Szabó János szerk.: Fragmenta Mineralogica Et Palaentologica 26. 2008. (Budapest, 2008)

Shape — Dextral form with gradate spire. Whorlsection nearly pentagonal. Narrow ramp below suture, being bordered by rounded angulation abapically. Outer face feebly concave in it middle. Peripher}

7 rounded angular. Rather wide selenizone in deepest part of depression of outer face. Base flattened, and moderately phaneromphalous with rounded angular umbilical rim. Peristome unknown. Sculpture — Both whorls and base covered by network of rather evenly spaced spiral and transverse cords. One of these spiral cords divides selenizone into two parts. Growth-lines extremely fine and prosocline above selenizone, prosocyrt between selenizone and periphery, and opisthocyrt on base but becoming prosocline again at umbilical rim. Continuous course of collabral sculpture elements disrupted only by selenizone, bearing lunulae of same strength as cords. Remarks — The a\

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ailable specimens are well identifiable with GEMMELLARO's (1874) description. Most similar species is Anodomaria trochotomopsis (G. G. GEMMELLARO, 1874), having wider spire angle, and different other measurements; no concavity is on its shell surface Distribution — Western Sicily: "Terebratula Aspasia Zone" (Pliensbachian); Bakony Mts: Lókút, Kericser: Davoei to Stokesi Zones; Tés, Hamuháza: Stokesi Zone. Figure 31 —Anodomaria scacchi (GEMMELLARO, G. G., 1874) — A-B: "apertural" and basal views of the best preserved specimen from Lókút, Kericser (Bakony Mts), xl; C-D: magnified varieties of the same views to show the details of the sculpture, x3. Family Pleurotomariidae SWAINSON, 1840 Genus Pleurotomaria DEFRANCE, 1826 Type species: Trochus anglicus SOWERBY, 1818 Pleurotomaria eplenyensis n. sp. (Figure 32) 1980: Pleurotomaria (Pleurotomaria) anglica (Sow.) — SZABÓ, p. 57, pi. 2, fig. 5. Holotype — HGM J.08.

10.1. (Figure 32: A-F). Type locality — Eplény (Mn-ore mine), Bakony Mts. Type strata — Upper Pliensbachian massive, red, micritic limestone with accumulation of shells that frequently have Fe-Mn-oxide coating, found as fissure-filling in Upper Triassic to lowermost Jurassic platform limestone (Dachstein Limestone and Kardosrét Limestone Formations). Name — From the village next to the locality. Diagnosis — Medium high, gradate shell with strongly rounded angulation on whorls and at peripher}

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; rather sparse ridges de\

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eloped both at ramp angle and at periphery; juvenile ramp ridges have opisthocline-opisthocyrt shape (crossing growth-lines) and extend to upper suture; ridges confined to abaxial part of ramp on last whorl; ornament consists of spiral cords of different strength on whorls and base, growth-lines cross them and subregularly repeating collabral threads visible on ramp in subsutural belt. Material — Two damaged specimens, one strongly fragmentary (HGM). Measurements H HL HP D W AA AL holotype **42 *30 *22 *47 - 88° 88° Shape — Rather large shell with moderately high, gradate spire. Whorls having narrow, slighdy convex ramp of low slope, abaxially bordered by strongly rounded (obscure) angulation. Outer face markedly oblique to axis, slighdy convex, bearing flattened selenizone on its middle. Base flattened-convex, narrowly phaneromphalous. Outer lip conspicuously prosocline above selenizone. Inner lip, as rather large callus, overlaps partially base and umbilicus