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

of Wortheniopsis (Sisenna) Jancsii n. sp. demonstrate a rather high morphological stability on the species level (see Figure 25). Two strongly different specimens are saved in STO­LICZKA's (1861) original collection under the name "Pleu­rotomaria foveolatd\ One has been found also in the Bakony Alts but both are unknown in the "stable" European faunas [Wortheniopsis (Wortheniopsis) urkutensis n. sp. and Wortheniopsis (Sisenna) hierlat^ensis n. sp., respectively]. In the available material, further Wortheniopsis (Sisenna) species are also indicated, but most of them are known only in small areas of a few localities. The morphes/species of the "stable" European "faveolata" group are not or only doubt­fully identifiable. Subgenus WortheniopsisJ. BÖHM, 1895 Wortheniopsis (Wortheniopsis) aff. procera (J. A. EUDES-DESLONGCHAMPS, 1849) (Figure 22) aff. 1849: Pleurotomaria faveolata var. procera — J. A. EUDBS-DESLONGCHAMPS, p.74, pl. 15, figs 5a-b. aff. 1854: Pleurotomaria procera D'ORB. — D'ORBIGNY, p. 409, pi. 351, figs 3-4. non 1980: Sisenna cf. procera (J. A. EUDES-DESLONGCHAMPS) — SZABÓ, p. 55, pl. 1: 2-3. aff. pars 1997: Sisenna faveolata (J. A. EUDES-DESLONGCHAMPS) — FISCHER & W'l.BI R. p. 159, pi. 25, fig. 8. Material — A single damaged, shelly specimen without earliest shell parts and peristome (HGM J. 08.3.1.). Measurements H HL HP HGMJ.08.3.1. **26 **15.5 *10 Shape — Rather high spired shell, consisting of convex whorls, separated by deeply impressed (subcanali­culate) suture. Whorl surface separated by rounded angula­tion into narrow, steep and flat ramp with concave seleni­zone on its abapical edge, and feebly concave, rather wide outer face. Rounded peripher} 7 gives transition into convex, narrowly phaneromphalous base. Peristome not preserved. Sculpture — Predominant ornament of spiral cords at peripheral region, and spiral threads on remain­ing parts of shell. Selenizone bordered also by two cords. Disregarding earliest preserved whorl, no collabral orna­ment beside growth-lines observable, even lunulae lacking from selenizone. Granules developed on all spiral orna­mental elements but became obscure on (or eroded? from) some cords of last whorl. Strength of peripheral cords gradually decreases towards umbilicus. Remarks — The available specimen is a damaged shell, slighdy more slender than that one, figured by FISCHER & WEBER (1997) as holotype of Sisenna procera (J. A. EUDES-DESLONGCHAMPS, 1849). The ornament of the single Hierlatz Limestone (Úrkút, Bakony Mts) find is more significantly different because its spiral cords are much stronger. This might be the second known specimen in W. (W.)procera (J. A. EUDES-DESLONGCHAMPS, 1849). D W AA AL **15.5 **8 50° The shape and ornament of this species strongly recall that of the type species of Wortheniopsis J. BÖ1 IM, 1895. Distribution — Lower? Sinemurian Hierlatz Limestone, Úrkút (Bakony Mts). Figure 22 — Wortheniopsis (Wortheniopsis) aff. procera (J. A. EUDES-DESLONGCHAMPS, 1849) — A-B : apertural and dorsal view, Xl; C: apertural view with details of the ornament, X2.7. Wortheniopsis (Wortheniopsis) urkutensis n. sp. (Figure 23) pars 1861: Pleurotomariafoveolata DESLONG. — STOLICZKA, p. 186, pi. 4, fig. 1. Holotype — GBa 2008/69/39/1/1, paratype: HGM J. 08.2.1. Type locality — Hallstatt, Hierlatz Alpe. Type strata — Upper Sinemurian (Oxynotum Zone) Hierlatz Limestone. Name — From the locality 7 of the paratype (Úrkút, Bakony Mts, Hungary). Diagnosis — Turbiniform shell of whorls with lacking or obscure angulation; "ramp" feebly convex; selenizone running above flattened outer face; subregular network ornament on belt between upper suture and selenizone ("ramp"); spiral cords predominate ornament of outer face and base.

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