Nannotax3 - ntax_mesozoic - Hemipodorhabdus Nannotax3 - ntax_mesozoic - Hemipodorhabdus

Hemipodorhabdus


Classification: ntax_mesozoic -> Podorhabdales -> Axopodorhabdaceae -> Hemipodorhabdus
Sister taxa: Podorhabdus, Hemipodorhabdus, Axopodorhabdus, Tetrapodorhabdus, Hexapodorhabdus, Octocyclus, Octopodorhabdus ⟩⟨ Dodekapodorhabdus, Perissocyclus, Teichorhabdus ⟩⟨ Cribrosphaerella, Ethmorhabdus, Nephrolithus, Psyktosphaera ⟩⟨ Cribrocorona

Distinguishing features:
Parent taxon (Axopodorhabdaceae): Regular placoliths; central-area, with cross-bars or perforated plate; often with tall, hollow spines.
Distal shield elements non-imbricate V-units; proximal shield and inner cycle formed from R-units. Rim often appears beaded in LM

This taxon: Elliptical; central area narrow, spanned by a transverse bar.


Daughter taxa (time control age-window is: 0-800Ma)
Hemipodorhabdus gorkae
Podorhabdids with narrow central area spanned by a transverse bar bearing a hollow spine.
Hemipodorhabdus sp.
Specimens not identified to species level

Taxonomy:

Citation: Hemipodorhabdus Black, 1971
taxonomic rank: Genus
Type species: Podorhabdus gorkae Reinhardt, 1969, designated by Grün in Grün and Allemann, 1975.

Farinacci & Howe catalog pages: Hemipodorhabdus *

Distinguishing features:
Parent taxon (Axopodorhabdaceae): Regular placoliths; central-area, with cross-bars or perforated plate; often with tall, hollow spines.
Distal shield elements non-imbricate V-units; proximal shield and inner cycle formed from R-units. Rim often appears beaded in LM

This taxon: Elliptical; central area narrow, spanned by a transverse bar.

Search data:
LITHS: placolith, elliptical, CA: ca_disjunct, process, bar, CROSS-POLARS: rim-bicyclic, V-prominent, R-prominent,
Lith size: 5->6µm;
Data source notes: 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 Turonian Stage (100% up, 89.4Ma, in Turonian stage). Data source: Total of ranges of the species in this database
First occurrence (base): within Berriasian Stage (137.70-143.10Ma, base in Berriasian stage). Data source: Total of ranges of species in this database

Plot of occurrence data:

References:

Black, M. (1971a). Coccoliths of the Speeton Clay and Sutterby Marl. Proceedings of the Yorkshire Geological Society. 38: 381-424. gs

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

Grün, W. & Allemann, F. (1975). The Lower Cretaceous of Caravaca (Spain): Berriasian Calcareous Nannoplankton of the Miravetes Section (Subbetic Zone, Prov. of Murcia). Eclogae Geologicae Helvetiae. 68: 147-211. gs O


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Hemipodorhabdus compiled by Jeremy R. Young, Paul R. Bown, Jacqueline A. Lees viewed: 11-10-2024

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Short stable page link: https://mikrotax.org/Nannotax3/index.php?id=10516 Go to Archive.is to create a permanent copy of this page - citation notes
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