Daughter taxa (time control age-window is: 0-800Ma)![]() | Granddaughter taxa | ||||
Holococcoliths formed from multiple blocks | |||||
![]() | ![]() | ![]() | Daktylethra Domed cavate holococcoliths with surficial shallow pits. | ||
![]() | ![]() | Holodiscolithus Elliptical holococcoliths with perforations. | Holodiscolithus agniniae Holodiscolithus catellus Holodiscolithus geisenii Holodiscolithus lippertii Holodiscolithus liui Holodiscolithus macroporus Holodiscolithus minolettii Holodiscolithus serus Holodiscolithus solidus Holodiscolithus whitesideae Holodiscolithus sp. | ||
![]() | ![]() | ![]() | ![]() | Lanternithus Cavate holoccoliths with distinct crystallographic blocks. | Lanternithus arcanus Lanternithus duocavus Lanternithus jawzii Lanternithus minutus Lanternithus procerus Lanternithus simplex Lanternithus unicavus Munarinus emrei Lanternithus sp. |
![]() | Multipartis Holococcoliths with multiple elements in the central area | ||||
![]() | Octolithus Holoccoliths with distinct rim and cover blocks, typically eight. | ||||
![]() | ![]() | ![]() | ![]() | Quadrilateris Rectangular holococcoliths formed from four thin blocks that are birefringent in XPL. | |
![]() | ![]() | Semihololithus Paleogene holococcoliths usually seen in side view and comprising a thick proximal plate and spine or process, typically with a cavity or axial canal. | Semihololithus biskayae Semihololithus dimidius Semihololithus kanungoi Semihololithus pseudobiskayae Semihololithus sp. cf. S. biskayae Semihololithus tentorium Naninfula figularia Naninfula hexaporus Semihololithus sp. | ||
![]() | ![]() | ![]() | ![]() | Varolia Cavate, thin walled, box-like holococcoliths usually seen in side view. | |
![]() | ![]() | ![]() | ![]() | Youngilithus Geometrically shaped non-birefringent holococcoliths typically possessing lateral rim spines and central area bars. | Youngilithus arcaeformis Youngilithus bipons Youngilithus oblongatus Youngilithus pyxis Youngilithus quadraeformis Youngilithus transversipons Youngilithus sp. |
![]() | ![]() | Zygrhablithus Spinose holococcoliths, which are birefringent in side view. In plan view the coccoliths are non-birefringent with a distinct figure-of-eight shaped central structure. | |||
Holococcoliths formed from a single block | |||||
![]() | ![]() | ![]() | ![]() | Aubrysphaera | |
![]() | ![]() | ![]() | Corannulus Discoidal holococcoliths with large central openings and marginal perforations or indentations; non-birefringent in plan view. | ||
![]() | ![]() | ![]() | ![]() | Orthozygus Single-block holococcoliths that typically have a spine or process and transverse bridge or bars. | Orthozygus arcus Orthozygus aureus Orthozygus brytika Orthozygus occultus Orthozygus sudis Orthozygus suggrandis Orthozygus sp. |
![]() | ![]() | ![]() | ![]() | Peritrachelina Unusual holococcoliths with non-coccolith morphology typically comprising an elliptical, concavo-convex, domed, perforate framework. | Peritrachelina arenaria Peritrachelina joidesa Peritrachelina minuta Peritrachelina ornata Peritrachelina sp. |
Unidentified fossil holococcoliths |
Taxonomy:
Distinguishing features:
Parent taxon (Holococcoliths): Haploid life-cycle stages, with liths formed of numerous rhombohedral microcrystals
This taxon: Holococcolith genera only known from the fossil record
Farinacci & Howe catalog pages: Calyptrosphaeraceae [no catalog entry yet]
Morphology:
Lith size: 0->0µm; |
Geological Range:
Last occurrence (top): in upper part of Ionian Stage (75% up, 0.3Ma, in Ionian stage). Data source: Total of range of species in this database
First occurrence (base): at base of Campanian Stage (0% up, 83.6Ma, in Campanian stage). Data source: Total of range of species in this database
Plot of occurrence data:
![]() |
fossil holococcoliths compiled by Jeremy R. Young, Paul R. Bown, Jacqueline A. Lees viewed: 10-6-2023
Short stables page link: https://mikrotax.org/Nannotax3/index.php?id=595 Go to Archive.is to create a permanent copy of this page - citation notes |
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