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Fig. 5 in Moulladella Jourdanensis (Foury & Moullade, 1966) N. Gen., N. Comb.: Valanginian-Early Late Barremian Larger Benthic Foraminifera From The Northern Neotethyan Margin

Fig. 5 (a–p) Moulladella jourdanensis (Foury & Moullade) n. gen., n. comb.: (a, e) (sub)axial sections, note the densely filled central zone ("secondary deposits") in the upper part of (a). (b, p) tangential sections. (c–d, f–g, i–l, m) oblique sections. (h, n) slightly oblique transverse sections. Note anastomizing pillars in (h). (o) slightly oblique transverse section displaying densely filled central zone. b, beam; col, columella; f, foramen; p, protoconch; pi, pillar, s, septum. Thin-sections: 12562-5 (a), 12563-6 (b), 12564-1 (c), 12563-3 (d), 3779-PdC (e), 12570 (f), 12569-5 (g), 13679 (h), 14099 (i), 14095A (j), 14098-2 (k), 12563-6 (l), 14097 (m), 12562-6 (n), 14734 (o), 14099-2 (p). Location and age: (a-n, p) Dâmbovicioara area, Southern Carpathians, Romania (Early Valanginian); (e) Pădurea Craiului, Apuseni Mountains, Romania (Early Barremian). (o) Jerma River Canyon, Estern Serbia (Early Valanginian).

Fig. 7 in Moulladella Jourdanensis (Foury & Moullade, 1966) N. Gen., N. Comb.: Valanginian-Early Late Barremian Larger Benthic Foraminifera From The Northern Neotethyan Margin

Fig. 7 Benthic foraminifera associated with Moulladella jourdanensis (Foury & Moullade) n. gen., n. comb. from the Dâmbovicioara area, Romania. (a) Coscinoconus campanellus (Arnaud-Vanneau, Boisseau & Darsac), slightly oblique axial section. (b) Coscinoconus cherchiae (Arnaud-Vannaeu, Boisseau & Darsac), axial section. (c) Danubiella gracillima Neagu, subaxal section. (d) Protopeneroplis ultragranulata (Gorbatchik), oblique section. (e, h) Paracoskinolina? pfenderae Canerot & Moullade, axial and slightly oblique transverse sections. (f, g) Montsalevia salevensis (Charollais, Brönnimann & Zaninetti), slightly oblique axial section, and transverse section together with Haplophragmoides joukowsky Charollais, Brönnimann & Zaninetti (axial section) (H). Thin-sections: 14096 (a), 12562 (b), 12569 (c), 13697 (d), 12568- 2 (e), 12563 (f), 12564 (g) and 11867-6 (h). Scale bars 0.3 mm.

Fig. 4 in Moulladella Jourdanensis (Foury & Moullade, 1966) N. Gen., N. Comb.: Valanginian-Early Late Barremian Larger Benthic Foraminifera From The Northern Neotethyan Margin

Fig. 4 Moulladella jourdanensis (Foury & Moullade) n. gen., n. comb. (a, g) Tangential-oblique sections of microspheric specimens exhibiting voluminous initial spire. (b) Axial section of a macrospheric specimen. (c, k) Tangential sections showing alternating chamberlets of the marginal zone connected by oblique foramina. (d) Oblique-tangential section. (e, j, m) Axial sections. (h, l) Oblique sections. (f, i) Juvenile specimens in tangential sections. (n) Oblique section of the initial spire of a macrospheric specimen. b, beam; f, foramen; p, protoconch; pi, pillar, s, septum. Thin-sections: 14729 (a), 12563-5 (b), 14099-2 (c), 12561-2 (d, f), 12558A (e), 42-Irimieş (g), 12562-5 (h), 12563-4 (i), 12563-6 (j), 14098-2 (k), 12563 (l), 12563-2 (m), 12563-4 (n). Location and age: (a) Jerma River Canyon, Eastern Serbia, Early Valanginian; (b–f, h–n) Dâmbovicioara area, Southern Carpathians, Romania (Early Valanginian); (g) Reşiţa-Moldova Nouă zone, Southern Carpathians, Romania (Early Barremian).

Fig. 3 in Moulladella Jourdanensis (Foury & Moullade, 1966) N. Gen., N. Comb.: Valanginian-Early Late Barremian Larger Benthic Foraminifera From The Northern Neotethyan Margin

Fig. 3 Paracoskinolina (Meyendorffina) jourdanensis Foury & Moullade, Barremian of France (a–d); holotype specimen in (a) (from Foury and Moullade, 1966, pl. 1, figs. 2–3, 5–6). e–h Conicopfenderina? balkanica Peybernès, Valanginian of Bulgaria; holotype specimen in (f) (from Peybernès, 2004, pl. 1, figs. 7, 1, 8–9).

Fig. 8 in Moulladella Jourdanensis (Foury & Moullade, 1966) N. Gen., N. Comb.: Valanginian-Early Late Barremian Larger Benthic Foraminifera From The Northern Neotethyan Margin

Fig. 8 Geographic distribution of occurrences of Moulladella jourdanensis (Foury & Moullade) n. gen., n. comb. 1: Organya, Pyrenees, Spain 2: Alpilles, Southern France 3: Provence, Southern France 4: Alpes occidentales and Jura, South- Eastern France and Switzerland 5: Northern Calcareous Alps, Austria 6: Pădurea Craiului, Apuseni Mountains, Romania 7: Reşiţa-Moldova Nouă zone, Southern Carpathians, Romania 8: Vâlcan and Vânturariţa Mountains, Southern Carpathians, Romania 9: Dâmbovicioara zone, Southern Carpathians, Romania 10: Dobrogea, South-East Romania 11: Jerma River canyon, Eastern Serbia 12: Western Bulgaria.

Fig. 2 in Moulladella Jourdanensis (Foury & Moullade, 1966) N. Gen., N. Comb.: Valanginian-Early Late Barremian Larger Benthic Foraminifera From The Northern Neotethyan Margin

Fig. 2 Schematic test reconstruction of Moulladella jourdanensis (Foury & Moullade) n. gen., n. comb. modified from Peybernès (2004, fig. 3, for Conicopfenderina? balkanica). Pseudo-kerioteka refers to the thin section 14731 Jerma river, Serbia (above), and RR4027 Kurilovo, Serbia (scale bar = 0.2 mm).

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.

Fig. 6 in Moulladella Jourdanensis (Foury & Moullade, 1966) N. Gen., N. Comb.: Valanginian-Early Late Barremian Larger Benthic Foraminifera From The Northern Neotethyan Margin

Fig. 6 Moulladella jourdanensis (Foury & Moullade) n. gen., n. comb. (a) Axial section of a megalospheric specimen. (b, f) Subaxial sections. (c–d, g, l) Oblique sections. (e, k, m–n, p) Slightly oblique transverse sections. (h, o) Tangential sections. (i–j) Tangential-oblique sections. Central zone highlighted in grey. b, beam; d,?deuteroconch; f, foramen; is, initial spire; p, proloculus; s, septum. Thin-sections: 14098-4 (a, c), 12568-4 (b), 12562-2 (d), 9-Mandrisag (e), 272-Ciclova (f), 4222- Ilidia (g), M10-Crivina (h), 14729 (i, l), 14734 (j–k), Lo 11 (m–n), 14733 (o). Location and age: (a-d) Dâmbovicioara area, Southern Carpathian, Romania (Early Valanginian); (e-h) Reşiţa-Moldova Nouă zone, Southern Carpathians, Romania (Early Barremian); (i-l, o) Jerma River Canyon, Eastern Serbia (Early Valanginian); (m-n) Losenstein, Northern Calcareous Alps, Austria (Early Barremian, cobbles in Albian-Cenomanian conglomerates).