{{Short description|Genus of troodontid dinosaurs}} {{Speciesbox | fossil_range = Late Cretaceous<br />{{fossil range|72|72|(late Campanian?)<ref name="sediments"/>}} | image = Harenadraco prima.png | image_caption = Life restoration | genus = Harenadraco | parent_authority = Lee et al., 2024 | species = prima | authority = Lee et al., 2024 }}
'''''Harenadraco''''' (meaning "sand dragon") is an extinct genus of troodontid theropod dinosaurs from the Late Cretaceous Baruungoyot Formation of Mongolia. The genus contains a single species, '''''H. prima''''', known from a fragmentary skeleton. ''Harenadraco'' represents the first troodontid known from the Baruungoyot Formation. Since members of this family are also known from the Nemegt and Djadochta Formations, the discovery of ''Harendraco'' indicates that troodontids were important faunal components of every formation within the Nemegt Basin.
== Discovery and naming == thumb|left|Outcrops of the Baruungoyot Formation (Hermiin Tsav locality), which produced the ''Harenadraco'' holotype and many other dinosaur specimens The ''Harenadraco'' holotype specimen, MPC-D 110/119, was discovered in 2018 in sediments of the Baruungoyot Formation (Hermiin Tsav locality) in Ömnögovi Province, Mongolia. The specimen consists of a fragmentary and partially articulated skeleton, comprising pieces of the right ilium, the end of the right femur, and several bones from the left hind leg, including the top of the femur, the end of the tibiotarsus, the second through fourth metatarsals, and several pedal phalanges. Some unidentified bone fragments are also associated with the skeleton.<ref name="Harenadraco">{{Cite journal|last1=Lee |first1=S. |last2=Lee |first2=Y.-N. |last3=Park |first3=J.-Y. |last4=Kim |first4=S.-H. |last5=Badamkhatan |first5=Z. |last6=Idersaikhan |first6=D. |last7=Tsogtbaatar |first7=K. |title=The first troodontid (Dinosauria: Theropoda) from the Upper Cretaceous Baruungoyot Formation of Mongolia |year=2024 |journal=Journal of Vertebrate Paleontology |volume=43 |issue=6 |at=e2364746 |doi=10.1080/02724634.2024.2364746 |doi-access=free }}</ref>
In 2024, Lee et al. described ''Harenadraco prima'' as a new genus and species of troodontid theropod based on these fossil remains. The generic name, ''Harenadraco '', combines the Latin words "''harena''", meaning "sand", and "''draco''", meaning "dragon". The specific name, ''prima'', is a Latin word meaning "first", referencing the fact that ''Harenadraco'' is the first troodontid known from its geological formation.<ref name="Harenadraco"/>
== Classification == In their phylogenetic analyses, Lee et al. (2024) recovered ''Harenadraco'', along with an unnamed specimen from the Wulansuhai Formation, as the earliest diverging members of an otherwise entirely Chinese clade of troodontids. This clade is the sister taxon to all other troodontids. Their results are displayed in the cladogram below:<ref name="Harenadraco"/>
{{clade |{{clade |1={{clade |1='''''Harenadraco''''' |2=LH PV39 {{small|(unnamed Wulansuhai Fm. taxon)}}<ref name="Wang2021">{{Cite journal |last1=Wang |first1=Shuo |last2=Zhang |first2=Qiyue |last3=Tan |first3=Qingwei |last4=Jiangzuo |first4=Qigao |last5=Zhang |first5=Huitao |last6=Tan |first6=Lin |date=2021-07-23 |title=New troodontid theropod specimen from Inner Mongolia, China clarifies phylogenetic relationships of later-diverging small-bodied troodontids and paravian body size evolution |journal=Cladistics |language=en |volume=38 |issue=1 |pages=59–82 |doi=10.1111/cla.12467 |pmid=35049080 |issn=0748-3007}}</ref> |3={{clade |1=''Mei'' |2={{clade |1=''Sinusonasus'' |2=''Sinovenator'' }} }} }} |3={{clade |1={{clade |1=MPC-D 100/44 {{small|("EK troodontid")}} |2=''Sinornithoides'' }} |3={{clade |1=MPC-D100/1126+D100/3500 {{small|(unnamed Djadokhta Fm. taxon)}}<ref name="Wang2021" /> |2={{clade |1=''Almas'' |2={{clade |1={{clade |1=''Philovenator'' |2={{clade |1=''Talos'' |2=''Gobivenator'' }} }} |3={{clade |1=''Xixiasaurus'' |2=''Byronosaurus'' |3={{clade |1=''Zanabazar'' |2={{clade |1=''Saurornithoides'' |2={{clade |1=''Linhevenator'' |2=''Troodon''
}} }} }} }} }} }} }} }} }}|label1=Troodontidae}}
== Paleoecology == ''Harenadraco'' is known from the Hermiin Tsav locality of the Baruungoyot Formation.<ref name="Harenadraco"/> This locality is known for its abundant dinosaur remains. Based on stratigraphy and fossil content, the formation is consistently regarded as Late Cretaceous (possibly Upper Campanian) in age, although radiometric dates have not been determined.<ref name="sediments"/>
=== Paleoenvironment === The Baruungoyot Formation is largely characterized by red beds, with many light-colored well-cemented sands (yellowish, grey-brown, and some reddish). Some sandy claystones (often red-colored), siltstones, conglomerates, and cross-bedded sands are also common. The formation's geology indicates that sediments were likely deposited under relatively arid to semiarid climates in alluvial plain (flat land consisting of sediments deposited by highland rivers), lacustrine (lake), and aeolian (wind-shaped) paleoenvironments, with occasional short-lived water bodies.<ref name="sediments">{{cite journal|last1=Gradziński|first1=R.|last2=Jerzykiewicz|first2=T.|date=1974|title=Sedimentation of the Barun Goyot Formation|journal=Palaeontologia Polonica|volume=30|pages=111−146|url=http://www.palaeontologia.pan.pl/Archive/1974_30_111-146_34-42.pdf}}</ref><ref>{{cite journal|last1=Gradziński|first1=R.|last2=Jaworowska|first2=Z. K.|last3=Maryańska|first3=T.|date=1977|title=Upper Cretaceous Djadokhta, Barun Goyot and Nemegt formations of Mongolia, including remarks on previous subdivisions|journal=Acta Geologica Polonica|volume=27|number=3|pages=281–326|url=https://geojournals.pgi.gov.pl/agp/article/view/9555/8104}}</ref><ref name=Enerthh2018>{{cite journal|last1=Eberth|first1=D. A.|date=2018|title=Stratigraphy and paleoenvironmental evolution of the dinosaur-rich Baruungoyot-Nemegt succession (Upper Cretaceous), Nemegt Basin, southern Mongolia|journal=Palaeogeography, Palaeoclimatology, Palaeoecology|volume=494|pages=29–50|bibcode=2018PPP...494...29E|doi=10.1016/j.palaeo.2017.11.018}}</ref>
=== Contemporary fauna === {{multiple image | align = right | direction = vertical | width = | header = | image1 = Parvicursor.jpg | image2 = Quaesitosaurus.jpg | footer = Life restorations of the alvarezsaurid ''Parviscursor'' and the titanosaur ''Quaesitosaurus'', two Baruungoyot dinosaurs }}
Fossil remains of many vertebrates have been found in various layers of the Baruungoyot Formation. Most notably, dinosaurs are some of the most abundant, with many species having been described. Maniraptoran theropods are especially common, including dromaeosaurids (''Hulsanpes'', ''Kuru'', ''Natovenator'', and ''Shri devi''),<ref>{{cite journal|last1=Cau|first1=A.|last2=Madzia|first2=D.|date=2018|title=Redescription and affinities of ''Hulsanpes perlei'' (Dinosauria, Theropoda) from the Upper Cretaceous of Mongolia|journal=PeerJ|volume=6|article-number=e4868|doi=10.7717/peerj.4868|doi-access=free|pmc=5978397|pmid=29868277}}</ref><ref name="Natovenator">{{cite journal|last1=Lee|first1=S.|last2=Lee|first2=Y.-N.|last3=Currie|first3=P. J.|last4=Sissons|first4=R.|last5=Park|first5=J.-Y.|last6=Kim|first6=S.-H.|last7=Barsbold|first7=R.|last8=Tsogtbaatar|first8=K.|date=2022|title=A non-avian dinosaur with a streamlined body exhibits potential adaptations for swimming|journal=Communications Biology|volume=5|number=1185|page=1185 |doi=10.1038/s42003-022-04119-9|doi-access=free|pmid=36456823 |issn=2399-3642|pmc=9715538}}</ref><ref>{{cite journal|last1=Napoli|first1=J. G.|last2=Ruebenstahl|first2=A. A.|last3=Bhullar|first3=B.-A. S.|last4=Turner|first4=A. H.|last5=Norell|first5=M. A.|date=2021|title=A New Dromaeosaurid (Dinosauria: Coelurosauria) from Khulsan, Central Mongolia|journal=American Museum Novitates|number=3982|pages=1–47|doi=10.1206/3982.1|issn=0003-0082|hdl=2246/7286|hdl-access=free|url=https://digitallibrary.amnh.org/bitstream/handle/2246/7286/3982.pdf?sequence=1&isAllowed=y}}</ref> oviraptorids (''Conchoraptor'', ''Heyuannia'' and ''Nemegtomaia''),<ref>{{cite journal|last1=Funston|first1=G. F.|last2=Mendonca|first2=S. E.|last3=Currie|first3=P. J.|last4=Barsbold|first4=R.|last5=Barsbold|first5=R.|date=2018|title=Oviraptorosaur anatomy, diversity and ecology in the Nemegt Basin|journal=Palaeogeography, Palaeoclimatology, Palaeoecology|volume=494|pages=101–120|doi=10.1016/j.palaeo.2017.10.023|bibcode=2018PPP...494..101F}}</ref> alvarezsaurids (''Ceratonykus'', ''Jaculinykus'', ''Khulsanurus'', ''Ondogurvel'', and ''Parvicursor''),<ref name=Jaculinykus>{{Cite journal |last1=Kubo |first1=Kohta |last2=Kobayashi |first2=Yoshitsugu |last3=Chinzorig |first3=Tsogtbaatar |last4=Tsogtbaatar |first4=Khishigjav |date=2023-11-15 |title=A new alvarezsaurid dinosaur (Theropoda, Alvarezsauria) from the Upper Cretaceous Baruungoyot Formation of Mongolia provides insights for bird-like sleeping behavior in non-avian dinosaurs |journal=PLOS ONE |language=en |volume=18 |issue=11 |article-number=e0293801 |doi=10.1371/journal.pone.0293801 |issn=1932-6203|doi-access=free |pmid=37967055 |pmc=10651048 |bibcode=2023PLoSO..1893801K }}</ref> and birds (''Gobipipus'', ''Gobipteryx'' and ''Hollanda'').<ref>{{cite journal|last1=Bell|first1=A. K.|last2=Chiappe|first2=L. M.|last3=Erickson|first3=G. M.|last4=Suzuki|first4=S.|last5=Watabe|first5=M.|last6=Barsbold|first6=R.|last7=Tsogtbaatar|first7=K.|date=2010|title=Description and ecologic analysis of ''Hollanda luceria'', a Late Cretaceous bird from the Gobi Desert (Mongolia)|journal=Cretaceous Research|volume=31|issue=1|pages=16−26|doi=10.1016/j.cretres.2009.09.001|bibcode=2010CrRes..31...16B |url=https://www.researchgate.net/publication/229349737}}</ref><ref>{{Cite journal |last1=Kurochkin |first1=E. N. |last2=Chatterjee |first2=S. |last3=Mikhailov |first3=K. E. |date=2013-12-01 |title=An embryonic enantiornithine bird and associated eggs from the cretaceous of Mongolia |journal=Paleontological Journal |language=en |volume=47 |issue=11 |pages=1252–1269 |doi=10.1134/S0031030113110087 |bibcode=2013PalJ...47.1252K |issn=1555-6174}}</ref> Remarkably, ''Harenadraco'' is the first troodontid known from this formation, despite the fact that the Nemegt and Djadochta Formations—the other two similarly aged geological formations in the Mongolian Nemegt Basin—both preserve multiple troodontid taxa.<ref name="Harenadraco"/>
Several non-theropod dinosaurs are also present, including the titanosaurian sauropod (''Quaesitosaurus''),<ref>{{cite journal|last1=Kurzanov|first1=S. M.|last2=Bannikov|first2=A. F.|date=1983|title=A new sauropod from the Upper Cretaceous of Mongolia|journal=Paleontological Journal|volume=2|pages=90−96|url=https://moam.info/a-new-sauropod-from-the-upper-cretaceous-of-mongolia_5b764105097c4785168b45fe.html|archive-date=2022-02-19|access-date=2024-07-16|archive-url=https://web.archive.org/web/20220219211445/https://moam.info/a-new-sauropod-from-the-upper-cretaceous-of-mongolia_5b764105097c4785168b45fe.html}}</ref> ankylosaurids (''Saichania'', ''Tarchia'' and ''Zaraapelta''),<ref>{{cite journal|last1=Park|first1=J.-Y.|last2=Lee|first2=Y. N.|last3=Currie|first3=P. J.|last4=Ryan|first4=M. J.|last5=Bell|first5=P.|last6=Sissons|first6=R.|last7=Koppelhus|first7=E. B.|last8=Barsbold|first8=R.|last9=Lee|first9=S.|last10=Kim|first10=S.-H.|date=2021|title=A new ankylosaurid skeleton from the Upper Cretaceous Baruungoyot Formation of Mongolia: its implications for ankylosaurid postcranial evolution|journal=Scientific Reports|volume=11|number=4101|page=4101|doi=10.1038/s41598-021-83568-4|doi-access=free|pmc=7973727|pmid=33737515}}</ref> protoceratopsids (''Bagaceratops'' and ''Breviceratops''),<ref>{{cite journal|last1=Czepiński|first1=Ł.|date=2019|title=Ontogeny and variation of a protoceratopsid dinosaur ''Bagaceratops rozhdestvenskyi'' from the Late Cretaceous of the Gobi Desert|journal=Historical Biology|volume=32|issue=10|pages=1394–1421|doi=10.1080/08912963.2019.1593404|s2cid=132780322|url=http://dinosaurmailinglist.cmnh.org/2019Apr/pdfzmfpMk1aO4.pdf|archive-date=2021-07-08|access-date=2024-07-16|archive-url=https://web.archive.org/web/20210708144840/http://dinosaurmailinglist.cmnh.org/2019Apr/pdfzmfpMk1aO4.pdf}}</ref> and a pachycephalosaurid (''Tylocephale'').<ref>{{cite journal|last1=Sullivan|first1=R. M.|date=2006|title=A taxonomic review of the Pachycephalosauridae (Dinosauria: Ornithischia)|journal=New Mexico Museum of Natural History and Science Bulletin|issue=35|pages=347–365|url=https://www.researchgate.net/publication/240625747}}</ref>
Non-dinosaurian animals from the formation include several fossil fish, amphibians, turtles, and many lizards and mammals (including djadochtatheriids, eutherians, multituberculates, and tribosphenidans).<ref>{{Cite journal |last1=Jerzykiewicz |first1=Tomasz |last2=Currie |first2=Philip J. |last3=Fanti |first3=Federico |last4=Lefeld |first4=Jerzy |date=2021-02-10 |title=Lithobiotopes of the Nemegt Gobi Basin |journal=Canadian Journal of Earth Sciences |language=en |volume=58 |issue=9 |pages=829–851 |url=https://tspace.library.utoronto.ca/bitstream/1807/106213/1/cjes-2020-0148.pdf |doi=10.1139/cjes-2020-0148 |issn=0008-4077}}</ref>
== References == {{Reflist}}
{{Troodontidae}} {{Taxonbar|from1=Q127456847|from2=Q127456862}}
Category:Troodontidae Category:Dinosaur genera Category:Maastrichtian dinosaurs Category:Baruungoyot Formation Category:Fossil taxa described in 2024 Category:Dinosaurs of Mongolia