FORAMINIFERA OF THE PALEOGENE AND NEOGENE OF THE AUMINZATAU MOUNTAINS (CENTRAL KYZYLKUM)

Authors

Musaeva Nigora Abrarovna State Unitary Enterprise "Regionalgeology", head of the detachment, Uzbekistan, Tashkent

Keywords:

foraminifera, Kultaban, Sarbatir, Agitmina

Abstract

This article is the result of a study of Paleogene and Neogene boundary deposits based on the foraminifers of the Auminzatau Mountains. The urgency of setting these works was due to the fact that the Oligocene-Early Miocene sediments due to the paucity of faunal remains in them, did not have sufficient paleontological substantiation. The paleontological material collected and studied by the author of the article made it possible to determine the boundary between the Paleogene and Neogene based on foraminifers. The need to subdivide the Oligocene-Early Miocene deposits on the territory of the Auminzatau Mountains (Central Kyzylkum) is dictated by the fact that the current state of the validity of their subdivision and correlation does not provide the necessary accuracy of comparison with the International Stratigraphic Scale

References

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Bugrova E.M., Gladkova V.I., Dmitrieva T.V., Nevzorova L.S., Pinchuk T.V., Podobina V.M., Tverskaya L.A., Fregatova N.A. (2005). Practical guide on microfauna. Vol 8. Cenozoic foraminifera. St. Petersburg. VSEGEI printing house, 315.

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Musaeva.N.A, Kushakov A.R Border of paleogen and neogen by foraminifera of Auminzatau foothills (Central Kyzylkum) // Journal of Critical Reviews., v. 7, Issue 6, 2020, p.. 459-465.

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Published

2022-12-20

How to Cite

Musaeva Nigora Abrarovna. (2022). FORAMINIFERA OF THE PALEOGENE AND NEOGENE OF THE AUMINZATAU MOUNTAINS (CENTRAL KYZYLKUM). European Journal of Agricultural and Rural Education, 3(12), 58-66. Retrieved from https://scholarzest.com/index.php/ejare/article/view/3051