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  Victoria
Country  Australia

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
Genus Species Presence Notes Images

Atlascopcosaurus[1]

A. loadsi[1]

Geographically present in Victoria, Australia.[1]

"Maxilla [and] teeth."[2]

Diluvicursor[3]

D. pickeringi[3]

Geographically present in Victoria, Australia.[3]

Partial poscranial skeleton.[3]

Leaellynasaura[1]

L. amicagraphica[1]

Geographically present in Victoria, Australia.[1]

"Skull fragments teeth, [and] isolated postcrania."[4]

Timimus[1]

T. hermani[1]

Geographically present in Victoria, Australia.[1]

Later determined to be indeterminate ornithomimmosaur remains.[1] "Tibiae [and] vertebrae."[5]

Aves indet.[6]

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. 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.
  2. "Table 18.1," in Weishampel, et al. (2004). Page 394.
  3. 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.
  4. "Table 18.1," in Weishampel, et al. (2004). Page 395.
  5. "Table 6.1," in Weishampel, et al. (2004). Page 139.
  6. 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.
  7. Owen, James. "New Dinosaur May Link S. American, Aussie Dinos". National Geographic News. Retrieved July 12, 2016.
  8. 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.
  9. 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.
  10. 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.


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