Pseudomegachasma comanchensis
(Shimada, 2007)
Classification: Elasmobranchii Lamniformes Odontaspididae
Reference of the original description
Mesozoic origin for megamouth shark (Lamniformes: Megachasmidae). Journal of Vertebrate Paleontology, 27(2), 512–516
Mesozoic origin for megamouth shark (Lamniformes: Megachasmidae). Journal of Vertebrate Paleontology, 27(2), 512–516
Synonyms / new combinations and misspellings
Megachasma comanchensis
Megachasma comanchensis
Types
Pseudomegachasma comanchensis
Megachasma comanchensis
Holotype: FHSM: VP-15095; Paratype: FHSM: VP-15176;
Pseudomegachasma comanchensis
Megachasma comanchensis
Holotype: FHSM: VP-15095; Paratype: FHSM: VP-15176;
Description:
Citation: Pseudomegachasma comanchensis (Shimada, 2007): In: Database of fossil elasmobranch teeth www.shark-references.com, World Wide Web electronic publication, Version 12/2024
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Description
Original diagnose after Shimada (2007) p. 513 [2178]: Small lamnoid teeth (holotype as the largest specimen measuring 6 mm in total tooth height) consisting of tall crown (variably inclined distally), well-marked tooth neck, and massive root, with the following combination of characters: osteodont tooth histology (note absence of pulp cavity in Figure 1F); crown triangular in labial and lingual views, with pointed tip and sprawling base (except along the labial side); crown tip strongly directed lingually, giving hook-like appearance; mesial and distal cutting edges weak and blunt towards to apex and base of crown, and absent at mid-portion of crown outlining nearly perfect circle in transverse cross-section; crown surfaces smooth; lingual crown face strongly convex and labial face moderately convex; basal margin of crown gently convex or concave on labial face and broadly and deeply concave on lingual face (particularly noticeable in mesial and distal views); labiolingual length and mesiodistal length at crown base about equal; root massive and short apicobasally, with deep nutritive groove that bisects pronounced lingual protuberance and may possess prominent nutritive pore near center of the groove; apical face of lingual protuberance flat or weakly convex; basal face of each root lobe flat or weakly convex; and labiomesial corner of root labially pointing and labiodistal corner blunt and rounded. Mesiodistally oriented, low heel may occur at mesial and distal extremities of crown base along labial margin. Differing from teeth of Megachasma pelagios in possessing prominent nutritive groove that deeply bisects root longitudinally from the top of the lingual root protuberance.
Original diagnose after Shimada (2007) p. 513 [2178]: Small lamnoid teeth (holotype as the largest specimen measuring 6 mm in total tooth height) consisting of tall crown (variably inclined distally), well-marked tooth neck, and massive root, with the following combination of characters: osteodont tooth histology (note absence of pulp cavity in Figure 1F); crown triangular in labial and lingual views, with pointed tip and sprawling base (except along the labial side); crown tip strongly directed lingually, giving hook-like appearance; mesial and distal cutting edges weak and blunt towards to apex and base of crown, and absent at mid-portion of crown outlining nearly perfect circle in transverse cross-section; crown surfaces smooth; lingual crown face strongly convex and labial face moderately convex; basal margin of crown gently convex or concave on labial face and broadly and deeply concave on lingual face (particularly noticeable in mesial and distal views); labiolingual length and mesiodistal length at crown base about equal; root massive and short apicobasally, with deep nutritive groove that bisects pronounced lingual protuberance and may possess prominent nutritive pore near center of the groove; apical face of lingual protuberance flat or weakly convex; basal face of each root lobe flat or weakly convex; and labiomesial corner of root labially pointing and labiodistal corner blunt and rounded. Mesiodistally oriented, low heel may occur at mesial and distal extremities of crown base along labial margin. Differing from teeth of Megachasma pelagios in possessing prominent nutritive groove that deeply bisects root longitudinally from the top of the lingual root protuberance.
References
Global impact and selectivity of the Cretaceous-Paleogene mass extinction among sharks, skates, and rays. Science, 379, 802–806
DOI: 10.1126/science.abn2080
Climate cooling and clade competition likely drove the decline of lamniform sharks. Proceedings of the National Academy of Sciences of the United States of America, 116(41), 20584–20590
DOI: 10.1073/pnas.1902693116
A new clade of putative plankton-feeding sharks from the Upper Cretaceous of Russia and the United States. Journal of Vertebrate Paleontology, 35(5), Article e981335
DOI: 10.1080/02724634.2015.981335
A new clade of putative plankton-feeding sharks from the Upper Cretaceous of Russia and the United States. Journal of Vertebrate Paleontology, 35(5), Article e981335
DOI: 10.1080/02724634.2015.981335
A New Late Cretaceous Marine Vertebrate Assemblage from the Lincoln Limestone Member of the Greenhorn Limestone in Southeastern Colorado. Transactions of the Kansas Academy of Science, 115(3–4), 107–116
DOI: 10.1660/062.115.0303
Mid-Cenomanian vertebrate faunas of the WesternInterior Seaway of North America and their evolutionary, paleobiogeographical, and paleoecological implications. Palaeogeography, Palaeoclimatology, Palaeoecology, 295(1–2), 199–214
DOI: 10.1016/j.palaeo.2010.05.038
Mesozoic origin for megamouth shark (Lamniformes: Megachasmidae). Journal of Vertebrate Paleontology, 27(2), 512–516
DOI: 10.1671/0272-4634(2007)27[512:MOFMSL]2.0.CO;2
Global impact and selectivity of the Cretaceous-Paleogene mass extinction among sharks, skates, and rays. Science, 379, 802–806
DOI: 10.1126/science.abn2080
Climate cooling and clade competition likely drove the decline of lamniform sharks. Proceedings of the National Academy of Sciences of the United States of America, 116(41), 20584–20590
DOI: 10.1073/pnas.1902693116
A new clade of putative plankton-feeding sharks from the Upper Cretaceous of Russia and the United States. Journal of Vertebrate Paleontology, 35(5), Article e981335
DOI: 10.1080/02724634.2015.981335
A new clade of putative plankton-feeding sharks from the Upper Cretaceous of Russia and the United States. Journal of Vertebrate Paleontology, 35(5), Article e981335
DOI: 10.1080/02724634.2015.981335
A New Late Cretaceous Marine Vertebrate Assemblage from the Lincoln Limestone Member of the Greenhorn Limestone in Southeastern Colorado. Transactions of the Kansas Academy of Science, 115(3–4), 107–116
DOI: 10.1660/062.115.0303
Mid-Cenomanian vertebrate faunas of the WesternInterior Seaway of North America and their evolutionary, paleobiogeographical, and paleoecological implications. Palaeogeography, Palaeoclimatology, Palaeoecology, 295(1–2), 199–214
DOI: 10.1016/j.palaeo.2010.05.038
Mesozoic origin for megamouth shark (Lamniformes: Megachasmidae). Journal of Vertebrate Paleontology, 27(2), 512–516
DOI: 10.1671/0272-4634(2007)27[512:MOFMSL]2.0.CO;2