Fig.2. A in Palaeoecological significance of coral-encrusting foraminiferan associations: A case-study from the Upper Eocene of northern Italy

Fig.2. A.The portion of the Nago Limestone type section corresponding to the second major cycle.Minor cycles and facies types are also indicated (from Bosellini 1998). B.Model of the uppermost shallowing−upward parasequence showing distribution of facies types along the Nago Limestone shelf−edge.