Faunistic Substantiation of Stratigraphic Occurrence of the Pleuromeia (Isoëtopsida) Plant in the Triassic of Gorny Mangyshlak, Republic of Kazakhstan

Stratigraphy and Geological Correlation - Tập 26 - Trang 283-297 - 2018
V. A. Gavrilova1, N. S. Snigirevskaya2
1Karpinskii Russian Geological Research Institute, St. Petersburg, Russia
2Komarov Botanical Institute, Russian Academy of Sciences, St. Petersburg, Russia

Tóm tắt

Joint burial places of mollusks and Pleuromeia plants allow specification of a period of stratigraphic occurrence of this genus in the west of the Republic of Kazakhstan within the Gorny Mangyshlak. Two places of occurrences of pleuromeias were found in marine Triassic rocks: one in the Karadzhatyk Formation of the northern slope of the Karatauchik Range close to the Dolnapa well, where the fossils of Pleuromeia sternbergii (Münster) Corda plants are associated with ammonoid shells, and the other one in the Karaduan Formation of the southern slope of Mt. Karashek, where this plant was found along with bivalves and gastropods. The mollusk fauna from both occurrences indicates that the Mangyshlak pleuromeias occurred from the late Olenekian Substage to Anisian Stage.

Tài liệu tham khảo

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