primary transverse partitions, shorter transverse partitions, and moderately developed
parallel partitions. The new species was found in shallow water limestone of the Island of
Brač: in the highest levels of the Gornji Humac Formation (Upper Santonian-Lower
Campanian) and also in the Pučišća Formation (Rasotica and Lovrečina Units; Lower-
Middle Campanian). It occurs frequently in foraminiferal-peloidal packstone and …