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{{Short description|Extinct genus of dinosaurs}}
{{italictitle}}{{speciesbox
| name = ''Ceratops''
| fossil_range = [[Late Cretaceous]], {{fossilrange|7577.5}}
| image = Ceratops.jpgpng
| image_caption = IllustrationHolotype ofleft the type specimen by Marshhorncore
| grandparent_authority = Marsh, 1888 [[Othnielsensu]] Charles[[Othenio MarshAbel|MarshAbel]], 18881919
| genus = Ceratops
| display_parents = 2
| parent_authority = Marsh, 1888
| species = montanus
| authority = Marsh, 1888
| synonyms = * ''Proceratops montanus'' <br><small>(Marsh, 1888) [[R. S. Lull|Lull]], 1906</small>
| synonyms =
* '''''ProceratopsTriceratops montanus''''' <br><small>(Marsh, 1888) [[R.Ostrom S.& Lull|Lull]]Wellnhofer, 19061986</small>
}}
 
'''''Ceratops''''' (meaning "horn face") is a [[nomen dubium|dubious]] [[genus]] of herbivorous [[ceratopsia]]n [[dinosaur]] which lived during the [[Late Cretaceous]]. Its fossils have been found in the [[Judith River Formation]] in [[Montana]]. Although poorly known, ''Ceratops'' is important in the history of dinosaurs, since it is the [[type speciesgenus]] for which both the [[Ceratopsia]] and the [[Ceratopsidae]] arehave been named. Unfortunately, the material is too poor to be confidently referred to better specimens, and ''Ceratops'' is considered a ''[[nomen dubium]]''.
 
==History==
[[File:Ceratops montanus.jpg|upright|thumb|left|Illustration of the horntype coresspecimen fromby 1907Marsh]]
The first remains referred to ''Ceratops'' — an [[occipital condyle#In dinosaurs|occipital condyle]] and a pair of [[Horn (anatomy)|horn cores]] — were found by [[John Bell Hatcher]] (1861–1904) in the late summer of 1888 near the [[Cow Creek (Montana)|Cow Creek]] in [[Blaine County, Montana|Blaine County]] in the uppermost [[Judith River Formation]] of Montana. Hatcher was at the time employed by Professor [[Othniel Charles Marsh]] who the same year named the find as the [[type species]] ''Ceratops montanus''. The generic name was derived from Greek κέρας, ''keras'', "horn", and ὤψ, ''ops'', "face". The [[specific name (zoology)|specific name]] referred to Montana. Marsh originally believed the animal to be similar to ''[[Stegosaurus]]'', but with two horns on the back of its head, a body length of twenty-five to thirty feet, horizontal plates on its back and bipedal. According to Marsh it would have "represented a very strange appearance".<ref name="Marsh1888">{{cite journal | last1 = Marsh | first1 = O.C. | year = 1888 | title = A new family of horned Dinosauria, from the Cretaceous | url = https://ajsonline.org/article/62691.pdf| journal = The American Journal of Science |series=Series 3 | volume = 36 | issue = 216| pages = 477–478 | doi = 10.2475/ajs.s3-36.216.477 | bibcode = 1888AmJS...36..477M | s2cid = 130243398 }}</ref> In his illustration of the horn pair, purportedly showing them from behind, Marsh had switched their position and rotated their outside to the rear to make them point inwards.<ref name="Lull1907">J.B. Hatcher, O.C. Marsh, and R.S. Lull'', 1907 The Ceratopsia''. Monographs of the United States Geological Survey 49 pp 198</ref>
The first remains referred to ''Ceratops'' (an [[occipital]] [[Condyle (anatomy)|condyle]] and a pair of [[horn cores]]) were found by [[John Bell Hatcher]] (1861–1904) in the summer of 1888 in the uppermost [[Judith River Formation]] of Montana. [[O. C. Marsh]] originally believed the animal to be similar to ''[[Stegosaurus]]'', but with two horns on its head.
 
The holotype, '''USNM 2411''', was found in a layer dating from the [[Campanian]]. It consists, apart from the occipital condyle, of two supraorbital horn cores of about twenty-two centimetres length.<ref name="Lull1907"/> The right horn is attached to a part of the prefrontal. Marsh later referred two [[squamosal]]s to the species, specimens USNM 4802 and USNM 2415. These however are more likely [[Centrosaurinae|centrosaurine]]; they have also been referred to ''[[Avaceratops]]''.<ref>Penkalski, P.G., 1993, "The morphology of ''Avaceratops lammersi'', a primitive ceratopsid from the Campanian of Montana", ''Journal of Vertebrate Paleontology'' '''13'''(3, supplement): 52A</ref>
In 1995, Trexler and Sweeney noted that complete material from a bonebed that had been found in [[Montana]] could enable ''Ceratops'' to be reexamined. The site, known as the Mansfield Bonebed, belongs to the same stratigraphic level as the one the yielded the original ''Ceratops'' remains. It had initially been interpreted as containing ''[[Styracosaurus]]'', but what earlier authors considered the frill spikes of ''Styracosaurus'' turned out to be chasmosaurine orbital horns. Trexler and Sweeney pointed out that these horns closely resembled those of ''Ceratops'', and could allow the genus to be rescued as a valid name.<ref name=trexler>Trexler, D. and Sweeney, F.G. (1995). "Preliminary work on a recently discovered ceratopsian (Dinosauria: Ceratopsidae) bonebed from the Judith River Formation of Montana suggests the remains are of ''Ceratops montanus'' Marsh." ''Journal of Vertebrate Paleontology'', '''15'''(3, Suppl.): 57A.</ref> The ceratopsids in the bonebed were later referred to the genus ''[[Albertaceratops]]'', and later re-classified in their own genus, ''[[Medusaceratops]]''.<ref name="Ryan2010">Ryan, Michael J.; Russell, Anthony P., and Hartman, Scott. (2010). "A New Chasmosaurine Ceratopsid from the Judith River Formation, Montana", In: Michael J. Ryan, Brenda J. Chinnery-Allgeier, and David A. Eberth (eds), ''New Perspectives on Horned Dinosaurs: The Royal Tyrrell Museum Ceratopsian Symposium'', Indiana University Press, 656 pp. ISBN 0253353580.</ref>
 
In 1906 [[Richard Swann Lull]] noted that the name ''Ceratops'' had been preoccupied by a bird, ''Ceratops'' Rafinesque 1815, but also that this had been an undescribed ''[[nomen nudum]]'', causing the name to have been still available in 1888. He nevertheless provisionally proposed a replacement name: ''Proceratops''.<ref>{{cite journal | last1 = Lull | first1 = R.S. | year = 1906 | title = A new name for the dinosaurian genus ''Ceratops'' | url =https://zenodo.org/record/1450144 | journal = The American Journal of Science |series=Series 4 | volume = 21 | issue = 122| page = 144 | doi = 10.2475/ajs.s4-21.122.144 | bibcode = 1906AmJS...21..144L }}</ref> This is thus a [[junior synonym]] of ''Ceratops''.
In 2005, remarkably well preserved cranial and post cranial elements of a [[Judith River Formation| Judithian]] ceratopsian were discovered in [[Fergus County, Montana]]. Examination suggests close affinity with ''C. montanus''. The locality has been determined to be on or in close proximity to the stratigraphic layer of ''C. montanus'', and not too many miles away. The fossils have since been meticulously prepared, studied and evaluated. A team of writers is currently (Q1, 2011) in the process of preparing for publication. This specimen may or may not be referred to ''C. montanus''; debate on the merits of referring to a ''nomen dubium'' versus a new species designation continue.{{cn|date=February 2011}}
 
Already in the early twentieth century new finds made it increasingly difficult to distinguish the limited remains of ''Ceratops'' from several other related forms. Today, ''Ceratops'' is considered a ''nomen dubium''.<ref>P. Dodson and P. J. Currie, 1990, "Neoceratopsia". In: D.B. Weishampel, H. Osmolska, and P. Dodson (eds.), ''The Dinosauria''. First Edition. University of California Press, Berkeley pp 593-618</ref> However, from time to time claims are made about discoveries that, also taking into regard their provenance, might have a provable connection with the ''Ceratops'' holotype.
==Classification==
''Ceratops'' belonged to the Ceratopsia (the name is [[Ancient Greek]] for "horned face"), a group of herbivorous dinosaurs with [[parrot]]-like beaks which thrived in [[North America]] and [[Asia]] during the [[Cretaceous Period]], which ended roughly 65 million years ago.
 
In 1995, [[David Trexler]] and F.G. Sweeney noted that complete material from a bonebed that had been found in [[Montana]] could enable ''Ceratops'' to be reexamined. The site, known as the Mansfield Bonebed, belongs to the same stratigraphic level as the one thethat yielded the original ''Ceratops'' remains. It had initially been interpreted as containing ''[[Styracosaurus]]'', but what earlier authors considered the frill spikes of ''Styracosaurus'' turned out to be chasmosaurine orbital horns. Trexler and Sweeney pointed out that these horns closely resembled those of ''Ceratops'', and could allow the genus to be rescued as a valid name.<ref name=trexler>Trexler, D. and Sweeney, F.G. (1995). "Preliminary work on a recently discovered ceratopsian (Dinosauria: Ceratopsidae) bonebed from the Judith River Formation of Montana suggests the remains are of ''Ceratops montanus'' Marsh." ''Journal of Vertebrate Paleontology'', '''15'''(3, Suppl.): 57A.</ref> The ceratopsids in the bonebed were later referred to the genus ''[[Albertaceratops]]'', and later re-classified in their own genus, ''[[Medusaceratops]]''.<ref name="Ryan2010">Ryan, Michael J.; Russell, Anthony P., and Hartman, Scott. (2010). "A New Chasmosaurine Ceratopsid from the Judith River Formation, Montana", In: Michael J. Ryan, Brenda J. Chinnery-Allgeier, and David A. Eberth (eds), ''New Perspectives on Horned Dinosaurs: The Royal Tyrrell Museum Ceratopsian Symposium'', Indiana University Press, 656 pp. {{ISBN 0253353580|0-253-35358-0}}.</ref>
In 1999, Penkalski and Dodson concluded ''Ceratops'' is a [[nomen dubium]] because the material is too meager. They add that ''[[Avaceratops]]'' appears closely related and may even be a juvenile ''Ceratops'' but there is not enough material to prove it.<ref name=avaceratops>{{cite journal|doi=10.1080/02724634.1999.10011182|author=Penkalski, P & Dodson, P|year=1999|title=The morphology and systematics of ''Avaceratops'', a primitive horned dinosaur from the Judith River Formation (Late Campanian) of Montana, with the description of a second skull.|journal=Journal of Vertebrate Paleontology|volume=19|issue=4|pages=692&ndash;711}}</ref>
 
In 1999, [[Paul Penkalski]] and [[Peter Dodson]] concluded that ''Ceratops'', isdespite being a ''[[nomen dubium]]'' because the material is too meager., Theyappeared addclosely thatrelated to ''[[Avaceratops]]'' appears closely related andwhich may even be a juvenile ''Ceratops'' but; there is not enough material to prove it.<ref name=avaceratops>{{cite journal|doi=10.1080/02724634.1999.10011182|authorauthor1=Penkalski, P & |author2=Dodson, P|year=1999|title=The morphology and systematics of ''Avaceratops'', a primitive horned dinosaur from the Judith River Formation (Late Campanian) of Montana, with the description of a second skull.|journal=Journal of Vertebrate Paleontology|volume=19|issue=4|pages=692&ndash;711|bibcode=1999JVPal..19..692P }}</ref>
==Species==
Type:
*''Ceratops montanus'' Marsh 1888 (USNM 2411)
 
===Later species===
Others:
In 1889 Marsh named a second species of ''Ceratops'': ''Ceratops horridus''.<ref>{{cite journal | last1 = Marsh | first1 = O.C. | year = 1889 | title = Notice of new American Dinosauria | url = https://zenodo.org/record/2123893| journal = American Journal of Science | volume = 37 | issue = 220| pages = 331–336 | doi = 10.2475/ajs.s3-37.220.331 | bibcode = 1889AmJS...37..331M | s2cid = 131729220 }}</ref> This would almost immediately in a subsequent article be renamed into ''[[Triceratops]] horridus''. ''Ceratops horridus'' is thus the type species of ''Triceratops''. In the same article Marsh renamed ''Bison alticornis'', his misidentification of ceratopsid material for a giant [[Bovidae|bovid]], into ''Ceratops alticornis''.<ref>{{cite journal | last1 = Marsh | first1 = O.C. | year = 1889 | title = Notice of gigantic horned Dinosauria from the Cretaceous | url = https://zenodo.org/record/2140870| journal = American Journal of Science | volume = 38 | issue = 224| pages = 173–175 | doi = 10.2475/ajs.s3-38.224.173 | bibcode = 1889AmJS...38..173M | s2cid = 131187857 }}</ref> In 1890 Marsh renamed ''Hadrosaurus paucidens'' into ''Ceratops paucidens'';<ref>{{cite journal | last1 = Marsh | first1 = O.C. | year = 1890 | title = Description of new dinosaurian reptiles | url = https://zenodo.org/record/1964666| journal = The American Journal of Science |series=Series 3 | volume = 39 | issue = 229| pages = 81–86 | doi = 10.2475/ajs.s3-39.229.81 | bibcode = 1890AmJS...39...81M | s2cid = 131403178 }}</ref> but the original assessment of Hatcher that this represented [[Hadrosauridae|hadrosaurid]] material is probably correct.<ref name="Lull1907"/>
*''C. (Bison) alticornis'' (Marsh 1887/1889). This was the famous pair of horn cores that were originally thought by Marsh to be from a giant [[bison]]. Marsh realized his error in 1889 and referred the horns to his ''Ceratops''. Today they are recognized as the first ''[[Triceratops]]'' remains found and are, to date, the southernmost known ''Triceratops'' fossils. Even as ''Triceratops'', it also is a ''[[nomen dubium]]''.
 
*''C.'' ''([[Chasmosaurus]]) belli'' (Lambe 1902/Hatcher vide Stanton & Hatcher 1905)
In 1905 Hatcher renamed three ''Monoclonius'' species into ''Ceratops'' species: ''Monoclonius recurvicornis'' Cope 1889 became ''Ceratops recurvicornis''; ''Monoclonius belli'' Lambe 1902 was made ''Ceratops belli'' and ''Monoclonius canadensis'' Lambe 1902 was renamed ''Ceratops canadensis''.<ref>{{cite journal | last1 = Stanton | first1 = T.W. | last2 = Hatcher | first2 = J.B. | year = 1905 | title = Geology and paleontology of the Judith River Beds | journal = Journal of Geology| volume = 257 | issue = 6| pages = 1–174 | bibcode = 1907JG.....15..601S | doi = 10.1086/621438 | doi-access = }}</ref> ''C. canadensis'' later was made the separate genus ''[[Eoceratops]]'', and ''C. belli'' was made the separate genus ''[[Chasmosaurus]]''; in 1925 [[William King Gregory]] concluded that ''Ceratops'' and ''Chasmosaurus'' were identical,<ref>{{cite journal | last1 = Gregory | first1 = W.K. | last2 = Mook | first2 = C.C. | year = 1925 | title = On ''Protoceratops'', a primitive ceratopsian dinosaur from the Lower Cretaceous of Mongolia | journal = American Museum Novitates | issue = 156 | pages = 1–9 }}</ref> but this was rejected by most researchers.
*''C.'' ''([[Eoceratops]]) canadensis'' (Lambe 1902/Hatcher vide Stanton & Hatcher 1905)
 
*''C.'' ''(Triceratops) horridus'' (Marsh 1889). This was the first intact ceratopsian skull discovered and led Marsh to realize the significance of the other specimens. As with the aforementioned species, it too is currently recognized as ''Triceratops''.
In 2005, remarkably well preserved cranial and postcranial elements of a [[Judith River Formation|Judithian]] ceratopsian were discovered in [[Fergus County, Montana]]. Nicknamed "Judith", preliminary examination suggested a close affinity with ''C. montanus''. The locality has been determined to be on or in close proximity to the stratigraphic layer of ''C. montanus'', and not too many miles away.<ref name=judiththedinosaur>"[http://www.judiththedinosaur.com Judith the Dinosaur] {{Webarchive|url=https://web.archive.org/web/20210119043702/http://www.judiththedinosaur.com/ |date=2021-01-19 }}". Accessed 17-AUG-2013.</ref> In 2016, the new animal was named ''[[Spiclypeus]]'', and the authors stated that it may be identical to ''Ceratops'', which they considered a ''nomen dubium'', or a growth stage of ''Albertaceratops''.<ref>{{cite journal|last1=Mallon|first1=Jordan C.|last2=Ott|first2=Christopher J.|last3=Larson|first3=Peter L.|last4=Iuliano|first4=Edward M.|last5=Evans|first5=David C.|last6=Evans|first6=Alistair R.|title=''Spiclypeus shipporum'' gen. et sp. nov., a Boldly Audacious New Chasmosaurine Ceratopsid (Dinosauria: Ornithischia) from the Judith River Formation (Upper Cretaceous: Campanian) of Montana, USA|journal=PLOS ONE|date=2016|volume=11|issue=5|pages=e0154218|doi=10.1371/journal.pone.0154218|pmid=27191389|pmc=4871577|bibcode=2016PLoSO..1154218M|doi-access=free}}</ref>
*''C. paucidens'' (Marsh 1889/1890); ''nomem dubium'' included with ''[[Lambeosaurus]] lambei''
 
*''C. (Chasmosaurus) recurvicornis'' (Cope 1890/Hatcher vide Stanton & Hatcher 1905)
===Species list===
The naming history can be summarised in a species list.
 
*''Ceratops montanus'' Marsh 1888: ''nomen dubium''; type species of ''Ceratops'' Marsh 1888; = ''Proceratops montanus'' (Marsh 1888) Lull 1906
*''Ceratops horridus'' Marsh 1889: = ''[[Triceratops]] horridus'' (Marsh 1889) Marsh 1889
*''Ceratops alticornis'' (Marsh 1887) Marsh 1889: ''nomen dubium''; = ''Bison alticornis'' Marsh 1887, = ''Triceratops alticornis'' (Marsh 1887) Lull vide Hatcher, Marsh & Lull 1907
*''C.Ceratops paucidens'' (Marsh 1889/1890); Marsh 1890: ''nomemnomen dubium''; = ''Hadrosaurus paucidens'' Marsh 1889; perhaps includedmaterial withof ''[[Lambeosaurus]] lambei''
*''Ceratops belli'' (Lambe 1902) Hatcher vide Stanton & Hatcher 1905: = ''Monoclonius belli'' Lambe 1902; = ''[[Chasmosaurus]] belli'' (Lambe 1902) Lambe 1914
*''Ceratops canadensis'' (Lambe 1902) Hatcher vide Stanton & Hatcher 1905: = ''Monoclonius canadensis'' Lambe 1902; = ''[[Eoceratops]] canadensis'' (Lambe 1902) Lambe 1915
*''C. (Chasmosaurus)Ceratops recurvicornis'' (Cope 1890/1889) Hatcher vide Stanton & Hatcher 1905): = ''Monoclonius recurvicornis'' Cope 1889
 
==Classification==
''Ceratops'' was placed by Marsh in the [[Ceratopsidae]] in 1888.<ref name="Marsh1888"/> It thus belonged to the Ceratopsia, a group of herbivorous dinosaurs with [[parrot]]-like beaks which thrived in [[North America]] and [[Asia]] during the Late [[Cretaceous Period]], which ended roughly 66 million years ago. In 1919 the group [[Ceratopsinae]] was named by [[Othenio Abel|Othenio Lothar Franz Anton Louis Abel]],<ref>Abel, O.L.F.A.L., 1919, ''Die Stämme der Wirbeltiere'', Berlin und Leipzig : W. de Gruyter, 914 pp</ref> but this concept is problematic: [[Paul Sereno]] has defined it as equivalent to the [[Chasmosaurinae]] but other researchers limit it to ''Ceratops'' itself as its direct relationships are uncertain.
 
==Diet==
''Ceratops'', like all Ceratopsiansceratopsians, was a [[herbivore]] biting off plant material with its beak and processing it with its tooth batteries.
 
==See also==
{{Portal|Dinosaurs}}
* [[Timeline of ceratopsian research]]
 
==References==
{{reflistReflist}}
 
==External links==
* https://web.archive.org/web/20090531083004/http://www.dinosaurvalley.com/Visiting_Drumheller/Kids_Zone/Groups_of_Dinosaurs/index.php
{{Portal|Dinosaurs}}
 
* http://www.dinosaurvalley.com/Visiting_Drumheller/Kids_Zone/Groups_of_Dinosaurs/index.php
{{Marginocephalia|T.}}
{{Taxonbar|from=Q134704}}
 
[[Category:Ceratopsids]]
[[Category:Late Cretaceous dinosaurs of North America]]
[[Category:Dinosaurs of North America]]
[[Category:Nomina dubia]]
[[Category:Fossil taxa described in 1888]]
 
[[Category:Taxa named by Othniel Charles Marsh]]
[[ca:Ceratop]]
[[Category:Fossils of Montana]]
[[cs:Ceratops]]
[[Category:Campanian genera]]
[[de:Ceratops]]
[[Category:Ornithischian genera]]
[[es:Ceratops]]
[[Category:Cretaceous Montana]]
[[it:Ceratops montanus]]
[[Category:DinosaursCeratopsians of North America]]
[[pl:Ceratops]]
[[Category:Late Cretaceous ceratopsians]]
[[zh:角龙]]