Hypsibema
From Greek hypsi (high) and bema (step); meaning 'high step', because Edward Cope believed the animal walked particularly erect on its toes
Hypsibema is a dubious genus of very large dinosaur from the Late Cretaceous of eastern North America, of uncertain affinities. The type species, H. crassicauda, is known mainly from the Tar Heel Formation of North Carolina and the Marshalltown Formation of New Jersey, and its fragmentary material has been interpreted as sauropod as well as hadrosaurian. A second species, H. missouriensis from the Maastrichtian of Missouri, was originally named Neosaurus and then Parrosaurus before being referred to Hypsibema by Baird and Horner (1979); Brownstein (2018) returns it to Parrosaurus.
Under dispute
Baird and Horner (1979) restricted Hypsibema crassicauda to a lectotype caudal, the type series being a mixture of three suborders, and referred it to Sauropoda, a placement later work rejects. Prieto-Márquez and colleagues (2016) list H. crassicauda and the Missouri species among the nondiagnostic Appalachian hadrosaurids, while Brownstein (2018) treats both as valid giant hadrosauroids, the Missouri species as Parrosaurus missouriensis, of uncertain placement within or outside Hadrosauridae. It is placed at Hadrosauroidea incertae sedis.
Species (2)
Hypsibema crassicauda Cope, 1869 Nomen dubium
Type species
From Latin 'crassus' meaning 'thick' or 'fat' and 'cauda' meaning 'tail', together meaning 'with a fat tail', in reference to the massively constructed tail of the species.
- Holotype
- USNM 7189 , National Museum of Natural History, Smithsonian Institution
- Material
- Humerus, tibia, fibula, metatarsus, caudal vertebra, cervical vertebrae, ungueal phalange
- Horizon
- Black Creek Formation, Campanian, Late Cretaceous , 83.6–72.2 million years ago
- Locality
- Marl pits of James King, North Carolina, United States
Hypsibema missouriensis (Gilmore & Stewart, 1945) Disputed
First named as Neosaurus missouriensis
Named for Missouri, the U.S. state where the holotype was discovered, with the Latin suffix '-ensis'.
- Holotype
- USNM 16735 , National Museum of Natural History, Smithsonian Institution
- Material
- 13 caudal centra and two unidentified fragments; all neural arches missing
- Horizon
- McNairy Sand Member, Ripley Formation, Maastrichtian, Late Cretaceous , 72.2–66.0 million years ago
- Locality
- Chronister farm, Missouri, United States
- Diagnosis
-
- Caudal centra amphicoelous, longer than wide, with angularly rounded sides shallowly concave from end to end
- Articular ends with a flattened peripheral border surrounding a concave central area bearing radiating bumps and depressions
- Sides of the centra divided subequally by a low longitudinal ridge that fades posteriorly
- Chevron facets restricted to the posterior ends of the centra, the ventral surface scooped out between them
Synonyms
-
Neosaurus missouriensis reassigned
Original combination (Gilmore and Stewart, 1945); the genus name Neosaurus was preoccupied.
-
Parrosaurus missouriensis reassigned
Combination under Parrosaurus, the replacement name Gilmore (1945) coined for the preoccupied Neosaurus; referred to Hypsibema by Baird and Horner (1979).
Synonyms of the genus
| Name | Type | Reason |
|---|---|---|
| Neosaurus | preoccupied | Name preoccupied by Neosaurus (Reptilia). |
| Parrosaurus | reassigned | Coined by Gilmore (1945) as a replacement for the preoccupied Neosaurus; its type species was referred to Hypsibema by Baird and Horner (1979). Brownstein (2018) uses Parrosaurus missouriensis. |
References
-
Cope, E. D. (1869). [Remarks on Eschrichtius polyporus, Hypsibema crassicauda, Hadrosaurus tripos, and Polydectes biturgidus]. Proceedings of the Academy of Natural Sciences of Philadelphia 21: 191-192.
Records the type material from Sampson County, North Carolina, of Cretaceous age but intrusive in Miocene beds, without a closer locality.
cope1869a -
Gilmore, C. W.; Stewart, D. R. (1945). A new sauropod dinosaur from the Upper Cretaceous of Missouri. Journal of Paleontology 19(1): 23-29. https://www.jstor.org/stable/1299165
Original description of the type material, as the sauropod Neosaurus missouriensis.
gilmore1945a -
Gilmore, C. W. (1945). Parrosaurus, n. name, replacing Neosaurus Gilmore, 1945. Journal of Paleontology 19(5): 540. https://www.jstor.org/stable/1299009
Replacement genus name (Parrosaurus) for the preoccupied Neosaurus Gilmore, 1945.
gilmore1945b -
Baird, D.; Horner, J. R. (1979). Cretaceous dinosaurs of North Carolina. Brimleyana 2: 1-28. https://www.biodiversitylibrary.org/part/442233
Referred Parrosaurus missouriensis to Hypsibema. Traces the type material of H. crassicauda to the marl pits of James King in Sampson County, in the "blue marl", now the Black Creek Formation.
baird1979a -
Horner, J. R. (1979). Upper Cretaceous dinosaurs from the Bearpaw Shale (marine) of south-central Montana with a checklist of Upper Cretaceous dinosaur remains from marine sediments in North America. Journal of Paleontology 53(3): 566-577.
Lists the type of Parrosaurus missouriensis, now this genus's second species, as USNM 16733; Gilmore (1945) prints U.S.N.M. 16735.
horner1979b -
Prieto-Márquez, A.; Erickson, G. M.; Ebersole, J. A. (2016). Anatomy and osteohistology of the basal hadrosaurid dinosaur Eotrachodon from the uppermost Santonian (Cretaceous) of southern Appalachia. PeerJ. PeerJ.
Lists Hypsibema crassicauda and Parrosaurus missouriensis among the nondiagnostic hadrosaurids of the Appalachian record.
prieto-márquez2016b -
Brett-Surman, M. K. (1989). A revision of the Hadrosauridae (Reptilia: Ornithischia) and their evolution during the Campanian and Maastrichtian. 1-272. Doctoral thesis, The George Washington University.
Finds none of the elements diagnostic and calls Hypsibema a nomen dubium, questioning its transfer to Sauropoda.
brett-surman1989a -
Brownstein, C. D. (2018). The biogeography and ecology of the Cretaceous non-avian dinosaurs of Appalachia. Palaeontologia Electronica 21.1.5A: 1-56. doi:10.26879/801
Treats Hypsibema crassicauda and the Missouri species, as Parrosaurus missouriensis, as valid giant hadrosauroids of uncertain placement within or outside Hadrosauridae.
brownstein2018a