
handle: 10272/11360
The 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 assumption
Bivalves, Crustacean decapods, Lower Pliocene, Guadalquivir Basin, Paleoichnocoenosis
Bivalves, Crustacean decapods, Lower Pliocene, Guadalquivir Basin, Paleoichnocoenosis
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