Sundance Formation
{{Short description|Geological formation in Western North America}}
{{Infobox rockunit
| name = Sundance Formation
| image =
| caption =
| type = Geological formation
| period = Callovian
| age = Bathonian - Oxfordian {{fossilrange|168|157}}
| prilithology = shale
| otherlithology = limestone, sandstone
| namedfor =Sundance, Wyoming
| namedby =Darton
| region = Western North America
| country = United States
| coordinates =
| unitof =
| subunits =Canyon Springs Sandstone Member, Hulett Sandstone Member, Lak Member, Pine Butte Member, Redwater Shale Member, Stockade Beaver (Shale) Member, Windy Hill Sandstone Member
| underlies = Morrison Formation
| overlies = Gypsum Springs Formation
| thickness =Up to 100 m
| extent =
| area =
| map =
| map_caption =
|year_ts=1904}}
The Sundance Formation is a western North American sequence of Middle Jurassic to Upper Jurassic age{{cite journal|last = Jennings|first = Debra S.|author2=Stephen T. Hasiotis |title = Taphonomic analysis of a dinosaur feeding site using Geographic Information Systems (GIS), Morrison Formation, Southern Bighorn Basin, Wyoming, USA|journal = PALAIOS |date=2006|volume=21|issue=5|pages=480–492|publisher=SEPM Society for Sedimentary Geology|doi=10.2110/palo.2005.P05-062R| s2cid=55369947 | url=http://doc.rero.ch/record/13869/files/PAL_E796.pdf }} Dating from the Bathonian to the Oxfordian, around 168-157 Ma, It is up to 100 metres thick{{Cite journal|last1=Syzdek|first1=Joseph|last2=Malone|first2=David|last3=Craddock|first3=John|date=2019-08-01|title=Detrital Zircon U-Pb Geochronology and Provenance of the Sundance Formation, Western Powder River Basin, Wyoming|url=http://dx.doi.org/10.31582/rmag.mg.56.3.295|journal=The Mountain Geologist|volume=56|issue=3|pages=295–317|doi=10.31582/rmag.mg.56.3.295|s2cid=210290670 |issn=0027-254X|url-access=subscription}} 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.{{Cite journal |last1=Mcmullen |first1=Sharon K. |last2=Holland |first2=Steven M. |last3=O'keefe |first3=F. Robin |date=June 2014 |title=The Occurrence of Vertebrate and Invertebrate Fossils in a Sequence Stratigraphic Context: The Jurassic Sundance Formation, Bighorn Basin, Wyoming, U.S.A. |url=https://bioone.org/journals/palaios/volume-29/issue-6/pal.2013.132/THE-OCCURRENCE-OF-VERTEBRATE-AND-INVERTEBRATE-FOSSILS-IN-A-SEQUENCE/10.2110/pal.2013.132.full |journal=PALAIOS |volume=29 |issue=6 |pages=277–294 |doi=10.2110/pal.2013.132 |s2cid=126843460 |issn=0883-1351|url-access=subscription }}
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.[http://www.blm.gov/wy/st/en/field_offices/Worland/Tracksite.html BLM−Bureau of Land Management, Wyoming Office: "Red Gulch Dinosaur Tracksite" website], info, maps, photo gallery, accessed 8.21.2015
Paleobiota
= Vertebrates =
class="wikitable" align="center" width="100%" |
Genus
! Species ! Member ! Material ! Notes |
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style="background:#FEF6E4;"|
PteraichnusLockley, 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}}. |style="background:#FEF6E4;"|
|style="background:#FEF6E4;"|
|style="background:#FEF6E4;"| Trace fossils |style="background:#FEF6E4;"| A Pteraichnid belonging to the Pterodactyloidea. |
Tatenectes
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Pantosaurus
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Megalneusaurus
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Baptanodon
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style="background:#E6E6E6;"|
|style="background:#E6E6E6;"|
|style="background:#E6E6E6;"| |style="background:#E6E6E6;"| |style="background:#E6E6E6;"| Possibly a Plesiosaurid Plesiosaur. |
= Invertebrates =
class="wikitable" align="center" width="100%" |
Genus
! Species ! Member ! Material ! Notes |
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Pachyteuthis
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| | | A Belemnoid. |
= Fish =
References
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{{Chronostratigraphy of Colorado|Mesozoic state=expanded}}
Category:Jurassic geology of South Dakota
Category:Jurassic geology of Wyoming
Category:Jurassic System of North America
Category:Upper Jurassic Series
Category:Geology of the Rocky Mountains
Category:Geologic formations of Montana
Category:Geologic formations of Wyoming
Category:Paleontology in Wyoming
{{Wyoming-geologic-formation-stub}}
Category:Middle Jurassic Series
Category:Shale formations of the United States