Nannotax3 - ntax_cenozoic - Rhomboasteraceae Nannotax3 - ntax_cenozoic - Rhomboasteraceae


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

Daughter taxa (time control age-window is: 0-800Ma)Granddaughter taxa
Solid nannoliths that include rhombic, rhombic with spinose extensions and forms composed of two superimposed tri-radiate cycles.
Rhomboaster bramlettei
Rhomboaster calcitrapa
Rhomboaster cuspis
Rhomboaster sp.

Solid nannoliths with three rays that typically have terminal bifurcations.
Tribrachiatus contortus
Tribrachiatus digitalis
Tribrachiatus orthostylus
Tribrachiatus absidatus
Tribrachiatus lunatus
Tribrachiatus sp.


Citation: Rhomboasteraceae Bown, 2005
taxonomic rank: Family
Taxonomic discussion: Rhomboaster and Tribrachiatus nannoliths comprise an evolutionary lineage from the oldest, rhombic nannoliths (cuspis-type), through intermediate forms with two superimposed tri-radiate cycles (bramlettei-type), to the youngest, single-cycle tri-radiate forms (orthostylus-type). Bybell & Self-Trail (1995, 1997) argued for the use of one genus only, whereas others have retained both (e.g. Aubry, 1996), see also von Salis et al. (2000). Both genera are included here: Rhomboaster for nannoliths with three-dimensional, rhombic to bicyclic tri-radiate morphologies, and Tribrachiatus for flatter morphologies with a single tri-radiate cycle.

Distinguishing features:
Parent taxon (Nannolith families inc sed): Haptophytes forming calcareous structures not obviously homologous with heterococcoliths, holococcoliths, or discoasteralids
This taxon: Nannoliths with rhombic and tri-radiate morphologies, and non-birefringent images in XPL. Incorporating the genera Rhomboaster and Tribrachiatus.

Farinacci & Howe catalog pages: Rhomboasteraceae [no catalog entry yet]


Crystallography: the c-axis is parallel to rotational axis of the nannolith and so in plan view they show no birefringence, they are, however, often tilted and so show moderate birefringence. In side view they show high birefringence.

Search data:
Lith size: 5->20µm;
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 NP12 zone (100% up, 50.5Ma, in Ypresian stage). Data source: Total of ranges of the species in this database
First occurrence (base): within NP9 zone (55.86-57.21Ma, base in Thanetian stage). Data source: Total of ranges of species in this database

Plot of occurrence data:


Aubry, M. -P. (1996). Towards an Upper Paleocene-Lower Eocene high resolution stratigraphy based on calcarous nannofossil stratigraphy. Israel Journal of Earth Sciences. 44(239-253): -. gs

Bown, P. R. (2005d). Palaeogene calcareous nannofossils from the Kilwa and Lindi areas of coastal Tanzania (Tanzania Drilling Project 2003-4). Journal of Nannoplankton Research. 27(1): 21-95. gs O

Bybell, L. M. & Self-Trail, J. (1995). Evolutionary, biostratigraphic and taxonomic study of calcareous nanofossils from a continuous Palaeocene-Eocene boundary section in New Jersey. U.S. Geological Survey, Professional Paper. 1554: 1-36. gs O

Bybell, L. & Self-Trail, J. (1997). Late Paleocene and Early Eocene calcareous nannofossils from three boreholes in an onshore-offshore transect from New Jersey to the Atlantic continental rise. Proceedings of the Ocean Drilling Program, Scientific Results. 150: 91-110. gs O

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

von Salis, K., Monechi, S., Bybell, L. M., Self-Trail, J. & Young, J. R. (2000). Remarks on the calcareous nannofossil genera Rhomboaster and Tribrachiatus around the Paleocene/Eocene Boundary. GFF. 122(138-140): -. gs


Rhomboasteraceae compiled by Jeremy R. Young, Paul R. Bown, Jacqueline A. Lees viewed: 19-4-2024

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