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Stephanolithiales


Classification: ntax_mesozoic -> Stephanolithiales
Sister taxa: Arkhangelskiales, Eiffellithales, Stephanolithiales, Podorhabdales, Watznaueriales, Syracosphaerales, Heterococcoliths inc sedis ⟩⟨ Holococcoliths, Braarudosphaerales, Nannoliths inc sedis, Mesozoic non–coccoliths, hidden

Distinguishing features:
Parent taxon (ntax_mesozoic): Mesozoic nannofossils - Cenozoic and extant taxa are in a separate module
This taxon: Murolith coccoliths with a distal/outer cycle of non-imbricating elements, i.e., in side view, the sutures are vertical or near-vertical.


Daughter taxa (time control age-window is: 0-800Ma)Granddaughter taxa
Parhabdolithaceae
Murolith (protolith type) coccoliths with bicylic rims and central-areas spanned by an axial-cross or transverse bar bearing a broad, often long, spine.
Bucanthus
Calcivascularis
Crucirhabdus
Diductius
Mitrolithus
Parhabdolithus
Timorella
Umbria

Stephanolithiaceae
Murolith (protolith type) coccoliths with rims of non-imbricate V-units and weakly-developed, or vestigial, proximal/inner-cycles (R-units), with central-areas spanned by one to numerous bars.

Taxonomy:

Citation: Stephanolithiales Bown & Young, 1997
Taxonomic rank: order
Taxonomic discussion: The order Stephanolithiales probably gave rise to the Order Syracosphaerales, since Calciosolenia is very similar to various Stephanolthaceae genera and early Syracosphaera species are similar to Stradnerlithus. This is also compatible with molecular gentic data since the Syracosphaerales appear to have diverged from he other coccolithophres in the basal radiatition of the group (i.e. in the Early Jurassic). So, it may well prove useful to subsume the Stephanolithiales into the Syracosphaerales, see also discussion in Bown et al. (2017)

Farinacci & Howe catalog pages: Stephanolithiales *

Distinguishing features:
Parent taxon (ntax_mesozoic): Mesozoic nannofossils - Cenozoic and extant taxa are in a separate module
This taxon: Murolith coccoliths with a distal/outer cycle of non-imbricating elements, i.e., in side view, the sutures are vertical or near-vertical.


Morphology:

Muroliths with a distal/outer-cycle composed of non-imbricating elements, i.e. in side view, the sutures are vertical or near vertical. This feature is not distinguishable from imbrication in the LM. The term protolith is applied to this rim structure (Bown, 1987). The order comprises (1) the Parhabdolithaceae a group of murolith coccoliths typified by thick, robust, high walls, which are characteristic component of Early Jurassic nannofloras, and (2) the Stephanolithaceae which have similar wall-structure but a more diverse range of morphologies and which occur throughout the Jurassic and Cretaceous.
Crystallographically the rims consist of an outer cycle of V-units and inner cycle of R-units, giving a bicyclic apearnce in cross-polars. The central structures are disjunct, and most often show low birefringence.   

Search data:
LITHS: murolith, elliptical, CA: ca_disjunct, CROSS-POLARS: R-prominent, V-prominent, rim-bicyclic,
Lith size: 0->0µm;
The morphological data given here can be used on the advanced search page. See also these notes

See also: Syracosphaerales ;

Geological Range:
Last occurrence (top): at top of Maastrichtian Stage (100% up, 66Ma, in Danian stage). Data source: Total of ranges of the species in this database
First occurrence (base): within NT2b subzone (194.83-218.41Ma, base in Norian stage). Data source: Total of ranges of species in this database

Plot of occurrence data:

References:

Bown, P. R. & Young, J. R. (1997). Mesozoic calcareous nannoplankton classification. Journal of Nannoplankton Research. 19(1): 21-36. gs

Bown, P. R. (1987a). Taxonomy, evolution, and biostratigraphy of Late Triassic-Early Jurassic calcareous nannofossils. Special Papers in Palaeontology. 38: 1-118. gs

Bown, P. R. (1998b). Triassic. In, Bown, P. R. (ed.) Calcareous Nannofossil Biostratigraphy. British Micropalaeontological Society Publication Series . 29-33. gs

Bown, P. R., Rutledge, D. C., Crux, J. A. & Gallagher, L. T. (1998). Lower Cretaceous. In, Bown, P. R. (ed.) Calcareous Nannofossil Biostratigraphy. British Micropalaeontological Society Publication Series . 86-131. gs O

Bown, P. R., Lees, J. A. & Young, J. R. (2017). On the Cretaceous origin of the Order Syracosphaerales and the genus Syracosphaera. Journal of Micropalaeontology. 36(2): 153-165. gs

Young, J. R. & Bown, P. R. (1997). Proposals for a revised classification system for calcareous nannoplankton. Journal of Nannoplankton Research. 19(1): 15-47. gs


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Stephanolithiales compiled by Jeremy R. Young, Paul R. Bown, Jacqueline A. Lees viewed: 20-1-2025

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Short stable page link: https://mikrotax.org/Nannotax3/index.php?id=11145 Go to Archive.is to create a permanent copy of this page - citation notes
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