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Tortugas continentales (Pleurodira: Chelidae) en la Formación Roca (Daniano), provincia de Río Negro, Argentina

2009; Asociación Paleontológica Argentina; Volume: 46; Issue: 2 Linguagem: Inglês

1851-8044

Paula Bona, Susana Heredia, Marcelo de la Fuente,

Ichthyology and Marine Biology

Roca Formation is a stratigraphic succession of marine and continental sediments that belongs to Malargue Group, which was deposited from the Late Campanian to the Danian in the Neuquen Basin, western Argentina. Fossil vertebrates recovered at different outcroppings of this lithostratigraphic unit correspond to marine taxa. The turtle material studied here was collected from the lower section of Roca Formation (Maastrichtian?-Danian) in northeastern Lago Pelegrini (38o 40’ 06’’S, 67o 52’ 02’’ O), Rio Negro Province. Remains of carapace and plastron of continental turtles were assigned to indeterminate chelid pleurodires and to Yaminuechelys cf. maior (Staesche, 1929). This record of chelid turtles in Roca Formation confirms the existence of marine paleoenvironments with continental influence and represents the first record of Danian continental vertebrates in the Neuquen Basin.