Daughter taxa (time control age-window is: 0-800Ma)![]() | ||||
| Lapideacassis glans 0 spines; dome shaped; proximal collar | ||||
| Lapideacassis mariae 0 spines; elongate, tiered; proximal collar | ||||
| Lapideacassis asymmetrica 1 spine; asymmetric cone | ||||
| Lapideacassis blackii 1 spine; symmetric cone, tiered | ||||
| Lapideacassis magnifica 1 spine, with apical cross-shaped calyx; | ||||
| Lapideacassis bispinosa 2, asymmetric, spines; proximal collar | ||||
| Lapideacassis cornuta 2, apical spines at about 45 degrees. | ||||
| Lapideacassis wisei 3, asymmetric, spines; proximal collar | ||||
| Lapideacassis trispina 3 spines sub-horizontal, evenly spaced; tiered; proximal collar | ||||
| Lapideacassis tricornus 3, near-vertically orientated, tapering apical spines. | ||||
| Lapideacassis multispinata >3 spines; tiered; proximal collar | ||||
| Lapideacassis sp. Specimens which cannot be assigned to any established species | ||||
Distinguishing features:
Parent taxon (Lapideacassaceae): Hemispherical to cylindrical nannoliths, with walls constructed from one to several cycles of thin elements, enclosing a hollow central space; the nannolith tapers distally, and may have long apical spines or processes.
This taxon: Hemispherical to cylindrical nannoliths, with walls constructed from one to several cycles of thin elements, enclosing a hollow central space; the nannolith tapers distally, and may have long apical spines or processes.
Species arranged here by number of spines.
| LITHS: circular, cylindrical, hollow, CROSS-POLARS: R-prominent, |
| Lith size: 4->18µm; |
Geological Range:
Last occurrence (top): at top of Eocene Epoch (100% up, 33.9Ma, in Priabonian stage). Data source: Total of ranges of the species in this database
First occurrence (base): within Early Aptian Substage (118.70-121.40Ma, base in Aptian stage). Data source: Total of ranges of species in this database
Plot of occurrence data:
Black, M. (1971b). Problematical Microfossils from the Gault Clay. Geological Magazine. 108(4): 325-327. gs Black, M. (1971a). Coccoliths of the Speeton Clay and Sutterby Marl. Proceedings of the Yorkshire Geological Society. 38: 381-424. gs Burnett, J. A. (1997c). New species and new combinations of Cretaceous nannofossils and a note on the origin of Petrarhabdus (Deflandre) Wise & Wind. Journal of Nannoplankton Research. 19(2): 133-146. gs Crux, J. A. (1981). New calcareous nannofossil taxa from the Cretaceous of South East England. Neues Jahrbuch für Geologie und Paläontologie, Monatshefte. 1981: 633-640. gs Forchheimer, S. & Stradner, H. (1973). Scampanella, eine neue Gattung kretazischer Nannofossilien. Verhandlungen der Geologischen Bundesanstalt (Wien). 1973(2): 286-289. gs Kennedy, W. J., et al. (2000). Integrated stratigraphy across the Aptian-Albian boundary in the Marnes Bleues, at the Col de Pre _-Guittard, Arnayon (Drome), and at Tartonne (Alpes-de-Haute-Provence), France: a candidate Global Boundary Stratotype Section and Boundary Point for the base of the Albian Stage. Cretaceous Research. 21: 591-720. gs Perch-Nielsen, K. & Franz, H. E. (1977). Lapideacassis and Scampanella, calcareous nannofossils from the Paleocene at sites 354 and 356, DSDP Leg 39, Southern Atlantic. Initial Reports of the Deep Sea Drilling Project. 39: 849-862. gs References:

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Lapideacassis compiled by Jeremy R. Young, Paul R. Bown, Jacqueline A. Lees viewed: 11-8-2026
Short stable page link: https://mikrotax.org/Nannotax3/index.php?id=798 Go to Archive.is to create a permanent copy of this page - citation notes |
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