Abstract
The nannofossil biostratigraphy of the Campanian-Maastrichtian of the Nierental Fm. is investigated. Although reworking of older sediments is partly observed, especially within turbiditic marlstones, standard nannofossil zonations for the Late Cretaceous of the low-latitude Tethyan realm can be applied. The base of the Maastrichtian, drawn at the level of the last occurrence of the planktonic foraminifera Globotruncanita calcarata, corresponds to a horizon within the nannofossil zone CC22ab, below the last occurrence of Eiffellithus eximius and Reinhardtites anthophorus, both in the Gosau and the Gams sections. -Authors
| Originalsprache | Englisch |
|---|---|
| Seiten (von - bis) | 67-77 |
| Seitenumfang | 11 |
| Fachzeitschrift | Zitteliana |
| Jahrgang | 20 |
| Publikationsstatus | Veröffentlicht - 1 Jan. 1993 |
ÖFOS 2012
- 105123 Stratigraphie
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