Onate Formation
{{Use American English|date=December 2020}}
{{Short description|A geologic formation in New Mexico}}
{{Infobox rockunit
| name = Onate Formation
| image =
| caption =
| type = Formation
| age = Givetian
{{fossilrange|387.7|382.7}}
| period = Givetian
| prilithology = Siltstone
| otherlithology = Shale, sandstone
| namedfor = Onate Mountain
| namedby = F.V. Stevenson
| year_ts = 1945
| region = New Mexico
| country = United States
| coordinates = {{coord|32.742|N|106.572|W|display=inline}}
| unitof =
| subunits =
| underlies = Sly Gap Formation
| overlies = Fusselman Formation, Montoya Group
| thickness = {{convert|85-95|feet|meters}}
| extent =
| area =
| map = {{Location map+ | United States#New Mexico
| relief = 1
| width = 250
| float = center
| places =
{{Location map~ | United States#New Mexico
| lat_deg = 32.742
| lon_deg = -106.572
| mark = Brown pog.svg
| marksize = 12
}}
}}
| map_caption =
}}
The Onate Formation is a geologic formation that is exposed in most of the highlands of south-central New Mexico.{{sfn|Kues|2004}} It preserves fossils dating back to the middle Devonian period.{{sfn|Flower|1955}}{{sfn|Cooper|Dutro|1982}}{{sfn|Sorauf|1987}}
Description
At the type section, the Onate Formation consists of about {{convert|85-95|feet|meters}} of orange yellow-weathering dolomitic siltstone with shales and sandstone.{{sfn|Flower|1955}} Elsewhere the thickness is more typically {{cvt|15 to 32|feet}}.{{sfn|Kottlowski|1963}} The base of the formation is a profound regional unconformity, so that the formation rest on either the Fusselman Formation or the Montoya Group. It is overlain by the Sly Gap Formation and thins to the north and south.{{sfn|Cooper|Dutro|1982}}
The formation is interpreted as having been deposited on a shallow shelf environment deepening to a euxenic basin to the south.{{sfn|Kues|2004|p=62}}
Fossils
The formation contains the fossil brachiopod Spirifer acuminatu, as well as crinoids and bryozoans.{{sfn|Flower|1955}} The brachiopod assemblage includes 34 genera and 41 species. Conodonts are rare but a few tabulate corals, ichnofossils, and the receptaculid Sphaerospongia is present. The receptaculids provided a solid substrate for colonization by the rugose coral Tabulophyllum traversensis.{{sfn|Sorauf|1987}} The fossil assemblage gives an age of late Givetian. The formation is highly bioturbated.{{sfn|Cooper|Dutro|1982}}
History of investigation
The beds assigned to the formation were previously correlated with the Canutillo Formation of west Texas. However, F.V. Stevenson questioned the correlation, and designated a new Onate Formation including the beds in 1945.{{sfn|Stevenson|1945}} In 1985, G.A. Cooper and J.T. Dutro, Jr., conducted the first thorough study of the fossil assemblage of the formation.{{sfn|Cooper|Dutro|1982}} The fossils were further characterized by James E. Souraf in 1987.{{sfn|Sorauf|1987}}
See also
{{Portal|Earth sciences|Paleontology}}
Footnotes
{{Reflist}}
References
- {{cite journal |last1=Cooper |first1=G.A. |last2=Dutro |first2=J.T. Jr. |year=1982 |title=Devonian brachiopods of New Mexico |journal=Bulletins of American Paleontology |volume=82-83 |number=325}}
- {{Cite journal|last=Flower|first=Rousseau|date=1955|title=Pre-Pennsylvanian stratigraphy of southern New Mexico|url=https://nmgs.nmt.edu/publications/guidebooks/downloads/6/6_p0065_p0070.pdf|journal=New Mexico Geological Society Field Conference Series |volume=6|pages=65–70}}
- {{cite journal |last1=Stevenson |first1=Frank V. |title=Devonian of New Mexico |journal=The Journal of Geology |date=July 1945 |volume=53 |issue=4 |pages=217–245 |doi=10.1086/625283}}
- {{cite journal |last1=Kottlowski |first1=Frank E. |title=Paleozoic and Mesozoic Strata of Southwestern and South-Central New Mexico |journal=New Mexico Bureau of Mines and Mineral Resources Bulletin |date=1963 |volume=79 |url=https://geoinfo.nmt.edu/publications/monographs/bulletins/downloads/79/B79.pdf |access-date=13 December 2020}}
- {{cite encyclopedia |last1=Kues |first1=B.S. |year=2004 |title=Devonian of New Mexico |editor1-last=Mack |editor1-first=G.H. |editor2-last=Giles |editor2-first=K.A. |encyclopedia=The geology of New Mexico. A geologic history: New Mexico Geological Society Special Volume 11 |pages=59–75 |isbn=9781585460106}}
- {{Cite journal|last1=Sorauf|first1=James E.|title=The rugose coral Tabulophyllum traversensis from the Oñate Formation (Middle Devonian) of the Mud Springs Mountains, New Mexico|url=https://www.cambridge.org/core/journals/journal-of-paleontology/article/abs/rugose-coral-tabulophyllum-traversensis-from-the-onate-formation-middle-devonian-of-the-mud-springs-mountains-new-mexico/7CB2688F2EDB0F4126E2DF687722FCA7|journal=Journal of Paleontology|language=en|volume=61|issue=1|pages=14–20|doi=10.1017/S0022336000028158|issn=0022-3360|year=1987|jstor=1305128|url-access=subscription}}
{{Use dmy dates|date=April 2017}}
Category:Devonian formations of New Mexico
Category:Devonian southern paleotemperate deposits
Category:Siltstone formations of the United States