Tamara I. Nemyrovska
Abstract
The study of Ukrainian Paleozoic conodonts began in the 1960s in western Ukraine, when Danylo Drygant (State Museum of
Natural History, L’viv) started to investigate the Silurian and Devonian conodonts of the Podolian and Volhynian sections. The
Carboniferous conodonts of the Donets Basin, Dnieper-Donets Depression and L’viv-Volhyn Basin began to be studied in the
early 1970s by four students of Prof. Dr. David Ye. Aisenverg: Oleg Ye. Kotlyar, Oleg M. Lipnyagov, Raisa I. Kozitska and
Tamara I. Nemyrovska (Institute of Geological Sciences NASU). Carboniferous conodonts from the boreholes of the southwestern
part of the Donets Basin were studied by Zoya A. Kossenko from “Artemgeology” in the town of Artemovsk, now
Bakhmut. During their investigations a great number of new Carboniferous genera and species were described and the
Carboniferous conodont zonation of the Donets Basin was constructed. In addition, Carboniferous conodonts from different
areas of Europe and Asia were studied to provide reliable correlation to the Donets Basin, resulting in publication of many
pertinent taxonomic and biostratigraphic papers. Several conodont species established in the Donets Basin were proposed
as markers for the global Bashkirian/Moscovian and Moscovian/Kasimovian boundaries. A significant extinction of Early
Carboniferous conodonts was defined for the first time in Eastern Europe at the Mississippian–Pennsylvanian boundary in
the Kal’miuss section of the Donets Basin. It was one of the first sections proposed as a candidate for the Mid-Carboniferous
boundary GSSP.
Keywords
conodonts; Silurian; Carboniferous; stratigraphy; zonal scheme; correlation
Full Text

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Tamara I. Nemyrovska