Características paleoambientales de las «facies de tránsito» (Plioceno inferior) en el sector N.O de la Cuenca del Guadalquivir (Albaida del Aljarafe, Sevilla, España)

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Caracteristicas-paleoambientales.pdf (843.65 KB)

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1996

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http://hdl.handle.net/10272/11360

Abstract

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

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Bivalves; Crustacean decapods; Paleoichnocoenosis; Lower Pliocene; Guadalquivir Basin

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Geogaceta -- Nº 20-1, (1996)
Atribución-NoComercial-SinDerivadas 3.0 España
The license for this item is described as Atribución-NoComercial-SinDerivadas 3.0 España