Paleobiogeographic relationships of Devonian provinces of the Pacific Rim (on the example of tetracorals)
Authors:
Abstract
Almost throughout the Devonian, there were marine basins around the Pacific Ocean that belonged mainly to geosynclines. Caledonian folding, which occurred in the second half of the Silurian in the Paleozoic geosynclines, led to the formation of young mountain chains and island archipelagos that disconnected the continental seas.
Область исследования:
(Archived) Without section
Funding:
None
References
- Dubatolov V. N., Spassky N. Ya. Corals of the main Devonian paleobiogeographic provinces. Laws of distribution of Paleozoic corals of the USSR. Tr. II Vsesoyuznogo simpoziuma po izucheniyu iskopaemykh korallov, iss. 3. Nauka, 1970. (in Russian)
- Strakhov N. M. Fundamentals of the Theory of Lithogenesis. Vol. III, AN SSSR, 1962. (in Russian)
- Oliver W. A. Succession of Rugose Coral Faunas in the Lower and Middle Devonian of Eastern North America. Intern. Symposium on the Devonian System. Alberta, 1968.
Similar articles
On the two-member division of the Asselian Stage in the Mezen River basin based on the study of fusulinids
1972 I. A. Alekseeva, A. N. Polozova
On the distribution of pelecypods in the Carboniferous sediments of the Kalba Range and Southern Altai
1972 A. Kh. Kagarmanov
Stratigraphic distribution of brachiopods in the Artinskian Stage of the western slope of the Middle Urals
1972 E. N. Mikhailova
Boundary deposits of the Ordovician and Silurian systems of the Altai-Sayan folded region
1972 E. V. Vladimirskaya, V. D. Chekhovich, A. V. Krivobodrova