Lower Famennian conodont-based stratigraphy of the Pripyat Trough

T. V. Strel’chenko1, S. A. Kruchek2
1Belarus Research Geological-Prospecting Institute (BelNIGRI), Minsk, Belarus
2Institute of Geochemistry and Geophysics, National Academy of Sciences, Minsk, Belarus

Tóm tắt

Three conodont assemblages characterizing the standard triangularis, crepida, and rhomboidea zones can be defined in lower Famennian sections of the Pripyat Trough. The defined local conodont units include the Icriodus iowaensis, Palmatolepis wolskae-Palmatolepis circularis, Palmatolepis klapperi-Polygnathus semicostatus, Icriodus divergentus, and Palmatolepis subperlobata helmsi beds. The defined conodont assemblages are correlated with their coeval standard counterparts of the East European Platform. New conodont species and subspecies are described: Palmatolepis klapperi biparapetus, Polygnathus barskovi, Po. chegodaevi, Po. semeni, Po. inaequilateralis, Polynodosus nodocostatus productus, Icriodus divergentus, I. pushkini.

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