Daughter taxa (time control age-window is: 0-800Ma)![]() | |||||
both cycles low | |||||
![]() | Heliolithus kleinpellii Large, heliolith with two low birefringent cycles. The narrow cycle is around 3/4 the width of the wider cycle. | ||||
![]() | ![]() | ![]() | ![]() | Heliolithus bukryi Heliolith with two low birefringent cycles: The narrow cycle is around 1/3 the width of the wider cycle. | |
one cycle high | |||||
Heliolithus cantabriae Heliolith with a broad, low cycle and a higher, narrower cycle. The narrower cycle is over 3/4 the width of the wider cycle. | |||||
![]() | ![]() | ![]() | ![]() | Heliolithus knoxii Heliolith a broad, thin cycle and a higher, narrower cycle. The narrower cycle is about 1/2 the width of the wider cycle. | |
both cycles high | |||||
Heliolithus riedelii Heliolith with two high cycles, the narrower cycle is around 2/3 the width of the broader. | |||||
Heliolithus aktasii Two relatively high cycles of similar diameter. | |||||
Heliolithus sp. Specimens which cannot be assigned to any established species |
Taxonomy:
Distinguishing features:
Parent taxon (Heliolithaceae): Discoidal discoasteralids with several distinct cycles including at least one that is birefringent.
This taxon: Discoidal discoasteralids formed of two superposed birefringent cycles.
Farinacci & Howe catalog pages: Heliolithus * , Heliotrochus *
Morphology:
In well preserved specimens/with favourable orientation a third cycle is visble between these two in at least some species (notably H. cantabriae), in the EM this cycle is visible at the base of the column.
Romein (1979) used crystallographic orientation to infer origin from Fasciculithus bitectus (= Lithoptychius s.l.) and suggested that the disk was distal.
LITHS: nannolith-radiate, circular, star-shaped, CROSS-POLARS: V-prominent, R-prominent, |
Lith size: 6->18µm; |
Geological Range:
Last occurrence (top): in upper part of Thanetian Stage (70% up, 56.9Ma, in Thanetian stage). Data source: Total of range of species in this database
First occurrence (base): at base of Selandian Stage (4% up, 61.5Ma, in Selandian stage). Data source: Total of range of species in this database
Plot of occurrence data:
Aubry, M. -P. (2014). Cenozoic Coccolithophores: Discoasterales. Micropaleontology Press, American Museum of Natural History, New York. 1-400. 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 427-555. gs Romein, A. J. T. (1979). Lineages in Early Paleogene calcareous nannoplankton. Utrecht Micropaleontological Bulletin. 22: 1-231. gs OReferences:
![]() |
Heliolithus compiled by Jeremy R. Young, Paul R. Bown, Jacqueline A. Lees viewed: 26-3-2023
Short stables page link: https://mikrotax.org/Nannotax3/index.php?id=698 Go to Archive.is to create a permanent copy of this page - citation notes |
Comments
(0)