Planktonic foraminiferal turnover across the Cenomanian – Turonian boundary (OAE2) in the northeast of the Tethys realm, Kopet-Dagh Basin
Two Late Cenomanian – Early Turonian (C–T) intervals of the eastern part of the Kopet-Dagh basin, NE Iran have been investigated to evaluate the response of planktonic foraminifera to the geological event OAE2. The Gharesu and Taherabad sections with the thicknesses of 30 m and 22.5 m are composed o...
| Main Authors: | , , , |
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| Format: | Article |
| Language: | English |
| Published: |
Earth Science Institute, Slovak Academy of Sciences, Slovakia
2016-10-01
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| Series: | Geologica Carpathica |
| Subjects: | |
| Online Access: | http://www.degruyter.com/view/j/geoca.2016.67.issue-5/geoca-2016-0028/geoca-2016-0028.xml?format=INT |