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Conodont study of the Crna Rijeka borehole CR-17, positioned in the frontal part of the Durmitor Nappe (Fo~a – Pra~a Paleozoic complex, SE Bosnia and Herzegovina) is presented. The obtained fauna indicates an Early-Middle Devonian age and due to poor preservation an identification at a generic level is possible only. The recovered conodont elements have a high Color Alteration Index (CAI = 6,5–7) indicating a degree of metamorphism correspon ding to a temperature interval from 440 °C to 720 °C.

Devonian conodonts from the Fo~a–Pra~a Paleozoic complex (Durmitor Nappe, southeastern Bosnia and Herzegovina)