The original description of Vidalina martana by Farinacci (1959) is not valid, firstly because no type specimen was determined and, secondly, because the proposed reconstruction of the species
does not match the specimens illustrated. Furthermore, Farinacci’s (1959) material is probably polyspecific and even polygeneric (see also Wernli, 1972).
Gale, L. (2012). Rhaetian foraminiferal assemblage from the Dachstein Limestone of Mt. Begunjščica (Košuta Unit, eastern Southern Alps). Geologija. 55(1): 17-44.