Road of Winds Across the Mongolian Plains
- Autores: Zhuravlev A.Y.1,2
-
Afiliações:
- Lomonosov Moscow State University
- Borissiak Paleontological institute, Russian Academy of Sciences
- Edição: Nº 11 (2023)
- Páginas: 26-38
- Seção: Articles
- URL: https://journals.eco-vector.com/0032-874X/article/view/627861
- DOI: https://doi.org/10.7868/S0032874X23110030
- ID: 627861
Citar
Texto integral
Acesso aberto
Acesso está concedido
Acesso é pago ou somente para assinantes
Resumo
Ancient Mongolia is imaged as a country of dinosaurs and other Mesozoic fauna and flora. However already joint Soviet-Mongolian expeditions of the last century have revealed even more interesting palaeontological remains and sedimentological features in the Precambrian and Palaeozoic strata of this country, important for the understanding of the development of the entire Earth. Nowadays, numerous international expeditions are especially interested in the period of 1000–500 Ma that covers a blustery diversification of unicellular eukaryotes, global glaciations, one of the main stage of the phosphate accumulation process, and an establishment of animals with mineral skeletons. More than that, Mongolia of that time was represented not by a single marine basin but rather a number of seas associated with various microcontinents and volcanic arcs, which provides an opportunity to conceive the differences in the succession of these events under different conditions.
Palavras-chave
Sobre autores
A. Zhuravlev
Lomonosov Moscow State University; Borissiak Paleontological institute, Russian Academy of Sciences
Email: ayzhur@mail.ru
Moscow, Russia; Moscow, Russia
Bibliografia
- Ефремов И. А. Дорога ветров (Гобийские заметки). М., 1962.
- Andrews R. C. Across Mongolian Plains. A Naturalist’s Account of China’s «Great Northwest». New-York; London, 1921.
- Коробов М. Н. Биостратиграфия и полимерные трилобиты нижнего кембрия Монголии. М., 1989. (Труды Совместной Советско-Монгольской научно-исследовательской геологической экспедиции АН СССР. Т. 48).
- Дроздова Н. А. Водоросли в органогенных постройках нижнего кембрия Западной Монголии. М., 1980. (Труды Совместной Советско-Монгольской палеонтологической экспедиции АН СССР. Т. 10).
- Воронин Ю. И., Воронова Л. Г., Григорьева Н. В. и др. Граница докембрия и кембрия в геосинклинальных областях (опорный разрез Саланы-Гол, МНР). М., 1982. (Труды Совместной Советско-Монгольской палеонтологической экспедиции АН СССР. Т. 18).
- Hood A. v. S., Wallace M. W. Neoproterozoic marine carbonates and their paleoceanographic significance. Global and Planetary Change. 2018; 160: 28–45. doi: 10.1016/j.gloplacha.2017.11.006.
- Wood R. A., Zhuravlev A. Yu., Sukhov S. S. et al. Demise of Ediacaran dolomitic seas marks widespread biomineralization on the Siberian Platform. Geology. 2017; 45(1): 27–30. doi: 10.1130/G38367.1.
- Sun Z., Yang A., Zhao F., Zhuravlev A. Yu. et al. New trilobite assemblage from the lower Cambrian (upper Stage 4) of the Lake Zone, western Mongolia. Journal of Paleontology. 2023; 97(3): 577–590. doi: 10.1017/jpa.2023.23.
- Zhuravlev A. Yu., Wood R. A., Bowyer F. T. Cambrian radiation speciation events driven by sea level and redoxcline changes on the Siberian Craton. Science Advances. 2023; 9: eadh2558. doi: 10.1126/sciadv.adh2558.
Arquivos suplementares
