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...
Main Authors: | , , , , |
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Format: | Article |
Language: | English |
Published: |
Earth Science Institute, Slovak Academy of Sciences, Slovakia
2018-06-01
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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 |