The Albian–Cenomanian Kotroman Formation of Mokra
2008-12-30u2002·u2002in Fig. 2). The type section is at the Uro{evi}i hamlet (43°46'1.44'' N, 19°28'7.11'' E). Nodules of floatstone and wackestone are enclosed in an intimate mixture of clay and carbonate. Extremely small crystals of quartz, pyrite and hematite can be found in the clayey matrix. The microfauna assemblage consists of codiacean frag-
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