Joaquín Rodríguez Vidal, Genaro Álvarez García, José Manuel Alcaraz Pelegrina, Aránzazu Martínez Aguirre, Luis Miguel Cáceres Puro, Mercedes Cantano Martín, José Antonio Caro Gómez
The geological and geomorphological studies in Los Covachos cave reveal a wide collection of speleothems and a thick archaeological stratigraphies. Both isotopie dating of speleothems C^ThP^U) and charcoal layers C4C), in chemical and terrigenous sediments, show a Quaternary sequence of palaeoenvironmental evolution related with an alternating phases of biostatic and rhexistatic genesis. The first ones are partially situated in a warm and wet isotopie stages (7, 5, 3, and 1) and the others in a wider warm and dry stages (6, 4 and 2)
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