Daughter taxa (time control age-window is: 0-800Ma)![]() | Granddaughter taxa | ||||
| Diantholitha Squat fasciculiths divided into sub-equal upper and lower cycles with different optical orientations. Conical openings on both sides, no fenestrae | |||||
| Fasciculithus Conical or cylindrical fasciculiths formed of a single cycle of elements, outer surface is usually covered by fenestrae. | |||||
| Gomphiolithus Fasciculiths formed of a single cycle, arguably with central body, deep cavity on the distal side, no fenestrae | |||||
| Lithoptychius Complex fasciculiths - formed of three discrete cycles; no fenestrae | Lithoptychius ulii Lithoptychius chowii Lithoptychius galeottii Lithoptychius maioranoae Lithoptychius varolii Lithoptychius felis Lithoptychius collaris Lithoptychius schmitzii Lithoptychius sp. | ||||
| Tectulithus Complex fasciculiths - formed of two discrete cycles; no fenestrae | Tectulithus merloti Tectulithus janii Tectulithus stonehengei Tectulithus pileatus Tectulithus pagodiformis Tectulithus stegastos Tectulithus sp. | ||||
Distinguishing features:
Parent taxon (Discoasterales): Radially symmetrical nannoliths formed from one to several separate cycles of elements that radiate from a common centre or axis.
This taxon: Conical or cylindrical discoasteralids consisting of 10-30 wedge-shaped, radially-arranged elements, in one to three superposed cycles.
Farinacci & Howe catalog pages:
Fasciculithaceae *
| Lith size: 0->0µm; |
Geological Range:
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:
Aubry, M. P., Bord, D. & Rodriguez, O. (2011). New taxa of the Order Discoasterales Hay 1977. Micropaleontology. 57(3): 269-287. gs Aubry, M. -P., Rodriguez, O., Bord, D., Godfrey, L., Schmitz, B. & Knox, R. W. O. B. (2012). The first radation of the Fasciculiths: Morphologic adaptations of the coccolithophores to oligotrophy. Australian Journal of Earth Sciences. 105(1): 29-38. gs Hay, W. W. & Mohler, H. P. (1967). Calcareous nannoplankton from Early Tertiary rocks at Point Labau, France and Paleocene-Early Eocene correlations. Journal of Paleontology. 41(6): 1505-1541. gs Miniati, F., Cappelli, C. & Monechi, S. (2021). Revised taxonomy and early evolution of fasciculiths at the Danian–Selandian transition. Journal of Micropalaeontology. 40: 101-144. gs O Monechi, S., Reale, V., Bernaola, G. & Balestra, B. (2012). Taxonomic review of early Paleocene fasciculiths. Micropaleontology. 58(4): 351-365. gs Monechi, S., Reale, V., Bernaola, G. & Balestra, B. (2013). The Danian/Selandian boundary at Site 1262 (South Atlantic) and in the Tethyan region: Biomagnetostratigraphy, evolutionary trends in fasciculiths and environmental effects of the Latest Danian Event. Marine Micropaleontology. 98(1): 28-40. 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 OReferences:

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Fasciculithaceae compiled by Jeremy R. Young, Paul R. Bown, Jacqueline A. Lees viewed: 8-6-2026
Short stable page link: https://mikrotax.org/Nannotax3/index.php?id=563 Go to Archive.is to create a permanent copy of this page - citation notes |
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