Distinguishing features:
Parent taxon (Biscutaceae): Regular placoliths; rim broad, central area relatively narrow, with variable central structures.
The distal shield is formed from V-units and the proximal shield and tube cycle are formed from R-units.
This taxon: Elliptical with prominent, birefringent, axial cross.
Daughter taxa (time control age-window is: 0-800Ma)![]() | |||||
Late Cretaceous species | |||||
![]() | ![]() | ![]() | ![]() | Crucibiscutum hayi Medium-sized (ca 5-6 µm)Crucibiscutum with relatively wide central area, relatively narrow rim and slender-armed axial cross. | |
Podorhabdus quadriperforatus | |||||
Early Cretaceous species | |||||
![]() | ![]() | ![]() | ![]() | Crucibiscutum bastetanum Small (3.5-5.5 µm) with slightly rotated cross, central area narrow, tube cycle (R-units) broader than outer rim | |
![]() | ![]() | ![]() | ![]() | Crucibiscutum gracile Small (3.5-5 µm) sub-circular or broadly elliptical, central area wide, cross bars slender | |
![]() | ![]() | ![]() | ![]() | Crucibiscutum neuquenensis Medium-sized (ca 5-7 µm), broadly elliptical Crucibiscutum; central-area relatively wide, with off-axial (slightly-rotated) cross-bars. | |
![]() | ![]() | Crucibiscutum pinnatus Small (ca 3-5 µm)Crucibiscutum with central cross that is only weakly birefringent and does not fill the central area, delineating four perforations that are clearly visible in XPL. | |||
Crucibiscutum ryazanicum Small (4-5 µm) with an asymmetrical central cross. | |||||
![]() | Crucibiscutum salebrosum Small (ca 3-5 µm) Crucibiscutum with narrow central area and birefringent cross. The central cross practically fills the narrow central area, and has the same intensity birefringence as the tube cycle (white). | ||||
![]() | ![]() | ![]() | ![]() | Crucibiscutum trilensis Medium-sized (ca 5-6 µm), Crucibiscutum; broadly elliptical with a relatively wide central-area . | |
Crucibiscutum sp. Specimens not identified to species level |
Taxonomy:
Farinacci & Howe catalog pages: Crucibiscutum *
Distinguishing features:
Parent taxon (Biscutaceae): Regular placoliths; rim broad, central area relatively narrow, with variable central structures.
The distal shield is formed from V-units and the proximal shield and tube cycle are formed from R-units.
This taxon: Elliptical with prominent, birefringent, axial cross.
Search data:
LITHS: placolith, elliptical, CA: cross-axial, ca_disjunct, process, diagonal cross, CROSS-POLARS: rim-bicyclic, V-prominent, R-prominent, |
Lith size: 3->7µm; Data source notes: size range of included species |
Geological Range:
Last occurrence (top): at top of Cenomanian Stage (100% up, 93.9Ma, in Cenomanian stage). Data source: Total of range of species in this database
First occurrence (base): at base of Berriasian Stage (0% up, 145Ma, in Berriasian stage). Data source: Total of range of species in this database
Plot of occurrence data:
Black, M. (1971a). Coccoliths of the Speeton Clay and Sutterby Marl. Proceedings of the Yorkshire Geological Society. 38: 381-424. gs V O Bown, P. R., Rutledge, D. C., Crux, J. A. & Gallagher, L. T. (1998). Lower Cretaceous. In, Bown, P. R. (ed.) Calcareous Nannofossil Biostratigraphy. British Micropalaeontological Society Publication Series . 86-131. gs O Burnett, J. A. (1998). Upper Cretaceous. In, Bown, P. R. (ed.) Calcareous Nannofossil Biostratigraphy. British Micropalaeontological Society Publication Series . 132-199. gs O Jakubowski, M. (1986). New calcareous nannofossil taxa from the Lower Cretaceous of the North Sea. INA Newsletter. 8(1): 38-42. gs V OReferences:
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Crucibiscutum compiled by Jeremy R. Young, Paul R. Bown, Jacqueline A. Lees viewed: 31-3-2023
Short stables page link: https://mikrotax.org/Nannotax3/index.php?id=10316 Go to Archive.is to create a permanent copy of this page - citation notes |
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