Eumeralla Formation
Eumeralla Formation Stratigraphic range: Aptian-Albian[1] | |
---|---|
Type | Geological formation |
Unit of | Otway Group |
Sub-units | Windermere Sandstone Member, Heathfield Sandstone Member |
Underlies | Sherbrook Group |
Overlies | Katnook Sandstone, Laira Formation (Crayfish Subgroup} |
Thickness | Up to 3000 m |
Lithology | |
Primary | Volcanilithic sandstone, siltstone, mudstone, conglomerate |
Location | |
Region |
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Country |
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The Eumeralla Formation is a geological formation in Victoria, Australia whose strata date back to the Early Cretaceous. Dinosaur remains are among the fossils that have been recovered from the formation.[1] It is equivalent to the Wonthaggi Formation.
Dinosaurs
Indeterminate dinosaur tracks as well as indeterminate ornithischian tracks are present in Victoria, Australia.[1] Indeterminate euornithopod remains are present in Victoria, Australia.[1] Indeterminate theropod, ornithomimmosaur, and possible indeterminate oviraptorosaur and dromaeosaurid remains are present in Victoria, Australia.[1]
Dinosaurs of the Eumeralla Formation | ||||
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Genus | Species | Presence | Notes | Images |
A. loadsi[1] |
Geographically present in Victoria, Australia.[1] |
"Maxilla [and] teeth."[2] |
| |
D. pickeringi[3] |
Geographically present in Victoria, Australia.[3] |
Partial poscranial skeleton.[3] | ||
L. amicagraphica[1] |
Geographically present in Victoria, Australia.[1] |
"Skull fragments teeth, [and] isolated postcrania."[4] | ||
T. hermani[1] |
Geographically present in Victoria, Australia.[1] |
Later determined to be indeterminate ornithomimmosaur remains.[1] "Tibiae [and] vertebrae."[5] | ||
No formal name. |
Possibly from a species also found at the Wonthaggi Formation (single furcula). |
Footprints belonging to a crane-sized bird, determined to be an ornithurine or enantiornithe. | ||
Megaraptora indet.[7] |
No formal name |
Known from a hand. |
Related to the South American Megaraptor. | |
Spinosaurinae indet.[8] [9] |
No formal name |
Known from a single cervical vertebra. |
Related to the African Spinosaurus. | |
Ankylosauria indet.[10] | No formal name | Dinosaur Cove | Dorsal vertebra | |
See also
References
- 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 Weishampel, David B; et al. (2004). "Dinosaur distribution (Early Cretaceous, Australasia)." In: Weishampel, David B.; Dodson, Peter; and Osmólska, Halszka (eds.): The Dinosauria, 2nd, Berkeley: University of California Press. Pp. 573-574. ISBN 0-520-24209-2.
- ↑ "Table 18.1," in Weishampel, et al. (2004). Page 394.
- 1 2 3 4 Herne, M.C.; Tait, A.M; Weisbecker, V.; Hall, M.; Nair, J.P; Cleeland, M.; Salisbury, S.W. "A new small-bodied ornithopod (Dinosauria, Ornithischia) from a deep, high-energy Early Cretaceous river of the Australian–Antarctic rift system". PeerJ. doi:10.7717/peerj.4113.
- ↑ "Table 18.1," in Weishampel, et al. (2004). Page 395.
- ↑ "Table 6.1," in Weishampel, et al. (2004). Page 139.
- ↑ Martin, Anthony J.; Vickers-Rich, Patricia; Rich, Thomas H.; Hall, Michael (2013). "Oldest known avian footprints from Australia: Eumeralla Formation (Albian), Dinosaur Cove, Victoria". Palaeontology. 57: 7–19. doi:10.1111/pala.12082.
- ↑ Owen, James. "New Dinosaur May Link S. American, Aussie Dinos". National Geographic News. Retrieved July 12, 2016.
- ↑ Barrett, Paul (June 21, 2011). "First spinosaurid from Australia and the cosmopolitanism of Cretaceous dinosaur faunas". Biology Letters. 7: 933–936. doi:10.1098/rsbl.2011.0466. Retrieved July 12, 2016.
- ↑ Arden, T.M.S.; Klein, C.G.; Zouhri, S.; Longrich, N.R. (2018). "Aquatic adaptation in the skull of carnivorous dinosaurs (Theropoda: Spinosauridae) and the evolution of aquatic habits in Spinosaurus". Cretaceous Research. In Press. doi:10.1016/j.cretres.2018.06.013.
- ↑ Barrett, Paul M.; Rich, Thomas H.; Vickers-Rich, Patricia; Tumanova, Tat'yana A.; Inglis, Matthew; Pickering, David; Kool, Lesley; Kear, Benjamin P. (September 2010). "Ankylosaurian dinosaur remains from the Lower Cretaceous of southeastern Australia". Alcheringa: An Australasian Journal of Palaeontology. 34 (3): 205–217. doi:10.1080/03115511003655430. ISSN 0311-5518.