Corollithion exiguum Stradner, 1961
The outer protolith wall remains in constant extinction because the optic axis (c‑axis) is perpendicular to the microscope stage. In contrast, the inner protolith wall, radial bars, and distal process exhibit greyish‑white interference colours.
Hexagonal species of Corollithion are characterised by a double protolith wall and a large central area spanned by six radial bars that extend to the midpoints of the sides, each supporting a stellate distal process. Short spines commonly arise only from the vertices.
Stradner, H. 1961. Vorkommen von Nannofossilien im Mesozoikum und Alttertiär. Erdoel-Zeitschrift 77(3): 77-88.
Corollithion exiguum
Stradner, 1961
Senonian
Waidach, State of Salzburg, Austria.