Daughter taxa (time control age-window is: 0-800Ma) | Granddaughter taxa | ||||
Lapideacassis 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. | Lapideacassis glans Lapideacassis mariae Lapideacassis asymmetrica Lapideacassis blackii Lapideacassis magnifica Lapideacassis bispinosa Lapideacassis wisei Lapideacassis trispina Lapideacassis multispinata Lapideacassis sp. | ||||
Tintinnabuliformis Bell shaped nannofossil with basal flange and apical horn(s), formed of single cycle of elements |
Taxonomy:
Distinguishing features:
Parent taxon (Nannolith families inc sed): Haptophytes forming calcareous structures not obviously homologous with heterococcoliths, holococcoliths, or discoasteralids
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.
Original description: 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 ?apical spines or processes.
Farinacci & Howe catalog pages: Lapideacassaceae + *
Morphology:
: hollow, |
Lith size: 0->0µm; |
Geological Range:
Last occurrence (top): at top of NN7 zone (100% up, 10.9Ma, in Tortonian 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:
Bown, P. R. & Young, J. R. (1997). Mesozoic calcareous nannoplankton classification. Journal of Nannoplankton Research. 19(1): 21-36. 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. gsReferences:
Lapideacassaceae compiled by Jeremy R. Young, Paul R. Bown, Jacqueline A. Lees viewed: 11-10-2024
Short stable page link: https://mikrotax.org/Nannotax3/index.php?id=797 Go to Archive.is to create a permanent copy of this page - citation notes |
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