José Luis Goy Goy, Caridad Zazo, Ana Cabero del Río, Norbert Mercier, Teresa Bardaji Azcárate, Vincent Francesc Soler Selva, Pablo G. Silva Barroso, Cristino José Dabrio González
Based on geomorphological mapping, petrography, paleontology and luminescence data (OSL), suggest rapid climate and sea-level changes during the peak of MIS 5. Tropical fauna is present during the first part of this interstadial when oceanographic and climate conditions favoured oolite generation.
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