Eomobula aff. stehmanni
Herman, Hovestadt-Euler & Hovestadt, 1989
Classification: Elasmobranchii Myliobatiformes Mobulidae
Reference of the original description
Additions to the Eocene fish fauna of Belgium. 9. Discovery of Eomobula gen. et sp. nov. (Mobulidae, Chondrichthyes) from the Ypresian. Tertiary Research, 10(4), 175–178
Additions to the Eocene fish fauna of Belgium. 9. Discovery of Eomobula gen. et sp. nov. (Mobulidae, Chondrichthyes) from the Ypresian. Tertiary Research, 10(4), 175–178
Types
Eomobula aff. stehmanni
Eomobula aff. stehmanni
Description:
Citation: Eomobula aff. stehmanni Herman, Hovestadt-Euler & Hovestadt, 1989: In: Database of fossil elasmobranch teeth www.shark-references.com, World Wide Web electronic publication, Version 12/2024
No image available.
Please send your images of "Eomobula aff. stehmanni" to
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Please send your images of "Eomobula aff. stehmanni" to
info@shark-references.com
Description
Original diagnose after Herman et al. (1989) p. 176 [1132]: A mobulaform known from isolated teeth only. The teeth have a similarity with the female characters of those of Mobula. The broad, massive crown has a subquadrate profile. Externally the crown is convex with a deep basal depression and leans strongly forward over the root. The blunt cutting edge tends to form a median cusp. The root is low, basally flat and subpolyaulacorhize. Most of the parallel intermedian grooves are closed, leaving several basal foramina and apertures. Foramina are abundant on both inner and outer faces.
Original diagnose after Herman et al. (1989) p. 176 [1132]: A mobulaform known from isolated teeth only. The teeth have a similarity with the female characters of those of Mobula. The broad, massive crown has a subquadrate profile. Externally the crown is convex with a deep basal depression and leans strongly forward over the root. The blunt cutting edge tends to form a median cusp. The root is low, basally flat and subpolyaulacorhize. Most of the parallel intermedian grooves are closed, leaving several basal foramina and apertures. Foramina are abundant on both inner and outer faces.
Remarks
shark-references Species-ID=10909;
shark-references Species-ID=10909;
References
The marine and terrestrial vertebrate faunas from the Paleogene of the Ouarzazate basin, Morocco. In S. Zouhri(Ed.), Mémoires de la Société Géologique de France, vol. 180, Paléontologie des vertébrés du Maroc: état des connaissancess: 485-525
Aznag (bassin d'Ouarzazate, Maroc), nouvelle localité à sélaciens et mammifères de l'Eocène moyen (Lutétien) d'Afrique. Bulletin de la Société géologique de France, 176(4), 381–400
DOI: 10.2113/176.4.381
The marine and terrestrial vertebrate faunas from the Paleogene of the Ouarzazate basin, Morocco. In S. Zouhri(Ed.), Mémoires de la Société Géologique de France, vol. 180, Paléontologie des vertébrés du Maroc: état des connaissancess: 485-525
Aznag (bassin d'Ouarzazate, Maroc), nouvelle localité à sélaciens et mammifères de l'Eocène moyen (Lutétien) d'Afrique. Bulletin de la Société géologique de France, 176(4), 381–400
DOI: 10.2113/176.4.381
