The Rupelian–Chattian transition in the north-western Transylvanian Basin (Romania) revealed by calcareous nannofossils: implications for biostratigraphy and palaeoenvironmental reconstruction

Sediments belonging to the Oligocene Vima Formation (located in the north-western part of the Transylvanian Basin, Romania) have been investigated for calcareous nannofossils content. Biostratigraphically, the sedimentary succession is late Rupelian–Chattian in age, belonging to the NP24 — Sphenolit...

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Bibliographic Details
Main Authors: Kallanxhi Mădălina-Elena, Bălc Ramona, Ćorić Stjepan, Székely Szabolcs-Flavius, Filipescu Sorin
Format: Article
Language:English
Published: Earth Science Institute, Slovak Academy of Sciences, Slovakia 2018-06-01
Series:Geologica Carpathica
Subjects:
Online Access:http://www.degruyter.com/view/j/geoca.2018.69.issue-3/geoca-2018-0016/geoca-2018-0016.xml?format=INT