“…In contrast, sediments of El Cien Formation were deposited no deeper than 200 m, suggesting shelf environments, coastal lagoons, estuaries and deltas (Schwennicke, 1994). Past studies of diatoms (Kim and Barron, 1986), planktonic foraminifera (Kim, 1987), and calcareous nannofossils Schwennicke, 1992), shark and ray faunas (González-Barba, 2008), macroinvertebrates -e.g. mollusks and crabs (Smith, 1991;Grimm and Föllmi, 1994;Schweitzer et al, 2002;Vera-Dimas, 2013), phosphorites (Galli-Olivier et al, 1990;Galli-Olivier, 1993;Schwennicke, 1994;Schwennicke and Vázquez-García, 1996), and sedimentological studies (Grimm, 1992) have elucidated the paleobiological and paleoceanographic history of the region during the Late Oligocene and indicate a subtropical environment characterized by high primary productivity.…”