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Udanoceratops: An Abnormally Large, Hornless Ceratopsian From Late Cretaceous Mongolia.
Velociraptor - The Swift Striker of the Cretaceous
Achillobator Giganticus the Achilles Tendon of the Late Cretaceous Period
Velociraptor - Documentary
Transcription
Description
It was previously known as the Lower Nemegt Beds occurring beneath the Nemegt Formation and above the Djadokhta Formation. It has been suggested that the Djadokhta and Barun Goyot Formations are lower and upper parts, respectively, of the same lithological unit and the boundary between the two does not exist. The stratotype of the Barun Goyot Formation is the Khulsan locality, east of Nemegt. At Nemegt, only the uppermost barungoyotian beds are visible. The Red Beds of Khermeen Tsav are also considered part of the Barun Goyot Formation. It is approximately 110 metres (360 ft) in thickness,[1] and was laid down roughly 72-71 million years ago. Given the new date for the start of the Maastrichtian (72.1 MYA) a basal Maastrichtian age seems probable. The Barun Goyot Formation preserves an environment of sand dunes, created from wind-eroded rocks (aeolian dunes).
^Gradzinski, R.; & Jerzykiewicz, T. (1974). Sedimentation of the Barun Goyot formation. Palaeontologica Polonica, 30, 111-146.
^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
^ abcArbour, V. M.; Currie, P. J.; Badamgarav, D. (2014). "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.
^ abPenkalski, P.; Tumanova, T. (2017). "The cranial morphology and taxonomic status of Tarchia (Dinosauria: Ankylosauridae) from the Upper Cretaceous of Mongolia". Cretaceous Research. 70: 117−127. Bibcode:2017CrRes..70..117P. doi:10.1016/j.cretres.2016.10.004.
^K. Mikhailov, K. Sabath, and S. Kurzanov. (1994). Eggs and nests from the Cretaceous of Mongolia. In K. Carpenter, K. F. Hirsch, and J. R. Horner (eds.), Dinosaur Eggs and Babies, Cambridge University Press, Cambridge 88-115.
^Kurzanov, S. and Bannikov, A. (1983). "A new sauropod from the Upper Cretaceous of Mongolia". Paleontologicheskii Zhurnal 2: 90–96.
^Alifanov, V. R.; Barsbold, R. (2009). Ceratonykus oculatus gen. et sp. nov., a new dinosaur (? Theropoda, Alvarezsauria) from the Late Cretaceous of Mongolia. Paleontological Journal 43 (1): 94−106.
^Alifanov, V. R.; Saveliev, S. V. (2011). Brain structure and neurobiology of alvarezsaurians (Dinosauria), exemplified by Ceratonykus oculatus (Parvicursoridae) from the Late Cretaceous of Mongolia. Paleontological Journal. 45 (2), 183−190.
^Karhu, A. A.; Rautian, A. S. (1996). A new family of Maniraptora (Dinosauria: Saurischia) from the Late Cretaceous of Mongolia. Paleontological Journal. 30, 583−592.
^ abcKurochkin, E. N.; Chatterjee, S.; Mikhailov, K. E. (2013). An embryonic enantiornithine bird and associated eggs from the cretaceous of Mongolia. Paleontol. J. 47, 1252–1269.
^Elzanowski, A. (1977). Skulls of Gobipteryx (Aves) from the Upper Cretaceous of Mongolia. Results of the Polish-Mongolian Paleontological Expeditions - Part VII. Palaeontologica Polonica. 37, 153-165.
^Elzanowski, A. (1995). Cretaceous birds and avian phylogeny. Cour. Forschungsinst. Senckenb. 181, 37-53.
^Kurochkin, E. N. (2004). The truth about Gobipteryx. Sixth International Meeting of the Society of Avian Paleontology and Evolution. Abstracts. 33-34.
^Bell, A.K., Chiappe, L.M., Suzuki, S., Watabe, M. (2008). "Phylogenetic and morphometric analysis of a new ornithuromorph from the Barun Goyot Formation, Southern Mongolia." Abstracts of the 7th International Meeting of the Society of Avian Paleontology and Evolution.1.
^Bell, A.K., Chiappe, L.M., Erickson, G.M., Suzuki, S., Watabe, M., Barsbold, R. and Tsogtbaatar, K. (2010). "Description and ecologic analysis of Hollanda luceria, a Late Cretaceous bird from the Gobi Desert (Mongolia)." Cretaceous Research, 31(1): 16-26. doi:10.1016/j.cretres.2009.09.001
^Weishampel, D. B.; Barrett, P. M.; Coria, R. A.; Loeuff, J. L.; Xing, X.; Xijin, Z.; Sahni, A.; Gomani, E. M. P. (2004). "Dinosaur Distribution". In Weishampel, D. B.; Dodson, P.; Osmolska, H. (eds.). The Dinosauria (2nd ed.). University of California Press. pp. 596−598. ISBN0520242092.
^Kundrat, M. (2007). Avian-like attributes of a virtual brain model of the oviraptorid theropod Conchoraptor gracilis. Naturwissenschaften. 94: 499−504.
^Kundrat, M.; Janacek, J. (2007). Cranial pneumatization and auditory perceptions of the oviraptorid dinosaur Conchoraptor gracilis (Theropoda, Maniraptora) from the Late Cretaceous of Mongolia. Naturwissenschaften. 94(9): 769−778.
^ abFunston, G. F.; Mendonca, S. E.; Currie, P. J.; Barsbold, R.; Barsbold, R. (2018). "Oviraptorosaur anatomy, diversity and ecology in the Nemegt Basin". Palaeogeography, Palaeoclimatology, Palaeoecology. 494: 101−120. Bibcode:2018PPP...494..101F. doi:10.1016/j.palaeo.2017.10.023.
^ abFunston, G. F. (2019). "Chapter 4 – Oviraptoridae"(PDF). Anatomy, systematics, and evolution of Oviraptorosauria (Dinosauria, Theropoda) (PhD thesis). University of Alberta.