Year: 2018
Pages: 111-118
UDC: 551.736.1: 563.12: 470.57
Number: 1
Type: scientific article
DOI: http://doi.org/10.31084/2619-0087/2018-1-10
Topic: ARTICLES AND PUBLICATIONS
Authors: Isakova, Tatiana N., Filimonova, Tatiana V., Kulagina, Elena I.
The results of the study of distribution of foraminifers in the Mechetlino section, a potential candidate for the stratotype of the lower boundary of the Kungurian stage of the Cisuralian Series (Lower Permian) are presented. 20 samples were selected in 2015–2016 years. Specific complexes of fusulinides and smaller foraminifers were obtained at 17 levels of the section. Foraminifers were found only on three levels before these studies. The most representative complex of fusulinides is determined from the lower part of the section in layers 3–6. This assemblage is characteristic for the Sargian horizon of the Urals. The morphologically similar group of Pseudofusulina urasbajevi and Uralofusulinella arkaulensis group are located in this interval of the section. The single shells of fusulinides or fragment of shells are found in the layers 8, 10, 14 and 15. Smaller foraminifers are found on 17 levels and are represented by 59 species of 22 genera. The first foraminiferal complex belong to the Sargian horizon, the second — to the Saranian, the third has a more general Kungurian image. Markers of the Saranian horizon of the Kungurian among smaller foraminifers are determined above the assumed boundary. It is shown that the stratigraphic potential of foraminifers makes it possible to use this group of microfauna for a detailed subdivision of the Mechetlino section and interregional correlation of deposits.
Permian system, Kungurian stage, International Stratigraphic Scale, fusulinides, smaller foraminifers