
handle: 10366/79865 , 10272/10040
[ES] El estudio de las asociaciones de ostr?codos de las arenas basales con microforamin?feros de la Formaci?n "Calcarenita de Niebla" (Civis et al., 1987) indican una edad Tortoniense para estos materiales. Su dep?sito se produjo en un medio infralitoral muy somero, bien oxigenado y con una importante vegetaci?n.
[EN] The ostracod assemblages of the basal sands with Heterostegina of the "Calcarenita de Niebla" Formation (Civis et al, 1987) indicates a Tortonian age. These materials were deposited in an infralittoral environment, well oxigenated and vegetated.
Bioestratigrafía, Fm. Calcarenita de Niebla, SW Spain, Ostracods, Biostratigraphy, Palaeoecology, Geology, Ostrácodos, Paleoecología, Geolog?a, Calcarenita de Niebla Fm., Geología, S.O. España
Bioestratigrafía, Fm. Calcarenita de Niebla, SW Spain, Ostracods, Biostratigraphy, Palaeoecology, Geology, Ostrácodos, Paleoecología, Geolog?a, Calcarenita de Niebla Fm., Geología, S.O. España
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