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Continental sedimentation during early Cretaceous in the Central part of the Iberian basin took place in two sedimentary sub-basins, the Oliete and Aguil&#243;n sub-basins. The stratigraphic analysis carried out in these units allows us to define new lithostratigraphical units. The biostratigraphy analysis of these units was based on charophytes. The identification of regional unconformities allows to define three depositional sequences. These sequences span from the Valanginian or Hauterivian to the Early Barremian, and may be correlated to sequences K1.2 or K1.3, K1.4 and K1.5 or K1.6 D.S., previously defined by Salas et al. (1991) and Salas & Casas (1993) in the eastem Maestrazgo basin. These results indicate that the stratigraphic record of the central part of the Iberian basin is as completed as that of the margin of the neighbouring Maestrazgo, Aliaga-Pe&#241;agolosa and Cameros basins.  El Cret&#225;cico inferior continental de la Cordillera Ib&#233;rica Central est&#225; representado en dos subcuencas de sedimentaci&#243;n: las Cubetas de Aguil&#243;n y Oliete. Los estudios realizados sobre estos materiales han permitido definir nuevas unidades litoestratigr&#225;ficas, cuya caracterizaci&#243;n bioestratigr&#225;fica se realiza a partir de su contenido en carofitas. La identificaci&#243;n de discontinuidades significativas permiten definir tres secuencias de dep&#243;sito que abarcan el intervalo temporal Valanguniense y/o Hauteriviense-Barremiense inferior y que son correlacionables con las S.D.K1.2 y/o K1.3, K1.4 YK1.5 y/o K1.6 definidas en Salas et al. (1991) y Salas y Casas (1993) para la Cuenca del Maestrazgo. Estos resultados ponen de manifiesto que el registro estratigr&#225;fico de la zona central de la Cordillera Ib&#233;rica tiene una entidad similar al de los m&#225;rgenes de las Cuencas del Maestrazgo, Aliaga- Pe&#241;agolosa y Cameros

Estratigrafía del Cretácico inferior continental de la Cordillera Ibérica Central