Abstract
The succession of five formations (Auleliai, ViluÄiai, Alvitas, Å akiai, JakÅ¡iai) corresponding to the upper Sandbian and lower Katian in southern Lithuania is dated based on new bio- and chemostratigraphical data from the Pajevonys-13 core section. The dating of the Auleliai and ViluÄiai formations is controversial: chitinozoans suggest younger ages (Keila and Oandu) than brachiopods (Haljala and Keila) for this interval. Chemostratigraphical data (δ13Ccarb and δ13Cbrach) agree better with the dating based on brachiopods: the Alvitas and Å akiai formations correspond to the Oandu Stage, the older ViluÄiai Formation is of Keila age. The JakÅ¡iai Formation is commonly dated as of Rakvere age, but it is problematic in the studied section. However, its upper boundary is well defined by the appearance of subzonal chitinozoans Armoricochitina reticulifera characteristic of the lowermost Nabala Stage. The Ancyrochitina bornholmensis and Fungochitina spinifera chitinozoan zones, and the upper Amorphognathus tvaerensis, A. superbus and the lowermost A. ordovicicus conodont zones were identified in the studied section.
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CITATION STYLE
Hints, L., Paškevičius, J., Martma, T., Männik, P., & Nõlvak, J. (2016). Upper Sandbian–lower Katian bio- and chemostratigraphy in the Pajevonys-13 core section, Lithuania; pp. 85–97. Estonian Journal of Earth Sciences, 65(2), 85–97. https://doi.org/10.3176/earth.2016.08
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