Fig. 2 in Emergence and extinction of the Givetian to Frasnian bryozoan faunas in the Kostomłoty facies zone, Holy Cross Mountains, Poland

Fig. 2. Position of the bryozoan−bearing sections under study (see Fig. 1B) against developmental stages of the Middle to Late Devonian bank−to−reef complex of the Holy Cross Mountains; stratigraphic−facies cross−section (after Racki 1993: fig. 3, changed) is shown to emphasise eustatic rhythmic control of the depositional pattern and main bryzozoan immigrational events in the Kostomłoty basin (asterisked); Ic–IId, transgressive−regressive cycles modified from Johnson et al. (1985); GC, Góra Cmentarna; GŁ, Góra Łgawa; M, Marzysz; P, Posłowice; GZ, Góra Zamkowa; SG, Sowie Górki; JB, Jurkowice−Budy; Sk, Skały; K, Kostomłoty (eastern hill).