Siats
{{Short description|Extinct genus of theropod dinosaurs}}
{{about|the dinosaur genus|text="Siats" can also refer to a man-eating monster in Ute mythology, after which the genus was named}}
{{Automatic taxobox
| display_parents = 3
| taxon = Siats
| fossil_range = Cenomanian, {{fossilrange|99|94.5}}
| image = Siats meekerorum skeletal diagram.jpg
| image_caption = Skeletal reconstruction of known elements
| authority = Zanno & Makovicky, 2013
| type_species = {{extinct}}Siats meekerorum
| type_species_authority = Zanno & Makovicky, 2013
|subdivision_ranks=|subdivision=}}
Siats (/see-ats/) is an extinct genus of large theropod dinosaurs known from the Late Cretaceous Cedar Mountain Formation (Mussentuchit Member) of Utah, United States. The genus contains a single species, Siats meekerorum. It was initially classified as a megaraptoran, a clade of large theropods with controversial relationships. Alternative positions within the Neovenatoridae, Allosauroidea, and Tyrannosauroidea have also been proposed.
Discovery and naming
File:Siats Dorsal Vertebra.jpg
Siats was described by Lindsay E. Zanno and Peter J. Makovicky in 2013. The generic name references a man-eating monster in Ute mythology. The specific name meekerorum honors the geologist John Caldwell Meeker and his family for their support of paleontological research.{{Cite journal | last1 = Zanno | first1 = L. E. | last2 = Makovicky | first2 = P. J. | doi = 10.1038/ncomms3827 | title = Neovenatorid theropods are apex predators in the Late Cretaceous of North America | journal = Nature Communications | volume = 4 | pages = 2827 | year = 2013 | pmid = 24264527| bibcode = 2013NatCo...4.2827Z | doi-access = free }}
Siats is known from the holotype specimen, FMNH PR 2716, a partial postcranial skeleton housed at the Field Museum of Natural History, Chicago. The specimen consists of five dorsal vertebrae, eight caudal vertebrae, a chevron, a partial right ilium, ischium, fibula, tibia, and several right and left pedal phalanges. The specimen was discovered by Lindsay Zanno as a part of a 2008 Field Museum expedition with Peter Makovicky. The bones were first seen protruding out of a hillside, prompting the excavation. It was collected between 2008 and 2010 from the Mussentuchit Member of the Cedar Mountain Formation in Emery County of Utah, dating to the early Cenomanian stage of the Late Cretaceous, approximately 94.5 million years ago.{{Cite news |last=Johnson |first=Steve |date=22 November 2013 |title=New dinosaur discovered by Field Museum expedition |url=http://www.chicagotribune.com/entertainment/chi-new-dinosaur-siats-meekerorum-discovered-20131121,0,4656361.story |archive-url=https://web.archive.org/web/20180923124235/http://www.chicagotribune.com/entertainment/chi-new-dinosaur-siats-meekerorum-discovered-20131121-story.html |archive-date=23 September 2018 |access-date=22 November 2013 |work=Chicago Tribune}}{{cite journal |last1=Tucker |first1=R.T. |last2=Zanno |first2=L.E. |last3=Huang |first3=H.-Q. |last4=Makovicky |first4=P.J. |year=2020 |title=A refined temporal framework for newly discovered fossil assemblages of the upper Cedar Mountain Formation (Mussentuchit Member), Mussentuchit Wash, Central Utah |journal=Cretaceous Research |volume=110 |page=104384 |doi=10.1016/j.cretres.2020.104384|bibcode=2020CrRes.11004384T |s2cid=213733376 }}
Description
The Siats holotype specimen consists of material from a single individual that is considered skeletally immature based on the incomplete fusion of neural arches to the centra of the dorsal vertebrae. Siats is characterized by seven traits, including four autapomorphies. These include the subtriangular cross section of the distal caudal vertebrae, elongated centrodiapophyseal laminae lacking noticeable infradiapophyseal fossae on the proximal caudals, a transversely concaved acetabular rim of iliac pubic peduncle, and the presence of a notch on the end of the truncated lateral brevis shelf. Other notable traits include the broad neural spines on the dorsal vertebrae.
File:Siats reconstruction.png]]
Siats represents one of the largest known theropods from the 'mid'-Cretaceous of North America. Using a femur circumference regression, Zanno and Mackovicky (2013) estimated its mass at roughly {{convert|3.9|MT|ST}}. They further wrote that the holotype was already comparable in size to Saurophaganax and Acrocanthosaurus despite its immaturity.
Classification
In its 2013 description, Siats was initially classified as a megaraptoran within the Neovenatoridae, based on the presence of pronounced centrodiapophyseal laminae bracketed by deep infradiapophyseal fossa on the caudal neural arches, similar to that of the megaraptoran Aerosteon. These results, following Zanno & Makovicky (2013), are displayed in the cladogram below:
{{clade| style=font-size:85%;line-height:85%
|label1=Allosauroidea
|1={{clade
|label2=Allosauria
|2={{clade
|label1=Allosauridae
|1={{clade
|label2=Carcharodontosauria
|2={{clade
|label1=Neovenatoridae
|1={{clade
|2={{clade
|1=Chilantaisaurus tashuikouensis
|label2=Megaraptora
|2={{clade
|1=Siats meekerorum
|2={{clade
|1=Australovenator wintonensis
|2=Fukuiraptor kitadaniensis}}
|3={{clade
|2=Megaraptor namunhuaiquii}} }} }} }}
|label2=Carcharodontosauridae
|2={{clade
|1={{clade
|2={{clade
|2={{clade
}} }} }} }} }} }} }}
In the 2014 description of a juvenile Megaraptor specimen, the referral of Siats to Megaraptora was contested, and megaraptorans were found to more likely be tyrannosauroids rather than neovenatorids such as Siats. The paper noted that, although sharing various features with Neovenator, Siats could be distinguished from megaraptorans in the structure of its dorsal vertebrae, ilium, and fibula.{{Cite journal|last1=Porfiri|first1=Juan D.|last2=Novas|first2=Fernando E.|last3=Calvo|first3=Jorge O.|last4=Agnolín|first4=Federico L.|last5=Ezcurra|first5=Martín D.|last6=Cerda|first6=Ignacio A.|date=2014-09-01|title=Juvenile specimen of Megaraptor (Dinosauria, Theropoda) sheds light about tyrannosauroid radiation|journal=Cretaceous Research|volume=51|issue=Supplement C|pages=35–55|doi=10.1016/j.cretres.2014.04.007|bibcode=2014CrRes..51...35P |hdl=11336/12129|hdl-access=free}} A subsequent analysis conducted by Coria and Currie (2016), which even placed megaraptorans as neovenatorids, still placed Siats and Chilantaisaurus as neovenatorids outside of Megaraptora.{{Cite journal|last1=Coria|first1=Rodolfo A.|last2=Currie|first2=Philip J.|date=2016-07-20|title=A New Megaraptoran Dinosaur (Dinosauria, Theropoda, Megaraptoridae) from the Late Cretaceous of Patagonia|journal=PLOS ONE|volume=11|issue=7|pages=e0157973|doi=10.1371/journal.pone.0157973|issn=1932-6203|pmc=4954680|pmid=27439002|bibcode=2016PLoSO..1157973C|doi-access=free}} However, Bell et al. (2016) recovered Siats as a member of Coelurosauria of uncertain phylogenetic placement within this group; their analyses found variable positions for Siats, as a relative of ornithomimosaurs, a theropod more closely related to maniraptorans than tyrannosauroids, a basal megaraptoran, or a tyrannosauroid more closely related to tyrannosaurids than Xiongguanlong.{{cite journal |author1=Phil R. Bell |author2=Andrea Cau |author3=Federico Fanti |author4=Elizabeth T. Smith |year=2016 |title=A large-clawed theropod (Dinosauria: Tetanurae) from the Lower Cretaceous of Australia and the Gondwanan origin of megaraptorid theropods |journal=Gondwana Research |volume=36 |pages=473–487 |doi=10.1016/j.gr.2015.08.004 |bibcode=2016GondR..36..473B }}
Naish and Cau (2022) recovered the taxon as the basalmost megaraptoran, with this clade diverging after Xiongguanlong, and supported Siats and Chilantaisaurus as representing a wave of gigantism in tyrannosauroids preceding the Tyrannosauridae.{{Cite journal |last1=Naish |first1=Darren |last2=Cau |first2=Andrea |date=2022-07-07 |title=The osteology and affinities of Eotyrannus lengi, a tyrannosauroid theropod from the Wealden Supergroup of southern England |journal=PeerJ |volume=10 |pages=e12727 |doi=10.7717/peerj.12727 |doi-access=free|issn=2167-8359 |pmc=9271276 |pmid=35821895}} In their 2025 analysis of allosauroid phylogenetics, Kellermann, Cuesta & Rauhut consistently recovered Siats as a megaraptoran, noting that it shares a specific position of pneumatic fossa with this clade.{{Cite journal |last1=Kellermann |first1=Maximilian |last2=Cuesta |first2=Elena |last3=Rauhut |first3=Oliver W. M. |date=2025-01-14 |title=Re-evaluation of the Bahariya Formation carcharodontosaurid (Dinosauria: Theropoda) and its implications for allosauroid phylogeny |journal=PLOS One |language=en |volume=20 |issue=1 |pages=e0311096 |doi=10.1371/journal.pone.0311096 |issn=1932-6203 |doi-access=free|pmid=39808629 |pmc=11731741 |bibcode=2025PLoSO..2011096K }} The cladogram below follows Naish and Cau (2022), who found Siats within Megaraptora as part of Tyrannosauroidea:
{{clade| style=font-size:85%;line-height:85%
|label1=
|1={{clade
|1=Yutyrannus
|2={{clade
|1=Eotyrannus
|2={{clade
|2={{clade
|1={{clade
|label1=Megaraptora
|1={{clade
|1=Siats
|2={{clade
|1=Aniksosaurus
|2={{clade
|2={{clade
|1=Fukuiraptor
|2={{clade
|1=Aerosteon
|3=Megaraptor
|4=Orkoraptor
}}}}}}}}}}
|2={{clade
|1=Dryptosaurus
|2={{clade
|2={{clade
|1={{clade
}}
|label2=Tyrannosauridae
|2={{clade
|1=Gorgosaurus
|2={{clade
|1=Alioramus
|2={{clade
|1=Lythronax
}}}}}}}}}}}}}}}}}}}}}}}}
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{{wikispecies|siats}}
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References
{{Reflist}}
{{Theropoda|A.}}
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Category:Cedar Mountain Formation
Category:Taxa named by Lindsay Zanno