Nannotax3 - ntax_main - Staurolithites aenigma Nannotax3 - ntax_main - Staurolithites aenigma

Staurolithites aenigma


Classification: ntax_main -> Mesozoic nannofossils -> Eiffellithales -> Chiastozygaceae -> Staurolithites -> Staurolithites aenigma
Sister taxa: << < S. coroniformis, S. gausorhethium, S. leptostaurus ⟩⟨ S. ormae, S. handleyi, S. laffittei, S. dorfii, S. lumina ⟩⟨ S. imbricatus, S. dicandidula, S. mitcheneri ⟩⟨ S. angustus, S. mutterlosei, S. zoensis ⟩⟨ S. aachenus, S. aenigma, S. ellipticus, S. elongatus, S. integer, S. mielnicensis, S. parma, S. sp.

Taxonomy:

Citation: Staurolithites aenigma Burnett, 1997
Taxonomic rank: species
Taxonomic discussion: The species is tentatively placed in Staurolithites but is dissimilar to other species in this genus because of the unusual situation of the cross sitting in a central plate. It is easily distinguishable from other species of the genus because of this feature. [Burnett 1997]

Distinguishing features:
Parent taxon (Staurolithites): Loxolith muroliths with relatively narrow rim and wide central area spanned by axial cross bars. The cross is usually spine bearing. Inner/proximal rim cycle is variably developed and so the LM image may be unicyclic or bicyclic. NB The bicyclic/unicyclic separation is simply controlled by how far the inwards the R-units develop so, although it is a useful identification criterion, it almost certainly has no real phylogenetic significance and would be a very poor character for defining genera.
This taxon: Rim bicyclic central area with plate around the cross

Farinacci & Howe catalog pages: S. aenigma *


Morphology:

Small- to medium-sized, elliptical coccolith with a bicyclic rim. The rims are equally narrow, the outer one being dark and the inner one bright. The central area contains a plate: this is unclear from LM observation but has been observed in the SEM. The axial cross is com-posed of laths and sits partially within the plate. This cross tends to be highly birefringent in the LM. [Burnett 1997]

Search data:
LITHS: murolith, elliptical, CA: cross-axial, ca_disjunct, plate, process, CROSS-POLARS: rim-bicyclic, V-prominent, R-prominent,
Lith size: 4->6µm;
Data source notes: illustrated specimens
The morphological data given here can be used on the advanced search page. See also these notes

Geological Range:
Notes: The range is not well consttained but the species has been recorded from Late Albian to the Turonian (Gale et al. 2019, pers. comms Emma Sheldon, Jackie Lees April 2024)
Last occurrence (top): within Turonian Stage (89.39-93.90Ma, top in Turonian stage). Data source: pers. comm Emma Sheldon, Jackie Lees (April 2024)
First occurrence (base): within Late Albian Substage (100.50-107.59Ma, base in Albian stage). Data source: Burnett 1998

Plot of occurrence data:

References:

Burnett, J. A. (1997c). New species and new combinations of Cretaceous nannofossils and a note on the origin of Petrarhabdus (Deflandre) Wise & Wind. Journal of Nannoplankton Research. 19(2): 133-146. gs

Burnett, J. A. (1998). Upper Cretaceous. In, Bown, P. R. (ed.) Calcareous Nannofossil Biostratigraphy. British Micropalaeontological Society Publication Series . 132-199. gs O

Gale, A. S., Kennedy, W. J., Burnett, J. A., Caron, M. & Kidd, B. E. (1996). The Late Albian to Early Cenomanian succession at Mont Risou, near Rosans (Drôme, SE France): an integrated study (ammonites, inoceramids, planktonic foraminifera, nannofossils, oxygen and carbon isotopes). Cretaceous Research. 17: 515-606. gs

Missing or ambiguous references: Gale et al. 2019;


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Staurolithites aenigma compiled by Jeremy R. Young, Paul R. Bown, Jacqueline A. Lees viewed: 21-6-2025

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Short stable page link: https://mikrotax.org/Nannotax3/index.php?id=11111 Go to Archive.is to create a permanent copy of this page - citation notes



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