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		<summary type="html">&lt;p&gt;&lt;a href=&quot;https://en.wikipedia.org/wiki/OABOT&quot; class=&quot;extiw&quot; title=&quot;wikipedia:OABOT&quot;&gt;Open access bot&lt;/a&gt;: url-access updated in citation with #oabot.&lt;/p&gt;
&lt;p&gt;&lt;b&gt;New page&lt;/b&gt;&lt;/p&gt;&lt;div&gt;{{Short description|North American faunal stage}}&lt;br /&gt;
The &amp;#039;&amp;#039;&amp;#039;Chadronian&amp;#039;&amp;#039;&amp;#039; is a [[North American land mammal age|North American Land Mammal Age]] typically set from around 37,000,000 to 33,700,000 years [[Before Present|BP]], a period of  {{Mya|37-33.7|million years}}.&amp;lt;ref name=&amp;quot;:0&amp;quot;&amp;gt;{{Cite book |last=Prothero |first=Donald R. |url=https://www.degruyter.com/document/doi/10.7312/wood13040/html |title=Late Cretaceous and Cenozoic Mammals of North America: Biostratigraphy and Geochronology |last2=Emry |first2=Robert J. |date= |publisher=Columbia University Press |year=2004 |isbn=978-0-231-13040-0 |editor-last=Woodburne |editor-first=Michael O. |pages=156–168 |chapter=5. The Chadronian, Orellan, and Whitneyan North American Land Mammal Ages |doi=10.7312/wood13040-007 |chapter-url=https://www.degruyter.com/document/doi/10.7312/wood13040-007/html}}&amp;lt;/ref&amp;gt; The Chadronian is preceded by the [[Duchesnean]] and followed by the [[Orellan]] NALMA stages. Relative to global geological [[chronology]] (the [[geologic time scale]]), it is usually considered to fall within the later part ([[Priabonian]] stage) of the [[Eocene]] epoch, ending around the same time as the Eocene-[[Oligocene]] boundary.&lt;br /&gt;
&lt;br /&gt;
The Chadronian is named after the [[Chadron Formation]], a widespread component of the [[White River Group]] in [[Nebraska]] and [[South Dakota]]. The most well-studied examples of Chadronian strata in the White River Group/Formation are the Flagstaff Rim area of eastern [[Wyoming]] and the Toadstool Park area of northwest Nebraska.&amp;lt;ref name=&amp;quot;:0&amp;quot; /&amp;gt;&lt;br /&gt;
&lt;br /&gt;
The beginning of the Chadronian is defined by the first appearance of &amp;#039;&amp;#039;[[Bathygenys]]&amp;#039;&amp;#039; (a [[Merycoidodontidae|merycoidodontid]], or &amp;quot;[[oreodont]]&amp;quot;). Other mammals which first appear at the start of the stage include &amp;#039;&amp;#039;[[Merycoidodon|Merycoidodon dunagani]]&amp;#039;&amp;#039; (a merycoidodontid), &amp;#039;&amp;#039;[[Brachyrhynchocyon|Brachyrhynchocyon dodgei]]&amp;#039;&amp;#039;, (a [[Daphoeninae|daphoenine]] [[Amphicyonidae|amphicyonid]], or &amp;quot;bear dog&amp;quot;), and &amp;#039;&amp;#039;[[Archaeotherium]]&amp;#039;&amp;#039; (an [[Entelodontidae|entelodont]]). The early horse &amp;#039;&amp;#039;[[Mesohippus]]&amp;#039;&amp;#039; appears only slightly before the start of the Chadronian.&amp;lt;ref name=&amp;quot;:0&amp;quot; /&amp;gt;&lt;br /&gt;
&lt;br /&gt;
== Subdivisions ==&lt;br /&gt;
Four subdivisions of the Chadronian were informally proposed by Prothero and Emry (1996), later formalized by the same authors in 2004.&amp;lt;ref name=&amp;quot;:0&amp;quot; /&amp;gt; Type assemblages (diagnostic fossil faunas used to define the subdivision) are bolded and underlined. From youngest to oldest:&lt;br /&gt;
{| class=&amp;quot;wikitable&amp;quot;&lt;br /&gt;
|- style=&amp;quot;text-align:center; background:gainsboro;&amp;quot;&lt;br /&gt;
|&amp;#039;&amp;#039;&amp;#039;Subdivision&amp;#039;&amp;#039;&amp;#039;&lt;br /&gt;
|&amp;#039;&amp;#039;&amp;#039;Primary index fossil&amp;#039;&amp;#039;&amp;#039;&lt;br /&gt;
|&amp;#039;&amp;#039;&amp;#039;Estimated age&amp;#039;&amp;#039;&amp;#039;&lt;br /&gt;
|&amp;#039;&amp;#039;&amp;#039;Component assemblages&amp;#039;&amp;#039;&amp;#039;&lt;br /&gt;
|-&lt;br /&gt;
|Late Chadronian&lt;br /&gt;
|&amp;#039;&amp;#039;[[Miniochoerus|Miniochoerus chadronensis]]&amp;#039;&amp;#039;&lt;br /&gt;
|33.7 - 34.7 Ma&lt;br /&gt;
|&lt;br /&gt;
* &amp;lt;u&amp;gt;&amp;#039;&amp;#039;&amp;#039;upper Flagstaff Rim, White River Formation&amp;#039;&amp;#039;&amp;#039;&amp;lt;/u&amp;gt; (around ash J) (Wyoming)&lt;br /&gt;
* Upper Chadron Formation (Nebraska)&lt;br /&gt;
* Peanut Peak Member, Chadron Formation (South Dakota)&lt;br /&gt;
* [[Florissant Formation]] (Colorado)&lt;br /&gt;
* Ash Springs local fauna, [[Vieja Group]] (Texas)&lt;br /&gt;
|-&lt;br /&gt;
|Middle Chadronian&lt;br /&gt;
|&amp;#039;&amp;#039;[[Leptomeryx|Leptomeryx mammifer]]&amp;#039;&amp;#039;&lt;br /&gt;
|34.7 - 35.7 Ma&lt;br /&gt;
|&lt;br /&gt;
* &amp;lt;u&amp;gt;&amp;#039;&amp;#039;&amp;#039;middle Flagstaff Rim, White River Formation&amp;#039;&amp;#039;&amp;#039;&amp;lt;/u&amp;gt; (around ashes B-G) (Wyoming)&lt;br /&gt;
* Pipestone Springs and Little Pipestone Creek local faunas, [[Renova Formation]] (Montana)&lt;br /&gt;
* Raben Ranch local fauna, Chadron Formation (Nebraska)&lt;br /&gt;
* Crazy Johnson Member, Chadron Formation (South Dakota)&lt;br /&gt;
|-&lt;br /&gt;
|Late Early Chadronian&lt;br /&gt;
|&amp;#039;&amp;#039;[[Leptomeryx|Leptomeryx yoderi]]&amp;#039;&amp;#039;&lt;br /&gt;
|35.7 - 36.5 Ma&lt;br /&gt;
|&lt;br /&gt;
* &amp;lt;u&amp;gt;&amp;#039;&amp;#039;&amp;#039;lower Flagstaff Rim, White River Formation&amp;#039;&amp;#039;&amp;#039;&amp;lt;/u&amp;gt; (around ash A) (Wyoming)&lt;br /&gt;
* Yoder local fauna, White River Formation (Wyoming)&lt;br /&gt;
* Pipestone Springs local fauna, Renova Formation (Montana)&amp;lt;ref name=&amp;quot;:1&amp;quot;&amp;gt;{{Cite journal |last=Hanneman |first=Debra |last2=Lofgren |first2=Don |last3=Hasiotis |first3=Stephen |last4=McIntosh |first4=William |date=2022 |title=Late Eocene (Priabonian) chronostratigraphy, depositional environment, and paleosol-trace fossil associations, Pipestone Springs, southwest Montana |url=http://dx.doi.org/10.4202/app.00901.2021 |journal=Acta Palaeontologica Polonica |volume=67 |pages=5-20 |doi=10.4202/app.00901.2021 |issn=0567-7920|doi-access=free }}&amp;lt;/ref&amp;gt;&lt;br /&gt;
* McCarty&amp;#039;s Mountain local fauna (Montana)&lt;br /&gt;
* Ahearn Member, Chadron Formation (South Dakota)&lt;br /&gt;
* Medicine Pole Hills local fauna (North Dakota)&lt;br /&gt;
* Airstrip local fauna, [[Capote Mountain Tuff]] (Texas)&lt;br /&gt;
|-&lt;br /&gt;
|Earliest Chadronian&lt;br /&gt;
|&amp;#039;&amp;#039;[[Bathygenys]]&amp;#039;&amp;#039;&lt;br /&gt;
|36.5 - 37 Ma&lt;br /&gt;
|&lt;br /&gt;
* &amp;#039;&amp;#039;&amp;#039;&amp;lt;u&amp;gt;Little Egypt local fauna, upper [[Chambers Tuff]] (Texas)&amp;lt;/u&amp;gt;&amp;#039;&amp;#039;&amp;#039;&lt;br /&gt;
* Rancho Gaitan local fauna, [[Preitos Formation]] ([[Chihuahua (state)|Chihuahua]], Mexico)&lt;br /&gt;
* lowermost Flagstaff Rim, White River Formation? (Wyoming)&lt;br /&gt;
* Pipestone Springs local fauna, Renova Formation (Montana)&amp;lt;ref name=&amp;quot;:1&amp;quot; /&amp;gt;&lt;br /&gt;
* Diamond O Ranch local fauna, Renova Formation? (Montana)&amp;lt;ref&amp;gt;{{Cite journal |last=Fostowicz-Frelik |first=Łucja |last2=Tabrum |first2=Alan R. |date=2009 |title=Leporids (Mammalia, Lagomorpha) from the Diamond O Ranch Local Fauna, Latest Middle Eocene of Southwestern Montana |url=https://www.researchgate.net/publication/269036748 |journal=Annals of Carnegie Museum |language=en |volume=78 |issue=3 |pages=253–271 |doi=10.2992/007.078.0303 |issn=0097-4463}}&amp;lt;/ref&amp;gt;&lt;br /&gt;
|}&lt;br /&gt;
Part of the [[Cypress Hills Formation]] (Saskatchewan, Canada) is also considered to be Chadronian in age.&amp;lt;ref name=&amp;quot;:0&amp;quot; /&amp;gt; In Colorado, Chadronian mammal faunas are found in the Florissant Formation, the [[Antero Formation]],&amp;lt;ref&amp;gt;{{Cite journal |last=Sweedler |first=Rory E. |last2=Eberle |first2=Jaelyn J. |last3=Mihlbachler |first3=Matthew C. |date=2021-06-01 |title=A latest Eocene (Chadronian) brontothere (Mammalia, Perissodactyla) from the Antero Formation, South Park, Colorado |url=https://pubs.geoscienceworld.org/uwyo/rmg/article/56/1/37/599894/A-latest-Eocene-Chadronian-brontothere-Mammalia |journal=Rocky Mountain Geology |language=en |volume=56 |issue=1 |pages=37–50 |doi=10.24872/rmgjournal.56.1.37 |issn=1555-7340|url-access=subscription }}&amp;lt;/ref&amp;gt; and the White River Formation in the Kings Canyon area.&amp;lt;ref&amp;gt;{{Cite journal |last=Lloyd |first=K. J. |last2=Eberle |first2=J. J. |date=2012-09-01 |title=A late Eocene (Chadronian) mammalian fauna from the White River Formation in Kings Canyon, northern Colorado |url=http://rmg.geoscienceworld.org/cgi/doi/10.2113/gsrocky.47.2.113 |journal=Rocky Mountain Geology |language=en |volume=47 |issue=2 |pages=113–132 |doi=10.2113/gsrocky.47.2.113 |issn=1555-7332|url-access=subscription }}&amp;lt;/ref&amp;gt; In New Mexico, the [[Conejos Formation|Conejos]], [[Espinaso Formation|Espinaso]], [[Spears Group|Spears]], [[Sanders Canyon Formation|Sanders Canyon]], [[Bell Top Formation|Bell Top]], upper [[Rubio Peak Formation|Rubio Peak]], and upper [[Palm Park Formation|Palm Park]] formations all overlap with the Chadronian NALMA.&amp;lt;ref&amp;gt;Lucas, Spencer G. (2015). &amp;quot;[https://www.google.com/books/edition/Vertebrate_Paleontology_in_New_Mexico/S--oDQAAQBAJ?hl=en&amp;amp;gbpv=1&amp;amp;pg=PA149&amp;amp;printsec=frontcover Eocene fossil vertebrates of New Mexico]&amp;quot;. &amp;#039;&amp;#039;New Mexico Museum of Natural History and Science Bulletin&amp;#039;&amp;#039;. Vol. 68. pp. 149–157.&amp;lt;/ref&amp;gt; The Iniyoo local fauna ([[Oaxaca]], Mexico) was initially reported to be Chadronian,&amp;lt;ref&amp;gt;{{Cite journal |last=Jiménez-Hidalgo |first=Eduardo |last2=Smith |first2=Krister T. |last3=Guerrero-Arenas |first3=Rosalia |last4=Alvarado-Ortega |first4=Jesus |date=2015 |title=The first Late Eocene continental faunal assemblage from tropical North America |url=https://linkinghub.elsevier.com/retrieve/pii/S0895981114001667 |journal=Journal of South American Earth Sciences |language=en |volume=57 |pages=39–48 |doi=10.1016/j.jsames.2014.12.001|url-access=subscription }}&amp;lt;/ref&amp;gt; though revised dating suggests that it is [[Arikareean]] (late Oligocene) instead.&amp;lt;ref&amp;gt;{{Cite journal |last=Jiménez-Hidalgo |first=Eduardo |last2=Lander |first2=E. Bruce |last3=Israde-Alcántara |first3=Isabel |last4=Rodríguez-Caballero |first4=Nadia Wendoline |last5=Guerrero-Arenas |first5=Rosalía |date=2021 |title=Earliest Arikareean (later early Oligocene) Iniyoo local Fauna from Chilapa Formation of Santiago Yolomécatl area in northwestern Oaxaca, southern Mexico |url=https://www.researchgate.net/publication/350530655 |journal=Journal of South American Earth Sciences |language=en |volume=109 |pages=103307 |doi=10.1016/j.jsames.2021.103307}}&amp;lt;/ref&amp;gt;&lt;br /&gt;
&lt;br /&gt;
==References==&lt;br /&gt;
{{reflist}}&lt;br /&gt;
&lt;br /&gt;
{{Paleogene Footer}}&lt;br /&gt;
&lt;br /&gt;
[[Category:Chadronian| ]]&lt;br /&gt;
[[Category:Eocene life]]&lt;br /&gt;
[[Category:Eocene animals of North America]]&lt;br /&gt;
&lt;br /&gt;
{{geochronology-stub}}&lt;/div&gt;</summary>
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