Article · Wikipedia archive · Last revised Jul 20, 2026

Sundance Formation

The Sundance Formation is a western North American sequence of Middle Jurassic to Upper Jurassic age Dating from the Bathonian to the Oxfordian, around 168-157 Ma, It is up to 100 metres thick and consists of marine shale, sandy shale, sandstone, and limestone deposited in the Sundance Sea, an inland sea that covered large parts of western North America during the Middle and early Late Jurassic.

Last revised
Jul 20, 2026
Read time
≈ 3 min
Length
665 w
Citations
9
Source
Sundance Formation
Stratigraphic range: Bathonian - Oxfordian
TypeGeological formation
Sub-unitsCanyon Springs Sandstone Member, Hulett Sandstone Member, Lak Member, Pine Butte Member, Redwater Shale Member, Stockade Beaver (Shale) Member, Windy Hill Sandstone Member
UnderliesMorrison Formation
OverliesGypsum Springs Formation
ThicknessUp to 100 m
Lithology
Primaryshale
Otherlimestone, sandstone
Location
RegionWestern North America
CountryUnited States
Type section
Named forSundance, Wyoming
Named byDarton
Year defined1904

The Sundance Formation is a western North American sequence of Middle Jurassic to Upper Jurassic age1 Dating from the Bathonian to the Oxfordian, around 168-157 Ma, It is up to 100 metres thick2 and consists of marine shale, sandy shale, sandstone, and limestone deposited in the Sundance Sea, an inland sea that covered large parts of western North America during the Middle and early Late Jurassic.

Geology

The Sundance Formation underlies the western North American Morrison Formation, the most fertile source of dinosaur fossils in the Americas, and is separated by a disconformity from the underlying Middle Jurassic Gypsum Springs Formation.

Fossils

The Sundance Formation is known for fossils of an extinct species of marine cephalopod, the belemnite Pachyteuthis densus, as well as several extinct species of oyster, including Deltoideum, Liostrea, and Gryphaea nebrascensis. Other common invertebrates include crinoids, echinoids, gastropods, insects, ostracods, and foraminifera.3

Fossil dinosaur 'footprints' on an ancient ocean shoreline are preserved in the formation and protected at the Red Gulch Dinosaur Tracksite, located in the Bureau of Land Management Red Gulch/Alkali National Back Country Byway, near Shell in Big Horn County, Wyoming.4

Two unusual trackways from the formation are not easily identifiable to taxonomic group, though one could have been from an injured pterosaur.5

Paleobiota

Reptiles

Genus Species Member Material Notes

Pteraichnus6

  • P. stokesi
  • Alcova/Grey Reef Reservoir, Seminoe Reservoir and Bighorn Canyon National Recreation area. (Wyoming)6

Trace fossils

Pterosaur tracks

Tatenectes

  • T. laramiensis
  • Redwater Shale Member

A cryptoclidid plesiosaur

Pantosaurus

  • P. striatus
  • Redwater Shale Member

A cryptoclidid plesiosaur

Megalneusaurus

  • M. rex
  • Redwater Shale Member

A thalassophonean pliosaur

Baptanodon

  • B. natans
  • Redwater Shale Member

An ophthalmosaurid ichthyosaur

Plesiosaurus

  • "P." shirleyensis

Material now lost.7

Possibly a junior synonym of Pantosaurus striatus

Fish

Genus Species Member Material Notes

Occithrissops

  • O. willsoni

An ichthyodectiform

Caturus

  • C. dartoni

A caturid amiiform

Hybodontiformes

  • indeterminate
  • Redwater Shale Member

Teeth

Belongs to a group of shark like cartilaginous fish called the Hybodontiformes. This might either be Hybodus or Asteracanthus.8 Found in association with Tatenectes.

Invertebrates

Genus Species Member Material Notes

Pachyteuthis

  • P. densus

A belemnite

References

References

  1. Jennings, Debra S.; Stephen T. Hasiotis (2006). "Taphonomic analysis of a dinosaur feeding site using Geographic Information Systems (GIS), Morrison Formation, Southern Bighorn Basin, Wyoming, USA" (PDF). PALAIOS. 21 (5). SEPM Society for Sedimentary Geology: 480–492. doi:10.2110/palo.2005.P05-062R. S2CID 55369947.
  2. Syzdek, Joseph; Malone, David; Craddock, John (2019-08-01). "Detrital Zircon U-Pb Geochronology and Provenance of the Sundance Formation, Western Powder River Basin, Wyoming". The Mountain Geologist. 56 (3): 295–317. doi:10.31582/rmag.mg.56.3.295. ISSN 0027-254X. S2CID 210290670.
  3. Mcmullen, Sharon K.; Holland, Steven M.; O'keefe, F. Robin (June 2014). "The Occurrence of Vertebrate and Invertebrate Fossils in a Sequence Stratigraphic Context: The Jurassic Sundance Formation, Bighorn Basin, Wyoming, U.S.A.". PALAIOS. 29 (6): 277–294. doi:10.2110/pal.2013.132. ISSN 0883-1351. S2CID 126843460.
  4. BLM−Bureau of Land Management, Wyoming Office: "Red Gulch Dinosaur Tracksite" website, info, maps, photo gallery, accessed 8.21.2015
  5. Harris, Jerald D.; Lacovara, Kenneth J. (2004). "Enigmatic Fossil Footprints from the Sundance Formation (Upper Jurassic) of Bighorn Canyon National Recreation Area, Wyoming". Ichnos. 11 (1–2): 151–166. doi:10.1080/10420940490442304. ISSN 1042-0940.
  6. Lockley, M.; Harris, J.D.; and Mitchell, L. 2008. "A global overview of pterosaur ichnology: tracksite distribution in space and time." Zitteliana. B28. p. 187-198. ISSN 1612-4138.
  7. W. R. O'Keete, F. R. and Wahl Current taxonomic status of the plesiosaur Pantosaurus striatus from the Upper Jurassic Sundance Formation, Wyoming, article on pages 37-47 of the complete issue, 2003, Paludicola, 4 (2) : 27-68. Paperback – January 1, 2003
  8. Massare, Judy A.; Wahl, William R.; Ross, Mike; Connely, Melissa V. (January 2014). "Palaeoecology of the marine reptiles of the Redwater Shale Member of the Sundance Formation (Jurassic) of central Wyoming, USA". Geological Magazine. 151 (1): 167–182. doi:10.1017/S0016756813000472. ISSN 0016-7568 – via Geological Magazine.

44°15′24″N 105°40′57″W / 44.2568°N 105.6824°W / 44.2568; -105.6824