Hokomata parva

Hodnett & Elliott, 2018


Classification: Elasmobranchii Xenacanthiformes Diplodoselachidae

Reference of the original description
Hodnett, J.-P.M. & Elliott, D.K. (2018)
Carboniferous chondrichthyan assemblages from the Surprise Canyon and Watahomigi formations (latest Mississippian–Early Pennsylvanian) of the western Grand Canyon, Northern Arizona. Journal of Paleontology, 92(Supplement S77), 1–33

Types
Hokomata parva
Holotype: MNA: V11264;


Description:


Citation: Hokomata parva Hodnett & Elliott, 2018: In: Database of fossil elasmobranch teeth www.shark-references.com, World Wide Web electronic publication, Version 08/2026

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Description
Original diagnosis after Hodnett & Elliott, 2018 [26883]: A small diplodoselachian xenacanth with tall, near erect cusps. All cusps are smooth, lacking verticle cristae, with a slight mesial incline. Lateral and distal cusps labiolingually compressed with un-serrated carina. Median cusp evenly spaced from the lateral cusps, labiolingually rounded, and half the height of the lateral and distal cusps. Tooth base ovate; oral-aborally compressed, orolingual button near circular with a lingual shaft. Basolabial projection small and elliptical. Kidney-shaped aboral depression with four large foramina.

Remarks
shark-references Species-ID=15287;
type species of Hokomata Hodnett & Elliott, 2018 [26883] by monotypy (Art. 68.3 ICZN);

References
Hodnett, J.-P.M. & Elliott, D.K. (2018)
Carboniferous chondrichthyan assemblages from the Surprise Canyon and Watahomigi formations (latest Mississippian–Early Pennsylvanian) of the western Grand Canyon, Northern Arizona. Journal of Paleontology, 92(Supplement S77), 1–33
DOI: 10.1017/jpa.2018.72