Similiscutum


Classification: Mesozoic -> Podorhabdales -> Biscutaceae -> Similiscutum
Sister taxa: Biscutum, Discorhabdus, Similiscutum, Boletuvelum, Chiastella, Crucibiscutum, Gaarderella, Gephyrobiscutum, Helicorhabdus, Jimenezberrocosoia, Seribiscutum, Sollasites,

Distinguishing features: Subcircular-elliptical with smooth, grey appearance in XPL and a narrow, bright inner-cycle; central-area narrow and may be empty or spanned by an axial cross.


Daughter taxa: (blue => in age window 0-800Ma)
Small (3.5-5 µm), elliptical, with narrow to closed central-area.
Small (4-5.5 µm), broadly elliptical, with narrow central area spanned by a small axial cross.
Larger (4-5 µm), with wide shields and very narrow or closed central area.
Small (3.5-4.5 µm), broadly elliptical, with very narrow central area closed by a spine bearing plate. Dark, unicyclic image in XPL with strongly striate shields.
Small (3.5-5 µm), subcircular to circular, with narrow to closed central-area.
Larger (4-5 µm), narrowly elliptical, with narrow central area spanned by a small axial cross.
Specimens not identified to species level

Taxonomy:

Citation: Similiscutum de Kaenel & Bergen, 1993
Rank: Genus
Type species: Similiscutum cruciulus de Kaenel and Bergen, 1993.
Notes & discussion: Taxonomic concepts within Similiscutum were revised by Mattioli et al. 2004 - and these are followed here.

Farinacci & Howe catalog pages: Similiscutum + *

Distinguishing features: Subcircular-elliptical with smooth, grey appearance in XPL and a narrow, bright inner-cycle; central-area narrow and may be empty or spanned by an axial cross.


Morphology remarks: The inner tube cycle is lower in height than in Biscutum and this results in the relatively dim collar in cross-polarised light (Mattioli et al. 2004).

Search data:
TagsLITHS: placolith, elliptical, CA: cross-axial, process, closed, V-UNITS: V-prominent, DETAILS: rim-unicyclic,
MetricsLith size: 3.5->5.5µm;
Sources: size range of included species
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 Bathonian Stage (100% up, 166.1Ma, in Bathonian stage). Data source: Total of range of species in this database
First occurrence (base): in mid part of Sinemurian Stage (47% up, 195.3Ma, in Sinemurian stage). Data source: Total of range of species in this database

Plot of occurrence data:

References:

Bown, P. R. & Cooper, M. K. E. (1998). Jurassic. In, Bown, P. R. (ed.) Calcareous Nannofossil Biostratigraphy. British Micropalaeontological Society Publication Series. 34-85. gs :: ::

de Kaenel, E. & Bergen, J. A. (1993). New Early and Middle Jurassic coccolith taxa and biostratigraphy from the eastern proto-Atlantic (Morocco, Portugal and DSDP Site 547B). Eclogae Geologicae Helvetiae. 86(861-907): -. gs :: view :: open

Mattioli, E., Pittet, B., Young, J. R. & Bown, P. R. (2004a). Biometric analysis of Pliensbachian-Toarcian (Lower Jurassic) coccoliths of the family Biscutaceae: intra- and interspecific variability versus palaeoenvironmental influence. In, Villa, G. , Lees, J. A. & Bown, P. R. (eds) Calcareous Nannofossil Palaeoecology and Palaeocenographic Reconstructions, Proceedings of the INA9 conference, Parma 2002. Marine Micropaleontology. 52(1-4): 5-27. gs :: ::


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Similiscutum compiled by Jeremy R. Young, Paul R. Bown, Jacqueline A. Lees viewed: 15-8-2020

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Short stable page link: http://mikrotax.org/Nannotax3/index.php?id=11084 Go to Archive.is to create a permanent copy of this page - citation notes



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