Conodonts and ostracodes from the late Tournaisian bathyal sequence of the Polar Urals
Early Carboniferous (late Tournaisian) conodonts, recovered from siliceous shales and silicites of the Nyan- Vorga Formation within the Lemva tectonic belt of the Polar Urals (Russia), include the biostratigraphically important taxa Siphonodella lanei, Gnathodus typicus, Dollymae hassi, and Scaliogn...
Main Authors: | , |
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Format: | Article |
Language: | English |
Published: |
Sciendo
2018-06-01
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Series: | Contemporary Trends in Geoscience |
Subjects: | |
Online Access: | http://www.degruyter.com/view/j/ctg.2018.7.issue-1/ctg-2018-0003/ctg-2018-0003.xml?format=INT |