Ukureyskaya Formation | |
---|---|
Stratigraphic range: Bajocian–Tithonian, 169–144 Ma PreꞒ Ꞓ O S D C P T J K Pg N | |
Type | Geological formation |
Sub-units | Lower, Middle and Upper subformations |
Underlies | Utanskaya Formation |
Overlies | Kulindinskaya Formation |
Thickness | Several hundred metres |
Lithology | |
Primary | Sandstone, siltstone, tuffite |
Other | Mudstone |
Location | |
Coordinates | 52°30′N 116°42′E / 52.5°N 116.7°E / 52.5; 116.7 |
Approximate paleocoordinates | 58°00′N 117°12′E / 58.0°N 117.2°E / 58.0; 117.2 |
Region | Zabaykalsky Krai |
Country | Russia |
Extent | Zabaykalsky Krai |
Ukureyskaya Formation (Russia)Show map of RussiaUkureyskaya Formation (Zabaykalsky Krai)Show map of Zabaykalsky Krai |
The Ukureyskaya Formation, also referred to as the Ukurey Formation, is a geological formation in Zabaykalsky Krai, part of the Russian Far East. It is made up of Middle Jurassic and Late Jurassic layers. It covers large areas around Kulinda.
History
The Ukureyskaya Formation was mentioned by Sinitsa & Starukhina (1986), and was first discovered by Sofia M. Sinitsa and her team from the Russian Academy of Sciences before being excavated in 2010 by a group of Russian and Belgian palaeontologists; during this time, the holotype of Kulindadromeus zabaikalicus was discovered. Excavations wrapped up in 2013 or 2014.
Description
The volcanic ash layers of the Ukureyskaya Formation form a Konservat-Lagerstätte with an exceptional preservation, and it likely represents a nearshore lacustrine or estuarine-deltaic environment similar to the Yixian Formation.
In total, two bone beds were identified during the excavations that took place between 2010 and 2013/14; Bonebed 4 is older than Bonebed 3.
Age
Sinitsa & Starukhina (1986) and Sinitsa (2011) suggested that the Ukureyskaya Formation dated to the Late Jurassic-Early Cretaceous.
Godefroit et al. (2014) and Alivanov & Saveliev (2014) have suggested that as a whole, the Ukureyskaya Formation dates to the Bajocian-Tithonian, while more recent dating work by Cincotta et al. (2019) suggests that the layers containing the remains of Kulindadromeus are Bathonian in age.
Paleofauna
Genus | Species | Location | Stratigraphic position | Material | Notes | Image |
---|---|---|---|---|---|---|
Crustacea | Indeterminate | Kulinda | "Indeterminate remains" | |||
Insecta | Indeterminate | Kulinda | Represented by multiple species. | |||
Kulindadromeus | K. zabaikalicus | Kulinda | "Base of the Ukureyska Formation" | "Hundreds of disarticulated skeletons including six skulls" | Synonyms include Daurosaurus olovus and Lepidocheirosaurus natalis. | |
Ornithopoda | Indeterminate | Kulinda | "Indeterminate remains" | Represents an unnamed genus that is distinct from Kulindadromeus. | ||
Theropoda | Indeterminate | Kulinda | "Single tooth" | Based on undiagnostic remains. |
References
- ^ Sinitsa, S.; Reshetova, S.; Vilmova, E. (2017). "Hypostratotypes of Ukureyskaya Formation of Novoberezovka and Olov Depressions of Transbaikalia (Part 1. Hypostratotype-1 of Ukureyskaya Formation of Novoberezovka Depression)". Transbaikal State University Journal (in Russian). 23 (6): 52–62. doi:10.21209/2227-9245-2017-23-6-52-62 (inactive 1 November 2024). ISSN 2227-9245.
{{cite journal}}
: CS1 maint: DOI inactive as of November 2024 (link) - ^ "The Kulinda fossil site", University of Bristol Palaeobiology Research Group. Retrieved 4 April 2015
- ^ Sinitsa S.M., Starukhina S. (1986) New data and problems in stratigraphy and palaeontology of the Upper Meso�zoic in East Transbaikalia. In: Novye Dannye po Geologii Zabaikal’ya. Min. Geol. RSFSR, Moscow, pp 46–51
- ^ Sinitsa S.M. (2011). Jurassic dinosaurs of Transbaikalia. In: Sinitsa SM (ed) Environmental cooperative studies in the cross-border ecological region: Russia, China, and Mongolia. Inst. Min. Res., Ecol. Cryol. SB RAS, Chita, pp 173–176
- ^ Godefroit, P.; Sinitsa, S.M.; Dhouailly, D.; Bolotsky, Y.L.; Sizov, A.V.; McNamara, M.E.; Benton, M.J.; Spagna, P. (2014). "A Jurassic ornithischian dinosaur from Siberia with both feathers and scales" (PDF). Science. 345 (6195): 451–455. Bibcode:2014Sci...345..451G. doi:10.1126/science.1253351. hdl:1983/a7ae6dfb-55bf-4ca4-bd8b-a5ea5f323103. PMID 25061209. S2CID 206556907. Archived from the original (PDF) on 2019-02-09. Retrieved 2016-07-27.
- ^ Dan Vergano, 2014, "Siberian Discovery Suggests Almost All Dinosaurs Were Feathered", National Geographic Daily News
- ^ Alifanov, V.R.; Saveliev, S.V. (2014). "Two new ornithischian dinosaurs (Hypsilophodontia, Ornithopoda) from the Late Jurassic of Russia" (PDF). Paleontologicheskii Zhurnal. 48 (4): 72–82. Bibcode:2014PalJ...48..414A. doi:10.1134/S0031030114040029. (in Russian; English translation published in Alifanov, V. R. (2014). "Two new ornithischian dinosaurs (Hypsilophodontia, Ornithopoda) from the Late Jurassic of Russia". Paleontological Journal. 48 (4): 414–425. Bibcode:2014PalJ...48..414A. doi:10.1134/S0031030114040029. S2CID 85539844.)
- Cincotta, Aude; Pestchevitskaya, Ekaterina B.; Sinitsa, Sofia M.; Markevich, Valentina S.; Debaille, Vinciane; Reshetova, Svetlana A.; Mashchuk, Irina M.; Frolov, Andrei O.; Gerdes, Axel; Yans, Johan; Godefroit, Pascal (2019-02-01). "The rise of feathered dinosaurs: Kulindadromeus zabaikalicus, the oldest dinosaur with 'feather-like' structures". PeerJ. 7: e6239. doi:10.7717/peerj.6239. ISSN 2167-8359. PMC 6361000. PMID 30723614.
- Andrea Cau (November 24, 2015). "Cosa è Lepidocheirosaurus?". Theropoda. Retrieved November 25, 2015.
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