Wahweap Formation
{{Short description|Geologic formation in the United States}}
{{Use mdy dates|date=July 2016}}
{{Infobox rockunit
| name = Wahweap Formation
| image = Wahweap in Shadow (8164183821).jpg
| caption = Wahweap Formation, Grand Staircase–Escalante National Monument, Utah
| type = Geological formation
| age = Campanian, {{fossilrange|82.2|77.3}}
| period = Campanian
| prilithology = sandstone
| otherlithology =
| namedfor = Wahweap Creek
| namedby =
| region = North America
| country = United States
| coordinates = {{coord|37.5|-111.7|display=inline,title}}
| unitof =Kaiparowits Plateau
| subunits =Last Chance Creek Member, Reynolds Point Member, Coyote Point Member, Pardner Canyon Member
| underlies =Kaiparowits Formation
| overlies =Straight Cliffs Formation
| thickness =
| extent = Southern Utah, Northern Arizona
| area =
| map =
| map_caption =
}}
The Wahweap Formation of the Grand Staircase–Escalante National Monument is a geological formation in southern Utah and northern Arizona, around the Lake Powell region, whose strata date back to the Late Cretaceous (Campanian stage). Dinosaur remains are among the fossils that have been recovered from the formation.Weishampel, David B; et al. (2004). "Dinosaur distribution (Late Cretaceous, North America)." In: Weishampel, David B.; Dodson, Peter; and Osmólska, Halszka (eds.): The Dinosauria, 2nd, Berkeley: University of California Press. Pp. 574–588. {{ISBN|0-520-24209-2}}.
Age
The Wahweap formation is divided into four members, which are listed below with their respective ages:{{Cite journal |last1=Beveridge |first1=Tegan L. |last2=Roberts |first2=Eric M. |last3=Ramezani |first3=Jahandar |last4=Titus |first4=Alan L. |last5=Eaton |first5=Jeffrey G. |last6=Irmis |first6=Randall B. |last7=Sertich |first7=Joseph J. W. |date=2022-04-01 |title=Refined geochronology and revised stratigraphic nomenclature of the Upper Cretaceous Wahweap Formation, Utah, U.S.A. and the age of early Campanian vertebrates from southern Laramidia |journal=Palaeogeography, Palaeoclimatology, Palaeoecology |language=en |volume=591 |pages=110876 |doi=10.1016/j.palaeo.2022.110876 |issn=0031-0182|doi-access=free |bibcode=2022PPP...59110876B }}
- Last Chance Creek Member: 82.17-81.55 Ma
- Reynolds Point Member: 81.55-80.61 Ma
- Coyote Point Member: 80.61-79 Ma
- Pardner Canyon Member: 79-77.29 Ma
Paleobiota
=Invertebrates=
The Wahweap Formation shows a substantial amount of invertebrate activity ranging from fossilized insect burrows in petrified logsDe Blieux, Donald D. "Analysis of Jim's hadrosaur site; a dinosaur site in the middle Campanian (Cretaceous) Wahweap Formation of Grand Staircase–Escalante National Monument (GSENM), southern Utah." Abstracts with Programs – Geological Society of America, vol. 39, no. 5, pp.6, May 2007 to various mollusks that characterize the shell beds. Large fossilized crabs are common at most shell bed sites in the Wahweap,Kirkland, James Ian. "An inventory of paleontological resources in the lower Wahweap Formation (lower Campanian), southern Kaiparowits Plateau, Grand Staircase–Escalante National Monument, Utah." Abstracts with Programs – Geological Society of America, vol.37, no.7, pp.114, Oct 2005. and over 1,900 gastropod specimens (of four likely genera) have been unearthed in the formation's siltstone.Williams, Jessica A J; Lohrengel, C Frederick. Preliminary study of freshwater gastropods in the Wahweap Formation, Bryce Canyon National Park, Utah. Abstracts with Programs – Geological Society of America, vol. 39, no. 5, pp.43, May 2007
=Elasmobranchs=
class="wikitable sortable"
|+ ! colspan="7" |Elasmobranchs of the Wahweap Formation |
Taxon
!Species !Locality !Member !Material !Notes !Images |
---|
Cantioscyllium{{Cite book|last1=Kirkland|first1=James I.|title=At the Top of the Grand Staircase: The Late Cretaceous of Southern Utah|last2=Eaton|first2=Jeffrey G.|last3=Brinkman|first3=Donald B.|publisher=Indiana University Press|year=2013|isbn=9780253008961|editor-last=Titus|editor-first=Alan L.|location=Bloomington|pages=153–194|chapter=Elasmobranchs from Upper Cretaceous Freshwater Facies in Southern Utah|editor-last2=Loewen|editor-first2=Mark A.|chapter-url=https://www.academia.edu/5063358}}
|C. estesi |
| |MNA V10230-32, MNA V10384-85, MNA 10390, UMNH VP 18915-16, UMNH VP 18919; teeth |A nurse shark which inhabited freshwater. | rowspan="7" |File:Chiloscyllium griseum.jpg)]]File:Hybodus hauffianus.JPG |
Chiloscyllium
|C. missouriense |
| |MNA V10386, UMNH VP 18880, UMNH VP 18882, UMMNH VP 18886, UMNH VP 18887, UMNH VP 18888; teeth |A bamboo shark which inhabited freshwater. One specimen is similar to Restesia americana. |
Columbusia
|C. deblieuxi |UMNH VP Locality 77 | |UMNH VP 18877, UMNH VP 18879, UMNH VP 18836, UMNH VP 18876, UMNH VP 18878; teeth |A sclerorhynchid ray, closely related to Squatirhina. |
Cristomylus
|C. ciffelli |
| |
|A small guitarfish, suited for handling hard-shelled prey. |
Hybodus?{{Cite journal |last1=Maisch |first1=Michael W. |last2=Matzke |first2=Andreas T. |date=2016-06-01 |title=A new hybodontid shark (Chondrichthyes, Hybodontiformes) from the Lower Jurassic Posidonienschiefer Formation of Dotternhausen, SW Germany |url=http://www.schweizerbart.de/papers/njgpa/detail/280/86202/A_new_hybodontid_shark_Chondrichthyes_Hybodontifor?af=crossref |journal=Neues Jahrbuch für Geologie und Paläontologie - Abhandlungen |language=en |volume=280 |issue=3 |pages=241–257 |doi=10.1127/njgpa/2016/0577 |issn=0077-7749|url-access=subscription }}
|H. sp |MNA Locality 456-2 | |MNA V10387; Tooth |A large hybodont shark reaching over {{Convert|2|m|ft|abbr=on}} in length. Normally a marine species but would enter freshwater environments |
Lonchidion
|L. sp. |UMNH VP Locality 82 | |UMNH VP 18917; Tooth |Smaller than Lonchidon selachos. |
Texatrygon
|T. brycensis |
| |
|A sawfish. |
= Osteichthyes =
= Salamanders =
=Dinosaurs=
Dinosaurs known from the Wahweap include at least 2 species of hadrosaur, at least two ceratopsians{{Cite web |date=2007 |title=New Horned Dinosaurs from the Wahweap Formation |url=http://geology.utah.gov/surveynotes/articles/pdf/horned_dinos_39-3.pdf |archive-url=https://web.archive.org/web/20210831105704/http://files.geology.utah.gov/surveynotes/articles/pdf/horned_dinos_39-3.pdf |archive-date=2021-08-31 |website=Utah Geological Survey}} and at least one theropod.John Wesley Powell Memorial Museum display, visited April 30, 2009
=Mammals=
Image:Saurornitholestes digging Burrows wahweap.jpgan dinosaur digging a primitive mammal out of its burrow, as per the 2010 discovery by Simpson et al. of trace fossils indicating a predator–prey relationship in the Wahweap Formation.{{Cite journal | doi=10.1130/G31019.1| title=Predatory digging behavior by dinosaurs| journal=Geology| volume=38| issue=8| pages=699–702| year=2010| last1=Simpson| first1=Edward L.| last2=Hilbert-Wolf| first2=Hannah L.| last3=Wizevich| first3=Michael C.| last4=Tindall| first4=Sarah E.| last5=Fasinski| first5=Ben R.| last6=Storm| first6=Lauren P.| last7=Needle| first7=Mattathias D.| bibcode=2010Geo....38..699S}}]]
A fair number of mammals spanning the lower Campanian are known from the Wahweap as well, including at least 15 genera of multituberculates, cladotherians, marsupials, and placental insectivores.Eaton, Jeffrey G; Cifelli, Richard L. "Review of Cretaceous mammalian paleontology; Grand Staircase–Escalante National Monument, Utah." Abstracts with Programs – Geological Society of America, vol.37, no.7, pp.115, Oct 2005
Trace fossils
Trace fossils are also relatively abundant in the Wahweap, and include vertebrate tracks as well as burrow activity. Tracks preserved in the capping sandstone indicate the presence of crocodylomorphs, which had been previously known in this area only from teeth elements, as well as ornithischian dinosaurs. At least one possible theropod track has been identified in this area as well.Tester, Edward et al. Isolated vertebrate tracks from the Upper Cretaceous capping sandstone member of the Wahweap Formation; Grand Staircase–Escalante National Monument, Utah Abstracts with Programs – Geological Society of America, vol. 39, no. 5, pp.42, May 2007
In 2010 a unique trace fossil from the Wahweap was discovered that indicates a predator–prey relationship between dinosaurs and primitive mammals. The trace fossil includes at least two fossilized mammalian den complexes as well as associated digging grooves presumably caused by a maniraptoran dinosaur. The proximity indicates a case of probable active predation of the burrow inhabitants by the owners of the claw marks.
See also
{{Portal|Earth sciences|Paleontology|Dinosaurs||}}
References
{{Reflist}}
{{Grand Staircase–Escalante National Monument}}
Category:Geologic formations of Arizona
Category:Geologic formations of Utah
Category:Cretaceous geology of Utah
Category:Grand Staircase–Escalante National Monument
Category:Upper Cretaceous Series of North America