Antlers Formation
Antlers Formation Stratigraphic range: Early Cretaceous | |
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Type | Geological formation |
Location | |
Region | North America |
The Antlers Formation occurs as a band of strata from Arkansas through southern Oklahoma into northeastern Texas. It consists of 150 m (490 ft) of silty to sandy mudstones, fine- to coarse grained sandstones that are poorly to moderately sorted and cemented with clay or calcium carbonate. In places the sandstone may be conglomeratic or ferruginous (rich in iron oxides).
Based on correlation with the Trinity Group of Texas, the Antlers Formation is estimated to be late Aptian-early Albian. This age range is supported by the presence of two dinosaurs that are also known from the Cloverly Formation, Deinonychus and Tenontosaurus.
Amphibians
Indeterminate frog remains. Possible indeterminate salamander remains.
Amphibians of the Antlers Formation | ||||||
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Genus | Species | Location | Stratigraphic position | Abundance | Notes | Images |
Albanerpeton arthridion |
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Basal vertebrates ("Fish")
References: Cifelli et al. 1999; Wedel et al. 2000, Kielan-Jarorowska and Cifelli 2001; Nydam and Cifelli 2002.
Cartilaginous fish
Chondrichthyans of the Antlers Formation | ||||||
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Genus | Species | Location | Stratigraphic position | Abundance | Notes | Images |
Hybodus buderi |
Hybodontidae |
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?Hybodus sp. |
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Lissodus anitae |
Polyacrodontidae | |||||
Ray-finned fish
Possible indeterminate amiid remains. Possible indeterminate lepisosteid remains. Possible indeterminate semionotidae remains.
Actinopterygians of the Antlers Formation | ||||||
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Genus | Species | Location | Stratigraphic position | Abundance | Notes | |
Gyronchus dumblei |
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?Palaeobalistum sp. |
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Mammals
Possible indeterminate deltatheroidan material. Indeterminate multituberculate remains. Indeterminate tribosphenidan remains.
Mammals of the Antlers Formation | ||||||
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Genus | Species | Location | Stratigraphic position | Abundance | Notes | |
Astroconodon |
Astroconodon sp. |
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Atokatherium |
Atokatherium boreni |
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Paracimexomys crossi |
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Reptiles
Crurotarsans
Possible indeterminate atoposaurid remains. Possible indeterminate goniopholidid remains. Possible indeterminate pholidosaurid remains.
Crurotarsans of the Antlers Formation | ||||||
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Genus | Species | Location | Stratigraphic position | Abundance | Notes | |
Bemissartia sp. |
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Lepidosaurs
Possible indetrminate scincid remains.
Lepidosaurs of the Antlers Formation | ||||||
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Genus | Species | Location | Stratigraphic position | Abundance | Notes | |
Atokasaurus metarsiodon |
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Bemissartia |
Bemissartia sp. |
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Ptilotodon wilsoni |
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Ornithischians
Ornithischians of the Antlers Formation | ||||||
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Genus | Species | Location | Stratigraphic position | Abundance | Notes | Images |
Tenontosaurus sp. |
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Saurischians
Possible indeterminate bird remains are known from the formation.
Saurischians of the Antlers Formation | ||||||
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Genus | Species | Location | Stratigraphic position | Material | Notes | Images |
Acrocanthosaurus atokensis |
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Astrodon sp. |
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Deinonychus sp. |
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Sauroposeidon proteles |
"[Four] cervical vertebrae."[1] |
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Turtles
Turtles of the Antlers Formation | ||||||
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Genus | Species | Location | Stratigraphic position | Abundance | Notes | |
Glyptops sp. |
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Naomichelys |
Naomichelys sp. |
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See also
References
- ↑ "Table 13.1," in Weishampel, et al. (2004). Page 267.
Further reading
- Cifelli, R. Gardner, J.D., Nydam, R.L., and Brinkman, D.L. 1999. Additions to the vertebrate fauna of the Antlers Formation (Lower Cretaceous), southeastern Oklahoma. Oklahoma Geology Notes 57:124-131.
- Nydam, R.L. and R. L. Cifelli. 2002a. Lizards from the Lower Cretaceous
(Aptian-Albian) Antlers and Cloverly formations. Journal of Vertebrate Paleontology. 22:286–298.
- Kielan-Jarorowska, Z., and Cifelli, R.L. 2001. Primitive boreosphenidan mammal (?Deltatheroida) from the Early Cretaceous of Oklahoma. Acta Palaeontologica Polonica 46: 377-391.
- Wedel, M.J., Cifelli, R.L., and Sanders, R. K. 2000. Sauroposeidon Proteles, A new sauropod from the Early Cretaceous of Oklahoma. Journal of Vertebrate Paleontology 20:109-114.