Pistas fósiles asociadas a la discontinuidad fini-Messiniense en el margen norte de la Cuenca del Bajo Segura (SE España)

A detailed analysis of the Upper Messinian-Lower Pliocene at the northern border of the Bajo Segura Basin (BSB) has been carried out. Trace fossils of firm- and rockground were collected, aiding in the recognition of three ichnofacies: Glossifungites (types A and B), Entobia and Gnathichnus. The ichnological data provide evidence that the Pliocene flooding of the BSB, after the Messinian Salinity Crisis, was developed in two pulses. In the first one, the ingression penetrated only along the paleovalleys and produced a coastal trasgressive lag (P0). In the second one, the ingression overflowed the margins of the paleovalleys and extended throughout the entire northern margin, also producing a coastal transgressive lag in the base of the P2 system. The record of the Entobia and Gnathichnus ichnofacies in the clasts of both lags evidences a relatively fast deepening-upward trend in both the transgressions.

Contradicciones del significado de la actividad físico-deportiva en las identidades corporales de las chicas adolescentes

Dentro de la estructura de género que impone la construcción social del cuerpo femenino, el sentimiento de inadecuación del propio cuerpo parece caracterizar la configuración de las identidades corporales femeninas en la adolescencia, motivando que la relación que establecen muchas chicas jóvenes con la actividad físico-deportiva sea compleja y a menudo problemática. Siguiendo un enfoque feminista post-estructuralista, este trabajo se centra en tres conflictos: 1) La actividad física para perder peso, instrumentalizada dentro de los discursos para alcanzar el ideal de belleza o luchar contra la obesidad; 2) El límite socialmente construido para las chicas deportistas entre lo que se considera un tono muscular atractivo y un cuerpo excesivamente musculoso; 3) Los procesos de sexualización y ansiedad física social debido a la exposición del cuerpo a una mirada masculina no deseada en diferentes contextos de práctica físico-deportiva.

The Pliocene Mediterranean infilling of the Messinian Erosional Surface: New biostratigraphic data based on calcareous nannofossils (Bajo Segura Basin, SE Spain)

The Bajo Segura Basin (eastern Betic Cordillera) is a Mediterranean marginal basin where the Messinian Erosional Surface (MES), formed during the Messinian Salinity Crisis sea-level fall, is well developed. Overlying this major discontinuity the lower Pliocene transgressive sediments record the reflooding of the Mediterranean and the return to an open marine environment, the continental shelf being rebuilt after the Messinian erosion. The stratigraphic and biostratigraphic study of six sections allows two transgressive-regressive sequences filling the MES to be distinguished, correlated with the previously distinguished Mediterranean offshore seismic units. Ten calcareous nannofossil bioevents have been identified. The lower sequence can be dated according to nannofossil biozones NN12 to NN14 and the upper sequence by NN15 to NN16. The boundary between both lower Pliocene sedimentary sequences occur after the first common occurrence (FCO) of Discoaster asymmetricus found in the uppermost sediments of the lower sequence and before the first occurrence (FO) of Discoaster tamalis in the lowermost part of the upper sequence. Thus this sequence boundary can be estimated at between 4.1 and 4.0Ma ago.