Vicinocerithium seni, Islamoğğlu & Dominio & Kowalke, 2011
publication ID |
https://doi.org/ 10.5252/g2011n2a7 |
persistent identifier |
https://treatment.plazi.org/id/147BFA4C-FFCA-8D2C-3E85-FEB3FEFEFA74 |
treatment provided by |
Marcus |
scientific name |
Vicinocerithium seni |
status |
sp. nov. |
Vicinocerithium seni View in CoL n. sp. ( Fig. 7 View FIG E-G)
HOLOTYPE. — MTA-Y. İ.-2007 -34.
PARATYPES. —SevenparatypesinAnkara( MTA-Y. İ.-2007 -35 to 41) and one paratype ( NHMV 2008z0310/0001).
ETYMOLOGY. — In honour of Şevket Şen (CNRS, MNHN).
OTHER MATERIAL EXAMINED. — 118 specimens (MTA- Y. İ.-2007 -42 to 44).
TYPE LOCALITY AND HORIZON. — Grey siltstone-mudstone, KIrkkavak Formation (Macunköy: samples G1, G2, G3).
DESCRIPTION
Angular whorls with 6-8 irregular, primary and secondary spiral riblets and 9-10 strong axial elements forming big, strong and smooth tubercules, connected by more pronounced spiral elements. Prominent axial elements are formed by the coalescence of thick tubercules in the adapical part of the whorls. This structure is oblique prosocline from the initial whorls towards the body whorl. The concave base is ornamented by spiral riblets similar to the riblets in the base of each spiral whorl. The anterior canal is elongated and the aperture is cerithioid with oblique ovoidal siphonostome.
REMARKS
The species differs from Vicinocerithium cf. subacutum and Batillaria praesubacuta by its prominent axial elements and prominent spiral threads ( Doncieux 1908).
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