Record of very high energy events in Plio-Pleistocene marine deposits of the Gulf of Cadiz (SW Spain): facies and processes

Abstract

The depositional conditions that characterized the sedimentary filling in the southern sector of the Guadalquivir Basin during the late post-orogenic Neogene have been established through the sedimentological study of the Plio-Pleistocene outcrops along the Cadiz coast (SW Spain). The study has contributed to a better interpretation of the regional stratigraphy and helped to establish both depositional mechanisms and processes. Deposits show different lithofacies according to the dominant climatic and prevailing environmental conditions. Pliocene deposits show bioclastic lithofacies with abundant warm-water fossils, whereas Pleistocene sediments have a low fossil content. Stratigraphic sections indicate important depositional changes: sandstone and grainstone were deposited under a seasonal regime, whereas accumulations of large boulders and bioclasts are interpreted as event deposits, the product of episodic oceanographic processes, such as huge storms or tsunamis. These deposits do not have a seasonal character; however, given their relative frequency in the stratigraphic sections, they were probably associated with neo-tectonic activity in the Guadalquivir Foreland Basin, which was an important controlling factor in this basin. The proximity to the Africa-Eurasia plate boundary together with several historically documented earthquakes and tsunamis in the study area, suggest that these processes could explain the origin of these deposits. The seismic-tectonic activity was more intense between the late Pliocene and early Pleistocene, as shown by the presence of a well-marked angular unconformity, as well as by a higher frequency of the very high energy clastic and bioclastic accumulations.