To refer to this article use this url: http://dpc.uba.uva.nl/ctz/vol72/nr02/art06
Abstract
At Monte Magrè a series of calcarenites of Ypresian and Lutetian age is exposed. The anomuran faunas were collected from the lower strata in this succession, along the road from Monte Magrè to Monte di Malo. These levels, indurated and white in color, contain nummulitid foraminifera, nodules and fragments of coralligenous algae, and moulds of corals, molluscs and other decapod crustaceans (e.g. Cyamocarcinus angustifrons Bittner, 1883).