Paleontological study of the lacustrine-palustrine facies of Peña Adrian, Late Miocene (Miranda de Ebro, Miranda-Trebiño basin)
DOI:
https://doi.org/10.55407/geogaceta98198Keywords:
Miranda-Trebiño Basin, palustrine-lacustrine, charophytes, gastropods, ostracods, MioceneAbstract
This work presents the results of the paleontological study of the Peña Adrián section (Miranda de Ebro, Burgos), formed by alluvial and palustrine-lacustrine facies from the Upper Miocene. Two levels of marls have been sampled, PAF15 and PAF24 (A and B) where different genera and species of gastropods, charophytes and ostracods have been identified. From the stratigraphic and paleontological study, it has been possible to recognize the environmental conditions of the lacustrine system and their variation throughout the succession, showing phases of higher and lower energy until the final retraction of the lake system.
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Copyright (c) 2023 Zuriñe Larena, Josep Sanjuan, Ana Pascual, Mariano Larraz, Asier Valenzuela, Concha Arenas, Xabier Murelaga Bereicua, Juan Ignacio Baceta
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