Fig. 11 in Faunal dynamics across the Silurian-Devonian positive isotope excursions (δ C, δ O) in Podolia, Ukraine: Comparative analysis of the Ireviken and Klonk events

Fig. 11. Lowermost Wenlock lithologic and faunal succession at Kytayhorod, against the key brachiopod assemblages (see Fig. 10) and a representative micritic microfacies of the Restiv Beds, i.e., bioturbated skeletal wackestone to packstone with shelly bioclasts, crinoids, and trilobites (compare Fig. 5). Note onset of the carbon isotope excursion (ESCIE) before the ending of Ireviken Event.