Abstract
A paleoecological analysys o fossils belonging to Uscari Formation (Miocene-Pliocene] at the Limón Province, Costa Rica is presented, Mollusk, foraminifers, arthopods, shark teeth, ichnofossil and plants led to the conclussion that litoral to infralitoral enviroment was developed in that area with dense communities of suspension feeders and deposit feeders. That association shows characteristics of "Skolitos Ichnofacies" and "Vital lipostrate biofacies".Comments
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