Jaculinykus

Jaculinykus
Temporal range: Late Cretaceous, 72–71 Ma
Holotype specimen and skeletal reconstruction
Scientific classification Edit this classification
Domain: Eukaryota
Kingdom: Animalia
Phylum: Chordata
Clade: Dinosauria
Clade: Saurischia
Clade: Theropoda
Family: Alvarezsauridae
Subfamily: Parvicursorinae
Genus: Jaculinykus
Species:
J. yaruui
Binomial name
Jaculinykus yaruui
Kubo et al., 2023

Jaculinykus (meaning "Jaculus claw") is an extinct genus of alvarezsaurid theropod dinosaur from the Late Cretaceous Baruungoyot Formation of Mongolia. The genus contains a single species, J. yaruui, known from a nearly complete articulated skeleton including bones of the skull. Jaculinykus is notable for its unique hand, which has a hypertrophied first digit and greatly reduced second digit, which is intermediate between the tridactyl hand of Shuvuuia and monodactyl hand of Linhenykus.[1]

Discovery and naming

[edit]
Occurrence of alvarezsaurids in Mongolia (Jaculinykus at center, zone 4)

The Jaculinykus holotype specimen, MPC-D 100/209, was discovered in sediments of the Baruungoyot Formation (Nemegt locality), of Ömnögovi Province, Mongolia. The specimen consists of a nearly complete skeleton with most of the skull.[1]

In 2023, Kubo et al. described Jaculinykus yaruui as a new genus and species of parvicursorine alvarezsaurid based on these fossil remains. The generic name, "Jaculinykus", combines a reference to the Jaculus, a small dragon in Greek mythology with the Greek word "onykus," meaning "claw". The specific name "yaruui" is derived from "yaruu" ("яаруу"), the Mongolian word for "speedy" or "hasty".[1]

Classification

[edit]
Life restoration

Jaculinykus was added to a phylogenetic analysis and found to be in the clade Parvicursorinae, in a clade consisting of all alvarezsaurs from the Nemegt Basin. The cladogram from Kubo et al. (2023) is shown below:[1]

Alvarezsauria

Paleoecology

[edit]
Restoration of the sleeping posture

Fossils of Ondogurvel, another parvicursorine alvarezsaurid, as well as fossils of Nemegtomaia, an oviraptorosaur, are also known from the Nemegt locality of the Mongolian Barun Goyot Formation.[2] Other localities from the formation have yielded dinosaurs including additional alvarezsaurids (Ceratonykus, Khulsanurus, and Parvicursor),[1] as well as dromaeosaurs (Hulsanpes,[3] Kuru, and Shri[4]), oviraptorosaurs (Conchoraptor and Heyuannia),[5] a sauropod (Quaesitosaurus),[6] ceratopsians (Bagaceratops and Breviceratops),[7] a pachycephalosaur (Tylocephale),[8] and ankylosaurs (Saichania,[9] Tarchia,[10] and Zaraapelta[11]).

References

[edit]
  1. ^ a b c d e Kubo, Kohta; Kobayashi, Yoshitsugu; Chinzorig, Tsogtbaatar; Tsogtbaatar, Khishigjav (2023-11-15). "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". PLOS ONE. 18 (11): e0293801. doi:10.1371/journal.pone.0293801. ISSN 1932-6203. PMC 10651048.
  2. ^ Fanti, F.; Currie, P. J.; Badamgarav, D.; Lalueza-Fox, C. (2012). "New specimens of Nemegtomaia from the Baruungoyot and Nemegt Formations (Late Cretaceous) of Mongolia". PLOS ONE. 7 (2): e31330. Bibcode:2012PLoSO...731330F. doi:10.1371/journal.pone.0031330. PMC 3275628. PMID 22347465.
  3. ^ Osmólska, H. (1982). "Hulsanpes perlei n.g. n.sp. (Deinonychosauria, Saurischia, Dinosauria) from the Upper Cretaceous Barun Goyot Formation of Mongolia". Neues Jahrbuch für Geologie und Paläontologie, Monatshefte. 1982 (7): 440–448. doi:10.1127/njgpm/1982/1982/440.
  4. ^ Napoli, J. G.; Ruebenstahl, A. A.; Bhullar, B.-A. S.; Turner, A. H.; Norell, M. A. (2021). "A New Dromaeosaurid (Dinosauria: Coelurosauria) from Khulsan, Central Mongolia" (PDF). American Museum Novitates (3982): 1–47. doi:10.1206/3982.1. hdl:2246/7286. ISSN 0003-0082. S2CID 243849373.
  5. ^ Funston, G. F.; Mendonca, S. E.; Currie, P. J.; Barsbold, R. (2018-04-01). "Oviraptorosaur anatomy, diversity and ecology in the Nemegt Basin". Palaeogeography, Palaeoclimatology, Palaeoecology. THE LATE CRETACEOUS NEMEGT ECOSYSTEM: DIVERSITY, ECOLOGY, AND GEOLOGICAL SIGNATURE. 494: 101–120. Bibcode:2018PPP...494..101F. doi:10.1016/j.palaeo.2017.10.023. ISSN 0031-0182.
  6. ^ Kurzanov, S. M.; Bannikov, A. F. (1983). "A new sauropod from the Upper Cretaceous of Mongolia". Paleontological Journal. 2: 90−96.
  7. ^ Czepiński, Łukasz (2020-11-25). "Ontogeny and variation of a protoceratopsid dinosaur Bagaceratops rozhdestvenskyi from the Late Cretaceous of the Gobi Desert". Historical Biology. 32 (10): 1394–1421. doi:10.1080/08912963.2019.1593404. ISSN 0891-2963. S2CID 132780322.
  8. ^ Maryańska, T.; Osmólska, H. (1974). "Pachycephalosauria, a new suborder of ornithischian dinosaurs" (PDF). Palaeontologica Polonica (30): 45−102.
  9. ^ Carpenter, K., Hayashi, S., Kobayashi, Y., Maryańska, T., Barsbold, R., Sato, K., and Obata, I., 2011,"Saichania chulsanensis (Ornithischia, Ankylosauridae) from the Upper Cretaceous of Mongolia", Palaeontographica, Abteilung A, 294(1-3): 1-61
  10. ^ Maryańska, T. 1977. "Ankylosauridae (Dinosauria) from Mongolia". Palaeontologia Polonica 37: 85-151
  11. ^ Arbour, Victoria M.; Currie, Philip J.; Badamgarav, Demchig (2014-10-27). "The ankylosaurid dinosaurs of the Upper Cretaceous Baruungoyot and Nemegt formations of Mongolia". Zoological Journal of the Linnean Society. 172 (3): 631–652. doi:10.1111/zoj.12185. ISSN 0024-4082.