Fig 1. 6.5 µm, Antalya-Manavgat Road, Turkey, Late Miocene
Fig 2. 9.6 µm, Malta, Middle Miocene
Fig 3. 11.6 µm, Malta, Middle Miocene
Discolithus multiporus Kamptner, 1948
Discolithina multipora (Kamptner, 1948) Martini, 1965
Pontosphaera multipora is noted for having a proximal plate with pores arranged in three concentric cycles and additional, randomly arranged pores in the centre, a defining characteristic of the species that distinguishes it from other Pontosphaera species. The similar height of the wall and distal cover results in uniform interference colours (first-order white), which is an essential characteristic for identifying this species in the plan view in XPL. Pontosphaera multipora exhibits laevogyre-inclined extinction at 68° on the distal side and length-fast elongation.
Kamptner, E. 1948. Coccolithen aus dem Torton des Inneralpinen Wiener Beckens. Anzeiger der Österreichische Akademie der Wissenschaften, Mathematische-Naturwissenschafliche Klasse, Wien. 157: 1-16.
Martini, E. 1965. Mid-Tertiary calcareous nannoplankton from Pacific deep-sea cores. Colston Papers 17: 393-411.
Roth, P. H. 1970. Oligocene calcareous nannoplankton biostratigraphy. Eclogae Geologicae Helvetiae 63: 799-881.
Discolithus multiporus
Kamptner, 1948
Late Miocene
Inner alpine Vienna basin