Karabastau
Description
Source: Wikipédia
The Karabastau Formation (Kazakh: Qarabastaý svıtasy) is a geological formation and lagerstätte in the Karatau Mountains of southern Kazakhstan whose strata date to the Middle to Late Jurassic. It is an important locality for insect fossils that has been studied since the early 20th century, alongside the rarer remains of vertebrates, including pterosaurs, salamanders, lizards and crocodiles.
Découvertes
Source: The Paleobiology Database
Site(s) correspondant(s) à cette formation: 1
Aulie, Mikhailovka, Karatau [PIN Loc. 2585] : ? - ? Publication(s)
La base comprend 6 publication(s).
Source: The Paleobiology Database
- ↑1 2 A. N. Riabinin. 1948. Zametka o letayushchem yashchere iz yury Kara-Tau [Note about a flying reptile from the Jurassic of Kara-Tau]. Trudy Paleontologicheskogo Instituta Akademiy Nauk SSSR 1:86-93
- ↑1 E. N. Kurochkin. 2000. Mesozoic birds of Mongolia and the former USSR. The Age of Dinosaurs in Russia and Mongolia
- ↑1 N. N. Bakhurina and D. M. Unwin. 1995. a survey of pterosaurs from the Jurassic and Cretaceous of the former Soviet Union and Mongolia. Historical Biology 10:197-245 (https://doi.org/10.1080/10292389509380522)
- ↑1 L. A. Nessov. 1984. Data on late Mesozoic turtles from the USSR. Studia Geologica Salamanticensia, vol. especial 1 (Studia Palaeocheloniologica I) 1:215-223
- ↑1 V. S. Bazhanov and V. V. Shevchenko. 1948. Krupnyy dinozavr iz Yury Karatau [Large dinosaur from the Jurassic of Karatau]. Vestnik Akademii Nauk Kazakhskoi SSR 5(43):88-89
- ↑1 A. K. Rozhdestvensky and L. I. Khozatsky. 1967. [Late Mesozoic terrestrial vertebrates from the Asiatic part of the USSR]. [Stratigraphy and Paleontology of the Mesozoic and Paleogene-Neogene continental deposits of the Asiatic part of the USSR]
Galerie d'image
Pas d'image.