Fig. 4 in A new vent-related foraminifer from the lower Toarcian black claystone of the Tatra Mountains, Poland

Fig. 4. Variability of ammosphaeroidinid foraminifer Recurvoides infernus sp. nov., Huciański Klin, Tatra Mts., Toarcian. A. Paratype, UJ 213 P2 (see Fig. 5J for rollogram), sample 3236 (4.8b/1m), in pseudospiral (A1), peripheral (A2), and side (A3) views. B. Paratype, UJ 213 P3 (see Fig. 5B for rollogram), sample 3213 (4.8b/16m), in pseudospiral (B1), peripheral (B2), and side (B3) views. C. Paratype, UJ 213 P4 (see Fig. 5U for rollogram), sample 3237 (4.8a/7.5m), in pseudospiral (C1), peripheral (C2), and side (C3) views. D. Test infilled with pyrite, sample 3236 (4.8b/1m), in pseudospiral (D1–D4), peripheral (D5), and apertural (D6) views; D1, dry specimen in reflected light; D2, wet in reflected light; D3, wet in transmitted light; D4–D6 SEM photographs. E. Strongly compressed specimen, sample 3236 (4.8b/1m), in side (E1, E3) and peripheral (E2) views; E1, specimen in reflected light; E2, E3 SEM photographs.