Abstract
The Upper Cretaceous of the Umbria-Marche Basin (Italy) consists of an alternation of calcareous and siliceous
fine-grained sedimentary rocks in which the calcareous lithologies are predominant. The Cenomanian
succession is dominated by white, micritic limestones and contains a black shale horizon (Bonarelli Level) in
its uppermost part which is the regional expression of
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