Rodríguez Vidal, JoaquínÁlvarez García, G.Alcaraz, J. M.Martínez Aguirre, AranchaCáceres Puro, Luis MiguelCantano Martín, MercedesCaro Gómez, J. A.2015-01-292015-01-292000http://hdl.handle.net/10272/9775The 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)spaAtribución-NoComercial-SinDerivadas 3.0 Españahttp://creativecommons.org/licenses/by-nc-nd/3.0/es/KarstQuaternarySpeleothemIsotopie datingSierra Morenajournal articleopen access