Muñiz Guinea, FernandoMayoral Alfaro, Eduardo2015-11-182015-11-181996http://hdl.handle.net/10272/11360The paleontological evidences (bivalves and crustacean decapods, mainly) of the «transitional facies» in Albaida del Aljarafe (SW. sector of the Guadalquivir Basin), indicate a relatively deep infralitoral plattform highly influenced by coastal terrigenous supply The paleoichnocoenosis data corroborate also, this assumptionspaAtribución-NoComercial-SinDerivadas 3.0 Españahttp://creativecommons.org/licenses/by-nc-nd/3.0/es/BivalvesCrustacean decapodsPaleoichnocoenosisLower PlioceneGuadalquivir BasinCaracterísticas paleoambientales de las «facies de tránsito» (Plioceno inferior) en el sector N.O de la Cuenca del Guadalquivir (Albaida del Aljarafe, Sevilla, España)Paleoenvironmental characteristics of the «transitional facies» (Lower Pliocene) in the Northwestern sector of the Guadalquivir Basin (Albaida del Aljarafe, Seville, Spain)journal articleopen access