Fig. 14. A in Conodont ecology in the Early-Middle Frasnian transition on the South Polish carbonate shelf

Fig. 14. A synthesis of main conodont events against other biotic and tectonic events, carbon isotopic curve and sea−level changes. Note a response of relative conodonts size to variation in δ13C curve. The essential biofacies turnovers, a sequence of conodont crisis and recovery episodes correlate positively with sea−level and productivity fluctuation.