Francisco Ruiz Muñoz, María Luz González-Regalado Montero, Juan Ignacio Baceta Caballero, José Gabriel Pendón Martín, Josep Tosquella Angrill
This work analyses the ostracofaune of the basal sands of the "Niebla“ Formation (Baceta and Pendón, 1 999). The associations permit to infer the beginning of a transgressive sequence, with a very shallow, vegetated, infralittoral environment in the lower part of the sandy body, and an externe, more energetic infralittoral environment near the top
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