Kakanaut Formation
Appearance
Kakanaut Formation | |
---|---|
Stratigraphic range: Maastrichtian ~ | |
Type | Geological formation |
Underlies | Danian marine deposits |
Overlies | Maastrichtian marine deposits |
Thickness | 1,000 m (3,300 ft) |
Lithology | |
Primary | Sandstone |
Other | Volcaniclastic |
Location | |
Coordinates | 62°54′N 177°06′E / 62.9°N 177.1°E |
Approximate paleocoordinates | 75°42′N 179°00′E / 75.7°N 179.0°E |
Region | Chukotka Autonomous Okrug |
Country | Russia |
Type section | |
Named for | Kakanaut River |
The Kakanaut Formation is a geological formation in Siberia, whose strata date back to the Late Cretaceous (Maastrichtian). Dinosaur remains are among the fossils that have been recovered from the formation.[1][2] The flora of the formation is relictual, containing some of the youngest remains of the extinct plant orders Bennettitales and Czekanowskiales.[3][4]
Fossil content
[edit]See also
[edit]References
[edit]- ^ Weishampel et al., 2004, pp.593-600
- ^ Godefroit et al., 2009
- ^ Gnilovskaya, Anastasia A.; Golovneva, Lina B. (February 2018). "The Late Cretaceous Pterophyllum (Bennettitales) in the North-East of Russia". Cretaceous Research. 82: 56–63. Bibcode:2018CrRes..82...56G. doi:10.1016/j.cretres.2017.09.013.
- ^ Zolina, Anastasia; Golovneva, Lina; Nosova, Natalya; Grabovskiy, Alexander (2020-12-01). "A new species of Phoenicopsis (Leptostrobales) from the Maastrichtian–Danian of Chukotka, Russia". Geobios. 63: 67–75. Bibcode:2020Geobi..63...67Z. doi:10.1016/j.geobios.2020.09.002. ISSN 0016-6995. S2CID 228928283.
Bibliography
[edit]- Godefroit, P.; Golovneva, L.; Shchepetov, S.; García, G.; Alekseev, P. (2009), "The last polar dinosaurs: high diversity of latest Cretaceous arctic dinosaurs in Russia", Naturwissenschaften, 96 (4): 495–501, Bibcode:2009NW.....96..495G, doi:10.1007/s00114-008-0499-0, PMID 19089398, retrieved 2019-03-29
- Weishampel, David B.; Dodson, Peter; Osmólska, Halszka (2004), The Dinosauria, 2nd edition, Berkeley: University of California Press, pp. 1–880, ISBN 0-520-24209-2, retrieved 2019-02-21