Earth:Trinity Group (geologic group)

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Trinity Group
Stratigraphic range: late Aptian-early Albian, 115–106 Ma
TypeGroup
Sub-units
UnderliesFredericksburg sands, Goodland Formation
OverliesCotton Valley Formation
Location
RegionTexas , Arkansas
CountryUnited States
Type section
Named forTrinity Rivers, Texas
Named byRobert Thomas Hill[1]
Trinity Group stratigraphic column in Texas

The Trinity Group is a group (sequence of rock strata) in the Lower Cretaceous lithostratigraphy of Texas , Arkansas, Mississippi, Louisiana and Oklahoma.[2][3][4] It is named for the Trinity River of Texas.

A stratigraphic column at the Mount Bonnell Fault location starts with the Lower Cretaceous Trinity Group overlain by the Edwards Group. Upper Cretaceous formations follow, starting with the Del Rio Clay, Buda Limestone, and then the Eagle Ford Group. Formations within the Trinity Group include the Hammett Formation, Cow Creek Formation, Hensel Formation, and Lower and Upper Glen Rose Formation. The Hammett and the lower portion of the Upper Glen Rose act as confining units (or aquitard) for the Middle Trinity Aquifer. The Upper Glen Rose contains the Upper Trinity Aquifer, which appears to have intra-aquifer groundwater flow with the Edwards Aquifer as water levels are at the same elevation.[5]


Vertebrate fauna

Crocodylomorphs

Crocodylomorphs reported from the Trinity Group
Genus Species Location Stratigraphic position Material Notes

Pachycheilosuchus[6]

P. trinquei

Glen Rose Formation

A neosuchian related to Eusuchia. Had procoelous vertebrae.

Paluxysuchus[7]

P. newmani

Twin Mountains Formation

A neosuchian related to Eusuchia

Dinosaurs

Dinosaurs reported from the Trinity Group
Genus Species Location Stratigraphic position Material Notes

Acrocanthosaurus

A. atokensis[8]

Twin Mountains Formation

A carcharodontosaurid

Arkansaurus[9]

A. fridayi

An ornithomimosaur

Astrophocaudia[10]

A. slaughteri

Paluxy Formation

A member of Somphospondyli

Cedarosaurus[10]

C. weiskopfae

Paluxy Formation

A brachiosaurid

Paluxysaurus[11]

P. jonesi

Twin Mountains Formation

Junior synonym of Sauroposeidon proteles

Sauroposeidon[10][11]

S. proteles

Twin Mountains Formation

A member of Somphospondyli

Tenontosaurus

T. dossi[12]

Twin Mountains Formation

An iguanodont

Convolosaurus[13]

C. marri[14]

Twin Mountains Formation

A basal ornithopod

Pterosaurs

Pterosaurs reported from the Trinity Group
Genus Species Location Stratigraphic position Material Notes

Radiodactylus[15]

R. langstoni

Glen Rose Formation

An azhdarchoid pterosaur

References

  1. Hill, R.T. (1888). "The Trinity formation of Arkansas, Indian Territory, and Texas". Science 11 (258): 21. doi:10.1126/science.ns-11.258.21. PMID 17742326. https://zenodo.org/record/2028772. 
  2. "Geologic Unit: Trinity". National Geologic Map Database. USGS. http://ngmdb.usgs.gov/Geolex/Units/Trinity_10950.html. Retrieved 31 May 2014. 
  3. Suarez, Celina A.; Frederickson, Joseph; Cifelli, Richard L.; Pittman, Jeffrey G.; Nydam, Randall L.; Hunt-Foster, ReBecca K.; Morgan, Kirsty (2021-10-21). "A new vertebrate fauna from the Lower Cretaceous Holly Creek Formation of the Trinity Group, southwest Arkansas, USA" (in en). PeerJ 9: e12242. doi:10.7717/peerj.12242. ISSN 2167-8359. PMC 8542373. https://peerj.com/articles/12242. 
  4. "Paleontologists Find Fossils of New Lizard and Fish Species in Arkansas | Sci-News.com" (in en-US). http://www.sci-news.com/paleontology/sciroseps-pawhuskai-anomoeodus-caddoi-10196.html. 
  5. Saribudak, Mustafa (September 2016). "Geophysical mapping of Mount Bonnell fault of Balcones fault zone and its implications on Trinity-Edwards Aquifer interconnection, central Texas, USA". The Leading Edge (Society of Exploration Geophysicists) 35 (9): 752–758. doi:10.1190/tle35090752.1. http://library.seg.org/doi/abs/10.1190/tle35090752.1. Retrieved 12 September 2016. 
  6. Rogers, Jack V., II (2003). "Pachycheilosuchus trinquei, a new procoelous crocodyliform from the Lower Cretaceous (Albian) Glen Rose Formation of Texas". Journal of Vertebrate Paleontology 23 (1): 128–145. doi:10.1671/0272-4634(2003)23[128:PTANPC]2.0.CO;2.
  7. Adams, T. L. (2013). "A new neosuchian crocodyliform from the Lower Cretaceous (late Aptian) Twin Mountains Formation of North-Central Texas". Journal of Vertebrate Paleontology 33: 85–10. doi:10.1080/02724634.2012.713277. edit
  8. Harris, J. D. 1998. A reanalysis of Acrocanthosaurus atokensis, its phylogenetic status, and paleobiogeographic implications, based on a new specimen from Texas. New Mexico Museum of Natural History and Science, Bulletin 13: 1-75.
  9. ReBecca K. Hunt; James H. Quinn (2018). "A new ornithomimosaur from the Lower Cretaceous Trinity Group of Arkansas". Journal of Vertebrate Paleontology. Online edition: e1421209. doi:10.1080/02724634.2017.1421209.
  10. 10.0 10.1 10.2 D'Emic, M. D. 2013. Revision of the sauropod dinosaurs of the Early Cretaceous Trinity Group, southern USA, with the description of a new genus. Journal of Systematic Palaeontology, 11:707-726.
  11. 11.0 11.1 Rose, P. J., 2007. A new titanosauriform sauropod (Dinosauria: Saurischia) from the Early Cretaceous of Central Texas and its phylogenetic relationships. Palaeontologia Electronica Vol. 10, Issue 2; 8A:65p, 2.6MB; http://palaeo-electronica.org/paleo/2007_2/00063/index.html (PDF: 65 pages)
  12. Winkler, D., P. A. Murry, and L. L. Jacobs. 1997. A new species of Tenontosaurus (Dinosauria, Ornithopoda) from the early Cretaceous of Texas. Journal of Vertebrate Paleontology, 17:330-348.
  13. Winkler, D. and P. A. Murry. 1989. Paleoecology and hypsilophodontid behavior at the Proctor Lake dinosaur locality (early Cretaceous) Texas. Geological Society of America, Special Paper 238:55-61.
  14. Andrzejewski, Kate A.; Winkler, Dale A.; Jacobs, Louis L.; Forster, Catherine (2019). "A new basal ornithopod (Dinosauria: Ornithischia) from the Early Cretaceous of Texas". PLOS ONE 14 (3): e0207935. doi:10.1371/journal.pone.0207935. PMID 30860999. 
  15. Andres, B.; Myers, T. S. (2013). "Lone Star Pterosaurs". Earth and Environmental Science Transactions of the Royal Society of Edinburgh: 1. doi:10.1017/S1755691013000303. edit