Almond Formation
{{Short description|Geological formation in Wyoming, U.S.}}
{{Infobox rockunit
| name = Almond Formation
| image =
| caption =
| type = Geological formation
| age = Campanian–Maastrichtian
{{Fossil range|73.6|71.1}}
| period = Maastrichtian
| prilithology = Sandstone
| otherlithology = Siltstone, shale, coalb
| namedfor =
| namedby =
| region = Wyoming
| country = United States
| coordinates = {{WikidataCoord|display=inline,title}}
| unitof =
| subunits =
| underlies = Lewis Shale
| overlies = Ericson Formation
| thickness =
| extent =
| area =
| map = Southwestern Wyoming Upper Cretaceous Unit cross section.jpg
| map_caption = Southwestern Wyoming, incl. Almond formation
}}
The Almond Formation is a geological formation of Late Cretaceous (Late Campanian-Early Maastrichtian{{Cite journal|last=Fowler|first=Denver Warwick|date=2017-11-22|title=Revised geochronology, correlation, and dinosaur stratigraphic ranges of the Santonian-Maastrichtian (Late Cretaceous) formations of the Western Interior of North America|journal=PLOS ONE|volume=12|issue=11|pages=e0188426|doi=10.1371/journal.pone.0188426|issn=1932-6203|pmc=5699823|pmid=29166406|bibcode=2017PLoSO..1288426F|doi-access=free}}) age in Wyoming. It was deposited in marsh, deltaic, lagoonal, estuarine, and shallow marine environments along the western shore of the Western Interior Seaway. It consists primarily of fine- to medium-grained sandstone, siltstone, shale, and coal.Kieft, R.L., Hampton, G.J., Jackson, C.A.-L., and Larsen, E., 2011. Stratigraphic architecture of a net-transgressive marginal- to shallow-marine succession: Upper Almond Formation, Rock Springs Uplift, Wyoming, U.S.A. Journal of Sedimentary Research, vol. 81, p. 513-533. Fossils from the Almond Formation include remains of dinosaursWeishampel, 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}}. and plants.Stockey, R.A., Rothwell, G.W., and Johnson, K.R., 2007. Cobbania corrugata gen. et. comb. nov. (Araceae): A floating aquatic monocot from the Upper Cretaceous of western North America. American Journal of Botany, vol. 94, no. 4, p. 609-624.
Vertebrate paleofauna
=Dinosaurs=
{{paleobiota-key-compact}}
= Other vertebrates =
Non-dinosaur vertebrates found in the Almond Formation include crocodyliforms (indet.), turtles (Adocus cf. and Basilemys cf.), and ray-finned fish (Ichthyodectidae indet.).{{Cite journal |last=Cowgill |first=Ethan |last2=Ashurst-mcgee |first2=Logan |last3=Storrs |first3=Glenn |last4=Johnson |first4=Christopher L. |last5=Affolter |first5=Matthew D. |last6=Law |first6=Lane |last7=Hawkins |first7=Quinlan |last8=Tamez-Galvan |first8=Evan |last9=Kosowatz |first9=Luke |date=2021 |title=A PRELIMINARY REPORT ON NEW VERTEBRATE FOSSILS FROM THE LATE CRETACEOUS ALMOND FORMATION, WYOMING |url=https://gsa.confex.com/gsa/2021AM/webprogram/Paper371282.html |journal=Geological Society of America Abstracts with Programs |volume=53 |issue=6 |doi=10.1130/abs/2021AM-371282}}
See also
{{Portal|Earth sciences|Paleontology|Dinosaurs||}}
Footnotes
{{Reflist}}
References
- Weishampel, David B.; Dodson, Peter; and Osmólska, Halszka (eds.): The Dinosauria, 2nd, Berkeley: University of California Press. 861 pp. {{ISBN|0-520-24209-2}}.
{{Authority control}}