Rodríguez, SergioRodríguez Curt, L.2014-11-202014-11-202002http://hdl.handle.net/10272/9377Calcareous breccias from Antolin (Guadiato Área, Córdoba Province) have been analysed. Paleontological and sedimentological studies of those breccias, allowed a reconstruction of a not-preserved calcareous platform or ramp. Breccias from Antolin show six types of clasts and blocks: oolithic grainstones originated in calcareous shoals, coral-algal boundstones originated in patch-reefs, packstones that are mainly composed of solitary corals and brachiopods produced in shallow quiet waters, crinoidal packstones originated in crinoida! prairies, mudstones-wackestones with micropeloidal and cryptalgal textures that were originated in mud mounds and calcareous sandstones originated in a mixed ramp. The debris flow was located in the photic zone of a middle, mixed ramp, because clasts show algal and bryozoan crusts; moreover, clasts and blocks show signs of short transportationspaAtribución-NoComercial-SinDerivadas 3.0 Españahttp://creativecommons.org/licenses/by-nc-nd/3.0/es/RugososPaleontologíaSedimentologíaCarbonatosÁrea del Guadiatojournal articleopen access