Contexto geocronológico y paleoclimático de la formación de playas fósiles sumergidas en el Mediterráneo Occidental
DOI:
https://doi.org/10.3989/scimar.05110.020Palabras clave:
Holoceno superior, depósitos de playa, 14C, OSL, restos arqueológicosResumen
En este artículo se describen las características geomorfológicas y petrológicas de 19 playas fósiles sumergidas localizadas en la costa norte catalana (Mediterráneo Occidental). Su longitud oscila entre 1039 m y 8 m, y su anchura entre 86.5 m y 1.5 m. Su espesor varía entre un mínimo de 0.4 m y un máximo de 3.25 m. Se trata de playas fósiles siliciclásticas, constituidas por gravas bien redondeadas, con matriz de arena muy gruesa. Presentan una baja proporción de bioclastos (<1%). La cementación se produjo en la zona de batida de la playa debido a la precipitación de calcita magnesiana. A partir de dataciones absolutas (14C y OSL) y de artefactos antrópicos, se han identificado tres fases de formación atribuibles al Holoceno superior. La fase I corresponde al periodo cálido y húmedo romano, y ha sido registrada en un nivel situado por debajo de los -3.75 m respecto del nivel medio del mar (MSL). La fase II encaja con la anomalía climática cálida y árida medieval, la cual ha sido registrada entre +0.25 m y -2.5 m MSL. La fase III corresponde a la pequeña edad del hielo y al periodo industrial, y ha sido registrada en niveles situados entre +0.5 m y -3.0 m MSL. Se puede establecer una buena correspondencia temporal entre la cronología de las distintas fases de cementación y las condiciones paleoclimáticas cálidas y/o áridas.
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