Nannotax3 - ntax_cenozoic - Fasciculithus Nannotax3 - ntax_cenozoic - Fasciculithus

Fasciculithus


Classification: ntax_cenozoic -> Discoasterales -> Fasciculithaceae -> Fasciculithus
Sister taxa: Diantholitha, Fasciculithus, Gomphiolithus, Lithoptychius, Tectulithus

Daughter taxa (time control age-window is: 0-800Ma)Granddaughter taxa
F. alanii group
Conical-shaped fasciculiths
Fasciculithus alanii
Fasciculithus clinatus
Fasciculithus lillianiae
Fasciculithus lobus
Fasciculithus thomasii

F. involutus group
Cylindrical fasciculiths
Fasciculithus involutus
Fasciculithus tympaniformis
Fasciculithus billii
Fasciculithus realeae
Fasciculithus vertebratoides

F. schaubii group
Ornate fasciculiths - with prominent fenestrae and sculpted outlines
Fasciculithus fenestrellatus
Fasciculithus mitreus
Fasciculithus richardii
Fasciculithus schaubii
Fasciculithus sidereus
Fasciculithus tonii

Fasciculithus sp.
Specimens which cannot be assigned to any established species

Taxonomy:

Citation: Fasciculithus Bramlette & Sullivan, 1961
taxonomic rank: Genus
Type species: Fasciculithus involutus Bramlette & Sullivan, 1961.
Taxonomic discussion: The subdivison into groups given here is based on Bown (2010).

Distinguishing features:
Parent taxon (Fasciculithaceae): Conical or cylindrical discoasteralids consisting of 10-30 wedge-shaped, radially-arranged elements, in one to three superposed cycles.
This taxon: Conical or cylindrical fasciculiths formed of a single cycle of elements, outer surface is usually covered by fenestrae.

Farinacci & Howe catalog pages: Fasciculithus + *


Morphology:

The c-axes are aligned radially in plan view but are inclined upward in side view. Hence the two halves of the nannolith show opposite extinction colours with a gypsum plate when vertical, with the left side blue in standard orientation (Romein 1979). Ths also means that in side view the nannolith does not go entirely into extinction in any position.

Search data:
LITHS: nannolith-radiate, circular, cylindrical,
Lith size: 4->20µm;
The morphological data given here can be used on the advanced search page. See also these notes

Geological Range:
Notes: Agnini et al. 2007 place top of Fasciculithus low (ca 20% up) in NP10
Last occurrence (top): at top of NP10 zone (100% up, 54.2Ma, in Ypresian stage). Data source: Total of ranges of the species in this database
First occurrence (base): within NP4 zone (61.51-63.25Ma, base in Danian stage). Data source: Total of ranges of species in this database

Plot of occurrence data:

References:

Agnini, C., Fornaciari, E., Raffi, I., Rio, D., Rohl, U. & Westerhold, T. (2007a). High-resolution nannofossil biochronology of middle Paleocene to early Eocene at ODP Site 1262: Implications for calcareous nannoplankton evolution. Marine Micropaleontology. 64: 215-248. gs

Bramlette, M. N. & Sullivan, F. R. (1961). Coccolithophorids and related nannoplankton of the Early Tertiary in California. Micropaleontology. 7(2): 129-188. gs

Perch-Nielsen, K. (1985). Cenozoic calcareous nannofossils. In, Bolli, H. M., Saunders, J. B. & Perch-Nielsen, K. (eds) Plankton Stratigraphy. Cambridge University Press, Cambridge (1): 427-555. gs

Romein, A. J. T. (1979). Lineages in Early Paleogene calcareous nannoplankton. Utrecht Micropaleontological Bulletin. 22: 1-231. gs O

Steurbaut, E. & Sztrákos, K. (2008). Danian/Selandian boundary criteria and North Sea Basin–Tethys correlations based on calcareous nannofossil and foraminiferal trends in SW France. Marine Micropaleontology. 67: 1-29. gs


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Fasciculithus compiled by Jeremy R. Young, Paul R. Bown, Jacqueline A. Lees viewed: 15-9-2024

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Short stable page link: https://mikrotax.org/Nannotax3/index.php?id=564 Go to Archive.is to create a permanent copy of this page - citation notes
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