Santonian Radiolarians and Foraminifers from Brežđe Section, Western Serbia
- Authors: Bragina L.G.1, Bragin N.Y.1, Kopaevich L.F.2, Beniamovsky V.N.1
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Affiliations:
- Geological Institute
- Department of Geology
- Issue: Vol 73, No 4 (2018)
- Pages: 333-345
- Section: Article
- URL: https://journals.rcsi.science/0145-8752/article/view/174763
- DOI: https://doi.org/10.3103/S014587521804004X
- ID: 174763
Cite item
Abstract
New data on the radiolarians and foraminifers (planktonic and benthic) from the lower part of Struganik limestones (Brežđe Section, Western Serbia) are presented. The Afens perapediensis Zone of a new detailed scale based on radiolarians for the Tethyan supra-region was traced for the first time. This allowed classification of the studied deposits to a narrow stratigraphic interval, that is, the upper Santonian. The age of the studied sediments is determined in the Santonian for planktonic foraminifera because of the joint presence of abundant Marginotruncana (extinct in the latest Santonian) and Globotruncana linneiana (d’Orbigny) (which appeared in the early Santonian). The radiolarian and planktonic and benthic foraminifera data agree with one another.
About the authors
L. G. Bragina
Geological Institute
Author for correspondence.
Email: l.g.bragina@mail.ru
Russian Federation, Moscow, 119017
N. Yu. Bragin
Geological Institute
Email: l.g.bragina@mail.ru
Russian Federation, Moscow, 119017
L. F. Kopaevich
Department of Geology
Email: l.g.bragina@mail.ru
Russian Federation, Moscow, 119991
V. N. Beniamovsky
Geological Institute
Email: l.g.bragina@mail.ru
Russian Federation, Moscow, 119017