Odontorhytis pappenheimi
Böhm, 1926
Classification: Elasmobranchii incert. sedis incert. fam.
Reference of the original description
Über tertiäre Versteinerungen von den Bogenfelser Diamantfeldern. Die Diamantenwüste Südwestafrikas, Bd. II: 55–87, pl. B, fig. 31, 33.
Über tertiäre Versteinerungen von den Bogenfelser Diamantfeldern. Die Diamantenwüste Südwestafrikas, Bd. II: 55–87, pl. B, fig. 31, 33.
Synonyms / new combinations and misspellings
Odontorhytis aff. pappenheimi
Odontorhytis aff. pappenheimi
Types
Odontorhytis pappenheimi
Odontorhytis pappenheimi
Description:
Citation: Odontorhytis pappenheimi Böhm, 1926: In: Database of fossil elasmobranch teeth www.shark-references.com, World Wide Web electronic publication, Version 11/2024
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References
Sharks and rays from the Mokattamian Stage (middle and late Eocene) of Egypt, including some species from the middle Eocene Midra Shale of Qatar. Egyptian Journal of Geology, 66(1), 105–153
DOI: 10.21608/EGJG.2022.173845.1028
Additions to the elasmobranch assemblage from the Bandah Formation (middle Eocene, Bartonian), Jaisalmer District, Rajasthan, India, and the palaeobiogeographic implications of the fauna. Palaeovertebrata, 44(2), Article e1
DOI: 10.18563/pv.44.2.e1
Diversity and renewal of tropical elasmobranchs around the Middle Eocene Climatic Optimum (MECO) in North Africa: New data from the lagoonal deposits of Djebel el Kébar, Central Tunisia. Palaeontologica Electronica, 23(2), Article a38
DOI: 10.26879/1085
A reworked elasmobranch fauna from Tunisia providing a snapshot of Eocene-Oligocene Tethyan faunas. Journal of African Earth Sciences, 149, 194–206
DOI: 10.1016/j.jafrearsci.2018.08.008
Stratigraphie et sédimentologie des dépôts marins et continentaux d’âge éocène moyen à miocène en Tunisie centrale (région du Djebel el Kébar). [Stratigraphy and sedimentology of the middle Eocene Miocene marine and continental deposits in central Tunisia (Djebel el Kebar region).] Bulletin de la Société géologique de France, 187(1), 11–25
DOI: 10.2113/gssgfbull.187.1.11
Shark and ray faunas in the Middle and Late Eocene of the Fayum Area, Egypt. Proceedings of the Geologists' Association, 122(1), 47–66
DOI: 10.1016/j.pgeola.2010.09.004
Paleo-environments of the exposed Eocene Sediments between Wadi El-Hitan and east Siwa in the Egyptian Western Desert based on their faunal content especially the vertebrates. Thesis, Zagazig University, Faculty of Science, Geology Department
A new Priabonian Chondrichthyans assemblage from the Western desert, Egypt: Correlation with the Fayum oasis. Journal of African Earth Sciences, 61(1), 27–37
DOI: 10.1016/j.jafrearsci.2011.04.005
A Freshwater Ichthyofauna from the Late Eocene Birket Qarun Formation, Fayum, Egypt. Journal of Vertebrate Paleontology, 30(3), 665–680
DOI: 10.1080/02724631003758060
Geology and Paleontology of the Eocene Drazinda Shale Member of the Khirthar Formation, central Western Pakistan, Part II Late Eocene fishes. Tertiary Research, 12(3–4), 105–120
The Eocene selachian fauna from the Fayum Depression in Egypt. Palaeontographica, Abt. A, 212(1–6), 1–30
Additions à la faune de sélaciens fossiles du Maroc. 1: Sur la présence des genres Heptranchias, Alopias et Odontorhytis dans l'Yprésien des Ouled Abdoun. Geobios, 14(5), 563–575
DOI: 10.1016/S0016-6995(81)80137-4
Über tertiäre Versteinerungen von den Bogenfelser Diamantfeldern. Die Diamantenwüste Südwestafrikas, Bd. II: 55–87, pl. B, fig. 31, 33.
Sharks and rays from the Mokattamian Stage (middle and late Eocene) of Egypt, including some species from the middle Eocene Midra Shale of Qatar. Egyptian Journal of Geology, 66(1), 105–153
DOI: 10.21608/EGJG.2022.173845.1028
Additions to the elasmobranch assemblage from the Bandah Formation (middle Eocene, Bartonian), Jaisalmer District, Rajasthan, India, and the palaeobiogeographic implications of the fauna. Palaeovertebrata, 44(2), Article e1
DOI: 10.18563/pv.44.2.e1
Diversity and renewal of tropical elasmobranchs around the Middle Eocene Climatic Optimum (MECO) in North Africa: New data from the lagoonal deposits of Djebel el Kébar, Central Tunisia. Palaeontologica Electronica, 23(2), Article a38
DOI: 10.26879/1085
A reworked elasmobranch fauna from Tunisia providing a snapshot of Eocene-Oligocene Tethyan faunas. Journal of African Earth Sciences, 149, 194–206
DOI: 10.1016/j.jafrearsci.2018.08.008
Stratigraphie et sédimentologie des dépôts marins et continentaux d’âge éocène moyen à miocène en Tunisie centrale (région du Djebel el Kébar). [Stratigraphy and sedimentology of the middle Eocene Miocene marine and continental deposits in central Tunisia (Djebel el Kebar region).] Bulletin de la Société géologique de France, 187(1), 11–25
DOI: 10.2113/gssgfbull.187.1.11
Shark and ray faunas in the Middle and Late Eocene of the Fayum Area, Egypt. Proceedings of the Geologists' Association, 122(1), 47–66
DOI: 10.1016/j.pgeola.2010.09.004
Paleo-environments of the exposed Eocene Sediments between Wadi El-Hitan and east Siwa in the Egyptian Western Desert based on their faunal content especially the vertebrates. Thesis, Zagazig University, Faculty of Science, Geology Department
A new Priabonian Chondrichthyans assemblage from the Western desert, Egypt: Correlation with the Fayum oasis. Journal of African Earth Sciences, 61(1), 27–37
DOI: 10.1016/j.jafrearsci.2011.04.005
A Freshwater Ichthyofauna from the Late Eocene Birket Qarun Formation, Fayum, Egypt. Journal of Vertebrate Paleontology, 30(3), 665–680
DOI: 10.1080/02724631003758060
Geology and Paleontology of the Eocene Drazinda Shale Member of the Khirthar Formation, central Western Pakistan, Part II Late Eocene fishes. Tertiary Research, 12(3–4), 105–120
The Eocene selachian fauna from the Fayum Depression in Egypt. Palaeontographica, Abt. A, 212(1–6), 1–30
Additions à la faune de sélaciens fossiles du Maroc. 1: Sur la présence des genres Heptranchias, Alopias et Odontorhytis dans l'Yprésien des Ouled Abdoun. Geobios, 14(5), 563–575
DOI: 10.1016/S0016-6995(81)80137-4
Über tertiäre Versteinerungen von den Bogenfelser Diamantfeldern. Die Diamantenwüste Südwestafrikas, Bd. II: 55–87, pl. B, fig. 31, 33.