Nannotax3 - ntax_cenozoic - Lapideacassaceae Nannotax3 - ntax_cenozoic - Lapideacassaceae

Lapideacassaceae


Classification: ntax_cenozoic -> Nannolith families inc sed -> Lapideacassaceae
Sister taxa: Ceratolithaceae, Ericiolacaea, Lapideacassaceae, Lithostromationaceae, Nannolith genera inc sed, Rhomboasteraceae

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
Tintinnabuliformis bicornus
Tintinnabuliformis unicorn
Tintinnabuliformis sp.

Taxonomy:

Citation: Lapideacassaceae Bown & Young, 1997
taxonomic rank: Family
Taxonomic discussion: Rare and sporadic stratigraphic distribution, but Cretaceous/Tertiary boundary survivor.

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:

Crystallographic orientations: The entire nannolith is formed of R-units, in side view the c-axes are inclined upward slightly (so with gypsum plate when vertical the left hand side is blue and the right hand side yellow). In apical view the c-axes are slightly oblique from radial. [JRY 2017 my obs, and interpretation of published micrographs] 

Search data:
: hollow,
Lith size: 0->0µm;
The morphological data given here can be used on the advanced search page. See also these notes

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:

References:

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. gs


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Lapideacassaceae compiled by Jeremy R. Young, Paul R. Bown, Jacqueline A. Lees viewed: 11-10-2024

Taxon Search:
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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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