Fig. 1 in Moulladella Jourdanensis (Foury & Moullade, 1966) N. Gen., N. Comb.: Valanginian-Early Late Barremian Larger Benthic Foraminifera From The Northern Neotethyan Margin

Fig. 1 Location of the studied sections on the Romanian (A) and Serbian (B) territory showing the occurrence intervals (red lines) of Moulladella jourdanensis (Foury & Moullade) n. gen., nov. comb. A1 – location of the two studied sections in Romania; 1, Reşiţa-Moldova Nouă zone; 2, Dâmbovicioara zone, A2 – Succession of the Lower Cretaceous deposits from the Reşiţa- Moldova Nouă zone (modified from Bucur, 1997): 1, conglomerates and sandstones; 2, alternating sandstones and shales; 3, bedded bioclastic limestones; 4, massive bioclastic limestones; 5, chert-bearing limestones; 6, marly-limestones and marls; 7, micritic limestones; 8, micritic limestones with chert intercalations. A3 – Succession of the Lower Cretaceous deposits from Dâmbovicioara zone (modified from Bucur et al., 2011): 1, alternating marls and limestones; 2, marls with patch-reef limestone intercalations; 3, marly-limestones and marls; 4, glauconite-bearing limestones; 5, bedded limestones; CNM = Cetatea Neamţului Member. B1 – Location of the studied section in Serbia. JRA = Jerma River Area. B2 – Succession of the Lower Cretaceous deposits from the Jerma River Canyon (modified from Bucur et al., 1995): 1, conglomerates, sandstones and shales; 2, bedded limestones.