Szabó János szerk.: Fragmenta Mineralogica Et Palaentologica 26. 2008. (Budapest, 2008)
1980. Beside these, the network ornament of GEMMELLARO's two species fully covers the base. Anodomaria latigradata JAITLY, SZABÓ & FÜRSICH, 2000 has similar spiral angle but its whorls are considerably higher, Anodomaria depressa J APTLY, SZABÓ & FÜRSICH, 2000 has much wider spire angle, fewer and lower whorls. Distribution — Hierlatz Alpe, Hallstatt, Sinemurian (Oxynotum Zone). Anodomaria anodosa (SZABÓ, 1980) (Figure 30) 1980: Pleurotomaria (Anodomaria) anodosa sp. n. — SZABÓ, p. 59, PI. 2, figs 8—9. 2003: Anodomaria anodosa SZABÓ, 1980 — SZABÓ in VÖRÖS et al., p. 61, pl. 5: 1. Material — Three fragmentary 7 specimens; holotype: HGM J 9597; figured juvenile shell: GBa 2008/69/49. Measurements H HL HP D W AA AL holotype **40 **14 **31 **16 **70° **70° Shape — Moderately high shell, having gradate spire with distinct spiral angulations. Ramp flattened, its abaxial border running slighdy above midwhorl, and sharply angular; carina makes it more conspicuous. Outer face flattened on earlier shell parts, but feebly concave on subsequent whorls. Sharp angulation, bearing also carina, separates it from base, being slightly convex and moderately phaneromphalous. Rather wide, flat selenizone courses slightly above middle of outer face. Sculpture — Juvenile whorls have marked network ornament with collabral elements, being more prominent than spiral ones. Post-juvenile whorls, as well as base covered only by spiral cords. Similar cords appear also on selenizone, and on carinae of angulations. Density of growth-lines changing, that may result in weak ridges, more or less periodically along upper suture. These ridges fade out rapidly away from suture. Remarks — In the studied material, Anodomaria anodosa most closely resembles in shape to Worthenia superstes SZABÓ, 1980. However, the position of the selenizone clearly distinguishes these two forms. The same feature marks out this species from all Bathrotomaria. With its different dimensions and dominandy longitudinal adult ornament, it is distinguishable from Anodomaria scacchi G. G. GEMMELLARO, 1874 and Anodomaria trochotomopsis G. G. GEMMELLARO, 1874 of cancellate sculpture. Some stratigraphically younger species were found also in the Kachchh (western India) Jurassic; they have different shape and rounded angulations. Anodomaria stojaspali SZABÓ, 2008 has low T er whorls with network ornament and less prominent angulations. With its sharp and carinate angulations, A. anodosa remains a morphologically unique member of Anodomaria. The holotype damaged in an accident of collection works (cleaning); the earliest whorls lost. In Figure 30: C—D, images of a young specimen from the Schafberg demonstrate the early shape and ornament. Distribution — Eplény manganese ore mine (Bakony Mts): Late Pliensbachian; Schafberg, Upper Pliensbachian. Figure 30 — Anodomaria anodosa SZABÓ, 1980 — A: copy of the original figure, showing the holotype, still having also juvenile part, xl; B: holotype in present state (after an accidental damage), x2; C—D: two views of a juvenile specimen from Schafberg to demonstrate the early shape and ornament; the midwhorl and peripheral keels have already appeared in early juvenile stage (roughly on the 3 rd whorl); X3. Anodomaria scacchi (G. G. GEMMELLARO, 1874) (Figure 31) 1874: Pleurotomaria scacchi GEMM. — GEMMELLARO, G. G., p. 92, pi. 12, fig. 18. 1980: Pleurotomaria (Anodomaria) scacchi GEMM. — SZABÓ, p. 58, pi. 2, figs 6-7. Material — Two (+ one?) specimens (HGM). Measurements H HL HP D W AA AL Figure 31: A-D 12.5 8.5 15.5 52° 52°
