Hijatus između sarmata i panona u oblasti Donje Trnove (SI Bosna)
A hiatus between Sarmatian and PAnnonian in Donja Trnova area, NE Bosnia
Abstract
Of a sea regression in the early Pannonian age was known earlier from the southem Pannonian margin. Micropaleontological analysis of the association fossil foraminifers and ostracods indicated a break in sedimentation between the Lower Sarmatian and Upper Pannonian. Complete Lower Pannonian and basal Upper Pannonian are missing. Besides microfauna, malacofauna also was used in the stratigraphical interpretations.
This contribution is tlie partly amended paper submitted under the same title to the 12th Intemational Symposium on Ostracods (Prague. 1994).
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