM, HIRM, ARM and ARM/IRM) were determined at room temperature for each of these fractions. The joint consideration of whole sediment and magnetic mineral grain-size distributions allows to address several important issues: (i) distinction of two aeolian sediment fractions, one carried by the north-easterly trade winds (40-63 µm) and the other by the overlying easterly Harmattan wind (10-20 µm) as well as a fluvial fraction assigned to the Senegal River (< 10 µm); (ii) identification of three terrigenous sediment source areas: southern Sahara and Sahel dust (low fine-grained magnetite amounts and a comparatively high haematite content), dust from Senegalese coastal dunes (intermediate fine-grained magnetite and haematite contents) and soils from the upper reaches of the Senegal River (high fine-grained magnetite content); (iii) detection of partial diagenetic dissolution of fine magnetite particles as a function of organic input and shore distance; (iv) analysis of magnetic properties of marine carbonates dominating the grain-size fractions 63-500 µm.

Dos Quijotes parecidos (1780-1797) : Cotejo de Programas Iconográficos

El presente trabajo está enfocado en algunos aspectos de la iconografía en diferentes ediciones del Quijote. Los resultados se desprenden de una investigación que aún se encuentra en curso, orientada a indagar y problematizar la recepción de la obra en diversos lugares y momentos. La iconografía presente en diversas ediciones nos permite acercarnos, al menos de manera parcial, a la recepción de la obra, atendiendo a diferentes problemáticas que se plasman en las imágenes, tales como el tipo del público al que estaba dirigido según su poder adquisitivo o el tipo de lectura que se realizaba del texto, entre otras cosas. En la investigación desarrollada se han cotejado diversas ediciones de la obra incluidas en la Colección Cervantina de la Biblioteca Pública de la Universidad Nacional de La Plata, con el fin de analizar dicha problemática para ampliar con un pequeño aporte el panorama de interpretación de la obra