Mauricio Beuchot, La semiótica. Teorías del signo y el lenguaje en la historia, México, Fondo de Cultura Económica, 2004, 208 pp.

Fil: Massini Correas, Carlos I..

Magnetostratigraphic age-depth tie points of ODP Leg 208 sites

We report the paleomagnetic and rock magnetic results from discrete sample analysis of sediments from Walvis Ridge, Leg 208 of the Ocean Drilling Program. In an effort to refine the shipboard magnetostratigraphy, alternating field and thermal demagnetization of discrete samples were carried out, predominantly on samples from Sites 1262 and 1267. Results are generally consistent with the shipboard pass-through cryomagnetometer data, though in some cases the discrete samples resolved ambiguities in the reversal record. Significantly, the C24r/C24n reversal boundary was identified at Sites 1262 and 1267, and most boundaries in the Paleocene and Upper Cretaceous sections are now identified to within 10-30 cm. Magnetic mineralogy results show that prior to the late Miocene, the predominant detrital magnetic component was coarse-grained magnetite and that after the late Miocene, titanomagnetite has also been present. This suggests a possible change in detrital source at that time.

Maximiliano Crespi, La conspiración de las formas. Apuntes sobre el jeroglífico literario. La Plata, UNIPE: Editorial Universitaria, 2011, Colección Boris Spicvacow, 208 páginas

Fil: Stedile Luna, Verónica. Universidad Nacional de La Plata. Facultad de Humanidades y Ciencias de la Educación; Argentina.