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, 1967a
Large (>8.0 μm) elliptical species of Reticulofenestra possess the following features:
• The distal shield is larger than the proximal shield.
• The void central area is surrounded by a tube cycle of variable width.
• The diameter of the central area varies in relation to the width of the pelaga.
Its optical properties, including inclined dextrogyre extinction lines (with angles typically around 9° on the distal shield and 77° on the tube cycles on the distal side) and length-fast (-) elongation, are consistent with those of the genus Reticulofenestra.
Gartner, S. 1967a. Calcareous nannofossils from Neogene of Trinidad, Jamaica, and Gulf of Mexico. University of Kansas Paleontological Contributions, Papers 29: 1-7.
Gartner, S. 1969b. 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.