Abstract

For the first time, nannofossils found in the marine stratigraphic unit named Patagoniano which crops out at Cerro Chenque and Cerro Hermitte in southeastern Chubut, Argentina, are documented. They were recovered from pelitic levels in the lower part of coarsening-upward siliciclastic sedimentary sequences. The nannofossils are assigned in part to the Discoaster kugleri Zone NN7 (MARTINI, 1971) and CN5b (BUKRY, 1971, 1973) thus allowing correlation of the productive levels with the Serravallian Stage (upper Middle Miocene).

Full Text
Published version (Free)

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call