Nuevos datos bio-cronoestratigráficos para el sector suroccidental de la cuenca del Guadalquivir (Área de Lepe-Ayamonte, Huelva, España)
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Abstract
The paleontological data of the marine neogene sediments in the Lepe-Ayamonte area, Huelva (SW of the Guadalquivir basin) allow to establish a relative chronology from the presence of calcareous nannoplancton and malacofaunes. These data are congruent with the previous radiometric age
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