Fig 1. Malta, Middle Miocene, Coccosphere: 11.0µm, Coccoliths: 8.3µm; Fig 2. Malta, Middle Miocene, 8.0µm; Fig 3. Silifke, Turkey, Middle Miocene, 9.2µm; Fig 4. Malta, Middle Miocene, 9.0µm
Fig 1. Antakya, Hatay, Turkey, Middle Miocene, 8.0µm; Fig 2. Adana Basin, Late Miocene, 8.4µm; Fig 3. Antalya-Manavgat Road, Turkey, Late Miocene, 8.5µm; Fig 4. Antalya-Manavgat Road, Turkey, Late Miocene, 9.4µm; Fig 5. Antalya-Manavgat Road, Turkey, Late Miocene, 8.4µm; Fig 6. Antalya-Manavgat Road, Turkey, Late Miocene, 9.2µm; Fig 7. Antalya-Manavgat Road, Turkey, Late Miocene, 8.2µm; Fig 8. Adana Basin, Turkey, Late Miocene, 9.5µm;
Coccolithus pseudoumbilicus Gartner, 1967
Large size [8.0 -10.0µm], elliptical species of Reticulofenestra have a featureless central area.
Gartner, S., (1967): Calcareous nannofossils from Neogene of Trinidad, Jamaica, and Gulf of Mexico. - University of Kansas Paleontological Contributions, Papers. 29: 1-7.
Gartner, S., (1969): Correlation of Neogene planktonic foraminifera and calcareous nannofossil zones. - Transactions of the Gulf-Coast Association of Geological Societies. 19: 585-599.
Coccolithus pseudoumbilicus
Gartner, 1967
Neogene
Sigsbee knolls, Gulf of Mexico.