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Maastrichtian planktonic foraminifera from the Germav Formation in Gercüş area SE Anatolia Turkey with notes on the suprageneric classification of globotruncanids
Date
1987-01-01
Author
Altıner, Sevinç
Metadata
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URI
https://hdl.handle.net/11511/81561
Journal
Revue de Paléobiologie
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Unverified, Article
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The Cankiri Basin, located in the northern part of the Central Anatolian Plateau, is a large Tertiary basin where thick Miocene to Quaternary continental sediments overlay the Cretaceous-Tertiary units. This investigation focuses on the Tuglu Formation, an Upper Miocene succession mainly composed of dark grey silty and organic rich clays. The type section of Tuglu has been sampled for an array of multidisciplinary analyses. The palaeontological proxies included ostracod, foraminifer, nannoplankton, pollen, ...
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S. Altıner, “Maastrichtian planktonic foraminifera from the Germav Formation in Gercüş area SE Anatolia Turkey with notes on the suprageneric classification of globotruncanids,”
Revue de Paléobiologie
, pp. 261–277, 1987, Accessed: 00, 2021. [Online]. Available: https://hdl.handle.net/11511/81561.