Authors

  • Kushakov Abdulla Romanovich
    Candidate of Geological and Mineralogical Sciences, Professor, Head of the Department of Geology, Faculty of Geology and Geoinformation Systems of National University of Uzbekistan (NUUz)
  • KurbanovaMohigulMamasaliyevna
    Lecturer, Department of Geology, Faculty of Geology and Geoinformation Systems of National University of Uzbekistan (NUUz)
  • MusaevaNigoraAbrarovna
    Lecturer, Department of Geology, Faculty of Geology and Geoinformation Systems of National University of Uzbekistan (NUUz)
  • AripovaMavjudaKarimjonovna
    Lecturer, Department of Geology, Faculty of Geology and Geoinformation Systems of National University of Uzbekistan (NUUz)
  • BoboyorovHusniddinAkromovich
    Lecturer, Department of Geology, Faculty of Geology and Geoinformation Systems of National University of Uzbekistan (NUUz)

DOI:

https://doi.org/10.37547/tajet/Volume04Issue03-02

Keywords:

Suite, nannoplankton, foraminifera, oyster, Kyzyltakyr,

Abstract

This research paper is the result of a study of the subdivisionofPaleogene sediments by foraminifera, bivalves and nannoplankton of the Central Kyzylkums. The relevance of these works is explained by the fact that the Paleogene sediments due to poverty of their faunal remains did not have sufficient paleontological substantiation. The need for stratigraphic subdivisionof the Paleogene sediments of the Central Kyzylkums is dictated by the fact that the current state of validity of their subdivisionand correlation does not provide the necessary accuracy with the International Stratigraphic Scale.