Eomobula 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
Synonyms / new combinations and misspellings
Eomobula aff. stehmanni
Eomobula aff. stehmanni
Description:
Citation: Eomobula stehmanni Herman, Hovestadt-Euler & Hovestadt, 1989: In: Database of fossil elasmobranch teeth www.shark-references.com, World Wide Web electronic publication, Version 11/2024
Please send your images of "Eomobula stehmanni" to info@shark-references.com
Eomobula stehmanniHerman, Hovestadt-Euler & Hovestadt, 1989, Eocene, Ypresian, NP12, Prémontré, Aisne, France © Jean-Francois LHOMME, www.vertebres-fossiles.com
Eomobula stehmanniHerman, Hovestadt-Euler & Hovestadt, 1989, Eocene, Ypresian, NP12, Prémontré, Aisne, France © Jean-Francois LHOMME, www.vertebres-fossiles.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=2111;
type species of Eomobula Herman et al., 1989 p. 176 [1132] by original designation (Art. 68.2 ICZN);
valid after Herman et al. (1989) p. 176 [1132];
shark-references Species-ID=2111;
type species of Eomobula Herman et al., 1989 p. 176 [1132] by original designation (Art. 68.2 ICZN);
valid after Herman et al. (1989) p. 176 [1132];
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
Generic Assessment and Reallocation of Cenozoic Myliobatinae based on new information of tooth, tooth plate and caudal spine morphology of extant taxa. Palaeontos, 24, 1–66
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
Les localités à mammifères des carrières de Grand Daoui, bassin des Ouled Abdoun, Maroc, Yprésien : premier état des lieux. Bulletin de la Société géologique de France, 174(3), 279–293
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
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
Generic Assessment and Reallocation of Cenozoic Myliobatinae based on new information of tooth, tooth plate and caudal spine morphology of extant taxa. Palaeontos, 24, 1–66
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
Les localités à mammifères des carrières de Grand Daoui, bassin des Ouled Abdoun, Maroc, Yprésien : premier état des lieux. Bulletin de la Société géologique de France, 174(3), 279–293
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
