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This paper presents the first results of a palynological investigation of the   Dinaride Ophiolite Belt - derived olistostrome melange at the northern slope   of Moračka Kapa (Montenegro). The analysis of microfloral association   provided a reconstruction of the Late Jurassic sedimentation conditions and   depositional environment in the Morača Kapa Unit. The samples (8) collected   from the different parts of ophiolite matrix yielded palynomorph assemblages   (fossil spores, pollen grains and dinoflagellates) of the Upper Jurassic   age. The uppermost part of the ophiolite suite on the presented palynomorphs   could also indicate the lowermost Lower Cretaceous. These palynological   results provide a very interesting framework of these widespread, but poorly   stratigraphically understood sediments. The paleoecological results suggest   humid and subtropical conditions in the hinterland

The age of the Dinaride Ophiolite Belt: Derived olistostrome melange at the northern slope of Moracka Kapa (Montenegro)