Research Article
Print
Research Article
Late Jurassic (Upper Kimmeridgian) gastropods from Saal near Kelheim (Germany, Bavaria)
expand article infoJoachim Gründel, Alexander Nützel§|
‡ Freie Universität Berlin, Berlin, Germany
§ SNSB-Bayerische Staatssammlung für Paläontologie und Geologie, München, Germany
| Ludwig-Maximilians-Universität München, München, Germany
Open Access

Abstract

A new collection of Upper Jurassic (Kimmeridgian) gastropods from the reefal limestones of the Saal quarry near Kelheim (Lower Bavaria, Germany) is reported. It has yielded 119 species of which 80 species are nominate species, the others are treated in open nomenclature. This increases the number of known gastropod species from the Saal quarry by 54 (31 nominate species). A total of 178 gastropod species (107 nominate species) have now been reported from this locality making this occurrence the richest one from the Late Jurassic. Despite the fact that previously studied collections are from the same quarry and have the same age, these collections differ considerably from each other in species composition and relative abundances of shared species. This reflects facies differentiation in the quarry as well as colletion biases. One new genus (Kelheimia gen. nov.) and 15 new species are described: Scurriopsis cragolis sp. nov., Pseudorhytidopilus ? quadratus sp. nov., Rimulopsis danuviensis sp. nov., Nododelphinula oblonga sp. nov., Creniturbo gibbosus sp. nov., Kelheimia triangulata sp. nov., Neritopsis ? rotundatus sp. nov., Oonia kimmeridgiensis sp. nov., Eustoma ? gracilis sp. nov., Cryptoptyxis ? spinosus sp. nov., Turritella lucagrita sp. nov., Neuburgensia angulata sp. nov., Neuburgensia rara sp. nov., Diarthema aspera sp. nov., and Aphanoptyxis sinerugae sp. nov. Leptomaria tuberosa Gründel, Keupp & Lang, 2017 is seen as subjective synonym of Leptomaria goldfussi (Sieberer, 1907). Gymnocerithium ? convexoconcavum Gründel, Keupp & Lang, 2019 is placed in the genus Neuburgensia (comb. nov.). Amphitrochus ? gerberi Gründel, Keupp & Lang, 2017 is placed in the genus Serrettella (comb. nov.). Neritopsis subvaricosa Brösamlen, 1909 is placed in the genus Hayamiella (comb. nov.). Gymnocerithium ? convexoconcavum Gründel, Keupp & Lang, 2019 is placed in the genus Neuburgensia (comb. nov.). Nerinea tricincta Münster, 1844 is placed in the genus Aptyxiella (comb. nov.). Nerinea staszycii (Zeuschner, 1850) is placed in the genus Endoplocus (comb. nov.). Polyptyxisella clio (d’Orbigny, 1852) is placed in the genus Ptygamtis (comb. nov.).

Keywords

Jurassic, Gastropoda, New Taxa, Diversity, Taxonomy

Introduction

The Saal quarry near Kelheim has yielded a highly diverse Late Jurassic gastropod fauna that was described together with material from the Late Jurassic silicified fauna from Nattheim (same age) in the past years (Gründel et al. 2015, 2017, 2019, 2022). Some years ago, a large collection of marine invertebrates including additional gastropods from the Saal quarry was obtained by the Bayerische Staatssammlung für Paläontologie and Geologie (SNSB–BSPG, Bavarian State Collection for Palaeontology and Geology), Munich. This material was collected by the private collector Jürgen Sylla. In addition, some material from Saal became available from other collectors. Together, this new material provides considerable additional information about the gastropod fauna from the Saal quarry which is among the most diverse known Late Jurassic faunas known so far.

Geological setting

The studied gastropod fauna comes from Upper Jurassic (Kimmeridgian) reefal limestones from the locality Saal near Kelheim, Lower Bavaria. The geological setting and depositional environment of the Upper Jurassic (Kimmeridgian) reefal limestones exposed in the Saal quarry has been treated in detail by Gründel et al. (2015, 2022).

Studied material

All specimens described in the following are from the Saal quarry (Saal near Kelheim, Bavaria) which is also the type locality for the new species described herein; all have an upper Kimmeridgian age (stratum typicum for new species). As mentioned, specimens were collected by Jürgen Sylla if not stated otherwise (by far most of the material studied herein comes from the Sylla collection). Jürgen Sylla collected this material over many years exclusively from the Saal quarry. In the following, this location is called ‚Saal‘, if the collectors has not provided further detail such as a specific location within the quarry and the beds from which the material was collected. If such information was provided by the collector Sylla, it is also given herein for the specimens in question. A few of the studied specimens derive from the collections of Fritz Lang, Helmut Keupp, and Olaf Neubauer. This material became available for us after the publication of the previous monographs on the gastropods from the Saal quarry (Gründel et al. 2015, 2017, 2019, 2022). If no collector name is mentioned, the specimens are from the Sylla collection.

Repository

Nearly all material including all type and illustrated specimens is housed in the Bayerische Staatssammlung für Paläontologie und Geologie in Munich under the general repository number SNSB–BSPG 2016 XXI. In addition, all illustrated and all type specimens have individual repository numbers. Some of the studied specimens were provided by other collectors (see above). Of those specimens, a few were returned to collectors if they are not illustrated or have type status.

Results

Systematic palaeontology

In principal, we use the suprageneric systematics as given by Bouchet et al. (2017).

Subclass Patellogastropoda Lindberg, 1986

Superfamily Patelloidea Rafinesque, 1815

Family Patellidae Rafinesque, 1815

Patella Linné, 1758

Type species

Patella vulgata Linné, 1758; Recent.

Patella sp.

Plate 1: fig. 1

Material

1 specimen, SNSB–BSPG 2016 XXI 1601 (collection O. Neubauer).

Description

Shell 7 mm long, with broadly oval outline and rounded edges in dorsal view; shell lowly limpet–shaped; apex in almost central position; central portion of shell lacks visible ornament (due to preservation?); shell otherwise with numerous strong, somewhat bulging radial ribs with 1 or 2 weaker radial ribs in between (details unclear); in addition shell ornamented with numerous weak concentric ribs.

Plate 1. 

(1) Patella sp., SNSB–BSPG 2016 XXI 1601, collection O. Neubauer, dorsal view, length 7 mm. (2–4) Scurriopsis cragolis sp. nov. holotype, SNSB–BSPG 2016 XXI 1602, (2–3) lateral and dorsal views, length 16 mm, (4) detail of ornament, height ca. 5.8 mm. (5–8) Scurriopsis sp., SNSB–BSPG 2016 XXI 1606, (5) dorsal view, length 8 mm, (6) detail in dorsal view, width 3.5 mm, (7–8) lateral view and detail of ornament, height 6 mm. (9–10) Pseudorhytidopilus ? quadratus sp. nov., holotype, SNSB–BSPG 2016 XXI 1607, dorsal and lateral views, largest diameter 21 mm. (11) Pseudorhytidopilus ? quadratus sp. nov., paratype, SNSB–BSPG 2016 XXI 1608, dorsal view, largest diameter 16 mm. (12) Leptomaria goldfussi (Sieberer, 1907), SNSB–BSPG 2016 XXI 1616, lateral view, height 25 mm. (13, 14) Leptomaria goldfussi (Sieberer, 1907), SNSB–BSPG 2016 XXI 1617, early whorls and detail of ornament, (13) height 16.5 mm, (14) height 14 mm. (15, 16) Leptomaria goldfussi (Sieberer, 1907), SNSB–BSPG 2016 XXI 1618, aperture and base, width 24 mm.

Remarks

Patella staceata Gründel, Hostettler and Menkveld-Gfeller, 2020 is very similar but differs in having numerous weaker radial ribs between the strong main radial ribs. The single, probably juvenile specimen is too poorly preserved for a better identification.

Superfamily Lottioidea Gray, 1840

Family Acmaeidae Forbes, 1850

Scurriopsis Gemmellaro, 1878

Type species

Scurriopsis neumayri Gemmellaro, 1878; Early Jurassic, Sinemurian; Italy.

Scurriopsis cragolis sp. nov.

Plate 1: figs 2–4

Etymology

Arbitrary word formation.

Holotype

SNSB–BSPG 2016 XXI 1602 (Plate 1: figs 2–4), Sylla collection.

Paratypes

3 specimens, SNSB–BSPG 2016 XXI 1603–1605.

Description

Limpet with almost straight to slightly convex sides in lateral view; distinctly longer than wide in dorsal view; outline in dorsal view oval to rounded subrectangular, slightly tapering posteriorly or anteriorly; apex distinctly decentral in direction of the tapering side of the shell; shell ornamented with numerous, densely spaced fine but distinct radial ribs and much finer co-marginal concentric threads. The holotype is 26 mm long.

Differential diagnosis

Hennocquia saalensis Gründel et al. (2017) from the same locality and stratigraphic position is smaller, the shell is broadly elliptic in dorsal view and has distinctly convex sides in lateral view; its very weak radial ribs are confined to the anterior and posterior parts of the shell and its dominant ornament consists of strengthened growth lines. Scurria oxyconus Zittel sensu di Stefano (1884) is larger and the shell is broader in dorsal view and has more convex sides in lateral view; its apex is situated in an almost central position. Fissurella kobyi Loriol, 1890 (in Loriol and Koby) is smaller and has more convex sides in lateral view; it has fewer and stronger axial ribs, its apex has a hole as is typical for fissurellids. Dietrichella moreana (Buvignier, 1843) sensu Gründel et al. (2020a) has more convex sides in lateral view, is broader oval in dorsal view and lacks axial ribs.

Scurriopsis sp.

Plate 1: figs 5–8

Material

1 specimen, SNSB–BSPG 2016 XXI 1606.

Description

Shell 8 mm long, high limpet-shaped; apex slightly decentral on anterior-posterior axis; on anterior-posterior axis, one side weakly convex in lateral view, other side almost straight; shell outline broadly oval in dorsal view; shell tapering, somewhat narrower in direction of apex; shell ornamented with numerous (ca. 50) radial ribs of equal strength, crenulated by much weaker concentric ribs; apex demarcated from rest of shell, with much weaker ornament (maybe due to preservation); shell edge wavy in dorsal view due to protruding radial ribs.

?Family Acmaeidae Forbes, 1850

Pseudorhytidopilus Cox, 1960 (in Knight et al.)

Type species

Pseudorhytidopilus lennieri Cox, 1960 (in Knight et al.); Kimmeridgian; France.

Remarks

The systematic placement of this genus is unclear (Gatto and Monari 2010; Szabó in Mandl et al. 2010). Most authors place it in Acmaeidae.

Pseudorhytidopilus ? quadratus sp. nov.

Plate 1: figs 9–11

Etymology

Latin quadratus – due to the quadratic outline of the shell.

Holotype

SNSB–BSPG 2016 XXI 1607 (Plate 1: figs 9–10).

Paratypes

6 specimens SNSB–BSPG 2016 XXI 1608–1613.

Diagnosis

Shell thin, with trapezoidal to subquadratic outline with rounded edges in dorsal view; apex approximately in central position; shell ornamented with irregular concentric bulges.

Type locality and stratum

Upper Jurassic (Kimmeridgian) reefal limestones from the locality Saal near Kelheim, Lower Bavaria (Gründel et al. 2015, 2022).

Description

Large specimen has a diameter of 21 mm; shell very thin, shallowly cap-shaped in lateral view; trapezoidal (one side of shell slightly narrower than the other side) to subquadratic outline with rounded edges in dorsal view; apex approximately in central position; shell ornamented with irregular concentric bulges.

Remarks

Species with a similar ornament of bulges (e. g., P. ? ledonii (Haber, 1932) sensu Gatto and Monari 2010, Fabercapulus semisculptus Monari et al. 2017) have an elliptic outline in dorsal view and a radial furrow. Other species with an oval outline in dorsal view lack a furrow and an ornament of bulges (P. latissima (Sowerby, 1816) sensu Munt in Martill and Etches 2020, Berlieria maeotis (Eichwald) sensu Gerasimov, 1992 and others).

Brunonia annulata (Yokoyama, 1890) from the Cretaceous of Japan is also cap-shaped and has a similar ornament but its type species is much larger and has a rounded, oval outline in dorsal view (Kase 1988; Dieni 1990). Patella (Helcion) sculptilis Zittel, 1873 has a straight shell end in lateral view, weak concentric wrinkles and numerous radial ribs.

Subclass Vetigastropoda Salvini-Plawen, 1980

Superfamily Pleurotomarioidea Swainson, 1840

Family Pleurotomariidae Swainson, 1840

Pleurotomaria Defrance, 1826

Type species

Trochus anglicus Sowerby, 1818; early Jurassic; England.

Pleurotomaria agassizii Münster in Goldfuss, 1844

pl. 1: figs 13–15, pl. 2: figs 1–9 in Gründel et al. (2017)

2017 Pleurotomaria agassizii Münster in Goldfuss, 1844 – Gründel, Keupp and Lang: 175; pl. 1, figs 13–15; pl. 2, figs 1–9 (here more synonymy and chresonymy).

Material

1 certain SNSB–BSPG 2016 XXI 1614 and 1 questionable specimen (SNSB–BSPG 2016 XXI 1615).

Remarks

This species was reported from the Nattheim area by Gründel et al. (2017). We report it from Saal for the first time.

Leptomaria Eudes-Deslongchamps, 1865

Type species

Pleurotomaria amoena Eudes-Deslongchamps, 1849; Bajocian; France.

Leptomaria goldfussi (Sieberer, 1907)

Plate 1: figs 12–16

2017 Leptomaria goldfussi (Sieberer, 1907) – Gründel, Keupp and Lang: 177, pl. 2, figs 13–15; pl. 3, figs 1–2 (here more synonymy and chresonymy).

2017 Leptomaria tuberosa sp. nov. – Gründel, Keupp and Lang: 177, pl. 3, figs 3–5.

2017 Leptomaria tuberosa Gründel, Keupp and Lang – Gründel: 27, pl. 3, fig. C.

Material

12 specimens, SNSB–BSPG 2016 XXI 1616–1627.

Description

Shell broadly trochiform, wider than high, with blunt, rounded apex; a specimen is 28 mm high; whorl face of first whorls straight, on late whorl slightly concave adapically and slightly convex abapically; selenizone separates these zones of whorl face; selenizone at about mid-whorl in early whorls, distinctly above mid-whorl in later whorls; earliest recognizable ornament consists of cancellate pattern of weak spiral threads and somewhat strengthened growth lines; spiral threads become stronger forming cords later in ontogeny; ca. 10 cords present on whorl face; growth lines may stay weak throughout ontogeny in some specimens; other specimens have strong, bulgy, prosocline axial ribs that are much broader than their interspaces on adapical portion of whorls; intersections of spiral cords and axial ribs are strongly nodular; subsutural row of nodules strongest; spiral cords strengthened below selenizone, commonly with alternation of strong and weak spiral cords; growth lines in this portion only developed as weak axial ribs; axial ribs crenulate spiral cords at intersections; base anomphalous, flat; transition from whorl face to base at rounded edge without nodes; base covered with numerous spiral cords of somewhat varying strength; strongest spiral cords towards center of base; growth lines on base sickle-shaped, straight near center opisthocyrt towards edge; aperture rounded quadratic, columellar lip somewhat broadened.

Remarks

Gründel et al. (2017) discussed the possibility that L. tuberosa Gründel, Keupp & Lang, 2017 is a varity of L. goldfussi . The new material corroborated this assumption and L. tuberosa is now considerd to be a synonym. Differences to Leptomaria sp. are explained below. Laevitomaria ? antoniae (Étallon, 1861 in Thurmann and Étallon sensu Gründel et al. 2020a) has more convex whorls and deeper sutures; it lacks strengthened subsutural axial ribs. Pleurotomaria agassizii Münster, 1844 (in Goldfuss) has distinct subsutural axial ribs and the edge at the transition from whorl face to base bears nodes.

Leptomaria sp.

Plate 2: figs 1, 2

Material

1 specimen, SNSB–BSPG 2016 XXI 1628.

Description

Shell broadly trochiform conical with straight sides; specimen 27 mm high; sutures indistinct; ornament of early whorls poorly preserved showing few spiral cords; selenizone visible as broad band in supra-median position on last whorls; whorl face ornamented with spiral cords, 3 above and 4–5 below selenizone; adapical spiral cords weaker than abapical cords; last whorl also ornamented with broad, bulging, prosocline, axial ribs that are poorly demarcated from their interspaces; interspaces between ribs approximately as broad as ribs; intersections of axial ribs and spiral cords usually not nodular or only weakly nodular; only one spiral cord below selenizone has distinct nodes; transition from whorl face to base at rounded edge; base flat, densely covered by spiral cords that are not nodular and broader than their interspaces; aperture not preserved.

Plate 2. 

(1, 2) Leptomaria sp., SNSB–BSPG 2016 XXI 1628, lateral and basal views, width 30 mm. (3–5) Leptomaria phacoides Zittel, 1873, SNSB–BSPG 2016 XXI 1629, lateral, apical and basal views, width 41 mm. (6) Leptomaria phacoides Zittel, 1873?, SNSB–BSPG 2016 XXI 1631, lateral view, height 22 mm. (7) Rimulopsis danuviensis sp. nov., holotype, SNSB–BSPG 2016 XXI 1653, collection Neubauer, lateral view, height 9 mm. (8) Rimulopsis danuviensis sp. nov., paratype, SNSB–BSPG 2016 XXI 1654, collection Neubauer, anterior view, height 7 mm. (9–11) Asperilla longispina (Rolle, 1861), SNSB–BSPG 2016 XXI 1661, lateral, apical and basal views, width including spines 24 mm. (12, 13) Falsataphrus ? valfinense Loriol, in Loriol and Bourgeat (1886–1888), SNSB–BSPG 2016 XXI 1696, apical and lateral views, width 12 mm. (14, 15) Caryomphalus globatus (Buvignier, 1843), SNSB–BSPG 2016 XXI 1713, basal and lateral views, width 15 mm.

Remarks

Leptomaria sp. differs from Leptomaria goldfussi (Sieberer, 1907) by having straighter shell sides, being more acute, having broad, bulging, poorly defined axial ribs and by largely lacking nodes at intersections of axial ribs and spiral cords.

Leptomaria phacoides Zittel, 1873

Plate 2: figs 3–5

?1844 Trochus iurensis Hartmann – Goldfuss: 57, pl. 180, fig. 12.

*1873 Pleurotomaria (Leptomaria) phacoides n. sp. – Zittel: 335, pl. 50, fig. 1.

?1907 Leptomaria umbilicata n. sp. – Sieberer: 61, pl. 5, fig. 9.

1997 Leptomaria phacoides Zittel – Hägele: 33, pl. 5, fig. 1, fig. p. 33 upper middle.

2013 Leptomaria phacoides Zittel – Monari and Gatto: 821, fig. 8 Q.

Material

1 specimen SNSB–BSPG 2016 XXI 1629 and 1 cast of an impression SNSB–BSPG 2016 XXI 1630 (the impression itself is lacking).

Description

Shell low trochiform, with low whorls; specimen 41 mm wide; suture shallow;

selenizone indistinct apparently at mid-whorl on last whorl, and suprasutural on spire whorls with a bulge below it; whorls with faint remains of spiral ornamentation; base flat, demarcated from whorl face by rounded edge, widely phaneromphalous; base without visible ornamentation except for indistinct growth lines; aperture not preserved.

Remarks

Leptomaria chryseis Laube sensu Gründel (2012) and Monari and Gatto (2013) has an ornament of spiral and axial ribs on the early teleoconch whorls, its whorls are more convex and the sutures are more distinct. Pleurotomaria onion d’Orbigny sensu Loriol in Loriol and Bourgeat (1886–1888) lacks ornamentation and its umbilicus is wider. Pleurotomaria cfr. philea d’Orbigny sensu Schlosser (1882) has more convex whorls, deeper sutures, and lacks an abapical bulge and furrow. Pleurotomaria umbilicata Sieberer, 1907 is maybe identical with Leptomaria phacoides but has a weak cancellate ornament of spiral cords and axial ribs.

Leptomaria phacoides Zittel, 1873?

Plate 2: fig. 6

Material

A single shell fragment, SNSB–BSPG 2016 XXI 1631.

Remarks

The fragment of ca. four whorls shows a well preserved ornament. It possibly belongs to Leptomaria phacoides but it has a higher and more slender spire than the specimen described above as L. phacoides. Both have the selenizone below mid-whorl on the last whorl and in a suprasutural position in spire whorls. The whorl face including selenizone is covered with numerous spiral cords which are broader than the furrows separating them. The growth lines are prosocline and prosocyrt between the adapical suture and selenizone and prosocyrt between selenizone and abapical suture. The base is not preserved.

Family Trochotomidae Cox, 1960 (in Knight et al.)

Placotoma Ferrari, Damborenea, Manceñido & Griffin, 2015

Type species

Ditremaria amata d’Orbigny, 1854; upper Oxfordian-lower Kimmeridgian; France.

Placotoma suevica (Quenstedt, 1884)

pl. 3: figs 10–15, pl. 4: figs 1, 2 in Gründel et al. (2017)

2017 Placostoma suevica (Quenstedt, 1881–1884) – Gründel, Keupp and Lang: 179, pl. 3, figs 10–15, pl. 4, figs 1–2 (here more synonymy and chresonymy).

2017 Placostoma suevica (Quenstedt, 1881–1884) – Gründel: 27, pl. 3, fig. D.

Material

5 specimens, SNSB–BSPG 2016 XXI 1632–1636.

Valfinia Cox, 1958

Type species

Trochus quinquecinctus Zieten, 1830–1833; upper Jurassic, South Germany.

Valfinia quinquecincta (Zieten, 1830–1833)

pl. 4: figs 3–11 in Gründel et al. (2017)

2017 Valfinia quinquecincta (Zieten, 1830–1833) – Gründel, Keupp and Lang: 180, pl. 4, figs 3–11 (here more synonymy and chresonymy).

2017 Valfinia quinquecincta (Zieten, 1830–1833) – Gründel: 27; pl. 4, fig. A.

Material

2 specimens, SNSB–BSPG 2016 XXI 1637–1638.

Superfamily Seguenzioidea Verrill, 1884

Family Chilodontidae Wenz, 1938

Chilodonta Étallon, 1862

Type species

Chilodonta clathrata Étallon, 1862; Kimmeridgian; France.

Chilodonta quadratofoveata Gründel, Keupp & Lang, 2017

pl. 6: figs 10–13 in Gründel et al. (2017)

2017 Chilodonta quadratofoveata n. sp. – Gründel, Keupp and Lang: 188, pl. 6, figs 10–13 (here more synonymy and chresonymy).

Material

4 specimens, SNSB–BSPG 2016 XXI 1639–1642.

Onkospira Zittel, 1873

Type species

Turbo ranellatus Quenstedt, 1852; Kimmeridgian, South Germany.

Onkospira ranellata (Quenstedt, 1852)

pl. 7: figs 3–7 in Gründel et al. (2017)

2017 Onkospira ranellata (Quenstedt, 1852) – Gründel, Keupp and Lang: 191, pl. 7, figs 3–7 (here more synonymy and chresonymy).

2017 Onkospira ranellata (Quenstedt, 1852) – Gründel: 28, pl. 5, fig. B.

Material

2 specimens SNSB–BSPG 2016 XXI 1643–1644 and a cast of an imprint, SNSB–BSPG 2016 XXI 1645 (imprint not at hand).

Superfamily Fissurelloidea Fleming, 1822

Family Fissurellidae Fleming, 1822

Subfamily Emarginulinae Children, 1834

Rimulopsis Haber, 1932

Type species

Emarginula goldfussi Roemer, 1836; higher Upper Jurassic, North Germany.

Rimulopsis perforata Gründel, Keupp & Lang, 2017

pl. 1: figs 10–12 in Gründel et al. (2017)

2017 Rimulopsis perforata n. sp. – Gründel, Keupp and Lang: 174, pl. 1, figs 10–12.

Material

3 specimens, SNSB–BSPG 2016 XXI 1646–1648.

Rimulopsis broesamleni Gründel, Keupp & Lang, 2017

pl. 1: figs 7–9 in Gründel et al. (2017)

2017 Rimulopsis broesamleni n. sp. – Gründel, Keupp and Lang: 173, pl. 1, figs 7–9 (here more synonymy and chresonymy).

2017 Rimulopsis broesamleni Gründel, Keupp and Lang – Gründel: 27, pl. 3, fig. B.

Material

4 specimens, SNSB–BSPG 2016 XXI 1649–1652.

Rimulopsis danuviensis sp. nov.

Plate 2: figs 7, 8

Etymology

After the river Donau, Latin Danubius.

Holotype

SNSB–BSPG 2016 XXI 1653 (Plate 2: fig. 7) (collection Neubauer).

Paratypes

3 specimens Saal (2 specimens collection Sylla, SNSB–BSPG 2016 XXI 1655–1656, 1 specimen collection Neubauer, SNSB–BSPG 2016 XXI 1654).

Type locality and stratum

Upper Jurassic (Kimmeridgian) reefal limestones from the locality Saal near Kelheim, Lower Bavaria (Gründel et al. 2015, 2022).

Diagnosis

Limpet ornamented with a repeated alternation of one strong and 1–3 weaker radial ribs and few bulgy concentric ribs; shell angulated at two of the prominent radial ribs that are nodular at intersections with concentric ribs; several weak concentric ribs are intercalated between two strong concentric ribs.

Description

Shell limpet-shaped; a shell is 9 mm high; apex strongly bent in posterior direction protruding the posterior shell margin in lateral and dorsal view; selenizone raised, forming crest; lunulae lamellar, concave anteriorly; at each side of selenizone, 1–2 weak and then one strong radial rib; at these strong radial ribs, shell is distinctly angulated; lateral shell sides ornamented with a repeated alternation of one strong and 1–3 weaker radial ribs and few, distantly spaced bulgy concentric ribs; intersections of radial and concentric ribs nodular, nodes especially strong on the two ribs that angulate the shell; in addition, weak concentric, co-marginal ribs are present.

Remarks

Rimulopsis broesamleni Gründel et al., 2017 has a regularly alternation of a weaker and a stronger radial rib as well as weaker concentric ribs. This produces a cancellate ornament including deep pits demarcated by radial and concentric ribs. Instead of concentric bulgy ribs, it has more regular and defined ribs. Intersections of radial and concentric are only weakly nodular. Rimula etalloni Loriol in Loriol and Bourgeat (1886–1888) sensu Gründel et al. (2020a) has an alternation of each one stronger and one weaker radial rib; it lacks weaker concentric ribs between the bulgy concentric ribs. Rimulopsis paucicostata (Étallon, 1861 in Thurmann and Étallon) sensu Gründel et al. (2020a) has an alternation of each, one strong and one weak radial rib; bulgy concentric ribs are confined to the apical portion of the shell whereas weak concentric ribs are present in the abapical portion of the shell.

Superfamily Trochoidea Rafinesque, 1815

Family Trochidae Rafinesque, 1815

Falsotectus Gründel, Keupp & Lang, 2017

Type species

Falsotectus parvus Gründel, Keupp & Lang, 2017; Kimmeridgian; South Germany.

Falsotectus parvus Gründel, Keupp & Lang, 2017

pl. 4: figs 14, 15; pl. 5: figs 1–7 in Gründel et al. (2017)

2017 Falsotectus parvus n. sp. – Gründel, Keupp and Lang: 182, pl. 4, figs 14–15; pl. 5, figs 1–7

2017 Falsotectus parvus Gründel, Keupp and Lang – Gründel: 28, pl. 4, fig. B.

Material

4 specimens (3 specimens Saal, SNSB–BSPG 2016 XXI 1657–1659; 1 specimen Saal, “Fundort 1985, über Korallenstock, Sohle 2” (= locality 1985, above coral stock, level 2), SNSB–BSPG 2016 XXI 1660.

Family Angariidae Gray, 1857

Asperilla Koken, 1896

Type species

Delphinula coronoserra Quenstedt, 1881–1884 (= Delphinula longispina Rolle, 1861); Kimmeridgian; South Germany.

Asperilla longispina (Rolle, 1861)

Plate 2: figs 9–11

2017 Asperilla longispina (Rolle, 1861) – Gründel, Keupp and Lang: 203, pl. 10, figs 11–17 (here more synonymy and chresonymy).

Material

2 specimens, SNSB–BSPG 2016 XXI 1661–1662.

Remarks

The present specimens have fewer spines on the keel (ca. 7) than those reported by Gründel et al. (2017). In addition, the present specimens have more nodes on the spiral cord at the transition from whorl face to base. According to the literature, the base of this species is smooth or has only a single nodular spiral cord close to the spiral cord at the transition to the whorl face (Gründel et al. 2017). However, the present specimen has three distinctly nodular spiral cords on the base, besides the spiral cord at the transition to the whorl face. The meaning of these differences the present material to that reported by Gründel et al. (2017) are difficult to judge without additional well-preserved material. Therefore, we tentatively keep the present specimens under the same species name.

Family Epulotrochidae Gründel, Keupp & Lang, 2017

Discotectus Favre, 1913

Type species

Trochus massalongoi Gemmellaro, 1868; Calcare a Terebratula janitor, Sicily, Italy.

Discotectus crassiplicatus (Étallon, 1859)

pl. 5, fig. 10–12; pl. 15: figs 3–6 in Gründel et al. (2017)

2017 Discotectus crassiplicatus (Étallon, 1859) – Gründel, Keupp and Lang: 183, pl. 5, fig. 10–12; pl. 15, figs 3–6 (here more synonymy and chresonymy).

2017 Discotectus crassiplicatus (Étallon, 1859) – Gründel: 28, pl. 4, fig. C.

Material

Saal: 8 specimens, SNSB–BSPG 2016 XXI 1663–1670; Saal, location 1985, “über Knollenkalkbank, Sohle 2” (=above nodular bed, level 2): 1 specimen, SNSB–BSPG 2016 XXI 1671.

Undatotectus Gründel, Keupp & Lang, 2017

Type species

Undatotectus glaber Gründel, Keupp & Lang, 2017; Kimmeridgian; South Germany.

Undatotectus glaber Gründel, Keupp & Lang, 2017

pl. 8: figs 7–12 in Gründel et al. (2017)

2017 Undatotectus glaber n. sp. – Gründel, Keupp and Lang: 184, pl. 8, figs 7–12.

2017 Undatotectus glaber Gründel, Keupp & Lang, 2071 – Gründel: 28, pl. 4, fig. D.

Material

12 specimens (SNSB–BSPG 2016 XXI 1672–1683); 1 specimen from Saal, locality 1985, above coral stock, Sohle 2, SNSB–BSPG 2016 XXI 1684 (all collection Sylla).

? Epulotrochidae Gründel, Keupp & Lang, 2017

Wernerocutus Gründel, Keupp & Lang, 2017

Type species

Trochus angulatoplicatus Münster in Goldfuss, 1844; upper Kimmeridgian; South Germany.

Wernerocutus angulatoplicatus (Münster in Goldfuss, 1844)

pl. 8: figs 13–15; pl. 9: figs 1–5 in Gründel et al. (2017)

2017 Wernerocutus angulatoplicatus (Münster in Goldfuss, 1844) – Gründel, Keupp and Lang: 185, pl. 8, figs 13–15; pl. 9, figs 1–5 (here more synonymy and chresonymy).

2017 Wernerocutus angulatoplicatus (Münster in Goldfuss, 1844) – Gründel: 25, fig. 2.

Material

11 specimens, SNSB–BSPG 2016 XXI 1685–1695.

Family Colloniidae Cossmann, 1917 in Cossmann and Peyrot

Subfamily Colloniinae Cossmann, 1917 in Cossmann and Peyrot

Falsataphrus Gründel, 2000

Type species

Falsataphrus circumcallosus Gründel, 2000; Callovian; NE–Germany.

Falsataphrus ? valfinense (Loriol, 1887 in Loriol and Bourgeat 1886–1888)

Plate 2: figs 12, 13

1886–1888 Teinostoma valfinense Loriol – Loriol in Loriol and Bourgeat: 189, pl. 21, figs 6–7.

?1997 Buckmannia sp. – Hägele: 52, fig. p. 52 lower left.

Material

2 specimens, SNSB–BSPG 2016 XXI 1696–1697.

Description

Shell lens-shaped with very low spire; larger specimen 12 mm wide; last whorl embracing most of previous whorls; sutures indistinct; apex rounded; shell smooth; periphery evenly rounded; base flat; base and aperture incompletely preserved; no umbilicus and ornament visible; it is unclear whether the broad callus covering the umbilicus that would be typical of the genus Falsataphrus is present or not.

Remarks

Falsataphrus corallensis (Buvignier, 1852) sensu Gründel et al. (2020a) has at least sometimes a higher spire (Gründel et al. 2020a: pl 12: figs 13, 14); other specimens are hardly distinguishable from the present specimens (Gründel et al. 2020a: pl 12: figs 10, 11). Falsataphrus corallensis sensu Loriol in Loriol and Koby (1890) cannot be distinguished from F. ? valfinense according to its description.

Torusataphrus Gründel, Keupp & Lang, 2017

Type species

Natica inornata Quenstedt, 1858; Upper Jurassic; South Germany.

Torusataphrus inornatus (Quenstedt, 1858)?

pl. 10: figs 4–7 in Gründel et al. 2017)

?2017 Torusataphrus inornatus (Quenstedt, 1858) nov. comb. – Gründel et al.: 196, pl. 10, figs 4–7

Material

1 specimen, SNSB–BSPG 2016 XXI 1698.

Remarks

The present specimen fits T. inornatus in general shell morphology. However, the characters typical for the genus Torusataphrus (callus on base and thickened outer lip) are not recognizable.

Family Metriomphalidae Gründel, Keupp & Lang, 2017

Metriomphalus Cossmann, 1916

(sensu Gründel 2009)

Type species

Turbo davousti d’Orbigny, 1850; Bathonian; France.

Metriomphalus parvotuberosus Gründel, Keupp & Lang, 2017

pl. 11: figs 10–16 in Gründel et al. (2017)

2017 Metriomphalus parvotuberosus n. sp. – Gründel, Keupp and Lang: 197, pl. 11, figs 10–16.

2017 Metriomphalus parvotuberosus Gründel, Keupp & Lang, 2017 – Gründel: 29, pl. 6, fig. B.

Material

Saal: 3 specimens, SNSB–BSPG 2016 XXI 1699–1701; 1 specimen “Fundort 1985, über Korallenstock, Sohle 2” (= locality 1985, above coral stock, level 2), SNSB–BSPG 2016 XXI 1702; 3 casts of imprints that are not present, SNSB–BSPG 2016 XXI 1703–1705.

Metriomphalus sp. 1

pl. 12: figs 1–4 in Gründel et al. (2017)

2017 Metriomphalus sp. 1 – Gründel, Keupp and Lang: 198, pl. 12, figs 1–4.

Material

1 specimen, SNSB–BSPG 2016 XXI 1706.

Planiturbo Fischer, 1969

(sensu Gründel et al. 2017)

Type species

Turbo planispira Cossmann, 1885; Bathonian; France.

Planiturbo funatus (Goldfuss, 1844)

pl. 12: figs 5–9 in Gründel et al. (2017)

2017 Planiturbo funatus (Goldfuss, 1844) – Gründel, Keupp and Lang: 199, pl. 12, figs 5–9.

Material

1 specimen “Fundort 1985, über Korallenstock, Sohle 2” (= locality 1985, above coral stock, level 2), SNSB–BSPG 2016 XXI 1707; 2 specimens Saal, SNSB–BSPG 2016 XXI 1708–1709.

Planiturbo procerus Gründel, Keupp & Lang, 2017

pl. 12: figs 10–13; pl. 15, fig. 7 in Gründel et al. (2017)

2017 Planiturbo procerus n. sp. – Gründel, Keupp and Lang: 200, pl. 12, figs 10–13; pl. 15, fig. 7.

2017 Planiturbo procerus Gründel, Keupp & Lang, 2017 – Gründel: 29, pl. 6, fig. C.

Material

3 specimens, SNSB–BSPG 2016 XXI 1710–1712.

Caryomphalus Gründel, Keupp & Lang, 2017

Type species

Delphinula fumatoplicosa Quenstedt, 1858; Kimmeridgian; South Germany.

Caryomphalus globatus (Buvignier, 1843)

Plate 2: figs 14, 15, Plate 3: fig. 1

2020 Caryomphalus globatus (Buvignier, 1843) n. comb. – Gründel, Hostettler and Menkveld-Gfeller: 238, pl. 9, figs 11–15, pl. 10, figs 1–13 (here more synonymy and chresonymy).

Material

3 specimens Saal, SNSB–BSPG 2016 XXI 1713–1715; 1 specimen Saal, “Fundort 1985, über Korallenstock, Sohle 2” (= locality 1985, above coral stock, level 2), SNSB–BSPG 2016 XXI 1716.

Description

Shell broadly turbiniform; illustrated specimen 18 mm high; mature whorls evenly convex with periphery at mid-whorl; sutures impressed; earliest preserved whorls have a pronounced edge below mid-whorl; whorl face between edge and adapical suture forms oblique ramp, vertical below edge; ramp initially with three, later with four spiral cords; shell below edge initially with one spiral cord, later with two spiral cords; edge becomes increasingly less pronounced and rounded on penultimate whorl; last whorl evenly rounded, markedly convex with periphery at mid-whorl and evenly rounded transition to moderately convex base; suture considerably deflected downward in last whorl so that another 4–5 spiral cords are exposed on penultimate whorl; 17 spiral cords are present on last whorl from suture to middle of base; all spiral cords are densely covered with small pustules; axial ribs absent, or only faint axial ribs on last third of last preserved whorl; base narrowly phaneromphalous; aperture circular.

Plate 3. 

(1) Caryomphalus globatus (Buvignier, 1843), SNSB–BSPG 2016 XXI 1713, lateral view, width 15 mm. (2, 3) Caryomphalus sp., cf. concavus Gründel, Keupp & Lang, 2017, SNSB–BSPG 2017 XXI 1717, lateral and basal views, height 14 mm, width 12 mm. (4) Proconulus? sp. 1 sensu Gründel, Keupp and Lang (2017), SNSB–BSPG 2016 XXI 1718, lateral and basal views, height 11 mm. (5–7) Nododelphinula oblonga sp. nov., holotype, SNSB–BSPG 2016 XXI 1721, lateral views, apertural and abapertural, basal view, width 26 mm. (8–9) Nododelphinula oblonga sp. nov., paratype, SNSB–BSPG 2016 XXI 1930, collection Lang, shell in lateral and dorsal view, width 27 mm. (10–12) Serrettella gerberi (Gründel, Keupp & Lang, 2017), SNSB–BSPG 2016 XXI 1722, lateral, basal views and aperture, width 13 mm. (13) Serrettella gerberi (Gründel, Keupp & Lang, 2017), locality 1985, above coral stock, level 2, SNSB–BSPG 2016 XXI 1723, lateral view, width 9.5 mm. (14, 15) Heliacanthus sp. 1, SNSB–BSPG 2016 XXI 1726, abapertural and apertural lateral views, height 12 mm.

Remarks

The variability of this species could not be assessed, because only few specimens are at hand. The two best preserved specimens resemble those intermediate between variants 1 and 3 of Caryomphalus globatus sensu Gründel et al. (2020).

Caryomphalus sp., cf. concavus Gründel, Keupp & Lang, 2017

Plate 3: figs 2–3

Material

1 specimen from Saal, SNSB–BSPG 2016 XXI 1717.

Description

Shell trochiform; illustrated specimen 14 mm high; whorls weakly convex, evenly expanding; earliest preserved whorl with two nodular spiral cords, one in suprasutural position, other spiral cord between edge and abapical suture; a further spiral cord soon appears above edge; this spiral cord is initially weaker than the other cords but rapidly becomes as strong as other cords; suture somewhat deflected downward on the last part of last whorl, so that another spiral cord becomes exposed on penultimate whorl; edge becomes weaker, and changes to a regular spiral cord on last whorl so that whorl face becomes convex with evenly rounded transition to base; base narrowly phaneromphalous, weakly convex, covered with ca. 10 spiral cords that are somewhat weaker than those on whorl face; all spiral cords bear fine tubercles that are elongated in prosocline direction; details of round aperture not preserved.

Remarks

In Caryomphalus concavus Gründel, Keupp & Lang, 2017, the late whorls are more rapidly increasing (more concave flanks of shell); it has axial ribs on the early whorls, and the inner spiral cords on the base are separated by wider interspaces than the outer spiral cords.

Family Proconulidae Cox, 1960 (in Knight et al.)

Proconulus Cossmann, 1918

Type species

Trochus (Ziziphinus) guillieri Cossmann, 1885; Bathonian; France.

Proconulus ? sp. 1 sensu Gründel, Keupp & Lang (2017)

Plate 3: fig. 4

2017 Proconulus? sp. 1 – Gründel, Keupp and Lang: 193, pl. 8, figs 5–6.

Material

3 specimens, SNSB–BSPG 2016 XXI 1718–1720.

Family Nododelphinulidae Cox in Knight et al. 1960

Nododelphinula Cossmann, 1916

Type species

Delphinula buckmanni Morris & Lycett, 1851; Middle Jurassic; England.

Nododelphinula oblonga sp. nov.

Plate 3: figs 5–9

Etymology

Latin oblongum – protruding, because of the protruding keel.

Holotype

SNSB–BSPG 2016 XXI 1721 (Plate 3: figs 5–7), collection Sylla.

Paratype

1 specimen, SNSB–BSPG 2016 XXI 1930, collection Lang.

Type locality and stratum

Upper Jurassic (Kimmeridgian) reefal limestones from the locality Saal near Kelheim, Lower Bavaria (Gründel et al. 2015, 2022).

Diagnosis

Whorl face with strongly projecting keel and subsutural row of nodes; base entirely covered with spiral cords, one of them encircles umbilicus and is stronger with larger nodes; aperture is more or less pentagonal.

Description

Shell lowly trochiform with gradate spire, about as wide as high; larger specimen is 29 mm wide; earliest whorls are poorly preserved; first recognizable sculpture is an edge roughly in the mid-whorl, which is reinforced to form a keel; area adapical to the edge/keel forming broad, oblique ramp; whorl face below edge/keel approximately vertical, concave; during growth, keel first approaches abapical suture and then moves away again as suture sinks; keel nodular (not always clearly); nodes weaken during ontogeny; a row of nodes present below adapical suture; whorl face completely covered with spiral cords; weak, blurry, barely recognizable axial ribs run from suture to suture; spiral cord at border to base slightly weaker than keel; whorl face between these keel and border spiral cord concave, covered with slightly nodular spiral cords; base flat with angular transition to whorl face where spiral cord is situated; base distinctly phaneromphalous, covered with several spiral cords; particularly strong spiral cord surmounts umbilicus, having significantly larger nodes than those on whorl face; nodes have a pit in apertural portion and thus resemble hollow spines; aperture only incompletely preserved, having pentagonal outline.

Remarks

Delphinula serrata Buvignier, 1852 has a lower shell, the keel has stronger nodes, lacks the strong spiral cord surrounding the umbilicus, and has fewer but stronger spiral cords on the base. Turbo valfinensis Étallon sensu Loriol in Loriol and Bourgeat 1886–1888 (pl. 20, fig. 2, non fig. 3) has a more pronounced tuberculate ornament, the axial ribs are more distinct, the spiral cords are weaker and more numerous, and it lacks the strong spiral cord surrounding the umbilicus. The latter characteristic applies also to Turbo plicatocostatus Zittel, 1873 and to the species of the same name sensu Loriol in Loriol and Koby (1894). In both cases, the keel is weaker and the subsutural row of nodes is missing, the aperture is more rounded.

Serrettella Fischer & Weber, 1997

Type species

Trochus humbertinus Buvignier, 1852; Oxfordian; France.

Serrettella gerberi (Gründel, Keupp & Lang, 2017), comb. nov.

Plate 3: figs 10–13

2017 Amphitrochus ? gerberi n. sp. – Gründel, Keupp and Lang: 194, pl. 9, figs 6–9.

Material

Saal, “Fundort 1985, über Korallenstock, Sohle 2” (= locality 1985, above coral stock, level 2): 3 specimens, SNSB–BSPG 2016 XXI 1722–1724, Saal, “Fossilnest Sohle 3–4” (= fossil nest level 3–4): 1 specimen, SNSB–BSPG 2016 XXI 1725.

Description

The shell is broadly trochiform; largest specimen 14 mm wide; first approximately 2 whorls convex, without visible ornament (due to preservation?); whorl face of later whorls become straight, and sutures become inconspicuous; above abapical suture, a distinctive keel-like protruding spiral cord is formed, as well as 4 weaker ones between this cord and the adapical suture; whorl face slightly angulated by the keel-like spiral cord; as suture sinks, first one and then a second spiral cord become visible on penultimate whorl; both almost as strong as the keel-like spiral rib; transition from whorl face to the moderately convex base evenly rounded; 7–8 spiral cords on the base; all spiral cords densely covered with small pustules (not always clear due to preservation); aperture round with adapical canal; abapical edge of aperture broadly rounded.

Remarks

In contrast to the description given by Gründel et al. (2017), the present material has only four additional, relatively strong spiral cords between the adapical suture and the keel-like spiral cord. Moreover, the base of the present material is completely covered with spiral cords. Based on the limited material available, it cannot be decided with certainty whether these differences indicate genuine morphological differences (in which case there would probably be two separate species) or whether they reflect intraspecific variation or are due to preservation.

Serrettella humbertina (Buvignier) sensu Gründel et al. (2020a) has a subsutural spiral cord covered with stronger nodes, more than 4 weaker spiral cords between the adapical suture and the keel-like reinforced spiral cord, the nodes of the keel-like spiral cord increase in size during ontogeny. “Serrettella nov. gen. humbertina (Buv.)” sensu Fischer and Weber (1997) has a more concave whorl face between the keel and the adapical suture, and the keel-like spiral cord is higher on the whorl face. Trochus humbertina Buvignier, 1852 also has a row of reinforced subsutural nodes, the shell is higher in relation to the width and thus more slender.

Heliacanthus Daqué, 1938 (in Wenz)

Type species

Turbo thurmanni Pictet & Campiche, 1863; Early Cretaceous; Switzerland.

Heliacanthus sp. 1

Plate 3: figs 14–15, Plate 4: Fig. 1

Material

4 specimens, SNSB–BSPG 2016 XXI 1726–1729.

Description

Shell broadly turbiniform with gradate spire; largest specimen 20 mm wide; first recognizable sculpture is a distinct edge situated high on whorl face which separates an approximately horizontal ramp from a vertical abapical part; subsutural spiral cord; two spiral cords appear on either side of edge; orthocline, bulging, blurred axial ribs run from suture to suture; nodules at intersections of axial ribs with subsutural spiral cord and edge; nodes have a pit in apertural direction; base phaneromphalous, slightly convex with angular transition to whorl face; base is covered with 5–6 relatively weak spiral cords in the outer area and three strong nodular spiral ribs near center; all weaker spiral cords are finely crenulated; axial ribs very weak on base; aperture not preserved.

Plate 4. 

(1) Heliacanthus sp. 1, SNSB–BSPG 2016 XXI 1726, basal view, width 12 mm. (2–6) Heliacanthus? sp. 2, SNSB–BSPG 2016 XXI 1730, (2, 5) lateral and apical view, width 20 mm, (3) apex in lateral view, height 11 mm, (4) shell detail in lateral view, height 11 mm, (6) detail apical view, width 15 mm. (7) Heliacanthus? sp. 2, SNSB–BSPG 2016 XXI 1731, apertural view, height of aperture 19 mm. (8–11) Nododelphinulidae? gen. and sp. indet., SNSB–BSPG 2016 XXI 1731, (8, 10) lateral and lapical views, width of specimen 17 mm, (9) apex in lateral view, height 10 mm, (11) detail of base, width 14 mm. (12, 13) Creniturbo gibbosus sp. nov. (specimen lost), collection Lang, apical and lateral views. (14, 15) Creniturbo gibbosus sp. nov., holotype, SNSB–BSPG 2016 XXI 1738, (collection Lang), oblique basal and lateral views, width 6.5 mm.

Remarks

?Nododelphinula sp. sensu Hägele (1997) is smaller, lacks clear axial ribs, the bordering spiral cord at the transition to the base lacks nodes, on the base there is only a hump-shaped spiral cord that surrounds the umbilicus. Heliacanthus epulus (d’Orbigny) sensu Hägele (1997) has smaller and more numerous nodes on the edge, while it lacks a reinforced spiral cord with larger nodes at the transition to the base. Metriomphalus (Metriacanthus) rugosus (Buv.) sensu Fischer and Weber (1997) lacks axial ribs, the nodes on the edge at the transition to the base are larger and less numerous, and its base lacks strong and nodular spiral cords.

Heliacanthus ? sp. 2

Plate 4: figs 2–7

Material

7 specimens, SNSB–BSPG 2016 XXI 1730–1736.

Description

Shell broadly trochiform with rapidly expanding whorls and gradate spire; one of the better preserved specimens 20 mm wide; earliest whorls clearly exposed due to rapid sinking of suture; whorls ornamented with spiral cords and axial ribs, with nodular intersections; last whorl with rapidly forming wide, oblique ramp; subsutural row of small tubercles; at least 5 slightly knobby spiral cords on ramp; strong keel delimits ramp; keel with rapidly enlarging tubercles (approximately 9 on the last whorl); whorl face below keel vertical and delimited abapically by second knobby keel; at least two weak knobby spiral cords between two keels; a third, somewhat weaker keel forms border to almost flat base; two weak, knobby spiral cords present between second and third keel; base incompletely preserved, covered with several spiral cords; growth lines approximately straight, prosocline; aperture very large, round.

Remarks

Turbo (Sarmaticus) stephanophorus Zittel, 1873 is more slender, it has fewer nodes on the keels and on the base, there is only a single nodular spiral cord visible (= bordering spiral cord)

Nododelphinulidae ? gen. et sp. indet.

Plate 4: figs 8–11

Material

1 specimen, SNSB–BSPG 2016 XXI 1737.

Description

Shell broadly turbiniform, with gradate spire; specimen 17 mm wide; earliest visible ornament consists of two edges, one at about mid-whorl, the other suprasutural; whorl face above adapical edge forms oblique ramp, approximately vertical below edge; nodular spiral cord in subsutural position; between this cord and adapical edge, first one, then a second spiral cord appear on ramp and also on whorl face between edges; whorl face ornamented with widely spaced, bulging axial ribs that continue onto center of base; axial ribs approximately orthocline on whorl face and distinctly opisthocline on base; adapical edge with numerous small nodes in early whorls but fewer and larger nodes on last whorl; same trend on abapical edge, but not as distinct; nodes spirally elongated, tapering in abapertural direction with narrow beginning and trumpet-like widening in apertural direction; spoon-like pits at apertural end of nodes, which terminate abruptly, immediately followed by narrow beginning of next node; widened spoon-like ending of elongate nodes lies at intersection of axial ribs and spiral cords; base flatly convex with angular transition to whorl face; base covered with nodular spiral cords; aperture not preserved.

Remarks

The morphology of the spirally elongated nodes is to our knowledge unique; we know of no other example from the literature.

Superfamily and family unclear

Creniturbo Cossmann, 1919

Type species

Trochus dirce d’Orbigny, 1853; Oxfordian; France.

Creniturbo gibbosus sp. nov.

Plate 4: figs 12–15

Etymology

Latin gibbus – nodes; for the abapical row of large nodes.

Holotype

SNSB–BSPG 2016 XXI 1738 (pl. 4, figs 14–15), collection Lang.

Paratypes

6 specimens from Saal (4 specimens collection Lang: SNSB–BSPG 2016 XXI 1739–1742, 2 specimens collection Sylla: SNSB–BSPG 2016 XXI 1743–1744)

Other material

A questionable specimen from Saal, collection Lang.

Type locality and stratum

Upper Jurassic (Kimmeridgian) reefal limestones from the locality Saal near Kelheim, Lower Bavaria (Gründel et al. 2015, 2022).

Diagnosis

Shell broadly trochiform, gyroscopic; whorl face slightly concave, with several weak spiral lirae; suture shallow, inconspicuous; edge at transition from whorl face to base with 10–13 large rounded nodes, visible slightly above suture in spire whorls; aperture has circular lumen; tongue-shaped callus covers center of base.

Description

Only juvenile specimens at hand are relatively well-preserved; fully grown but poorly preserved specimens up to 16 mm wide; shell broadly trochiform, gyroscopic; whorl face slightly concave; edge at transition from whorl face to base with 10–13 large rounded nodes, visible slightly above suture in spire whorls; suture wavy due to nodes; whorl face covered with very faint spiral lirae (usually not visible due to preservation); it is not certain whether spiral lirae are also present on nodes; base slightly convex and set off from whorl face at an angle; growth lines on base opisthocyrt; spiral lirae probably also present on base, but obscured by preservation; aperture has circular lumen, slightly tapering adapically; tongue-shaped callus covers center of base.

Remarks

Creniturbo dirce (d’Orbigny), the type species and the only other species assigned to Creniturbo, has a double row of nodes at the basal edge and it has a much stronger spiral cords.

Creniturbo sp. 1

Plate 5: figs 1–4

Material

4 specimens from Saal: SNSB–BSPG 2016 XXI 1745–1748 (2 specimens collection Sylla, 1 specimen collection Keupp, 1 specimen collection Lang).

Description

The present specimens are moderately to poorly preserved; shape, size and sculpture correspond – as far as can be seen – to those of the Creniturbo gibbosus n. sp.; however, the present specimens have a more or less distinct spiral cord on the base, directly below the basal edge; additional faint spiral cords obscured by poor preservation present on base; nodes on basal angulation much weaker than in Creniturbo gibbosus.

Plate 5. 

(1, 2) Creniturbo sp., SNSB–BSPG 2016 XXI 1745, lateral and basal views, width 13 mm. (3, 4) Creniturbo sp., SNSB–BSPG 2016 XXI 1746, collection Lang, (3) detail of base, width 3.2 mm, (4) lateral view, width 3.5 mm. (5–7) Kelheimia triangulata sp. nov., holotype, SNSB–BSPG 2016 XXI 1749, (5, 7) lateral and apical views, width 23 mm, (6) apex in lateral view, height 9 mm. (8–10) Kelheimia triangulata sp. nov., paratype, SNSB–BSPG 2016 XXI 1750, lateral, apical and basal views, width 47 mm. (11) Kelheimia triangulata sp. nov., paratype, SNSB–BSPG 2016 XXI 1751, oblique basal view with aperture, height of aperture 32 mm. (12–15) Vetigastropoda gen.and sp. indet., SNSB–BSPG 2016 XXI 1758, (12, 15) lateral and basal views, width 23 mm, (13) detail of lateral view, width 12 mm, (14) detail of ornament, height 10 mm. (16) Parvulatopsis? sp. 1, SNSB–BSPG 2016 XXI 1759, lateral view, width 12 mm.

Remarks

Cerithium binodum Buvignier, 1852 is larger, its base is more convex and it has two rows of nodes on the basal edge. Creniturbo dirce (d’Orbigny) sensu Loriol in Loriol and Koby (1890) is also larger with a double row of nodes on the basal edge and it has strong spiral cords on the base.

Kelheimia gen. nov.

Derivatio nominis

After the city of Kelheim that is close to the Saal quarry.

Type species

Kelheimia triangulata n. sp.; upper Kimmeridgian; South Germany.

Diagnosis

Shell broadly trochiform, conical, slightly coeloconoid with early whorls more slender than late whorls; early whorls with ornament of intersecting spiral cords and axial ribs; late whorls ornamented with few wide spiral cords; transition from whorl face to base at sharp, angular edge; base slightly convex, covered with spiral cords; aperture large with circular lumen and callous inner lip; growth lines straight, prosocline.

Remarks

Pyrgotrochus P. Fischer, 1885 and Conotomaria Cox, 1959 have more evenly increasing whorls, a less pronounced ontogenetic sculptural change, a flat base and a selenizone located well above the abapical suture.

Kelheimia triangulata sp. nov.

Plate 5: figs 5–11

Etymology

Latin triangulus – because of the triangular outline of the shell.

Holotype

SNSB–BSPG 2016 XXI 1749 (Plate 5: figs 5–7).

Paratypes

8 specimens, SNSB–BSPG 2016 XXI 1750–1757.

Type locality and stratum

Upper Jurassic (Kimmeridgian) reefal limestones from the locality Saal near Kelheim, Lower Bavaria (Gründel et al. 2015, 2022).

Diagnosis

As for genus.

Description

Shell broadly trochiform, conical, slightly coeloconoid; a specimen is 48 mm wide; early whorls slender with distinct sutures; later whorls increase more rapidly producing coeloconoid shell shape; late whorls with straight whorl face, separated by inconspicuous sutures; early whorls with edge above mid-whorl separating oblique ramp and vertical abapical whorl face; several spiral cords present on both whorl portions; approximately 9 bulging, relatively wide axial ribs run from suture to suture forming nodes on edge; as width growth accelerates, edge and axial ribs disappear; straight whorl face of late whorls covered with about 8 spiral cords; cords wider than separating furrows; growth lines straight to weakly prosocyrt, prosocline on whorl face and base; transition from whorl face to base at sharp, angular edge; base anomphalous, slightly convex, covered with wide spiral cords; aperture large with circular lumen and callous inner lip.

Remarks

Brachytrema (Petersia) sp. sensu Hägele (1997) has bulgy axial ribs on the last whorls and severeal folds inside the aperture (on olumella and outer lip). In Pyrgotrochus cyproea (d’Orbigny) sensu Fischer and Weber (1997), the whorls are has regularly increasing in width, it has a selenizone, its ornament does not show ontogenetic change, and its spiral cords are narrower. Pleurotomaria berlieri Loriol in Loriol and Girardot (1903) (based on a steinkern) is larger, lacks distinct ornamentation, and its aperture has an edge.

Vetigastropoda gen. et sp. indet.

Plate 5: figs 12–15

Material

1 specimen, SNSB–BSPG 2016 XXI 1758.

Description

Shell broadly trochiform, 22 mm high; whorls low, angulated somewhat above abapical suture; edge covered with numerous nodules, possibly representing base of hollow spines; two weak subsutural spiral cords without nodes appear on last whorl; whorl face straight and without sculpture between basal edge and abapical spiral cord; nodular basal edge emerges at suture; base flat, concave in center; transition from whorl face to base angular; base without visible ornament; aperture not preserved.

Remarks

This specimen resembles the Triassic genera Ampezzalina Bandel, 1993 and Bandelastraea Nützel & Kaim, 2014 (see Karapunar and Nützel 2021, figs 78, 79) but its preservation is too poor for identification.

Subclass Neritimorpha Koken, 1896

Superfamily Neritoidea Rafinesque, 1815

Family Pileolidae Bandel, Gründel & Maxwell, 2000

Dauterria Gründel, Keupp & Lang, 2015

Type species

Dauterria variocostata Gründel, Keupp & Lang, 2015; upper Kimmeridgian; South Germany.

Dauterria rotundata Gründel, Keupp & Lang, 2015

pl. 1: figs 1–4 in Gründel et al. (2015)

1997 Pileolus (Pileolus) minutus Zittel, 1873 – Hägele: 60, fig. p. 60, lower left.

2015 Dauterria rotundata n. sp. – Gründel, Keupp and Lang: 79, pl. 1, figs 1–4.

2017 Dauterria rotundata Gründel, Keupp & Lang, 2015 – Gründel: 30, pl. 8, fig. A.

Material

SNSB–BSPG 2016, Saal: 30 mostly juvenile specimens; „Sohle 2 über Korallenstock“ (= level 2 above coral block): 5 specimens.

Dauterria variocostata Gründel, Keupp & Lang, 2015

pl. 1: figs 5–9 in Gründel et al. (2015)

2015 – Dauterria variocostata n. sp. – Gründel, Keupp and Lang: 80, pl. 1, figs 5–9.

Material

3 specimens, SNSB–BSPG 2016 XXI.

Pileopsella Gründel, 2004

Type species

Pileolus laevis Sowerby, 1823; Bathonian; England.

Pileopsella biconvexa Gründel, Keupp & Lang, 2015

pl. 1: figs 10–13 in Gründel et al. (2015)

2015 Pileopsella biconvexa n. sp. – Gründel, Keupp and Lang: 82, pl. 1, figs 10–13.

Material

5 specimens, SNSB–BSPG 2016 XXI.

Family Parvulatopsidae Gründel, Keupp & Lang, 2015

Parvulatopsis Gründel, Keupp & Lang, 2015

Type species

Parvulatopsis quinquecostatus Gründel, Keupp & Lang, 2015; upper Kimmeridgian; South Germany.

Parvulatopsis quinquecostatus Gründel, Keupp & Lang, 2015

pl. 8: figs 1–7 in Gründel et al. (2015)

2015 Parvulatopsis quinquecostatus n. sp. – Gründel, Keupp and Lang: 85, pl. 8, figs 1–7.

2017 Parvulatopsis quinquecostatus Gründel, Keupp & Lang, 2015 – Gründel: 30, pl. 9, fig. A.

Material

5 specimens, SNSB–BSPG 2016 XXI.

Parvulatopsis ? sp.

Plate 5: fig. 16; Plate 6: figs 1, 2

Material

5 juvenile specimens, SNSB–BSPG 2016 XXI 1759–1763.

Description

Shell-broadly turbiniform, egg-shaped, low-spired with rapidly increasing whorls; largest specimen 12 mm wide; smallest specimen 7 mm wide (best preserved one); whorls convex; suture sinks significantly during ontogeny; whorl face ornamented with 5 strong, knobby spiral cords; distances between adapical suture and adapical spiral cord as well as between this and the 2nd spiral cord particularly wide; this portion of whorl face distinctly oblique; whorl face vertical between 2nd and 3rd spiral cords; 4–6 weak spiral cords without nodes between strong spiral cords; growth lines straight, prosocline from adapical suture to center of the base.

Plate 6. 

(1, 2) Parvulatopsis? sp. 1, SNSB–BSPG 2016 XXI 1759, lateral and apical views, width 12 mm. (3) Neridomus hemisphaerica (Roemer, 1836), SNSB–BSPG 2016 XXI 1764, lateral view, width 33 mm. (4, 5) Neridomus hemisphaerica (Roemer, 1836), SNSB–BSPG 2016 XXI 651, lateral views, height 35 mm. (6, 7) Neridomus hemisphaerica (Roemer, 1836) with color pattern, SNSB–BSPG 2016 XXI 1765, lateral and apical views, width 36 mm. (8–12) Neritopsis ? rotundatus sp. nov., holotype, SNSB–BSPG 2016 XXI 1767, (8–10) abapertural, apertural and apical views, width 15 mm, (11) detail in oblique apical view, width 11 mm, (12) basal view, width 15 mm. (13, 14) Wallowiella (Plicaropsis) cancellata (Stahl, 1824) (adult), SNSB–BSPG 2016 XXI 1773, lateral and basal views, width 21 mm.

Remarks

Juvenile specimens of Bipartopsis robustus Gründel et al., 2015 are smaller, the distances between the strong spiral cords are approximately the same but overall narrower than in Parvulatopsis? sp. and the adapical whorl face is not as oblique (in lateral view). Neritopsis jurensis Münster sensu Kuhn (1939) has 3 spiral cords at equal distances on the whorl face and strong axial ribs (according to the description, not visible in Kuhn’s (1939) illustration).

Family Neridomidae Bandel, 2008

Neridomus Morris & Lycett, 1851

Type species

Neridomus anglica Cox & Arkell, 1950 = Nerita (Neridomus) hemisphaerica Roemer sensu Morris & Lycett, 1851; middle Jurassic; England.

Neridomus hemisphaerica (Roemer, 1836)

Plate 6: figs 3–7

2019 Neridomidae oder Naticidae – Werner: 21, figs 15–16.

2019 Gastropode non det. – Werner: 21, fig. 17.

Material

10 specimens (illustrated ones SNSB–BSPG 2016 XXI 651, 1764–1765) from Saal.

Description

Shell oblique oval in lateral view, somewhat wider than high, with convex whorls; periphery low on whorls; largest specimen 39 mm high; spire very low; very large body whorl, embracing most of previous whorls; sutures very shallow, indistinct; aside from growth lines, no sculpture visible; growth lines prosocline and weakly prosocyrt from adapical suture to center of the base; aperture teardrop-shaped with strongly and asymmetrically convex outer lip and almost straight inner lip; aperture pointed adapically and broadly rounded abapically; callus very wide with a concave-convex outer edge; color patterns of irregular patches preserved on several specimens.

Remarks

It is possible that Neridomus hemisphaerica is identical with Neridomus sp. 1 as reported by Gründel et al. (2015) that had been only known from two poorly preserved specimens which are smaller and have an approximately evenly convex outer edge of the callus (maybe due to preservation). The numerous described but feature-poor Neridomus species show only few characters and can hardly be reliably distinguished from each other based on the literature. The present assignment to Neridomus hemisphaerica Roemer is not certain. Roemer (1836) described this taxon from the Portlandian. According to his illustrations, the present material could be identical with Roemer’s (1836) taxon. Hardly distinguishable forms have been repeatedly reported from the Upper Jurassic (e. g., Loriol 1881; Loriol in Loriol and Bourgeat 1886); Pčelintsev 1926; Cox 1965; Fischer and Weber 1997).

Superfamily Neritopsoidea Gray, 1847

Family Neritopsidae Gray, 1847

Subfamily Neritopsinae Gray, 1847

Neritopsis Grateloup, 1832

Type species

Neritopsis moniliformis Grateloup, 1832; Tertiary; France.

Neritopsis ? rotundatus sp. nov.

Plate 6: figs 8–12

2017 Metriomphalidae n. gen.? sp. 1 – Gründel, Keupp and Lang: 203, pl. 15, figs 8–13.

Etymology

Latin rotundatum – rounded (because of the round shell shape).

Holotype

SNSB–BSPG 2016 XXI 1767 (Plate 6: figs 8–12).

Paratypes

5 specimens from Saal. SNSB–BSPG 2016 XXI 1768–1772.

Type locality and stratum

Upper Jurassic (Kimmeridgian) reefal limestones from the locality Saal near Kelheim, Lower Bavaria (Gründel et al. 2015, 2022).

Diagnosis

Shell neritiform, low-spired with large last whorl that is evenly convex (from adapical suture to the center of the base) and evenly covered with more than 15 spiral cords; spiral cords are about as wide as spiral furrows separating them; spiral cords entirely covered with small nodes; axial ribs absent; no callous formations visible in apertural area.

Description

Shell neritiform, holotype (largest specimen) 14 mm wide and high;

late whorls strongly and evenly convex (including base); in some specimens, a spiral cord is reinforced near adapical suture, slightly angulating whorl face and delimiting a ramp with several spiral cords; first recognizable sculpture consists of 4–6 spiral cords lacking nodes; cords almost equally strong or alternation of stronger and weaker cords; further spiral cords evenly cover whorl face and base; holotype has 18 spiral cords from adapical suture to center of base; during growth, spiral cords become equal in strength; numerous small, densely packed nodes present on spiral cords of last whorl; nodes have deep pit in apertural direction, thus resembling short hollow spines; axial ribs absent, only weakly reinforced growth lines can be seen in spiral furrows; whorl face and base evenly rounded; base anomphalous; aperture broadly oval, slightly tapering adapically and widely rounded abapically; callous formations lacking.

Remarks

Neritopsis buchini Guirand & Ogérien, 1865 has fewer spiral cords, the spiral cords are wider than the separating grooves, the tubercles are less numerous and not as distinct. Neritopsis buchini sensu Loriol in Loriol and Bourgeat (1886–1888) also has fewer spiral cords. The spiral cords of Neritopsis buchini are significantly narrower than the spiral grooves separating them and there are fewer nodes on the spiral cords. Neritopsis imbricata Étallon sensu Loriol in Loriol and Bourgeat (1886–1888) has a more inflated last whorl, the nodes on the spiral cords are smaller and more numerous. Neritopsis imbricata sensu Zittel (1873) has a more transversely elongated shell shape, the outer lip of the aperture is strongly asymmetrically convex with the periphery is low on the whorls. Nerita goldfussi Keferstein sensu Goldfuss, (1844) is adapically flattened with a sunken apex and fewer spiral cords of variable thickness. The aperture of Neritopsis ? rotundatus n. sp. seems to be asymmetrical and not symmetrical as would be typical for the genus Neritopsis (see Kaim and Sztajner 2005).

Subfamily Cassianopsinae Bandel, 2007

Genus Wallowiella Frýda, Blodgett & Stanley, 2003

Wallowiella (Plicaropsis) Gründel, Keupp & Lang, 2015

Type species

Neritites cancellatus Stahl, 1824; upper Kimmeridgian; South Germany.

Wallowiella (Plicaropsis) cancellata (Stahl, 1824)

Plate 6: figs 13, 14 (adult), Plate 7: figs 1, 2 (juvenile)

2015 Wallowiella (Plicaropsis) cancellata (Stahl, 1824) – Gründel, Keupp and Lang: 88, pl. 4, figs 5–14; pl. 5, figs 1–4 (here more synonymy and chresonymy).

2016 Wallowiella (Plicaropsis) cancellata Stahl, 1824) – Gründel, Hostettler and Menkveld-Gfeller: 510, pl. 5, figs 5–11.

2017 Wallowiella (Plicaropsis) cancellata (Stahl, 1824) – Gründel: 30, pl. 9B.

Material

Total of 27 specimens; 17 specimens from Saal; 10 specimens from Saal level 4, location 1 (“Sohle 4, Fundstelle 1”); 2 specimens figured: SNSB–BSPG 2016 XXI 1773–1774.

Plate 7. 

(1, 2) Wallowiella (Plicaropsis) cancellata (Stahl, 1824) (juvenile), SNSB–BSPG 2016 XXI 1774, abapertural and apertural views, width 10 mm. (3, 4) Wallowiella (Plicaropsis) compacta Gründel, Keupp & Lang, 2015, SNSB–BSPG 2016 XXI 1775 (collection Lang), lateral and axial views, width 17 mm. (5–7) Wallowiella (Plicaropsis) compacta Gründel, Keupp & Lang, 2015, c SNSB–BSPG 2016 XXI 1776, abapertural and apertural views, width 18 mm. (8–10) Hayamiella subvaricosa (Brösamlen, 1909), SNSB–BSPG 2016 XXI 1777, abapertural, apertural and apical views, width 18 mm. (11, 12) Hayamiella? sp., SNSB–BSPG 2016 XXI 1778, abapertural and apical views, width 11 mm.

Remarks

Many of the studied specimens from the Sylla collection differ from those reported by Gründel et al. (2015) by having an alternation of weak and strong spiral cords. These weaker spiral cords are, however, distinctly stronger than the lirae of Hayamiella schaeferi Gründel et al., 2015 in the same position. The nodes at the intersections of axial ribs and spiral cords are sometimes elongated like spines. The attribution of the present material to the species Wallowiella (Plicaropsis) cancellata is supported by the square pits formed by axial ribs and spiral cords on the shell and the formation of a knob on the outer lip.

Wallowiella (Plicaropsis) compacta Gründel, Keupp & Lang, 2015

Plate 7: figs 3–7

2015 Wallowiella (Plicaropsis) compacta n. sp. – Gründel, Keupp and Lang: 89, pl. 5, figs 5–9.

Material

1 specimen from the Sylla collection and 1 from the Lang collection, SNSB–BSPG 2016 XXI 1775–1776.

Remarks

Here, we illustrate two additional well-preserved specimens for a better understanding of the species.

Cassianopsis Bandel, 2007

Type species

Naticella armata Münster, 1841; upper Triassic; St. Cassian Formation (Italy).

Cassianopsis quenstedti (Brösamlen, 1909)

pl. 2: figs 10–14; pl. 3: figs 1–6 in Gründel et al. (2015)

2015 Cassianopsis quenstedti (Brösamlen, 1909) – Gründel, Keupp and Lang: 92, pl. 2, figs 10–14; pl. 3, figs 1–6 (here more synonymy and chresonymy).

Material

2 specimens, SNSB–BSPG 2016 XXI.

Cassianopsis ratua Gründel, Keupp & Lang, 2015

pl. 3: figs 7–11 in Gründel et al. (2015)

2015 Cassianopsis ratua n. sp. – Gründel, Keupp and Lang: 94, pl. 3, figs 7–11.

Material

1 specimen, SNSB–BSPG 2016 XXI.

Hayamiella Kase, 1984

Type species

Neritopsis (Hayamiella) japonica Kase, 1984; Early Cretaceous; Japan.

Hayamiella schaeferi Gründel, Keupp & Lang, 2015

pl. 5: figs 10–15; pl. 6, fig. 1 in Gründel et al. (2015)

2015 Hayamiella schaeferi n. sp. – Gründel, Keupp and Lang: 96, pl. 5, figs 10–15; pl. 6, fig. 1.

Material

6 specimens and a cast of an imprint (imprint not at hand), SNSB–BSPG 2016 XXI.

Hayamiella decussata (Münster, 1844 in Goldfuss)

pl. 7: figs 1–4, pl. 8: figs 8–11 in Gründel et al. (2015)

2015 Hayamiella decussata (Münster in Goldfuss, 1844) – Gründel, Keupp and Lang: 98, pl. 7, figs 1–4; pl. 8, figs 8–11 (here more synonymy and chresonymy).

Material

1 specimen, SNSB–BSPG 2016 XXI.

Hayamiella subvaricosa (Brösamlen, 1909)

Plate 7: figs 8–10

1909 Neritopsis subvaricosa n. sp. – Brösamlen: 243, pl. 19, fig. 29.

1997 Neritopsis subvaricosa Broesamlen, 1909 – Hägele: 57, fig. p. 57, upper left, pl. 7, fig. 2.

Material

4 specimens and a cast of an imprint (imprint not at hand); illustrated specimen SNSB–BSPG 2016 XXI 1777.

Remarks

This species was not available for the study of Gründel et al. (2015). Brösamlen (1909) gave an accurate description. In the material at hand, only the illustrated specimen is almost complete. The aperture is rounded with a strongly convex outer lip. The callus is only partially preserved. At least three of the specimens are adults with a width of 16–17 mm. This species differs from the similar Hayamiella semiplicata (Brösamlen, 1909) by having fewer axial ribs (about 7–8 per whorl) and the axial ribs do not become weaker during late ontogeny.

Hayamiella semiplicata (Brösamlen, 1907)

pl. 6: figs 2–15 in Gründel et al. (2015)

2017 Hayamiella semiplicata (Brösamlen, 1907) – Gründel, Keupp and Lang: 100, pl. 6, figs 2–15 (here more synonymy and chresonymy).

Material

1 specimen, SNSB–BSPG 2016 XXI.

Remarks

In the present specimen, the reduction of the axial ribs occurs very early. Approximately 4/5ths of the last whorl have no axial ribs.

Hayamiella ? sp.

Plate 7: figs 11, 12

1997 Neritopsis sp. 1 – Hägele: 58, fig. p. 58, upper left, pl. 7, fig. 5.

Material

2 specimens, illustrated specimen SNSB–BSPG 2016 XXI 1778.

Description

Shell neritiform, low-spired, apex almost flat, barely protruding last whorl in lateral view; larger shell 11 mm wide; wide ramp is inclined towards whorl axis; ornament of last whorl consists of 5 strong spiral cords approximately equally spaced; approximately 10 strong, widely spaced axial ribs run from adapical suture to center of base; intersections of strong spiral cords and axial ribs nodular; several weak spiral cords on ramp and between two strong spiral cords of rest of shell; intersections these weak spiral cords with axial ribs lack nodes; aperture unknown.

Remarks

Neritopsis cottaldina d’Orbigny, 1852 as illustrated by Loriol in Loriol and Bourgeat (1886–1888, figs 3–4, non figs 1–2, 5) resembles Hayamiella? sp. 1, but has a distinctly elevated spire and more axial ribs per whorl.

Bipartopsis Gründel, Keupp & Lang, 2015

Type species

Bipartopsis robustus Gründel, Keupp & Lang, 2015; upper Kimmeridgian; South Germany.

Bipartopsis robustus Gründel, Keupp & Lang, 2015

pl. 7: figs 5–15 in Gründel et al. (2015)

2015 Bipartopsis robustus n. sp. – Gründel, Keupp and Lang: 55, pl. 7, figs 5–15.

Material

1 juvenile specimen, SNSB–BSPG 2016 XXI.

Subclass Caenogastropoda Cox, 1960

Cohort Sorbeoconcha Ponder & Lindberg, 1997

Superfamily unclear

Family Brachytrematidae Cossmann, 1906

Subfamily Brachytrematinae Cossmann, 1906

Saalensia Gründel, Keupp & Lang, 2019

Type species

Saalensia birugata Gründel, Keupp & Lang, 2019; upper Kimmeridgian; South Germany.

Saalensia birugata Gründel, Keupp & Lang, 2019

Plate 8: fig. 1

2019 Saalensia birugata n. sp. – Gründel, Keupp and Lang: 101, pl. 1, figs 10–16 (here more chresonymy and synonymy).

2020b Saalensia birugata Gründel, Keupp and Lang – Gründel, Hostettler and Menkveld-Gfeller: 111, pl. 1, figs 10–12.

Material

22 specimens, illustrated specimen SNSB-BSPG 2016 XXI 1779.

Plate 8. 

(1) Saalensia birugata Gründel, Keupp & Lang, 2019, SNSB-BSPG 2016 XXI 1779, lateral view, height 16 mm. (2–4) Loriolotrema sp., SNSB-BSPG 2016 XXI 1780, apertural, apical and basal view, width 18 mm. (5) Brachytrematidae? gen. and sp. indet., SNSB-BSPG 2016 XXI 1781, abapertural view, height 29 mm. (6, 7) Oonia kimmeridgiensis sp. nov., holotype, SNSB-BSPG 2016 XXI 1791, apertural and abapertural, height 18 mm. (8, 9) Globularia? sp., SNSB-BSPG 2016 XXI 1794, abapertural and oblique lateral view, width 42 mm. (10, 11) Pictavia? sp., SNSB-BSPG 2016 XXI 1790, abapertural and oblique abapertural view, height 20 mm. (12) Eustoma sp., SNSB-BSPG 2016 XXI 1801, apertural view, height 24 mm. (13, 14) Eustoma sp., SNSB-BSPG 2016 XXI 1802, (13) lateral view, height 31 mm, (14) basal view, width 10 mm. (15–17) Eustoma ? gracilis sp. nov., holotype, SNSB-BSPG 2016 XXI 1804, (15–16) basal and lateral view, width 18 mm, (17) detail of ornament of last whorl, height 15 mm.

Remarks

The weakening of the abapical strong spiral cord can begin in relatively early whorls. The adapical spiral cord then protrudes.

Subfamily Loriolotrematinae Gründel, Hostettler & Menkveld-Gfeller, 2020

Loriolotrema Gründel, Hostettler & Menkveld-Gfeller, 2020

Type species

Loriolotrema liriola Gründel, Hostettler and Menkveld-Gfeller, 2020; Oxfordian; Switzerland.

Loriolotrema sp.

Plate 8: figs 2–4

Material

1 specimen, SNSB-BSPG 2016 XXI 1780.

Description

Shell broadly biconical, with gradate spire, 17 mm high, whorls low, rapidly increasing in width; edge at about mid-whorl of first preserved whorls, delimiting oblique ramp from approximately vertical abapical portion; weak spiral cords present on both sides of edge; orthocline axial ribs run from suture to suture, with wide interspaces; nodes at intersections of ribs and edge; edge strengthened during ontogeny and axial ribs become broadly bulging and blurred; nodes on intersections of ribs and edge become larger, rounder and also include the spiral cord located between edge and bordering spiral cord as well as bordering spiral cord; several spiral cords can be seen on wide, oblique ramp; base slightly convex with 4 (5?) spiral cords broken down into individual segments; spiral cords on base crossed by weakly strengthened growth lines; base phaneromphalous; aperture strongly damaged.

Remarks

Loriolotrema ? nodosa Gründel, Hostettler and Menkveld-Gfeller is larger, the strong enlargement of the nodes begins later in ontogeny, the spiral cords on the base are not divided into partial segments. Brachytrema kobyi Loriol in Loriol and Koby (1889) is more slender, the whorls have a stronger keel and the base has more and unsegmented spiral cords. Brachytrema filosum (Buvignier) sensu Cossmann (1913) is more slender, has more spiral cords on the base, the axial ribs are not as wide and the nodes on the edge are not as large.

Brachytrematidae ? gen. and sp. indet.

Plate 8: fig. 5

Material

1 specimen, Saal, SNSB-BSPG 2016 XXI 1781.

Description

Shell turbiniform, 29 mm high, only partly preserved; whorls convex with numerous spiral cords and widely spaced axial ribs; first recognizable sculpture consists of edge directly above abapical suture; several weak spiral cords and axial ribs between edge and abapical suture; in the course of ontogeny, a spiral cord above edge and a weakly tubercular spiral cord appears between both; several spiral cords between edge and abapical suture; axial ribs become bulging and form rounded nodes at intersections with edge and several spiral cords on both sides of edge; adapical end of ribs thickened, node-like; some axial ribs thickened, varix-like; faint spiral lirae (that cannot be seen in detail due to preservation) between adapical suture and edge; spiral cord at border to base nodular; base slightly convex, with remains of spiral cords but shell largely chipped off so that only steinkern is exposed there.

Subcohort Campanilimorpha Haszprunar, 1988

Superfamily Campaniloidea Douvillé, 1904

Family Ampullinidae Cossmann, 1919 in Cossmann and Peyrot

Subfamily Ampullospirinae Cox, 1930

Pictavia Cossmann, 1925

Type species

Natica pictaviensis d’Orbigny, 1852; Bathonian; France.

Pictavia lactera Gründel, Keupp & Lang, 2019

pl. 3: figs 1–4 in Gründel et al. (2019)

2019 – Pictavia lactera n. sp. – Gründel, Keupp and Lang: 105, pl. 3, figs 1–4.

Material

8 specimens, SNSB-BSPG 2016 XXI 1782–1789.

Remarks

The Sylla collection contains additional poorly or fragmentarily preserved specimens that are similar in size and shape to those reported by Gründel et al. (2019). However, in the present specimens, a subsutural groove that is present in the material reported by Gründel et al. (2019) cannot be recognized. It is unclear whether this lack represents a genuine characteristic of another taxon or intraspecific variability, or is due to preservation.

Pictavia silicea (Quenstedt, 1858)

2019 Pictavia silicea (Quenstedt, 1858) – Gründel, Keupp and Lang: 105, pl. 2, figs 17–18 (here more chresonymy and synonymy).

Material

1 specimen, SNSB-BSPG 2016 XXI.

Pictavia ? sp.

Plate 8: figs 10, 11

Material

1 specimen, SNSB-BSPG 2016 XXI 1790.

Description

Shell naticiform, egg-shaped, significantly higher than wide, 20 mm high; spire small; whorl face convex; sutures distinctly deepened; last whorl very large, inflated, higher than wide but distinctly elevated; transition from whorl face to strongly convex base evenly convex; shell smooth; growth lines not visible; aperture not preserved or covered with rock.

Remarks

Natica amata d’Orbigny sensu Loriol in Loriol and Bourgeat (1886–1888) is larger and has higher spire whorls; its last whorl is higher than wide.

Oonia Gemmellaro, 1878

Type species

Melania abbreviata Terquem, 1855 (= Pseudomelania hettangiensis Cossmann, 1909); lower Jurassic; France.

Oonia kimmeridgiensis sp. nov.

Plate 8: figs 6, 7

Etymology

After the Kimmeridgian stage.

Holotype

SNSB-BSPG 2016 XXI 1791.

Paratypes

2 specimens, SNSB-BSPG 2016 XXI 1792–1793.

Type locality and stratum

Upper Jurassic (Kimmeridgian) reefal limestones from the locality Saal near Kelheim, Lower Bavaria (Gründel et al. 2015, 2022).

Diagnosis

Shell slender, oval; spire whorls low; body whorl much higher than spire, with weakly, evenly convex whorl face.

Description

Shell slender, oval, higher than wide; holotype 18 mm high; sutures distinct; body whorl nearly two times higher than spire, with weakly, evenly convex whorl face; periphery low on whorl; transition from whorl face to base evenly rounded; base stronly convex; shell smooth; growth lines weakly parasigmoidal; aperture incomplete, probably teardrop-shaped.

Remarks

Similar species (e. g., Oonia guirandi Loriol in Loriol and Bourgeat 1886–1888, Pseudomelania (Oonia) cornelia (d’Orbigny) sensu J.–C. Fischer et al. (2001) and Fischer and Weber 1997, Ampullospira (Pictavia) calypso (d’Orbigny) sensu Fischer and Weber 1997) usually have higher spire whorls, but above all, a wider and more convex body whorl.

Subfamily Globulariinae Wenz, 1941

Globularia Swainson, 1840

Type species

Globularia fluctuata (Sowerby); recent.

Globularia ? sp.

Plate 8: figs 8, 9

Material

1 specimen, SNSB-BSPG 2016 XXI 1794.

Description

Specimen largely preserved as steinkern, 42 mm wide, egg-shaped, much wider than high, low-spired; whorls rapidly increasing, convex, without visible ornament; spire whorls low; sutures shallow but distinct; last whorl large, largely covering previous ones; transition from whorl face to base evenly convex; outer lip of aperture extends far anteriorly, curved asymmetrically, with greatest width low on whorl; outer lip of aperture shows course of growth lines: almost orthocline, opisthocyrt in adapical part of whorl, prosocyrt in abapical part; aperture not exposed.

Remarks

Neridomus canalifera (Buvignier) sensu Gründel et al. (2016) is significantly wider in relation to the height and the outer lip is not as asymmetrically curved. Neritoma (Neridomus) ovula (Buvignier) sensu Fischer and Weber (1997) is smaller and the last whorl is higher. Nerita neumeyri Zittel, 1873 is higher in relation to its width and the spire is less elevated. The present species could well belong to Neritimorpha, for instance the Palaeozoic/ Triassic genus Naticopsis is similar. Specimens with known aperture would be needed for a safer systematic placement.

Family Tylostomatidae Stoliczka, 1868

Tylostoma Sharpe, 1849

Type species

Tylostoma globosum Sharpe, 1849; Turonian; Portugal.

Tylostoma sp. 1

pl. 3, fig. 19, pl. 4: figs 1–3 in Gründel et al. (2019)

2017 Pictavia sp. – Gründel: 32, pl. 11, fig. C.

2019 Tylostoma sp. 1 – Gründel, Keupp and Lang: 109, pl. 3, fig. 19, pl. 4, figs 1–3.

Material

6 specimens, SNSB-BSPG 2016 XXI 1794–1800 (5 specimens collection Sylla, 1 specimen collection Keupp).

Subcohort Cerithimorpha Golikov & Starobogatov, 1975

Taxa of uncertain placement

Family Eustomatidae Cossmann, 1906

Eustoma Piette, 1855

Type species

Eustoma tuberculosa Piette, 1855; Bathonian; France.

Eustoma sp.

Plate 8: figs 12–14

Material

3 specimens, SNSB-BSPG 2016 XXI 1801–1803.

Description

Shell high-spired, slender, with gradate spire and narrow ramp; a specimen 31 mm high; shell sides straight; whorl face with strong axially elongated subsutural nodes (9–10 per whorl) extending over more than of whorl height; broad, sometimes slightly nodular spiral cord at rounded angular transition to base; base slightly convex; whorls face and densely covered with spiral cords of variable strength separated by narrow furrows; aperture incompletely preserved with straight siphonal canal.

Remarks

Ditretus sp., cf. rostellaria (Buvignier, 1852) has a similar ornament but differs in its stouter (less slender) shell shape, in having fewer whorls, a more delicate sculpture, and a very short abapical canal. Eustoma tuberculosa Piette, 1855 is larger and more slender, the aperture of adult specimens terminates adapically in a long, triangular extension. Diatinostoma aff. germaini Étallon sensu Yin (1931) has a wider, more triangular shell shape, spiral cords are largely missing, the transition from whorl face to base has a clear cord-like edge.

Eustoma ? gracilis sp. nov.

Plate 8: figs 15–17

Etymology

Latin gracilis – slender; because of the slender shell shape.

Holotype

SNSB-BSPG 2016 XXI 1804.

Paratypes

4 specimens, SNSB-BSPG 2016 XXI 1805–1807.

Type locality and stratum

Upper Jurassic (Kimmeridgian) reefal limestones from the locality Saal near Kelheim, Lower Bavaria (Gründel et al. 2015, 2022).

Diagnosis

Shell moderately high-spired, relatively large and slender; whorls increase evenly in width; whorl face without distinct spiral cords; subsutural nodes become particularly large on the last whorls; transition from whorl face to base evenly rounded, with nodular spiral cord; base covered with nodose spiral cords, increasingly weaker towards center of base; nodes connected by bulbous, opisthocline axial ribs.

Description

Shell moderately high-spired, slender, with acute apex; large specimen 45 mm high; early whorls poorly preserved, with straight whorl face; late whorls with subsutural row of large rounded, axially elongated nodes (9–10 per whorl), giving spire gradate appearance by forming narrow ramp; subsutural nodes extending over more than half of whorl face height; suprasutural spiral cord with weaker and more numerous nodes; transition from whorl face to convex base evenly rounded; base with knobby spiral cords; spiral cords on base becoming weaker towards center of base while nodes on them become smaller; nodes connected by bulbous opisthocline axial ribs; whorls probably also with fine spiral lirae (obscured by poor preservation); base apparently with narrow umbilicus; aperture not preserved.

Remarks

Ditretus sp., cf. rostellaria (Buvignier) sensu Gründel et al. (2019) is smaller, the strong abapical spiral cord lies directly at the suture and has larger tubercles, on the base a third, clearer and tuberculated spiral cord is formed, the spiral cords on the base are more numerous and are not nodular, the flanks are covered with weak spiral cords. Cerithium rostellaria Buvignier, 1852 has smaller subsutural nodes, the whorls are angulated by the nodes, and axial ribs are missing on the base. Cerithium schardti Loriol in Loriol and Koby (1895) has smaller and barely abapically elongated nodes; it lacks a knobby spiral cord at the transition from whorl face to base and axial ribs on the base. Cerithium kelheimense Schlosser, 1882 is smaller and the shell is covered with weak spiral cords and it lacks a knobby spiral cord at the transition from whorl face to base. Ditretus nodosostriatus Peters sensu Yin (1931) has smaller and more numerous subsutural nodes, 1–2 spiral cords above the abapical suture; its base is unknown. Ditretus thurmanni Loriol sensu Yin (1931) is smaller, the nodes form only an indistinct ramp; it has 1–2 spiral ribs with small nodes between the upper row of nodes and the abapical suture. Nerinea orbignyana Zeuschner, 1850 has a series of small nodes above the abapical suture, the base is almost flat and lacks sculpture.

Ditretus Piette, 1875

Type species

Cerithium rostellaria Buvignier, 1852; Oxfordian; France.

Ditretus sp., cf. rostellaria (Buvignier, 1852)

Plate 9: figs 1–4

?1931 Ditretus valenensis n. sp. – Yin: 46, pl. 4, figs 1–3.

2019 Ditretus sp., cf. rostellaria (Buvignier, 1852) – Gründel, Keupp and Lang: 110, pl. 4, figs 4–7.

Material

11 specimens, SNSB-BSPG 2016 XXI 1808–1818.

Description

The description is based on specimens with relatively stout shell shape; shell acutely trochiform, stout, with few whorls; last whorl higher than spire; a specimen is 23 mm high (apex missing); whorl face of spire whorl low; shell sides straight (side view); whorl face with subsutural row of large, rounded nodes (approximately 10 nodes per whorl) with steep adapical slope producing ramp that accentuates suture; whorls including nodes covered with numerous weak spiral lirae; transition from whorl face to base rounded; nodular spiral cord at transition to base and a weaker one below it are more or less clearly developed (probably intraspecific variation); base also covered with spiral lirae; fully grown specimens with distinctly widened, large and rounded aperture; inner and outer lip strongly thickened and broadened; columellar inner lip is also thickened and somewhat detached; short abapical canal hardly visible in apertural view because canal is almost closed.

Plate 9. 

(1, 2) Ditretus sp., cf. rostellaria (Buvignier, 1852), SNSB SNSB-BSPG 2016 XXI 1808, (1) lateral view, height 25 mm, (2) detail of ornament, height 12 mm. (3, 4) Ditretus sp., cf. rostellaria (Buvignier, 1852), SNSB-BSPG 2016 XXI 1809, lateral views, height 23 mm. (5) Cryptoptyxis ? spinosus sp. nov., holotype, SSNSB-BSPG 2016 XXI 1824, apertural and abapertural lateral views, height 22 mm. (6, 7) Coninoda strekwera Gründel, Keupp & Lang, 2019, SNSB-BSPG 2016 XXI 1827, lateral view and longitudinal section, height 33 mm. (8, 9) Tropacerithium cumaritum Gründel, Keupp & Lang, 2019, SNSB-BSPG 2016 XXI 1830, (8) detail of last whorl, height 4 mm, (9) lateral view, height 7 mm. (10–12) Exelissa ? aff. corallense (Buvignier, 1843), SNSB-BSPG 2016 XXI 1835, locality 1985, above coral stock, level 2 (“Fundort 1985, über Korallenstock, Sohle 2”), (10) lateral view, height 12 mm, (11) apex in lateral view, height 5 mm, (12) last two whorls in lateral view, height 7 mm. (13, 14) Exelissa ursicina (Loriol in Loriol and Koby 1889), SNSB-BSPG 2016 XXI 1836, (13) lateral view, height 10 mm, (14) basal view, width 4.5 mm. (15–17) Turritella lucagrita sp. nov., holotype, SNSB-BSPG 2016 XXI 1840, (15) lateral view, height 75 mm, (16) earliest preserved whorls in lateral view, height 40 mm, (17) last whorls in lateral view, height 46 mm. (18) Nudivagus? sp. 2, SNSB-BSPG 2016 XXI 1844, lateral view, height 35 mm. (19) Neuburgensia angulata sp. nov., paratype, SNSB-BSPG 2016 XXI 1848, collection Lang, last whorl with aperture, height 6 mm.

Remarks

Ditretus rostellaria Buvignier, 1852 differs in having whorls that are angulated at a row of nodes, its shell is more slender, the columellar inner lip is neither thickened nor detached according to the illustrations. Diatinostoma germaini Étallon sensu Yin (1931) largely lacks spiral cords and its aperture is unknown. Ditretus valenensis Yin, 1931 is similar (identical?) to the variant with a knobby spiral cord at the transition from whorl face to base. Ditretus thurmanni Loriol in Loriol and Koby sensu Gründel et al. (2022) is more slender and has more whorls.

Family Maoraxidae Bandel, Gründel & Maxwell, 2000

Cryptoptyxis Cossmann, 1906

Type species

Cerithium wrighti Étallon, 1859; Kimmeridgian; France.

Cryptoptyxis rarenodosa Gründel, Keupp & Lang, 2019

pl. 4: figs 17–20, pl. 5: figs 1–5 in Gründel et al. (2019)

2017 Cryptoptyxis sp. – Werner, Nützel and Nose: 32, Abb. 3D.

2019 Cryptoptyxis rarenodosa n. sp. – Gründel, Keupp and Lang: 114, pl. 4, figs 17–20, pl. 5, figs 1–5 (here more chresonymy and synonymy).

Material

5 specimens Saal, SNSB-BSPG 2016 XXI 1819–1823; 1 specimen locality 1985, above coral stock, level 2 (“Fundort 1985, über Korallenstock, Sohle 2”).

Cryptoptyxis ? spinosus sp. nov.

Plate 9: fig. 5

Etymology

Latin spinosus – thorny; because of the thorn-like extension of the axial ribs of the last whorl.

Holotype

SNSB-BSPG 2016 XXI 1824.

Paratypes

2 juvenile specimens, SNSB-BSPG 2016 XXI 1825–1826.

Type locality and stratum

Upper Jurassic (Kimmeridgian) reefal limestones from the locality Saal near Kelheim, Lower Bavaria (Gründel et al. 2015, 2022).

Diagnosis

Early whorls with 5 narrow axial ribs that form rib strands running across the shell i. e., ribs are aligned over consecutive whorls; last whorl with axial ribs that terminate adapically in thorn-like extensions; a spiral sculpture could not be seen with certainty.

Description

Shell trochiform, conical, higher than wide, with last whorl higher than spire; largest specimen 22 mm high; whorls low; whorl face with straight; suture shallow but distinct; ornament consists of 5 axial ribs per whorl; axial ribs sharp, high and very narrow with a weak cusp at adapical end; axial ribs extend from adapical suture to center of base; ribs of last whorl of illustrated specimen increase significantly in height and terminate adapically in a thorn-like tip; ribs on spire whorls aligned to each other from whorl to whorl, only slightly offset from one another, forming rib strands that run weakly prosocline across shell; spiral cords or lirae absent (due to preservation?); only occasionally three faint cusps visible on crest of axial ribs that could indicate presence of spiral ornamentation; aperture not preserved.

Remarks

Cryptoptyxis rarenodosa Gründel et al., 2019 has a ramp, but above all, the entire shell is covered with strong spiral cords. Other similar species (e. g., Cryptoptyxis sp. sensu Hägele (1997) from the Upper Jurassic; Cerithium quinquangulare Hébert and Eudes-Deslongchamps, 1860, Callovian) lack the adapical extensions of the axial ribs on the last whorl. Cryptoptyxis ? fortiter Gründel et al., 2022 has distinct spiral cords with nodes at the intersections with the axial ribs. In this species, the nodes on the subsutural spiral cord are strongly enlarged on the last whorl, but the ribs do not have an adapical extension.

Family Cassiopidae Beurlen, 1967

Coninoda Kollmann, 1979

Type species

Coninoda mammata Kollmann, 1979; Albian-Cenomanian; Austria.

Coninoda strekwera Gründel, Keupp & Lang, 2019

Plate 9: figs 6, 7

2017 „Ditretus“ sp. – Gründel: 31, pl. 11, fig. D.

2019 Coninoda strekwera n. sp. – Gründel, Keupp and Lang: 112, pl. 4, figs 8–9, 12–14.

Material

2 specimens, SNSB-BSPG 2016 XXI 1827–1828.

Remarks

A typical specimen from the Sylla collection representing Coninoda strekwera shows in longitudinal section that this species has no plaits or folds inside the whorls (pl. 9, fig. 7).

Coninoda ? sp. 1

pl. 4: figs 10–11 in Gründel et al. (2019)

2019 Coninoda? sp. 1 – Gründel, Keupp and Lang: 113, pl. 4, figs 10–11.

Material

1 specimen, SNSB-BSPG 2016 XXI 1829, locality 1985, above coral stock, level 2 (“Fundort 1985, über Korallenstock, Sohle 2”).

Superfamily Cerithioidea Fleming, 1822

Family Cryptaulacidae Gründel, 1976

Subfamily Cryptaulacinae Gründel, 1976

Tropacerithium Gründel, Keupp & Lang, 2019

Type species

Tropacerithium cumaritum Gründel, Keupp & Lang, 2019; upper Kimmeridgian; South Germany.

Remarks

Deviating from the diagnosis of the genus given by Gründel et al. (2019), the few specimens presented here for Tropacerithium have around 5 somewhat reinforced spiral cords on the whorl face, with 2 weaker ones running in between. The intersections of the stronger spiral cords with the axial ribs are weakly knobby.

Tropacerithium cumaritum Gründel, Keupp & Lang, 2019

Plate 9: figs 8, 9

2019 Tropacerithium cumaritum n. sp. – Gründel, Keupp and Lang: 124, pl. 7, figs 4–7.

Material

1 specimen, SNSB-BSPG 2016 XXI 1830.

Tropacerithium danubii Gründel, Keupp & Lang, 2019

pl. 7: figs 8–12 in Gründel et al. (2019)

2019 Tropacerithium danubii n. sp. – Gründel, Keupp and Lang: 124, pl. 7, figs 8–12.

Material

2 specimens, SNSB-BSPG 2016 XXI 1831–1832.

Subfamily Exelissinae Guzhov, 2004

Exelissa Piette, 1860

Type species

Cerithium strangulatum d’Archiac, 1843; Bathonian; France.

Exelissa sp. 1

pl. 6: figs 17–19 in Gründel et al. (2019)

2019 Exelissa sp. 1 – Gründel, Keupp and Lang: 122, pl. 6, figs 17–19.

Material

2 specimens, SNSB-BSPG 2016 XXI 1833–1834.

Exelissa ? aff. corallense (Buvignier, 1843)

Plate 9: figs 10–12

Material

1 specimen from Saal, SNSB-BSPG 2016 XXI 1835: locality 1985, above coral stock, level 2 (“Fundort 1985, über Korallenstock, Sohle 2”) and a questionable specimen from Saal, SNSB-BSPG 2016 XXI 1931.

Description

Shell high-spired, slender with slightly convex flanks; the certain specimen has 6.5 whorls, 12 mm high; sutures distinct; 5 bulging axial ribs per whorl that are aligned from whorl to whorl; whorl face ornamented with 5 slightly nodular spiral cords; spiral cords wider than interspaces separating them; intersections of axial ribs and spiral cords not knobby; one axial rib on last whorl thickened, varix-like; base incompletely preserved, moderately convex, covered with spiral cords; axial ribs continue onto base; questionable, poorly preserved specimen larger (height 16 mm), with distinctly broader shell shape; whorls increasing more rapidly; axial ribs also continue onto base; base with at least 2 distinct spiral cords.

Remarks

Exelissa ursicina (Loriol, 1889 in Loriol and Koby) sensu Gründel et al. (2022) has 6–8 axial ribs per whorl and 6–7 spiral cords on whorl face. Forms are described in the literature as Cerithium/Uchauxia corallense (mostly from the Oxfordian) that are very similar to the present form (e. g., Buvignier 1852; Thurmann and Étallon 1861–1864; Quenstedt 1881–1884; Gründel et al. 2022; and herein), which differ in details (e. g., in the number of spiral cords on whorl face, in the number of axial ribs per whorl, in the convexity of the whorls). It is not always clear which of these differences are diagnostic for species or represent intraspecific variability or reflect preservation. Cerithium mojisovici Zittel, 1873 has a broader shell, about 7 strong spiral cords on whorl face and a weak axial rib between two strong axial ribs. Exelissa diacritica Cossmann, 1913 is less slender, its whorl face is more convex (more distinct sutures) and it has more axial ribs per whorl that form only indistinct rib strands stretching over the shell.

Exelissa ursicina (Loriol, 1889 in Loriol and Koby)

Plate 9: figs 13, 14

2022 – Exelissa ursicina (De Loriol, 1889 in De Loriol and Koby) – Gründel, Hostettler and Menkveld-Gfeller: 50, pl. 7, figs 14–20, pl. 8, figs 1–5 (here more chresonymy and synonymy).

Material

1 specimen, SNSB-BSPG 2016 XXI 1836.

Description

Shell high-spired, slender; specimen 10 mm high; sutures shallow but distinct; whorl face with approximately 7 strong, orthocline axial ribs which weaken on base; distance between axial ribs wider than axial ribs; 6–7 strong, spiral cords on whorl face; intersections of axial ribs and spiral cords without nodes; transition from whorl face to convex base evenly rounded; base covered with spiral cords that are slightly stronger than those on whorl face; aperture unknown.

Remarks

According to Gründel et al. (2022), Exelissa ursicina from the Oxfordian is a variable species. The present specimen shows no clear differences to some variants of the Oxfordian species (see e. g., Loriol in Loriol and Koby 1889, Plate 8: figs 1–2, 5).

Family Cerithiidae Fleming, 1822

Subfamily Uchauxiinae Kollmann, 2005

Provolibathra Kollmann, 2005

Type species

Cerithium sexangulatum Zekeli, 1852; Cretaceous Gosau Group; Austria.

Provolibathra ? sp., cf. septemplicata (Roemer, 1836)

pl. 5: figs 17–20, pl. 6: figs 1–5 in Gründel et al. (2019)

2019 – Provolibathra ? sp., cf. septemplicata (Roemer, 1836) – Gründel, Keupp and Lang: 119, pl. 5, figs 17–20, pl. 6, figs 1–5 (here more chresonymy and synonymy).

Material

3 specimens, SNSB-BSPG 2016 XXI 1837–1839.

Family Turritellidae Lovén, 1847

Turritella Lamarck, 1799

Type species

Turbo terebra Linnaeus, 1758; Indian and Pacific Ocean; recent.

Remarks

In classifying the species described below, we follow Das et al. (2018).

Turritella lucagrita sp. nov.

Plate 9: figs 15–17

Etymology

Arbitrary.

Holotype

SNSB-BSPG 2016 XXI 1840, the only specimens at hand.

Type locality and stratum

Upper Jurassic (Kimmeridgian) reefal limestones from the locality Saal near Kelheim, Lower Bavaria (Gründel et al. 2015, 2022).

Diagnosis

Shell high-spired, very slender; whorls face of early whorls barely converge, later whorls converge significantly towards the apex; early whorls with 3 spiral cords of approximately equal strength; on late whorls, abapical spiral cord (low on whorls) strengthened, prominently protruding, angulating whorl face.

Description

Shell high-spired, very slender; shell 75 mm high; shell flanks straight; sutures distinct; sculpture consists of 3 spiral cords; upper and lower spiral cord at clear distance from adapical and abapical suture respectively; on early whorls, all three spiral cords almost equally strong (middle one slightly weaker than others); whorl face of early whorls barely converge, later whorls converge significantly towards apex; no nodes visible on whorl face; on late whorls abapical spiral cord becomes stronger than others and protrudes noticeably forming an angulation low on whorl; shell ornament reduced on last preserved whorls; base and aperture not preserved; no plaits visible; narrow umbilicus present.

Remarks

Turritella amitava Das et al., 2018 from India (originally thought to be of Jurassic age but later found to be Miocene: Fürsich et al. 2023, and again as identified as being Upper Jurassic by Das et al. 2024) is smaller, secondary spiral cords are formed next to the 3 main spiral cords, and shows no ontogenetic reduction of the sculpture. Turritella dhosaensis Das et al., 2018 (also of disputed age, Jurassic vs Miocene) is smaller, the abapical and middle spiral cord is are closer to each other than the middle and adapical spiral cord; the abapical spiral cord does not protrude as much on late whorls, and the ontogenetic sculptural change is generally missing. Promathilda (Teretrina) sp. sensu Hägele (1997) is much smaller, has more numerous and weaker but equally strong spiral cords, there is no ontogenetic sculptural reduction. Aptyxiella tricincta (Münster) sensu Quenstedt (1881–1884) has a concave or almost straight and vertical whorl face, the subsutural spiral cord is the strongest and the abapical one is not reinforced and does not protrude.

Family uncertain

Nudivagus Wade, 1917

Type species

Nudivagus simplicus Wade, 1917; Upper Cretaceous; USA (Tennessee).

Nudivagus sp. 1

pl. 5: figs 6–8 in Gründel et al. (2019)

2019 – Nudivagus sp. 1 – Gründel, Keupp and Lang: 116, pl. 5, figs 6–8.

Material

3 specimens, SNSB-BSPG 2016 XXI 1841–1843.

Nudivagus ? sp. 2

Plate 9: fig. 18

Material

2 specimens from Saal, SNSB-BSPG 2016 XXI 1844–1845.

Description

Shell high-spired, slender with high whorls; a specimen is 35 mm high; shell flanks straight; whorl face slightly convex; periphery just above abapical suture; suture distinct; whorl face covered with numerous faint spiral cords that are wider than spiral furrows in between; some furrows consist of rows of minute pits; fine ornamentation only faintly visible due to preservation; transition from whorl face to moderately convex, anomphalous base evenly rounded; no sculpture visible on base; aperture damaged, oval, pointed adapically; it is unclear whether an abapical canal was present.

Remarks

Nudivagus sp. 1 sensu Gründel et al. (2019) has significantly lower whorls and the transition from whorl face to base has an edge. Pseudomelania valfinensis Loriol in Loriol and Bourgeat 1886–1888 is larger and more slender, the whorls are higher and the base is more convex. Pseudomelania kobyi Loriol in Loriol and Koby (1890) is taller and more slender, the whorls are higher and it lacks spiral sculpture.

Neuburgensia Gründel, Hostettler & Menkveld-Gfeller, 2022

Type species

Gymnocerithium concavum Janicke, 1966; Tithonian; South Germany.

Neuburgensia convexoconcava (Gründel, Keupp & Lang, 2019), comb. nov.

pl. 2: figs 10–12; pl. 11: figs 4–5 in Gründel et al. (2019)

2019 Gymnocerithium ? convexoconcavum n. sp. – Gründel, Keupp and Lang: 108; pl. 2, figs 10–12; pl. 11, figs 4–5.

Material

2 specimens, SNSB-BSPG 2016 XXI 1846–1847.

Neuburgensia angulata sp. nov.

Plate 9: fig. 19, Plate 10: figs 1–6

2017 Nerineoidea Nr. 4 – Gründel: 33, pl. 14, fig. A.

Etymology

Latin angulata – angular; after the angular transition from whorl face to the flat base.

Holotype

SNSB-BSPG 2016 XXI 1849 (Plate 10: fig. 1, collection Lang).

Plate 10. 

(1) Neuburgensia angulata sp. nov., holotype, SNSB-BSPG 2016 XXI 1849, collection Lang, lateral view, height 24 mm. (2–3) Neuburgensia angulata sp. nov., paratype, SNSB-BSPG 2016 XXI 1850, collection Lang, (2) earliest preserved whorls in lateral view, height 1 mm, (3) lateral view, height 6 mm. (4) Neuburgensia angulata sp. nov., paratype, SNSB-BSPG 2016 XXI 1851, collection Lang, lateral view, height 10 mm. (5) Neuburgensia angulata sp. nov., paratype, SNSB-BSPG 2016 XXI 1852, collection Schäfer¸basal view, width 6 mm. (6) Neuburgensia angulata sp. nov., paratype, SNSB-BSPG 2016 XXI 1853, collection Lang, oblique apical, width 6.5 mm. (7–9) Neuburgensia rara sp. nov., holotype, SNSB-BSPG 2016 XXI 1856, (7) lateral view, height 30 mm, (8) early whorls in lateral view, height ca. 7 mm, (9) middle whorls in lateral view, height 12 mm. (10, 11) Purpuroidea lapierrea (Buvignier, 1843), SNSB-BSPG 2016 XXI 1857, lateral and oblique views, height 30 mm. (12, 13) Columbellaria corallina (Quenstedt, 1852), SNSB-BSPG 2016 XXI 1859, (12) apex in lateral view, height 10 mm, (13) lateral view, height 19 mm. (14, 15) Columbellaria corallina (Quenstedt, 1852), SNSB 1860, lateral and slightly oblique lateral views, height 21 mm. (16) Diarthema aspera sp. nov., paratype, SNSB-BSPG 2016 XXI 1862, lateral view, height 44 mm.

Material

Holotype and 52 paratypes (mainly fragments of various ontogenetic stages): SNSB-BSPG 2016 XXI 1848, 1850–1855, 1932–1976; most from the collection Sylla, others from collections Keupp, Schäfer, and Neubauer, all from Saal.

Type locality and stratum

Upper Jurassic (Kimmeridgian) reefal limestones from the locality Saal near Kelheim, Lower Bavaria (Gründel et al. 2015, 2022).

Diagnosis

Shell very slender; whorl face with subsutural nodular bulge, also on late whorls; shell flanks straight; whorl face straight to slightly concave; base flat, set off from whorl face by sharp clear edge at an almost right angle.

Description

Shell high-spired, slender with numerous whorls; a specimen is 24 mm high; shell flanks straight; whorls significantly wider than high; as far as the fragmentary material can be seen, the early shell has a larger spire angle than later shell; whorl face of early whorls straight with distinct sutures; then, gradual development of subsutural knobby ridge (bulge) demarcating ramp; knobs limited to outer edge of the ramp, only occasionally visible, usually not preserved; ramp usually narrow, occasionally significantly widened and concave; outer whorl face of mature whorls straight to slightly concave; spiral sculpture not recognizable; base flat, set off from whorl face by sharp clear edge at an almost right angle; base without recognizable sculpture; aperture rounded-rectangular, with very clear, backward curved abapical canal; damaged specimens show that the columella axis is hollow.

Remarks

For, the differences to Neuburgensia rara n. sp. see below. Gymnocerithium ? convexoconcavum Gründel et al., 2019 (also from the Saal quarry) differs in having a convex whorl face in mature whorls as well as a subsutural concavity and the transitions from whorl face to base is evenly rounded. Neuburgensia perrotunda (Cossmann, 1913) sensu Loriol in Loriol and Koby 1889 in the sense of Gründel et al. (2022) and Cerithium valfinense Loriol in Loriol and Bourgeat 1886–1888 lack a subsutural bulge and the transition from whorl face to base is rounded. Proceritella infragranulata Janicke, 1966 has an angulated transition from whorl face to base and a slightly convex base, the suture lies on a ridge formed by two adjacent whorls, and the whorls increase in width more quickly.

Neuburgensia rara sp. nov.

Plate 10: figs 7–9

Etymology

Latin rare, because this species is rare.

Holotype

SNSB-BSPG 2016 XXI 1856, the only specimen, Saal, collection Sylla.

Diagnosis

Shell very slender, high-spired, with many whorls; early whorls have a subsutural, weakly tuberculate bulge that is reduced on later whorls; base flat; transition from whorl face to base at sharp angulation that is almost perpendicular.

Type locality and stratum

Upper Jurassic (Kimmeridgian) reefal limestones from the locality Saal near Kelheim, Lower Bavaria (Gründel et al. 2015, 2022).

Description

Shell very slender, high-spired, with many whorls; specimen is 30 mm high, with about 20 whorls, apex missing; early whorls increase more rapidly than the later ones and therefore, the early shell have a wider apical angle than later shell; early whorls with distinct subsutural bulge (sometimes nodular) emphasizing sutures; bulge reduced on later whorls; whorl face straight, sutures only slightly impressed; series of small cusps occasionally visible directly below suture; weak spiral lirae on whorl face (hardly visible due to preservation); base flat; transition from whorl face to base at sharp angulation, angle almost perpendicular with reinforced edge (visible above suture); growth lines weakly opisthocyrt on whorl face and prosocyrt on base; aperture outline rounded-rectangular, details of aperture not preserved; columella hollow.

Remarks

In other Neuburgensia species, the subsutural bulge is not reduced during ontogeny.

Subcohort Hypsogastropoda Ponder & Lindberg, 1997

Superfamily Littorinoidea Children, 1834

Family Purpuroideidae Guzhov, 2004

Purpuroidea Lycett, 1848

Type species

Purpura moreausia Buvignier, 1843; Oxfordian; France.

Purpuroidea lapierrea (Buvignier, 1843)

Plate 10: figs 10, 11

1886–1888 Purpuroidea gracilis n. sp. – Loriol in Loriol and Bourgeat: 60, pl. 4, figs 2–3.

1893 Purpuroidea lapierrea Buvignier – Loriol in Loriol and Lambert: 15, pl. 1, fig. 7.

1913 Purpuroidea gracilis (De Loriol) – Cossmann: 183, pl. 11, figs 1–2; fig. 44.

2022 Purpuroidea lapierrea (Buvignier, 1843) – Gründel, Hostettler and Menkveld-Gfeller: 55, pl. 9, figs 11–14, pl. 10, figs 1–5 (here more chresonymy and synonymy).

Material

2 specimens, SNSB-BSPG 2016 XXI 1857–1858.

Description

Shell globular turbiniform with gradate spire; illustrated specimen (probably juvenile) 30 mm high; spire high, slender for the genus; last preserved whorl distinctly higher than spire; earliest preserved whorls convex, without visible ornament; early whorls with subsutural concavity that rapidly widens into distinct ramp in later whorls; several weak spiral cords can be seen on one specimen; shoulder of ramp with distinct nodes on last two preserved whorls; nodes rapidly enlarging, becoming almost thorn-like; nodes terminate adapically and abapically in bulging, ill-defined axial ribs; transition from whorl face to strongly convex base evenly rounded; faint lirae are visible in places, probably originally covering entire surface of the shell; aperture unknown.

Remarks

The information about Purpuroidea lapierrea regarding the insertion of the nodes on the shoulder and the formation of a spiral sculpture varies in the literature.

„Rissoiform clade“

Superfamily Truncatelloidea Gray, 1840

Family Palaeorissoinidae Gründel & Kowalke, 2002

Buvignieria Cossmann, 1921

Type species

Rissoina unicarina Buvignier, 1843; Oxfordian; France.

Buvignieria racitana Gründel, Keupp & Lang, 2019

pl. 8: figs 14–20 in Gründel et al. (2019)

2019 Buvignieria racitana n. sp. – Gründel, Keupp and Lang: 130, pl. 8, figs 14–20 (here more chresonymy and synonymy).

Material

1 specimen SNSB-BSPG 2016 XXI 1976.

Superorder Latrogastropoda Riedel, 2000

Taxa of uncertain position

Family Colombellinidae P. Fischer, 1884

Columbellaria Rolle, 1861

Type species

Cassis corallina Quenstedt, 1852; upper Jurassic; South Germany.

Columbellaria corallina (Quenstedt, 1852)

Plate 10: figs 12–15

2017 Columbellaria cf. corallina (Quenstedt, 1852) – Werner, Nützel and Nose: 32, fig. 3 A–C.

2019 Columbellaria corallina (Quenstedt, 1852) – Gründel, Keupp and Lang: 133, pl. 9, figs 11–17 (here more chresonymy and synonymy).

2019 Columbellaria sp. 1 – Gründel, Keupp and Lang: 136, pl. 9, fig. 18, pl. 10, fig. 1.

Material

3 specimens, SNSB-BSPG 2016 XXI 1859–1861.

Description

Shell egg-shaped, higher than wide, with distinctly elevated, slender, gradate spire, consisting of more than 5 whorls; illustrated specimen (Plate 10: figs 14, 15) 21 mm high; already first preserved whorls angulated forming edge that later becomes a keel; keel separates oblique ramp and vertical abapical whorl face; ramp ornamented with several very weak spiral cords over several whorls; spiral cords no longer visible on last two spire whorls; instead, formation of subsutural spiral cord covered with small tubercles and a stronger spiral cord, also with nodes, between subsutural cord and keel; whorl face of early teleoconch with axial ribs (approximately 10 on last spire whorl); intersections of axial ribs and spiral cords nodular; all mentioned spiral cords continue onto body whorl without interruption; axial ribs disappear at transition from spire whorls to body whorl and keel is weakened into a spiral cord of equal strength as in other spiral cords; transition from convex whorl face to strongly convex base evenly rounded; body whorl covered with approximately 15 nodular spiral cords of approximately same strength; spiral cords on whorl face slightly more distant from each other than those on base; aperture with widened outer lip and spine-like protrusions where spiral cords are situated; aperture elongated with anterior and posterior siphonal canals (see Hägele 1997; Werner et al. 2017).

Remarks

The spire of the present specimens combines characteristics of Columbellaria corallina sensu Gründel et al. (2019) (the last whorl is approximately 10 mm wide; distinct spiral cord between adapical suture and keel) with that of Columbellaria sp. 1 sensu Gründel et al. (2019) (strong keel on whorls until end of spire, stronger nodes on keel). It is possible that all forms described Gründel et al. (2019) and described here are variants of a single species. Due to the lack of more extensive and better-preserved material, these forms are summarized herein under the name Columbellaria corallina (Quenstedt, 1852).

Columbellaria rara Gründel et al. (2022) has significantly fewer spiral cords on the body whorl and these are more bulging. Zittelia picteti Gemmellaro, 1870 has a wider and more convex body whorl, the spiral cords are at least as wide as the spiral furrows between them and the spire whorls are not keeled. Columbellaria victoria Guirand & Ogérien, 1865 and sensu Loriol in Loriol and Bourgeat (1886–1888) has spiral cords of equal strength on the body whorl, which are at least as wide as the spiral furrows between them. Its body whorl is more convex and it lacks a subsutural row of small nodes. Columbellaria denticulata Zittel, 1873 has more nodes on the last spire whorl and lacks subsutural row of small nodes is missing there; the outer lip of the body whorl lacks furrows.

Superfamily Stromboidea Rafinesque, 1815

Family Aporrhaidae Gray, 1850

Diarthema Piette, 1864

Type species

Rostellaria paradoxa Eudes-Deslongchamps, 1843; Bathonian; France.

Diarthema aspera sp. nov.

Plate 10: fig. 16, Plate 11: figs 1–4

2019 – Diarthema sp. 1 – Gründel, Keupp and Lang: 137, pl. 10, figs 6–7.

Etymology

Latin aspera – rough; because of the strong ornamentation.

Holotype

SNSB-BSPG 2016 XXI 1863.

Paratypes

7 specimens, SNSB-BSPG 2016 XXI 1862, 1864–1869 and a cast of an imprint (imprint not hand), SNSB-BSPG 2016 XXI 1870.

Plate 11. 

(1, 2) Diarthema aspera sp. nov., holotype, SNSB-BSPG 2016 XXI 1863, (1) lateral view, height 37 mm, (2) wing, height 16 mm. (3) Diarthema aspera sp. nov., paratype, SNSB-BSPG 2016 XXI 1864, lateral view, height 28 mm. (4) Diarthema aspera sp. nov., paratype, SNSB-BSPG 2016 XXI 1865, aperture, height 35 mm. (5, 6) Aporrhaidae gen. inc. schlosseri (Loriol in Loriol and Bourgeat 1886–1888), SNSB-BSPG 2016 XXI 1871, (5) lateral view, height 38 mm, (6) columellar section, height 32 mm. (7–9) Gen. indet. schlosseri (Loriol in Loriol and Bourgeat 1886–1888), SNSB-BSPG 2016 XXI 1872, (7) lateral view, height 35 mm, (8) last two whorls, height 19 mm, (9) basal view, width 16 mm (without wing), 23 mm (including wing). (10, 11) Gen. indet. monilitesta Zittel, 1873, SNSB-BSPG 2016 XXI 1874, lateral views, height 19 mm. (12–14) Gen. indet. sp. indet, SNSB-BSPG 2016 XXI 1875, apertural, apical and abapertural views, width of specimen 26 mm. (15, 16) Aptyxiella tricincta (Münster in Goldfuss, 1844), SNSB-BSPG 2016 XXI 1880, lateral view and columellar section, height 32 mm. (17, 18) Aptyxiella planata (Quenstedt, 1858), SNSB-BSPG 2016 XXI 1889, (17) longitudinal section, height 30 mm, (18) lateral view, height 48 mm.

Type locality and stratum

Upper Jurassic (Kimmeridgian) reefal limestones from the locality Saal near Kelheim, Lower Bavaria (Gründel et al. 2015, 2022).

Diagnosis

Spire whorls have a knobby angulation, axial ribs and a strong spiral cord between angulation and abapical suture; last whorl of adult specimens with two wing-like, broadened varices; wings semicircular, with 6–7 strong spiral cords forming node-like projections on outer edge wing; aperture with long vertical rostrum long.

Description

Shell with high, gradate spire and large, widened body whorl; largest specimen 45 mm high; shell slender consisting of numerous convex whorls; spire whorls angulated at mid-whorl face; suture distinct; oblique ramp demarcated by angulation; whorl face below angulation almost vertical; a weak spiral cord above angulation appears after several whorls; another spiral cord becomes visible above suture; ca. 7 strong axial ribs per whorl; axial ribs do not continue onto base in body whorl of fully grown specimens; intersections of angulation and axial ribs with strong nodes; weaker nodes at intersection abapical spiral cord; some axial ribs thickened varix-like; body-whorl of adults have strongly convex base; transition from whorl face to base evenly rounded; axial ribs disappear; former edge covered with small nodes; base with 4 strong spiral cords with fine nodes; two wing-like widened varices concave in apertural direction; outer lip of aperture widened into a semicircular wing; 6–7 strong spiral cords on the wing and several weak ones between strong cords; strong spiral cords form node-like projections on outer edge of the wing; uppermost strong spiral cord terminated in a spine pointing obliquely in apertural and adapical direction; long, vertically downward (abapical) pointing rostrum, covered with several weak spiral cords.

Remarks

Gründel et al. (2019, p. 138, as Diarthema sp. 1) reported a vertically upward directed shell-process attached on the penultimate for this species. This shell-process cannot be recognized in the present material. We assume that this is a silicified artifact that does not belong to the shell.

The similar Diempterus ? multicostatus Gründel et al. 2022 has more numerous spiral cords of varying strength (but generally weaker than in the present species), the varices on the last whorl have 3 spine-like elongated tubercles. A wing is unknown for Diempterus ? multicostatus. Rostellaria benoisti Guirand & Ogérien, 1865 (= Diarthema benoisti sensu Loriol in Loriol and Bourgeat 1886–1888) has numerous reinforced spiral cords on the wing, the wing is asymmetrical with a protruding abapical part. Cyphosolenus tetracer d’Orbigny sensu Loriol in Loriol and Bourgeat (1886–1888) has only 3 strong and numerous weaker spiral cords on the body whorl, the wing extends to the last spire whorl, the spire whorls lack the second strong spiral cord between angulation and abapical suture. Pterocera thurmanni sensu Thurmann and Étallon (1861–1864) as well as Pterocera ponti (Brongniart) sensu Loriol et al. (1872) and Pterocera polypoda Buvignier sensu Loriol in Loriol and Pellat (1874) have a similar wing, but a stouter shell with convex spire whorls, but lacks axial ribs and nodes on spire whorls.

Superfamily and family uncertain

Gen. indet. schlosseri (Loriol in Loriol and Bourgeat, 1886–1888)?

Plate 11: figs 5–9

?1886–1888 – Cerithium schlosseri P. de Loriol in Loriol and Bourgeat: 134, pl. 13, fig. 7.

Material. 4 specimens, SNSB-BSPG 2016 XXI 1871–1873, 1978.

Description. Largest specimen 36 mm high, apical whorls missing; shell slender; whorls significantly wider than high; first preserved whorl with subsutural bulge forming narrow ramp; bulge with numerous densely spaced axially elongated nodes; nodes change to larger, round, less numerous nodes on last preserved whorl; on last portion of last preserved whorl, only growth lines can be seen on bulge; there, growth lines approximately orthocline, without adapical sinus; whorl face between bulge and abapical suture with 2 somewhat stronger, nodular spiral cords and several spiral lirae; on last whorl of largest specimen, a spiral cord becomes particularly strong and knobby; transition from whorl face to weakly convex base formed by sharply projecting edge; base is entirely covered with spiral cords and lirae; base narrowly phaneromphalous; suture rises sharply shortly before the end of last preserved whorl (onset of a non-preserved wing-like apertural process?); aperture lacks folds.

Remarks. Between the bulge and the abapical suture, the two spiral cords vary from being strong to barely noticeable. In the latter case, spiral lirae are quite clear. When describing Cerithium schlosseri, Loriol (1886–1888, in Loriol and Bourgeat) only had the specimen at hand that was illustrated by him on pl. 13, fig. 7. It is a fragment with approximately 3 whorls, coming from the middle part of the shell. Therefore, statements about early or the final whorls of adult specimens are not possible. There are no noticeable differences to the present more completely preserved specimens. However, due to the incomplete type specimen, an identification remains tentative. Procerithium (Cosmocerithium) dorvali (Cossmann) sensu Reiner (1968) is more slender, the ramp is less pronounced, lacks the ontogenetic change of the sculpture (maybe comparable ontogenetic changes are not preserved). Cerithium (Eustoma) pagoda Zittel, 1873 has fewer subsutural nodes, the nodes are more rounded (not axially elongated), and ontogenetic changes of the ornament have not been reported.

The present specimens also resemble the Mesozoic genera Diatrypesis and Cimolithium but these genera lack the terminal extension of the outer lip. Also, some eustomatids are similar (e. g., Silberlingiella) which seem to have expanded outer lip (e. g., Hikuroa and Kaim 2007).

Gen. indet. monilitesta Zittel, 1873

Plate 11: figs 10, 11

1873 – Cerithium monilitesta Zit. – Zittel: 270, pl. 44, fig. 19.

Material. 1 specimen, SNSB-BSPG 2016 XXI 1874.

Description. Shell moderately slender; specimen 19 mm high; suture inconspicuous; whorl face with a directly subsutural row of nodes, lacking ramp; nodes slightly axially elongated; below, two weaker spiral cords covered with smaller, more numerous nodes; base flat; transition from base to whorl face at sharp edge that is partly exposed above abapical suture; details of base not visible; aperture damaged; approximately rectangular; no evidence for wing formation (corresponding shell area not preserved?); probably present vertical canal/rostrum is broken off.

Remarks. The sculpture is reminiscent of Gen. inc. schlosseri as described above. Both may represent the same, or at least to closely related, genera. Turritella staszycii Zeuschner, 1850 is stouter and has only 2 rows of nodes per whorl (one strong subsutural cord, one weaker above the abapical suture).

The present specimens also resemble the Mesozoic genera Diatrypesis, Cimolithium or Metacerithium.

Gen. indet. sp. indet

Plate 11, Figs 12–14

Material. 3 specimens, SNSB SNSB-BSPG 2016 XXI 1875–1877.

Description. Material moderately preserved, illustrated specimen 34 mm high; shell broadly trochoid with convex flanks; suture incised; whorls increase rapidly in height; ornament consists of strong, bulbous axial ribs, some of which are thickened varix-like; ribs approximately orthocline; ribs continue onto base but appear to weaken; early whorls with ca. 8 axial ribs per whorl, later whorls with ca. 5 ribs per whorl; distance between axial ribs increases during ontogeny (distance between two ribs eventually several times the width of the ribs) and ribs become stronger; ribs thickened, node-like near abapical suture; whorl face with barely visible spiral cords, approximately 5 spiral cords vaguely visible in illustrated specimen; they cross axial ribs without forming nodes; transition from whorl face to barely convex base at rounded edge; aperture rounded; in adult specimens, outer lip thickened and bulgy.

Remarks. Similar forms occur within the Brachytrematidae, but they usually have a clear abapical canal (Gründel et al. 2020b). Turbo valfinensis Étallon sensu Loriol in Loriol and Bourgeat (1886–1888) (pl. 20: fig. 3, non fig. 2) has a wider shell, the height of the whorls increases less rapidly and the last whorl has more nodes. Brachytrema sp. sensu Hägele (1997) is smaller and more slender; a spiral ornament was not reported for this species. Purpurina costellata sensu Piette (1856) is significantly smaller, more slender and has an abapical canal. This species also resembles species of Purpuroideidae but members of this family usually have an angulated whorl face.

Subclass Heterobranchia Burmeister, 1837

Superfamily Nerineoidea Zittel, 1873

Family unclear

Cossmannea Pčelintsev, 1927

Type species

Nerinea desvoidyi d’Orbigny, 1850; Oxfordian; France.

Cossmannea desvoidyi (d’Orbigny, 1850)

pl. 1: figs 1–3 in Gründel et al. (2022)

2022 – Cossmannea desvoidyi (d’Orbigny, 1851) – Gründel, Keupp, Lang and Nützel: 181, pl. 1, figs 1–3 (here more chresonymy and synonymy).

Material

2 fragments, SNSB-BSPG 2016 XXI 1878–1879, one large specimen 18 cm high, 5.5 cm wide: SNSB-BSPG 2016 XXI 1.

Remarks

This species has a very pronounced abapical siphonal canal.

Aptyxiella P. Fischer, 1885

Type species

Nerinea sexcostata d’Orbigny, 1850; Oxfordian-Kimmeridgian; France.

Aptyxiella tricincta (Münster, 1844) sensu Quenstedt (1881–1884), comb. nov.

Plate 11: figs 15, 16

2022 – Bactroptyxis ? tricincta (Münster) sensu Quenstedt (1881–1884) – Gründel, Keupp, Lang and Nützel: 199, pl. 13, figs 11–16 (here more chresonymy and synonymy).

Material

5 specimens, SNSB-BSPG 2016 XXI 1880–1884 and 4 questionable specimens, SNSB-BSPG 2016 XXI 1885–1888, from Saal.

Remarks

The longitudinal section of a specimen shows that there are no plates or folds inside the aperture. The species is therefore assigned to the genus Aptyxiella.

Aptyxiella planata (Quenstedt, 1858)

Plate 11: figs 17, 18

? 1979 – Pseudonerinea clytia (d’Orbigny, 1850) – Wieczorek: 319, pl. 6, figs 1–3.

2022 – Aptyxiella planata (Quenstedt, 1858) – Gründel, Keupp, Lang and Nützel: 183; pl. 1, figs 4–6 (here more chresonymy and synonymy).

Material

2 specimens, SNSB-BSPG 2016 XXI 1889–1890.

Remarks

This species has a palatal plait.

Aphanoptyxis Cossmann, 1896

Type species

Cerithium defrancei Eudes-Deslongchamps, 1843; Bathonian; France.

Aphanoptyxis sinerugae sp. nov.

Plate 12: figs 1–3

Etymology

Latin sine rugae – without folds, because of the lack of plaits or folds within the whorls.

Plate 12. 

(1, 2) Aphanoptyxis sinerugae sp. nov., holotype, SNSB-BSPG 2016 XXI 1891, (1) lateral view, height 98 mm, (2) basal view, width 40 mm. (3) Aphanoptyxis sinerugae sp. nov., paratype, SNSB-BSPG 2016 XXI 1892, columellar section, height 32 mm. (4–5) Pseudonerinea ? pseudomelaniformis Gründel, Keupp, Lang & Nützel, 2022, SNSB-BSPG 2016 XXI 1894, abapertural and apertural lateral views, height 32 mm. (6) Pseudonerinea ? pseudomelaniformis Gründel, Keupp, Lang & Nützel, 2022, SNSB-BSPG 2016 XXI 1895, lateral view, height 30 mm. (7) Nerinea donosa Gründel, Keupp, Lang & Nützel, 2022, SNSB-BSPG 2016 XXI 1896, lateral view, height 18 mm. (8–10) Nerinea donosa Gründel, Keupp, Lang & Nützel, 2022, SNSB-BSPG 2016 XXI 1897, (8, 10) lateral and basal view (9) detail of last whorl in lateral view, height of shell 19.5 mm, width 8 mm. (11) Nerinea donosa Gründel, Keupp, Lang & Nützel, 2022, SNSB-BSPG 2016 XXI 1898, lateral view, height 30 mm. (12) Nerinea donosa Gründel, Keupp, Lang & Nützel, 2022, SNSB-BSPG 2016 XXI 1899, lateral view, height 26 mm. (13, 14) Nerinea donosa Gründel, Keupp, Lang & Nützel, 2022, SNSB-BSPG 2016 XXI 1900, lateral and basal view, height 37 mm, width 11 mm. (15, 16) Nerinea moreana (d’Orbigny, 1851), SNSB-BSPG 2016 XXI 1901, abaperurtal and apertural view, height 85 mm. (17, 18) Nerinea moreana (d’Orbigny, 1851)?, SNSB-BSPG 2016 XXI 1902, lateral view and columellar section, height 27 mm. (19) Endoplocus inflatus Gründel, Keupp, Lang & Nützel, 2022, SNSB-BSPG 2016 XXI 1903, lateral view, height 34 mm.

Holotype

SNSB-BSPG SNSB-BSPG 2016 XXI 1891.

Paratypes

Saal, 2 specimens, SNSB-BSPG 2016 XXI 1892–1893.

Type locality and stratum

Upper Jurassic (Kimmeridgian) reefal limestones from the locality Saal near Kelheim, Lower Bavaria (Gründel et al. 2015, 2022).

Diagnosis

Shell moderately slender, cyrtoconoid, apical angle decreases during ontogeny; whorl face strongly concave, without ornament; suture situated on ridge formed by two adjacent whorls; a siphonal canal appears to have formed; whorls without plaits or folds.

Description

Shell slender, cyrtoconoid, apical angle decreases during ontogeny; holotype 98 mm high; suture situated on ridge formed by two adjacent whorls; whorl face strongly concave, without ornament except of occasionally weakly reinforced growth lines; growth lines on whorl face orthocline and almost straight, bent strongly backwards below adapical suture; base slightly convex, smooth with weakly prosocyrt growth lines, phaneromphalous; transition from whorl face to base at sharp edge forming almost right angle; aperture rhomboid mouth, seemingly with siphonal canal, without plaits or folds.

Remarks

Nerinea turbatrix Loriol in Loriol and Bourgeat (1886–1888) has a more slender shell, its shape is not cyrtoconoid and its whorls are higher. Cossmannea (Eunerinea) ursicina (Thurmann) sensu Fischer and Weber (1997) has a distinct spiral sculpture. Umbonata dilatata (d’Orbigny) sensu Fischer and Weber (1997) is more slender, the whorls are lower and 3 plaits are formed in the aperture. Nerinea arduennensis Buvignier, 1852 is more slender, the whorls are lower, the shell shape is not cyrtoconoid, and several plaits are present. Cryptoplocus engeli Geiger, 1901 has lower and less concave whorls and a strong columellar plait. Nerinea castor d’Orbigny sensu Maire (1926) has no cyrtoconoid shell shape, and plaits have not been reported for it (according to d’Orbigny 1851 and Fischer and Weber 1997, several plaits are formed).

Family Pseudonerineidae Pčelintsev, 1965

Pseudonerinea Loriol in Loriol & Koby, 1890

Type species

Pseudonerinea blauensis Loriol in Loriol and Koby 1890; Oxfordian (Rauracian); Switzerland.

Pseudonerinea ? pseudomelaniformis Gründel, Keupp, Lang & Nützel, 2022

Plate 12: figs 4–6

1965 – Pseudonerinea clio (d’Orbigny) – Cox: 172, pl. 30, figs 5–6.

?1997 – Ceritella (Fibula) cottaldina (d’Orb.) – Fischer and Weber: 31, pl. 4, fig. 10

2019 – Pseudomelania? sp. 2 – Gründel, Keupp and Lang: 100, pl. 1, figs 7–9.

*2022 – Pseudonerinea ? pseudomelaniformis n. sp. – Gründel, Keupp, Lang and Nützel 2022: 183; pl. 2, figs 1–7.

Material

27 specimens, illustrated specimens SNSB-BSPG 2016 XXI 1894–1895.

Description

Shell very slender; a specimen is 32 mm high; whorls high; whorl face straight; suture slightly impressed; transition from whorl face to base evenly rounded; whorls smooth, at least on later whorls; aperture damaged, high oval with adapical outlet and an oblique siphonal abapical canal; inner columellar lip widened and detached.

Remarks

Many species with a similar shell shape have been described, particularly in the genus Pseudomelania. Without knowledge of the aperture (it is unknown or insufficiently known in most cases), a comparison of these species is only possible to a limited extent.

Nudivagus? sp. 2 sensu Gründel et al. (2019) has a wider shell with lower whorls, a spiral sculpture on the whorl face, and lacks a widened and detached columellar inner lip. Ceritella (Fibula) cottaldina (d’Orbigny) as depicted by Fischer and Weber (1997) is larger according to its holotype, but shows no other significant differences. The shape of the aperture is unclear: According to d’Orbigny (1851), it is broadly rounded abapically, however according to Fischer and Weber (1997), it shows the onset of a (not preserved?) channel. If P. cottaldina has an abapical canal, then it is probably identical to P. pseudomelaniformis.

Family Nerineidae Zittel, 1873

Nerinea Deshayes, 1827

(Synonym: Phaneroptyxis Cossmann, 1896)

Type species

Nerinea mosae Deshayes, 1827; Oxfordian; France.

Remarks

Regarding the synonymy of Nerinea and Phaneroptyxis, see Kollmann (2014, p. 360).

Nerinea donosa Gründel, Keupp, Lang & Nützel, 2022

Plate 12: figs 7–13

2017 – Nerineoidea Nr. 7 – Gründel: 33, pl. 14, fig. D.

2022 – Nerinea donosa n. sp. – Gründel, Keupp, Lang and Nützel: 187, pl. 5, figs 1–5.

Material

45 specimens from Saal, illustrated specimens SNSB-BSPG 2016 XXI 1896–1900.

Description

The present new material allows a more detailed description of Nerinea donosa: Shell slender (especially early ontogenetic part) with numerous whorls; specimen 36 mm high; whorls about twice as wide as high; subsutural bulge with nodes formed very early in ontogeny; in later whorls, bulge is largely changed to a row of large nodes (8–10 per whorl); nodes extend to about half whorl height, forming narrow ramp; ramp emphasizes suture; whorl face concave between row of nodes and abapical suture are, with 1–2 slightly nodular spiral cords; strong bordering abapical spiral cord covered by the following whorl or slightly exposed above suture, covered with small nodes (not always noticeable); growth lines weakly prosocyrt, strongly backwards below adapical suture; transition from whorl face to base slightly angular at bordering abapical spiral cord; base strongly convex, conical; base with several weakly nodular spiral cords (only visible in well-preserved specimens); aperture (see Gründel et al. 2022) narrow with siphonal canal, with two columellar plaits, 1–2 parietal plaits and in some specimens one palatal plait; if two columellar plaits are present, the adapical one is weaker than the abapical one.

Remarks

Nerinea plassenensis Peters, 1855 is more slender, the subsutural nodes are stronger, it has columellar and parietal plates (Peters 1855: pl. 3: fig. 12); its base has not been described in detail. Nerinea orbignyana Zeuschner sensu Peters (1855) has a series of distinct small cusps in suprasutural position, the bordering spiral cord is very strong, and it apparently has two further spiral cords on the base which are devoid of nodes.

Nerinea moreana (d’Orbigny, 1851)

Plate 12: figs 15–16, 17–18?

1851 – Nerinea moreana n. sp. – d’Orbigny: 100, pl. 257, figs 1–2.

?1851 – Nerinea clymene n. sp. – d’Orbigny: 102, pl. 258, figs 1–3.

1855 – Nerinea moreana d’Orbigny: 351, pl. 3, figs 5–7.

1881–1884 – Nerinea moreana d’Orbigny – Quenstedt: 546, pl. 206, fig. 47.

1882 – Itieria moreana d’Orbigny – Schlosser: 82, pl. 12, figs 2–3.

1893 – Itieria moreana d’Orbigny), Zittel – Loriol in Loriol and Lambert: 23, pl. 2, fig. 5.

1896 – Phaneroptyxis moreana (d’Orb.) – Cossmann: 22, pl. 2, fig. 1.

1898 – Phaneroptyxis moreana d’Orbigny – Cossmann: 14, pl. 2, figs 1–2.

1997 – Phaneroptyxis moreana (d’Orbigny, 1851) – Fischer and Weber 39, pl. 13, figs 3–4, ?fig. 5.

Material

Saal: 202 specimens; Saal, illustrated specimens SNSB-BSPG 2016 XXI 1901–1902; 3 specimens from location 1, level 4 (“Fundstelle 1, Sohle 4”).

Remarks

This large, conspicuous species (the illustrated specimen is 85 mm high) is very common in the Sylla-collection, but is missing from the previously known material from Saal. According to d’Orbigny (1851: pl. 257: fig. 1), the row of nodes lies well below the adapical suture. However, the holotype of this species as reported by Fischer and Weber (1997: p. 40, pl. 13: fig. 3, lower Kimmeridgian, France) shows that the nodes are in a subsutural position, which can also be observed in the present material. Fischer and Weber (1997) gave a range from the middle Oxfordian to Portlandian for this species.

Nerinea moreana d’Orbigny sensu Buvignier (1852) (on p. 35 as Nerinea tornatella Buvignier, pl. 24: figs 10–12 - the specimen in fig. 13 probably does not belong to this species) is more slender and has fewer nodes per whorl. The shell shape possibly falls within the range of variation of the species N. moreana. Cerithium apicatum Eichwald, 1861 is more slender, the spire is significantly higher in relation to the height of the last whorl, the axial ribs run from suture to suture and the entire shell is covered with numerous weak spiral threads. Nerinea moreana d’Orbigny sensu Gemmellaro (1870) is partly broader (pl. 3: fig. 6), partly more slender (pl. 4: fig. 6) than the typical form from Central and Western Europe (a variable species or several different species).

Nerinea moreana was assigned to Phaneroptyxis by Cossmann (1896, 1898) and Fischer and Weber (1997) but Kollmann (2014) pointed out that Phaneroptyxis is a junior synonym of Nerinea.

Endoplocus Cox, 1954

Type species

Actaeon staszycii Zeuschner, 1849; Tithonian; Poland.

Endoplocus staszycii (Zeuschner, 1849)?

Plate 13: figs 1, 2

?1850 – Actaeon staszycii n. sp. – Zeuschner: 130, pl. 17, figs 16–19.

1855 – Nerinea staszycii Zeuschner – Peters: 350, Tas. 2, figs 6–9.

1870 – Nerinea staszycii Zeuschner – Gemmellaro: 16, pl. 3, figs 8–10.

1998 – Endoplocus staszycii (Zeuschner, 1849) – Wieczorek: 319, pl. 2, figs 4–6 (here more chresonymy and synonymy).

Material

4 specimens, SNSB-BSPG 2016 XXI 1905–1908.

Plate 13. 

(1) Endoplocus staszycii (Zeuschner, 1849)?, SNSB-BSPG 2016 XXI 1905, lateral view, height 27 mm. (2) Endoplocus staszycii (Zeuschner, 1849)?, SNSB-BSPG 2016 XXI 1906, tranverse section of whorl showing plaits, height 9 mm. (3, 4) Endoplocus sp. 1, SNSB, SNSB-BSPG 2016 XXI 1909, lateral view and columellar section, height 41 mm. (5, 6) Endoplocus sp. 2, SNSB-BSPG 2016 XXI 1912, (5) whorls in transverse section, height 45 mm, (6) columellar section, height 74 mm. (7, 8) Endoplocus sp. 2, SNSB-BSPG 2016 XXI 1913, lateral view and columellar section, height 74 mm. (9) Ptygmatis bruntrutana (Thurmann, 1832), SNSB-BSPG 2016 XXI 1915, lateral view, height 11 mm. (10) Ptygmatis bruntrutana (Thurmann, 1832), SNSB-BSPG 2016 XXI 1916, whorl in transverse section, height 11 mm. (11, 12) Ptygmatis clio (d’Orbigny, 1852), SNSB-BSPG 2016 XXI 1917, (11) detail of columellar section, height 36 mm, (12) lateral view, height 69 mm. (13) Ptygmatis clio (d’Orbigny, 1852), SNSB XXI 1918, 13a) lateral view, height 60 mm, (13b) whorl in transverse section, height 11 mm. (14, 15) Ptygmatis clio (d’Orbigny, 1852), SNSB XXI 1919, lateral views, height 45 mm. (16–18) Bactroptyxis ? subcochlearis (Münster in Goldfuss, 1844), SNSB XXI 1921, (16) lateral view, height 69 mm, (17) lateral view of early whorls, height 32 mm, (18) lateral view of late whorls, height 36 mm. (19) Cryptoplocus subpyramidalis (Münster in Goldfuss, 1844), SNSB-BSPG 2016 XXI 1922, lateral view, height 142 mm.

Description

Shell stout with egg-shaped outline, consisting of few whorls; largest specimen 27 mm high; body whorl higher than the spire; whorl face weakly convex; whorls relatively high, smooth; sutures marked by a narrow ramp; transition from whorl face to base evenly rounded; base strongly convex, smooth; aperture not preserved; 2 (3?) columellar and palatal plaites as well as a parietal plait visible in longitudinal section.

Remarks

According to Peters (1855), Nerinea staszycii Zeuschner, 1850 is a very variable species. The specimens illustrated by Peters (1855, pl. 2: figs 6–9) correspond to the present material assigned to this species. Actaeon staszycii Zeuschner, 1850 is more slender, the spire is higher and it has more whorls. Itieria austriaca Zittel, 1873 has a subsutural row of nodes. Nerinea staszycii Zeuschner sensu Gemmellaro (1870) has a lower last whorl in relation to the spire height and the shell is more slender. Phaneroptyxis simmenensis Ooster sensu Cossmann (1898) is more slender and its body whorl is more cylindrical.

Endoplocus acutus Gründel, Keupp, Lang & Nützel, 2022

pl. 7: figs 1–7 in Gründel et al. (2022)

2022 – Endoplocus acutus n. sp. – Gründel, Keupp, Lang and Nützel: 189, pl. 7, figs 1–7.

Material

All from Saal, 12 specimens (typical form), 6 specimens (variant form), 3 questionable specimens.

Endoplocus inflatus Gründel, Keupp, Lang & Nützel, 2022

Plate 12: fig. 19

2022 – Endoplocus inflatus n. sp. – Gründel, Keupp, Lang and Nützel: 190, pl. 8, figs 1–4.

Material

2 specimens, SNSB-BSPG 2016 XXI 1903–1904.

Remarks

The present specimens agree with the morphology of Endoplocus inflatus Gründel et al., 2022. However, they are significantly larger (height 34 mm and 54 mm). At least one columellar and one parietal fold are present.

Endoplocus sp. 1

Plate 13: figs 3, 4

Material

3 specimens, SNSB-BSPG 2016 XXI 1909–1911.

Description

Shell broadly trochospiral with strongly convex sides; illustrated specimen 41 mm high; suture somewhat impressed; last whorl large, inflated; transition from whorl face to strongly convex base evenly rounded; whorls smooth; aperture high and narrow; at least one columellar, parietal and palatal (?) plate present.

Remarks

The shell of Endoplocus inflatus Gründel et al. 2022 is more slender and not as rounded in lateral view. The spire is much more slender and higher. Itieria obtusiceps Zittel sensu Stefano (1884) has a more broadly oval outline in lateral view.

Endoplocus sp. 2

Plate 13: figs 5–8

Material

Saal: 3 specimens, SNSB-BSPG 2016 XXI 1912–1914.

Description

Shell highly trochoid; illustrated specimen 74 mm high; spire whorls significantly wider than high; sutures impressed; last whorl high; shell sides convex with evenly rounded transition to convex base; no ornament visible; aperture (always damaged) elongated, narrow, actute adapically; at least one columellar, parietal and palatal plait present.

Remarks

The available material is too sparse and poorly preserved for a sufficient description. The relationships to Endoplocus inflatus remain unclear. The latter may have more and lower spire whorls.

Family Ptygmatididae Pčelintsev, 1965

Subfamily Ptygmatidinae Pčelintsev, 1965

Ptygmatis Sharpe, 1850

Type species

Nerinea bruntrutana Thurmann, 1832; Oxfordian; Switzerland.

Ptygmatis ? tornata (Quenstedt, 1852)

pl. 10: figs 1–12 in Gründel et al. (2022)

2022 – Ptygmatis tornata (Quenstedt, 1852) – Gründel, Keupp, Lang and Nützel: 192, pl. 10, figs 1–12 (here more chresonymy and synonymy).

Material

Ptygmatis tornata sensu stricto (morphotype 1): Saal: 8 specimens; Saal, locality 1985, above coral stock, level 2 (“Fundort 1985, über Korallenstock, Sohle 2”): 17 specimens. Ptygmatis tornata (morphotype 1): Saal: 8 specimens. 2 questionable specimens.

Ptygmatis nodosa (Voltz, 1836)

pl. 11: figs 1–15 in Gründel et al. (2022)

1852 – Nerinea nodosa Voltz – Buvignier: 34, pl. 4, fig. 6.

2022 – Ptygmatis nodosa (Voltz, 1836) – Gründel, Keupp, Lang and Nützel: 194, pl. 11, figs 1–15 (here more chresonymy and synonymy).

Material

54 specimens, Saal: 51 specimens, locality 1985, above coral stock, level 2 (“Fundort 1985, über Korallenstock, Sohle 2”): 3 specimens.

Ptygmatis mandelslohi (Bronn, 1836)

pl. 9: figs 1–5 in Gründel et al. (2022)

2022 – Ptygmatis mandelslohi (Bronn, 1836) – Gründel, Keupp, Lang and Nützel: 191; pl. 9, figs 1–5 (here more chresonymy and synonymy).

Material

9 specimens (6 specimens from Saal, 3 specimens Saal, locality 1, level 4 (“Sohle 4, Fundstelle 1”).

Remarks

The weak adapical spiral groove described by Gründel et al. (2022) is not recognizable in the present material (due to preservation?). Gründel et al. (2022) emphasized the difficulties in distinguishing P. mandelslohi from similar species. The distinction between the species Ptygmatis mandelslohi and P. bruntrutana is problematic. Various authors (e. g., Fischer and Weber 1997) considered both to be conspecific. In our opinion, P. mandelslohi is characterized by a moderately wide shell, the apical angle decreases during ontogeny (resulting in cyrtoconoid shell shape), it usually has a straight to slightly concave whorl face, relatively low whorls and a sharp edge between flank and base. P. bruntrutana, on the other hand, has a more slender shell (with the same plate pattern), whorls are evenly increasing in width over the entire shell (not cyrtoconoid), whorls are generally higher, the whorl face is straight to slightly convex, the transition between whorl face and base lacks a sharp edge. However, there are specimens in the present material that cannot be clearly assigned to one of the two species (real differences or due to preservation?).

Ptygmatis bruntrutana (Thurmann, 1832)

Plate 13: figs 9, 10

non 1844 – Nerinea bruntrutana Thurmann – Goldfuss: 40, pl. 175, fig. 5.

1858 – Nerinea mandelslohi Bronn – Quenstedt: 767, pl. 94,.figs 14?, 15.

1861–1864 – Nerinea bruntrutana Th. – Thurmann and Étallon: 94, pl. 7, fig. 39.

?1869 – Nerinea bruntrutana Thurmann, 1830 – Ooster and Fischer-Ooster: 7, pl. 2; Fig: 12–16.

part. 1881–1884 – Nerinea bruntrutana Thurmann – Quenstedt: 533ff., pl. 206, figs 1–5, 13–14; non figs 18–20, 23.

1882 – Ptygmatis bruntrutana Thurmann – Schlosser: 79, pl. 11, figs 11–13.

Part 1889 – Ptygmatis bruntrutana Thurmann – Loriol in Loriol and Koby: 27, pl. 3, figs 4–5, 7?, 9–12.

1893 – Ptygmatis bruntrutana (Thurmann) Zittel – Loriol in Loriol and Lambert: 25, pl. 2, figs 6–8.

1898 – Ptygmatis bruntrutana Thurmann – Cossmann: 74, pl. 6, figs 13–17, 20–21?

1979 – Ptygmatis bruntrutana (Thurmann, 1832) – Wieczorek: 324, figs 10, 14, 19–21; pl. 8, figs 2–5, 7

1997 – Nerinea bruntrutana Thurmann – Hägele: 34, figures on p. 34 and 35

1997 – Nerinea bruntrutana (Thurmann, 1832) – Hägele: 128, pl. 12, fig. 5 [as Cossmannea (Eunerinea) subscalaris (Münster, 1844)] and 128 upper left.

1997 – Ptygmatis bruntrutana (Bronn ex Thurmann, 1850) – Fischer and Weber: 42, pl. 10, fig. 6.

Material

6 specimens from Saal, illustrated specimens SNSB-BSPG 2016 XXI 1915–1916.

Ptygmatis clio (d’Orbigny, 1852)

Plate 13: figs 11–15

2022 – Ptygmatis clio (d’Orbigny, 1852) – Gründel, Keupp, Lang and Nützel: 196; pl. 12, figs 1–3 (here more chresonymy and synonymy).

Material

29 specimens from Saal, illustrated specimens SNSB-BSPG 2016 XXI 1917–1919.

Ptygmatis ? ursicina (Thurmann in Thurmann and Étallon 1861)

pl. 12: figs 5–7 in Gründel et al. (2022)

2022 – Ptygmatis ? ursicina (Thurmann in Thurmann and Étallon 1861) – Gründel, Keupp, Lang and Nützel: 196; pl. 12, figs 5–7.

Material

A fragment of 4 whorls, SNSB-BSPG 2016 XXI 1920.

Bactroptyxis Cossmann, 1896

Type species

Nerinea implicata d’Orbigny, 1851; Bathonian; France.

Bactroptyxis ? subcochlearis (Münster in Goldfuss, 1844)

Plate 13: figs 16–18

2022 – Bactroptyxis ? subcochlearis (Münster in Goldfuss, 1844) – Gründel, Keupp, Lang and Nützel: 199, pl. 13, figs 6–8 (here more chresonymy and synonymy).

Material

6 specimens and fragments, illustrated specimen SNSB-BSPG 2016 XXI 1921.

Remarks

The illustrated specimen is 69 mm high. What was suspected in 2022 can now be proven: The early whorls have only 2 strong spiral cords, one directly subsutural, the other well above the abapical suture. Only gradually a weaker spiral cord is formed between the primary spiral cords. The secondary spiral cord remains significantly weaker than the other two throughout ontogeny.

Aptyxis kehlheimensis Schlosser, 1882 (pl. 11: figs 3, 5–7; non fig. 4 in Schlosser) has weaker spiral cords and lacks a secondary third spiral cord.

Subfamily Cryptoplocinae Pčelintsev in Pčelintsev and Korobkov, 1960

Cryptoplocus Pictet & Campiche, 1861

Type species

Nerinea depressa Voltz, 1836; Kimmeridgian?

Cryptoplocus subpyramidalis (Münster, 1844) in Goldfuss

Plate 13: fig. 19

1855 – Nerinea pyramidalis Münster – Peters: 361, pl. 4, figs 1–3.

1882 – Cryptoplocus subpyramidalis – Schlosser: 86, pl. 12, fig. 10.

2022 – Cryptoplocus subpyramidalis (Münster in Goldfuss, 1844) – Gründel, Keupp, Lang and Nützel: 200, pl. 14, fig. 6 (here more chresonymy and synonymy).

Material

20 specimens and fragments (19 specimens from Saal; 1 specimen Saal, location 2, level 4 (“Fundstelle 2, Sohle 4”); illustrated specimen SNSB-BSPG 2016 XXI 1922.

Remarks

The present material is only moderately preserved. The illustrated specimen is 14 cm high. The subsutural bulge is often not visible. The apical angle of the shell varies; there may be transitions to C. depressus. Cryptoplocus pyramidalis (Münster, 1844) in Goldfuss, sensu Wieczorek (1979) is more slender; its shell width lies approximately between C. subpyramidalis and C. depressus (Voltz, 1836).

Cryptoplocus depressus (Voltz, 1836)

pl. 14: figs 1–5 in Gründel et al. (2022)

1931 – Cryptoplocus depressus Voltz – Yin: 68, pl. 7, fig. 10.

1979 – Cryptoplocus depressus (Voltz, 1836) – Wieczorek: 327, pl. 9, figs 1–3, 5–6, textfig. 13a–b.

2022 – Cryptoplocus depressus (Voltz, 1836) – Gründel, Keupp, Lang and Nützel: 200, pl. 14, figs 1–5 (here more chresonymy and synonymy).

Material

39 specimens and fragments (37 specimens Saal; 2 specimens Saal, above coral stock, level 2 (“über Korallenstock, Sohle 2”).

Family Nerinellidae Pčelintsev in Pčelintsev and Korobkov, 1960

Nerinella Sharpe, 1850

Type species

Nerinea dupiniana d’Orbigny, 1842; lower Cretaceous; France.

Nerinella ornata (d’Orbigny, 1852)

pl. 15: figs 1–5 in Gründel et al. (2022)

2022 – Nerinella ornata (d’Orbigny, 1852) – Gründel, Keupp, Lang and Nützel: 202; pl. 15, figs 1–5 (here more chresonymy and synonymy).

Material

A fragment of 2 whorls from Saal.

Family Eunerineidae Kollmann, 2014

Eunerinea Cox, 1947

Type species

Nerinea castor d’Orbigny, 1852; Oxfordian; France.

Eunerinea sp. 1

Plate 14: figs 1–6

?1861–1864 – Nerinea speciosa Voltz – Thurmann in Thurmann and Étallon: 104, pl. 8, fig. 51.

part 1997 – Nerinella cf. laufonensis (Thurmann, 1859) – Hägele: 131, fig. on p. 131 upper middle (not upper right).

?1997 – Nerinella caecilia (d’Orbigny, 1852) – Fischer and Weber: 52, pl. 8, figs 1–2.

2022 – Gen. et sp. indet. – Gründel, Keupp, Lang and Nützel: 212, pl. 19, figs 9–11.

Material

20 specimens from Saal and 2 specimens from Saal, location 2, illustrated specimens SNSB-BSPG 2016 XXI 1923–1925.

Plate 14. 

(1) Eunerinea sp. 1, SNSB BSPG 2021 XV 92, lateral view, height 19 mm. (2, 3) Eunerinea sp. 1, SNSB-BSPG 2016 XXI 1923, lateral and basal view, height 33 mm, width 16 mm. (4, 5) Eunerinea sp. 1, SNSB-BSPG 2016 XXI 1924, (4) lateral view, height 34 mm, (5) last two whorls height 21 mm. (6) Eunerinea sp. 1, SNSB-BSPG 2016 XXI 1925, fragment of a single whorl in lateral view, height 34 mm. (7) Eunerinea sp. 2, SNSB-BSPG 2016 XXI 1926, fragment of a single whorl in lateral view, width 16 mm. (8) Eunerinea sp. 2, SNSB-BSPG 2016 XXI 1927, lateral view, height 38 mm. (9–11) Itieria cabanetiana (d’Orbigny, 1841), SNSB-BSPG 2016 XXI 1928, lateral views, height 67 mm, basal view, width 41 mm. (12, 13) Itieroptygmatis cylindrata Gründel et al., 2022, morphotype 2, SNSB-BSPG 2016 XXI 1929, lateral views, height 24 mm.

Description

Only fragments are present; fragment shown on Plate 14: figs 2, 3 is 34 mm high; shell slender; whorl face straight to slightly concave; subsutural nodular bulge; strength of bulge and nodes vary from distinct to almost absent; a specimen from the collection Lang (Plate 14: fig. 1) has very distinct nodes that are axially elongated and opisthocline; some specimens with distinct knobby spiral cord between subsutural bulge and abapical suture as well as one (or several?) weak, knobby spiral cords on either side of it; other specimens have only two weak knobby spiral cords of approximately equal strength; transition from whorl face to slightly convex base at slightly protruding edge that forms periphery of whorls; edge has strong strong nodes, some of which visible above suture; several knobby spiral cords cover base; late whorls of large specimens have blurred axial ribs on whorl face and base; base phaneromphalous; aperture with abapical canal; at least one columellar and one (or two?) parietal plaits present in aperture.

Remarks

The few available specimens are mainly poorly preserved and show quite some variation. A comparison of Plate 14: fig. 1 with Plate 14: figs 2, 3 shows two extreme morphotypes. However, most of the fragments cannot be assigned to one of these morphotypes with certainty because of insufficient preservation. It is also not certain whether these morphologies grade into each other. The grouping of the present material under the name Eunerinea sp. 1 is based on similarities in the general shell shape and the basic shell ornament, the occurrence at the same locality and in the same stratigraphic level. It remains unclear whether there is one variable species or two separate species. Several species described in the literature resemble either one or the other mentioned morphotype.

The neotype of Nerinella caecilia (d’Orbigny) (see Fischer and Weber 1997) closely resembles the present species, but apparently has more numerous spiral cords on the whorl face and lacks a subsutural row of nodes. The whorls are at least partially more concave. Nerinella subimbricata d’Orbigny, 1852 sensu Fischer and Weber (1997) is significantly more slender and the whorl face is more concave. Ptygmatis nodosa (Voltz, 1836) sensu Gründel et al. (2022) has, among other differences, a border spiral cord without nodes. Nerinea sequana Thirr sensu Bronn (1836) is more slender and the whorls are concave. Nerinea laufonensis Thurmann in Thurmann and Étallon 1861 lacks a subsutural row of nodes, the border spiral rib is hardly knobby and, in addition to two rows of nodes, several lirae are formed on the whorl face. Nerinea oppeli Gemmellaro, 1870 is similar to the specimen shown in Plate 14: fig. 1, but the subsutural row of nodes is weaker, whereas the nodes of the border spiral cord are stronger and are fully visible above the suture. Nerinea cf. heightneggeri Peters sensu Cossmann (1898) is more slender and has 7–8 spiral cords on the whorl face, two of which are tuberculate.

Eunerinea sp. 2

Plate 14: figs 7, 8

Material

1 specimen and a fragment from Saal, SNSB-BSPG 2016 XXI 1926–1927.

Description

Shell high-spired, slender; specimen 39 mm high; sutures inconspicuous; angular edge at transition from whorl face to base exposed somewhat above suture; strong spiral cord situated at a clear distance from adapical suture; whorl face between this spiral cord and adapical suture concave, between this cord and abapical suture straight to slightly concave; edge at transition from whorl face to base very pronounced, slightly protruding, forming whorl periphery; edge probably knobby, which is not entirely certain due to preservation; base moderately convex, details are not preserved.

Remarks

The similar Ptygmatis nogreti Guirand and Ogérien sensu Loriol in Loriol and Bourgeat (1886–1888) has a strong spiral cord directly below the suture. Ptygmatis carpathica sensu Loriol in Loriol and Bourgeat (1886–1888) is larger, not as slender and the subsutural spiral cord is not broadened.

Family Itieriidae Cossmann, 1896

Itieria Matheron, 1842

Type species

Acteon cabanetiana d’Orbigny, 1841; Kimmeridgian; France.

Itieria cabanetiana (d’Orbigny, 1841)

Plate 14: figs 9–11

1851 – Itieria cabanetiana d’Orbigny, 1847 – d’Orbigny: 99, pl. 255, fig. 3, pl. 256, figs 1–3.

1869 – Itieria cabaneti Matheron – Gemmellaro: 9, pl. 2, figs 1–3.

1898 – Itieria cabanetiana d’Orbigny – Cossmann: 12, pl. 1, figs 17–20.

1997 – Itieria cabanetiana (d’Orbigny, 1841) – Fischer and Weber: 39, pl. 14, figs 1–4.

2014 – Itieria cabanetiana (d’Orbigny, 1841) – Kollmann: 360, fig. 6 A–B.

Material

13 specimens and fragments, illustrated specimen SNSB-BSPG 2016 XXI 1928.

Description

Shell broadly egg-shaped with last whorl much higher than spire; illustrated specimen 67 mm high; apex concave; spire whorl much wider that high; suture emphasized by very narrow ramp; whorl face feebly convex to almost straight; transition from whorl face to base evenly rounded; whorls smooth; base distinctly umbilicated; umbilicus surmounted by strong ridge; aperture elongated, very narrow, widened abapically resulting in teardrop shape; apertural folds or plaits cannot be seen clearly.

Remarks

The lectotype of this species designated by Fischer and Weber (1997, pl. 14: fig. 1) is much larger and the spire is higher with more whorls than in the present material.

Itieroptygmatis Charvet & Termier, 1971

Type species

Itieroptygmatis ellipticata Charvet & Termier, 1971; Jurassic/Cretaceous transition; Bosnia and Herzegovina.

Itieroptygmatis cylindrata Gründel, Keupp, Lang & Nützel, 2022

Plate 14: figs 12, 13

2022 Itieroptygmatis cylindrata n. sp. – Gründel, Keupp, Lang and Nützel: 207, pl. 18, figs 1–14

Material

Morphotype 1: 53 specimens (Saal: 48 specimens; locality 1985, above coral stock, level 2 (“Fundort 1985, über Korallenstock, Sohle 2”): 5 specimens. Morphotype 2, Saal: 32 specimens, illustrated specimen SNSB-BSPG 2016 XXI 1929.

Remarks

Two morphotypes assigned to this species were described by Gründel et al. (2022). The extremes in this morphological spectrum differ greatly from each another. However, there are also specimens that are difficult to assign to one of the two morphotypes. As outlined previously, it is undecided whether a variable species or two separate species are present, mainly due the poor preservation of the material at hand. A well-preserved juvenile specimen (shell height 24 mm; Plate 14: fig. 12, 13) of morphotype 2 shows the plait structure: 2 columellar plaits (the adapical one is significantly weaker than the abapical one) and a strong parietal plait. Palatal plaits are not noticeable.

Itieroptygmatis sp. 1

pl. 18: figs 15–16 in Gründel et al. (2022)

2022 – Itieroptygmatis sp. 1 – Gründel, Keupp, Lang and Nützel: 209, pl. 18, figs 15–16.

Material

1 specimen from Saal, SNSB-BSPG 2016 XXI.

Rugalindrites Gründel & Nützel, 2012

Type species

Acteon cuspidatus Sowerby, 1824; Bathonian; England.

Rugalindrites cylindracea (Cornuel, 1841)

pl. 20: figs 1–9 in Gründel et al. (2022)

2022 – Rugalindrites cylindracea (Cornuel, 1841) – Gründel, Keupp, Lang and Nützel: 212, pl. 20, figs 1–9 (here more chresonymy and synonymy).

Material

17 specimens, SNSB-BSPG 2016 XXI.

Discussion

A new collection (mostly collected by Jürgen Sylla) of Upper Jurassic (Kimmeridgian) gastropods from the reefal limestones of the Saal quarry near Kelheim (Lower Bavaria, Germany) is reported. This new material provides considerable additional information about the gastropod fauna from the Saal quarry. It has yielded 121 species of which 80 species are nominate species, the others are treated in open nomenclature. Together with the gastropod previously described from the Saal quarry (Gründel et al. 2015, 2017, 2019, 2022), this increases the number of known gastropod species from this locality by 53 species (32 nominate species). A total of 179 gastropod species (108 nominate species) have now been reported from the Saal quarry (Tables 1, 2) making this gastropod occurrence one of the richest known from the Late Jurassic. One new genus and 15 new species are described herein. Thus, Saal is now type locality of 59 gastropod species. The high diversity of gastropods and other marine invertebrates (e. g., bivalves, brachiopods, corals) reflects the highly structured reefal, shallow water habitat (see Gründel et al. 2022). The high number of taxa that had to be treated in open nomenclature reflects the poor preservation of many of the specimens. Especially the fragmentary preservation of nerineoids and other high-spired taxa as well as the corrosion of the shell ornaments commonly hinder species identification.

Table 1.

Gastropod species diversity from the Saal Quarry.

Total number of species 179
Total number of nominate species 109
Number of species with type locality at Saal 59
Number of species only from Sylla collection (this study) 53
Number of species only previous collections 58
Number of species present in both, in previous and Sylla collections 68
Table 2.

Species and abundances of the gastropods from Saal, with differentaion of the previous collections and the Collection of J. Sylla. Attributions to subclass, Pat: Patellogastropoda, Vet: Vetigastropoda, Ner: Neritimorpha, Cae: Caenogastropoda, Het: Heterobranchia.

Specimens previous studies Specimens this study Specimens combined Species only in previous studies Species only in this study Species previous and this study
Pat Hennocquia saalensis Gründel et al., 2017 3 3 1
Pat Patella sp. 1 1 1
Pat Scurriopsis cragolis Gründel & Nützel, 2024 4 4 1
Pat Scurriopsis sp. 1 1 1
Pat Pseudorhytidopilus ? quadratus Gründel & Nützel, 2024 7 7 1
Vet Pleurotomaria agassizii Münster in Goldfuss, 1844 2 2 1
Vet Emarginula (Tauschia) sp. 1 1 1 1
Vet Rimulopsis broesamleni Gründel et al., 2017 7 4 11 1
Vet Rimulopsis perforata Gründel, Keupp & Lang, 2017 3 3 6 1
Vet Rimulopsis danuviensis Gründel & Nützel, 2024 4 4 1
Vet Leptomaria goldfussi (Sieberer, 1907) 5 12 17 1
Vet Leptomaria phacoides Zittel, 1873 2 2 1
Vet Leptomaria phacoides Zittel, 1873? 1 1 1
Vet Leptomaria sp. 1 1 1
Vet Placostoma suevica (Quenstedt, 1881–1884) 6 5 11 1
Vet Valfinia quinquecincta (Zieten, 1830–1833) 12 2 14 1
Vet Scissurella? sp. 1 1 1 1
Vet Falsotectus parvus Gründel et al., 2017 76 4 80 1
Vet Falsotectus sp. nov. 1 9 9 1
Vet Asperilla longispina (Rolle, 1861) 2 2 1
Vet Discotectus crassiplicatus (Étallon, 1859) 9 9 18 1
Vet Undatotectus glaber Gründel et al., 2017 9 11 20 1
Vet Wernerocutus angulatoplicatus (Münster in Goldfuss, 1844) 5 11 16 1
Vet Falsataphrus ? valfinense (Loriol in Loriol and Bourgeat, 1886–1888) 2 2 1
Vet Eucycloscalidae? gen. inc. sp. 1 1 1 1
Vet Torusataphrus inornatus (Quenstedt, 1858)? 1 1 1
Vet Chilodonta quadratofoveata Gründel et al., 2017 3 1 4 1
Vet Chilodonta haegelei Gründel et al., 2017 1 1 1
Vet Onkospira ranellata (Quenstedt, 1852) 1 3 4 1
Vet Proconulus? sp. 1 3 3 6 1
Vet Amphitrochus muensteri Gründel et al., 2017 1 1 1
Vet Serrettella gerberi (Gründel, Keupp & Lang, 2017) 1 4 5 1
Vet Nododelphinula magnotuberosa Gründel et al., 2017 2 2 1
Vet Nododelphinula oblonga Gründel & Nützel, 2024 2 2 1
Vet Heliacanthus? sp. 1 1 4 5 1
Vet Heliacanthus? sp. 2 7 7 1
Vet Nododelphinulidae? gen. and sp. indet. 1 1 2 1
Vet Torusataphrus inornatus (Quenstedt, 1858) 1 1 2 1
Vet Metriomphalus parvotuberosus Gründel et al., 2017 8 7 15 1
Vet Metriomphalus sp. 1 8 1 9 1
Vet Planiturbo funatus (Goldfuss, 1844) 3 3 1
Vet Planiturbo procerus Gründel et al., 2017 6 3 9 1
Vet Planiturbo validotuberosus Gründel et al., 2017 7 7 1
Vet Caryomphalus concavus Gründel et al., 2017 11 11 1
Vet Caryomphalus sp., cf. concavus Gründel, Keupp & Lang, 2017 1 1 1
Vet Caryomphalus globatus (Buvignier, 1843) 4 4 1
Vet Metriomphalidae gen. nov.? sp. 1 4 1 5 1
Vet Creniturbo gibbosus Gründel & Nützel, 2024 7 7 1
Vet Creniturbo sp. 1 4 4 1
Vet Kelheimia triangulata Gründel & Nützel, 2024 9 9 1
Vet Tegulacanthus tegulatus (Münster in Goldfuss, 1844) 1 1 1
Vet Sclarotrarda coronilla (Brösamlen, 1909) 6 6 1
Vet gen. inc., sp. inc. 9 9 1
Vet Vetigastropoda gen. and sp. indet. 1 1 1
Ner Dauterria rotundata Gründel et al., 2015 110 35 145 1
Ner Dauterria variocostata Gründel et al., 2015 100 3 103 1
Ner Pileopsella biconvexa Gründel et al., 2015 6 5 11 1
Ner Neridomus laevis (Gerasimov, 1955)? 112 112 1
Ner Neridomus hemisphaerica (Roemer, 1836) 10 10 1
Ner Neridomus sp. 1 2 2 1
Ner Parvulatopsis quinquecostatus Gründel et al., 2015 33 5 38 1
Ner Parvulatopsis? sp. 5 5 1
Ner Neritopsis ? rotundatus Gründel & Nützel, 2024 6 6 1
Ner Wallowiella (Plicaropsis) cancellata (Stahl, 1824) 28 27 55 1
Ner Wallowiella (Plicaropsis) compacta Gründel et al., 2015 2 2 4 1
Ner Cassianopsis quenstedti (Brösamlen, 1909) 7 2 9 1
Ner Cassianopsis ratua Gründel et al., 2015 2 1 3 1
Ner Cassianopsis eversi Gründel et al., 2015 5 5 1
Ner Hayamiella schaeferi Gründel et al., 2015 12 6 18 1
Ner Hayamiella semiplicata (Brösamlen, 1909) 2 1 3 1
Ner Hayamiella decussata (Münster, 1844 in Goldfuss) 1 1 1
Ner Hayamiella subvaricosa (Brösamlen, 1909) 4 4 1
Ner Hayamiella? sp. 2 2 1
Ner Bipartopsis robustus Gründel et al., 2015 8 1 9 1
Cae Pseudomelania sp. 1 8 8 1
Cae Pseudomelania? sp. 2 7 7 1
Cae Saalensia birugata Gründel et al., 2015 42 22 64 1
Cae Loriolotrema sp. 1 1 1
Cae Brachytrematidae? gen.and sp. indet. 1 1 1
Cae Petersia sp. 1 1 1 1
Cae Costazygia sp. 1 3 3 1
Cae Erratopleura sp. 1 1 1 1
Cae Ampullina sp. 1 7 7 1
Cae Pictavia silicea (Quenstedt, 1858) 1 1 2 1
Cae Pictavia lactera Gründel et al., 2019 2 8 10 1
Cae Pictavia? sp. 1 1 2 1
Cae Oonia kimmeridgiensis Gründel & Nützel, 2024 3 3 1
Cae Globularia? sp. 1 1 1
Cae Neuburgensia convexoconcava (Gründel, Keupp & Lang, 2019) 10 2 12 1
Cae Neuburgensia angulata Gründel & Nützel, 2024 53 53 1
Cae Neuburgensia rara Gründel & Nützel, 2024 1 1 1
Cae Metacerithium sp. 1 15 15 1
Cae Tylostoma sp. 1 6 6 12 1
Cae Eustoma ? gracilis Gründel & Nützel, 2024 5 5 1
Cae Eustoma sp. 3 3 1
Cae Ditretus sp., cf. rostellaria (Buvignier, 1852) 3 11 14 1
Cae Coninoda strekwera Gründel et al., 2019 10 2 12 1
Cae Coninoda? sp. 1 5 1 6 1
Cae Maoraxis sp. 1 1 1 1
Cae Cryptoptyxis rarenodosa Gründel et al., 2019 21 5 26 1
Cae Cryptoptyxis? spinosus Gründel & Nützel, 2024 3 3 1
Cae Nudivagus sp. 1 5 3 8 1
Cae Nudivagus sp. 2 2 2 1
Cae Uchauxia ex gr. limaeforme (Roemer, 1836) 44 44 1
Cae Provolibathra ? sp., cf. septemplicata (Roemer, 1836) 69 3 72 1
Cae Cryptaulax ? parvum Gründel et al., 2019 3 3 1
Cae Cryptaulax ? triangulare Gründel et al., 2019 3 3 1
Cae Tyrnoviella sp. 1 1 1 1
Cae Exelissa sp. 1 2 2 4 1
Cae Exelissa ? Aff. corallense (Buvignier, 1843) 1 1 1
Cae Exelissa ursicina (Loriol in Loriol & Koby, 1889) 1 1 1
Cae Shurovites robustus Gründel et al., 2019 5 5 1
Cae Shurovites sp. 1 1 1 1
Cae Tropacerithium cumaritum Gründel et al., 2019 9 1 10 1
Cae Tropacerithium danubii Gründel et al., 2019 15 2 17 1
Cae Turritella lucagrita Gründel & Nützel, 2024 1 1 1
Cae Bleytonella saalensis Gründel et al., 2019 10 10 1
Cae Juvenile cerithioid 1 1 1
Cae Palaeorissoina sp. 1 1 1 1
Cae Boreomica costaspiralis Gründel et al., 2019 10 10 1
Cae Boreomica sp. 1 1 1
Cae Boreomica sp. 2 1 1 1
Cae Purpuroidea lapierrea (Buvignier, 1843) 2 2 1
Cae Buvignieria sp. nov. 1 2 2 1
Cae Buvignieria racitana Gründel et al., 2019 106 1 107 1
Cae Buvignieria convexa Gründel et al., 2019 14 14 1
Cae Palaeorissoinidae? gen. inc., sp. 1 1 1 1
Cae Falsobuvigna peregrina Gründel et al., 2019 24 24 1
Cae Columbellaria corallina (Quenstedt, 1852) 7 3 10 1
Cae Columbellaria sp. 1 1 1 1
Cae Gen. indet. schlosseri (Loriol in Loriol & Bourgeat, 1886–1888) 4 4 1
Cae Gen. indet. monilitesta Zittel, 1873 1 1 1
Cae Strombidae gen. inc., sp. 1 1 1 1
Cae Diarthema aspera Gründel & Nützel, 2024 2 8 10 1
Cae Diempterus sp. 1 4 4 1
Cae Diempterus ? fusiformis (Münster in Goldfuss, 1844) 5 5 1
Cae Caenogastropoda gen. inc. 1, sp. 1 3 3 1
Het Cossmannea desvoidyi (d’Orbigny, 1851) 2 2 1
Het Ceritellopsis gramanni Huckriede, 1967 25 25 1
Het Ceritellopsis plicatula Huckriede, 1967 5 5 1
Het Ceritella convexa Gründel et al., 2022 26 26 1
Het Ceritella sp. 1 9 9 1
Het Nerinea donosa Gründel et al., 2022 10 45 55 1
Het Nerinea moreana (d’Orbigny, 1851) 202 202 1
Het Endoplocus acutus Gründel et al., 2022 17 18 35 1
Het Endoplocus inflatus Gründel et al., 2022 10 2 12 1
Het Endoplocus staszycii (Zeuschner, 1850)? 4 4 1
Het Endoplocus sp. 1 3 3 1
Het Endoplocus sp. 2 3 3 1
Het Pseudonerinea ? pseudomelaniformis Gründel et al., 2022 37 27 64 1
Het Ptygmatis mandelslohi (Bronn, 1836) 4 9 13 1
Het Ptygmatis ? tornata (Quenstedt, 1852) 37 33 70 1
Het Ptygmatis nodosa (Voltz, 1836) 142 54 196 1
Het Ptygmatis ? ursicina Thurmann in Thurmann & Étallon, 1861 19 1 20 1
Het Ptygmatis bruntrutana (Thurmann, 1832) 6 6 1
Het Ptygmatis clio (d’Orbigny, 1852) 2 29 31 1
Het Aptyxiella tricincta (Münster, 1844) 1 1 1
Het Aptyxiella tricincta (Münster, 1844) sensu Quenstedt 1881–1884 3 5 8 1
Het Aptyxiella planata (Quenstedt, 1858) 2 2 1
Het Aphanoptyxis sinerugae Gründel & Nützel, 2024 3 3 1
Het Bactroptyxis cf. fasciata (Voltz, 1836) 1 1 1
Het Bactroptyxis ? subcochlearis (Münster in Goldfuss, 1844) 5 6 11 1
Het Cryptoplocus depressus (Voltz, 1836) 3 39 42 1
Het Cryptoplocus subpyramidalis (Münster, 1844 in Goldfuss) 3 20 23 1
Het Nerinella sp. 1 4 4 1
Het Nerinella ornata (d’Orbigny, 1852) 1 2 3 1
Het Nerinella sp. 2 2 2 1
Het Nerinella sequana (Bronn ex Thirria, 1836) 1 1 1
Het Nerinella biplicata (Quenstedt, 1858) 4 4 1
Het Nerinella? sp. 3 1 1 1
Het Eunerinea sp. 1 1 22 23 1
Het Eunerinea sp. 2 1 2 3 1
Het Itieria cabanetiana (d’Orbigny, 1841) 13 13 1
Het Itieroptygmatis cylindrata Gründel et al., 2022 57 85 142 1
Het Itieroptygmatis sp. 1 2 1 3 1
Het Rugalindrites cylindracea (Cornuel, 1841) 48 17 65 1
Het Rugalindrites sp. 1 2 2 1
Het Volvocylindrites marcousana (Guirand & Ogérien, 1865) 39 39 1
Het Sulcoactaeon sp. 1 1 1 1
Total 1666 1095 2761 58 53 68

The Sylla collection has yielded quite a number of species that were not present in the previously studied material but also lacks taxa that are present in previously studied collections mainly gathered by Fritz Lang and additional material gathered by Helmut Keupp and Olaf Neubauer (Gründel et al. 2015, 2017, 2019, 2022). Fifty-nine species were only present in these collections studied earlier, and 54 species are only present in the Sylla collection. Sixty-five species are shared between previously studied and new collections, chiefly the Sylla collection. It is also noteworthy that species that are present in both collections commonly occur in strongly different abundances (Table 1). These differences in the faunal compositions probably reflects facies differences within the quarry at different sites. Moreover, collectors obviously used different methods (loot scheme, collection bias i. e., Sylla collected many more large specimens whereas Lang gathered preferably small specimens and species. We assume that many of the specimens treated in open nomenclature represent undescribed taxa and that the quarry yields many more species than are known to date. Currently, the quarry is not accessible due to safety reasons so that new material cannot be collected. It is possible that there are other private collections from Saal and if so, their study would be desirable.

Nerineoidea form a considerable part of the gastropod fauna from Saal. With the Lang and Sylla collections, there are two independently obtained large nerineoid gastropod collections from the same location and the same age. However, both differ significantly from each other in the abundances of the species present in both collections and in the fact that many species are only represented in one of the collections. From both collections together 38 nerineoid species are reported. Both collections are almost identical in terms of the number of nerineoid species (Lang collection provided 28 species, Sylla collection 27 species). In the Lang collection, 10 of the species identified in the Sylla collection are missing; the Sylla collection 11 species that are present in the Lang collection). Therefore, both collections complement each other. Some of the nerinoid species are large (up to 20 cm) so that this group also had the highest biomass amongst gastropods in this community.

The differences of the previous collections (mainly Lang-collection) and the Sylla-collection are especially pronounced regarding Nerineoidea. Species present with more than 10 specimens/fragments (= abundant species). Endoplocus acutus, Ptygmatis? tornata, Ptygmatis nodosa und Itieroptygmatis cylindrata are abundant in both collections. Ceritellopsis gramanni, Ceritella convexa and Ptygmatis ? ursicina are only abundant in the Lang collection. Pseudonerinea ? pseudomelaniformis, Nerinea donosa, Nerinea moreana (with 202 specimens which are commonly very large and therefore conspicuous), Ptygmatis clio, Cryptoplocus depressus, Cryptoplocus subpyramidalis, Eunerinea sp. 1 and Itieria cabanetiana are only abundant in the Sylla collection.

It is remarkable that Ceritellidae are completely absent in the Sylla collection. On the other hand, the Sylla collection has yielded several large species, that are absent or rare in the Lang collection (both Cryptoplocus–species, Nerinea moreana, and Itieria cabanetiana). As outlined above, such differences reflect facies differentiation (reef, fore reef, lagoon) and collection biases. It is obvious that both collectors had different size preferences: H. Lang collected preferably small specimens whereas J. Sylla found on the average much larger specimens. that It is also noteworthy, that Lang and Sylla did not collect during the same period of time so that it seems possible that different facies and beds were exposed by actively progressing quarrying.

Acknowledgments

We thank Andrzej Kaim (Warsaw) for his careful review.

References

  • Archiac EJAD d’ (1843) Description géologique du département de l’Aisne. Mémoires de la Société Géologique de France 5(2): 129–420.
  • Bandel K (1993) Trochomorpha (Archaeogastropoda) aus den St. Cassian-Schichten (Dolomiten, Mittlere Trias). Annalen des Naturhistorischen Museums Wien 95: 1–99.
  • Bandel K (2008) Operculum shape and construction of some Neritimorpha (Gastropoda) compared to those of modern species of the subclass. Vita Malacologica 7: 19–36.
  • Bandel K, Gründel J, Maxwell P (2000) Gastropods from the upper Early Jurassic/early Middle Jurassic of Kaiwara Valley, North Canterbury, New Zealand. Freiberger Forschungshefte C 490: 67–132.
  • Beurlen K (1967) As espécies do Cassiopinae, nova subfamilia dos Turritellidae, no Cretaceo do Brasil. Arquivos de Geologia Universidadae do Recife 5: 1–44.
  • Bouchet P, Rocroi JP, Hausdorf B, Kaim A, Kano Y, Nützel A, Parkhaev P, Schrödl M, Strong EE (2017) Revised classification, nomenclator and typification of gastropod and monoplacophoran families. Malacologica 61: 1–526. https://doi.org/10.4002/040.061.0201
  • Bronn HG (1836) Übersicht und Abbildungen der bis jetzt bekannten Nerinea–Arten. Neues Jahrbuch für Mineralogie, Geognosie, Geologie und Petrefaktenkunde 4: 544–566.
  • Burmeister H (1837) Handbuch der Naturgeschichte. Enslin, Berlin, , Zoologie 2: 369–858.
  • Buvignier A (1843) Mémoire sur quelques fossiles nouveaux des départements de la Meuse et des Ardennes. Mémoires de la Société Philomatique de Verdun (Meuse) 2: 225–252.
  • Buvignier A (1852) Statistique géologique, minéralogique, metallurgique et paléontologique du Département de la Meuse. JB Bailliére, Paris, 52 pp. [32 pls]
  • Charvet J, Termier G (1971) Les Nérinéacés de la limite Jurassique-Crétacé de Bjeliš (Nord de Sarajévo, Yougoslavie). Annales de la Société géologique du Nord 91: 187–191.
  • Children JG (1834) Mollusca. In: Synopsis of the contents of the British Museum, ed. 28: 88–118.
  • Cornuel J (1841) Mémoire sur les terrains crétacés inférieurs et supra-jurassiques de l’arrondissement de Vassy (Haute Marne). Mémoirs de la Société Geologique de France, sér. 1, 4: 229–290.
  • Cossmann M (1885) Contribution à l’étude de la faune de l’étage Bathonien en France (Gastropodes). Mémoirs de la Société géologique de France 3(3): 1–374.
  • Cossmann M (1898) Contribution à la Paléontologie française des terrains jurassiques: Nerinées. Mémoires de la Société gélogique de France, sér. Paléontologie (2) 8: 1–179.
  • Cossmann M (1906) Essais de paléoconchologie comparée 7. The author and FR de Rudeval, Paris, 261 pp.
  • Cossmann M (1909) Essais de paléoconchologie comparée 8. The author and FR de Rudeval, Paris, 248 pp.
  • Cossmann M (1913) Contributions à la paléontologie française des terrains jurassiques. III. Cerithiacea et Loxonematacea. Mémoires de la Société géologique de France, série Paléontologie 46: 1–263.
  • Cossmann M (1916) Essais de paléontologie comparée 10. The author, Paris, 292 pp.
  • Cossmann M (1918) Les coquilles des calcaires d’Orgon. Bulletin de la Société géologique de France, sér. 4, 16: 336–341.
  • Cossmann M (1919) see Cossmann M, Peyrot A (1919).
  • Cossmann M (1921) Essais de paléontologie comparée 12. The author, Paris, 349 pp.
  • Cossmann M (1925) Essais de paléontologie comparée 13. The author, Paris, 345 pp.
  • Cossmann M, Peyrot A (1917–1919) Conchologie néogénique de l’Aquitaine. 3: Gastropodes, Scaphopodes et Amphineures. Actes de la Société Linnéenne de Bordeaux 69: 157–365, 70: 181–491.
  • Cox LR (1930) The fossil fauna of the Samana Range and some neighbouring areas. Part VIII. The Mollusca of the Hangu shales. Memoirs of the Geological Survey of India, Palaeontologia Indica, new series 15: 129–222.
  • Cox LR (1947) On the genotype of Nerinea; with a new subgeneric name Eunerinea. Proceedings of the Malacological Society of London 27: 248–250.
  • Cox LR (1954) Notes relating to the taxonomy of the gastropod superfamily Nerineacea. Proceedings of the Malacological Society of London 29: 12–16.
  • Cox LR (1958) Three Mesozoic gastropod generic homonyms renamed. Proceedings of the Malacological Society of London 33: 71–72.
  • Cox LR (1960) see Knight et al. 1960.
  • Cox LR (1965) Jurassic Bivalvia and Gastropoda from Tanganyika and Kenya. Bulletin of the British Museum (National History), Geology, Supplement 1: 1–213. https://doi.org/10.5962/p.310409
  • Cox LR, Arkell WJ (1948–1950) A survey of the Mollusca of the British Great Oolite Series. Monographs Palaeontological Society London 102 (1948): 1–49; 103 (1950): 49–105, London.
  • Daqué E (1938) see Wenz 1938.
  • Das SS, Saha S, Bardhan S, Mallick S, Allmon WD (2018) The oldest turritelline gastropods from the Oxfordian (Upper Jurassic) of Kutch, India. Journal of Paleontology 92: 373–387. https://doi.org/10.1017/jpa.2017.89
  • Das SS, Saha S, Bardhan S, Mondal S, Paul S, Mallick S, Saha R, Allmon WD (2024) Comment on: Fürsich et al. 2023, Miocene instead of Jurassic: the importance of sound fieldwork for paleontological data analysis. Journal of Paleontology 2024: 1–12. https://doi.org/10.1017/jpa.2023.91
  • Defrance MJL (1826) Genus Pleurotomaria. In: Cuvier F (ed) Dictionnaire des Sciences Naturelles 41, Paris and Strasbourg, 381 pp.
  • Dieni I (1990) Brunonia annulata (Yokoyama, 1890) (Carinariidae, Mesogastropoda)
  • nel Cretaceo inferiore della Sardegna. Bollettino della Società Paleontologica Italiana 29: 43–51.
  • Douvillé H (1904) Mollusques fossiles. In: Morgan J de (Ed. ) Mission scientifique en Perse, Leroux, Paris, tome 3: 192–380.
  • Eichwald E von (1861) Der Grünsand in der Umgebung von Moskwa. Bulletin de la Société Impériale des Naturalistes de Moscou 34: 278–313.
  • Étallon A (1859–1862) Études paléontologiques sur les terrains jurassiques du Haute-Jura. Monographie de l’étage Corallien. Paris (Besançon).
  • Étallon A (1862) Études paléontologiques sur le Jura graylois. Mémoires de la Société d’émulation du Doubs, 3. Ser. 8: 286 pp.
  • Eudes-Deslongchamps JA (1843) Mémoire sur les Nérinées des terrains secondaires du Calvados. Mémoires de la Société Linnéenne de Normandie 7: 179–188.
  • Eudes-Deslongchamps JA (1849) Supplément au mémoire sur les Bulles et Tornatelles fossiles des terrains secondaires du Calvados. Mémoires de la Société Linnéenne de Normandie 8: 161–162.
  • Eudes-Deslongchamps E (1865) Note sur la délimitation des genres Trochotoma et Ditremaria. Bulletin de la Société Linnéenne de Normandie 9: 421–433.
  • Favre J (1913) see Joukowsky ME, Favre J (1913).
  • Ferrari SM, Damborenea SE, Manceñido MO, Griffin M (2015) Early Jurassic Trochotomidae (Vetigastropoda, Pleurotomarioidea) from the Neuquén Basin, Argentina. Journal of Paleontology 89: 331–345. https://doi.org/10.1017/jpa.2014.28
  • Fischer JC (1969) Géologie, paléontologie et paléoécologie du Bathonien au Sud–Ouest du Massif Ardennais. Mémoires du Muséum National d‘Histoire Naturelle, nouv. Série, Série C, Sciences de la Terre 20: 1–319.
  • Fischer JC, Weber C (1997) Révision critique de la paléontologie Française d‘Alcide d‘Orbigny. Vol. II: Gastropodes jurassiques. Masson, Paris, 300 pp.
  • Fischer P (1880–1887) Manuel de Conchyliologie et de Paléontologie conchyliologique. Savy, Paris, 1369 pp.
  • Fleming J (1822) The philosophy of Zoology, a general view of the structure, functions and classification of animals 2. Constable and Co., Edinburgh, 618 pp. https://doi.org/10.5962/bhl.title.24597
  • Forbes E (1850) Report of the 19th meeting of the British Association for the Advancement of Science (Birmingham, 1849): 75–76.
  • Frýda J, Blodgett RB, Stanley GD (2003) New neritopsoidean gastropods (Neritimorpha) from the Late Triassic (Late Carnian-Early Norian) of the Wallowa Terrane, northeastern Oregon. Mitteilungen des Geologisch-Paläontologischen Instituts der Universität Hamburg 87: 55–72.
  • Fürsich FT, Bhosale S, Alberti M, Pandey DK (2023) Miocene instead of Jurassic: the importance of sound fieldwork for paleontological data analysis. Journal of Paleontology 97: 341–346. https://doi.org/10.1017/jpa.2022.106
  • Geiger P (1901) Die Nerineen des Schwäbischen Jura. Jahreshefte des Vereins für vaterländische Naturkunde in Württemberg 57: 275–317.
  • Gemmelaro GG (1868–1875) Sullas fauna del calcare a Terebratula janitor del nord di Sicilia. Giornale di Scienze naturali ed economichi di Palermo 4 (1868): 72–105, (1869): 130–158; 5 (1870): 90–110; 11 (1875): 257–264.
  • Gemmelaro GG (1878–1882) Sui fossili del calcare cristallino delle montagne del Casale e di Bellampo nella Provincia di Palermo. Giornale di Scienze naturali ed economichi di Palermo 13 (1878): 116–212, 14 (1879): 157–212, 15 (1881–1882): 98–137.
  • Gerasimov PA (1992) Gastropody jurskich i progranichnych nizhnemelovych otloženij Evropejskoj Rossii. Moskau (Rossiyskaja Akademija Nauk), 190 pp.
  • Goldfuss A (1826–1844) Petrefacta Germaniae: Tam ea quae in Museo Universitatis Regiae Borussicae Fridericiae Wilhelmiae Rhenanae servantur quam alia quaecunque in Museis Hoeninghusiano Muensteriano aliisque extant; iconibus et descriptionibus illustrata. Arnz and Comp., Düsseldorf, 1. Teil (1826–1833): 252 pp., 2. Teil (1834–1840): 312 pp., 3. Teil (1841–1844): 128 pp.
  • Golikov AN, Starobogatov YI (1975) Systematics of prosobranch gastropods. Malacologia, 15(1): 185–232.
  • Grateloup JPS de (1832) Description d’un genre nouveau de coquilles appelé Neritopsidae. Actes de la Société linnéenne de Bordeaux 5: 125–131.
  • Gray JE (1840) Shells of molluscous animals. Synopsis of the contents of the British Museum 42: 105–152.
  • Gray JE (1847) A list of genera of Recent mollusca, their synonyma and types. Proceedings of the Zoological Society of London 15: 129–219.
  • Gray JE (1850) Figures of molluscous animals selected from various authors. Etched for the use of students by M. E. Gray, vol. 4. Longman, Brown, Green & Longmans, London. iv + 219 pp.
  • Gray JE (1857) Guide to the systematic distribution of Mollusca in the Brtish Museum. Part I. Taylor and Francis, London, 230 pp.
  • Gründel J (1976) Bemerkungen zur Family Diastomidae Cossmann, 1895 (Cerithiacea, Gastropoda). Zoologischer Anzeiger 197: 71–89.
  • Gründel J (2000) Archaeogastropoda aus dem Dogger Norddeutschlands und des nordwestlichen Polens. Berliner geowissenschaftliche Abhandlungen E 34: 205–253.
  • Gründel J (2004) Gastropoden aus dem oberen Bathonium von Luc-sur-Mer/Calvados (Normandie, France): I. Archaeogastropoda und Neritimorpha. Freiberger Forschungshefte C 502: 15–50.
  • Gründel J (2009) Zur Kenntnis der Genus Metriomphalus Cossmann, 1916 (Gastropoda, Vetigastropoda). Zitteliana A 48/49: 39–48.
  • Gründel J (2012) Neubearbeitung der von Laube 1867 beschriebenen Gastropodenfauna aus dem mittleren Jura von Balin/Polen. Annalen des Naturhistorischen Museums in Wien, Serie A 114: 193–288.
  • Gründel J (2017) Die Gastropoden-Fauna von Saal bei Kelheim. Der Steinkern, Heft 30: 20–47.
  • Gründel J, Kowalke T (2002) Palaeorissoinidae, a new family of marine and brackish water Rissooidea (Gastropoda, Littorinimorpha). Neues Jahrbuch für Geologie und Paläontologie Abhandlungen 226: 43–57. https://doi.org/10.1127/njgpa/226/2002/43
  • Gründel J, Nützel A (2012) On the early evolution (Late Triassic to Late Jurassic) of the Architectobranchia (Gastropoda: Heterobranchia), with a provisional classification. Neues Jahrbuch für Geologie und Paläontologie, Abhandlungen 264/1: 31–59. https://doi.org/10.1127/0077-7749/2012/0230
  • Gründel J, Hostettler B, Menkveld-Gfeller U (2016) Die Gastropoden der Korallenrifffazies der St-Ursanne-Formation (mittleres Oxfordien) des Schweizer Jura. 1. Die Unterklasse Neritimorpha Koken, 1896. Revue de Paléobiologie 35: 491–516.
  • Gründel J, Hostettler B, Menkveld-Gfeller U (2020a) Die Gastropoden aus der Korallenrifffazies der St-Ursanne-Formation (mittleres Oxfordien) des Schweizer Jura. 2. Patellogastropoda und Vetigastropoda. Revue de Paléobiologie 39: 199–247.
  • Gründel J, Hostettler B, Menkveld-Gfeller U (2020b) Die Gattungen der Brachytrematidae Cossmann, 1906 (Gastropoda: Caenogastropoda) im Jura Europas. Paläontologie, Stratigraphie, Facies (25), Freiberger Forschungshefte C 558: 109–119.
  • Gründel J, Hostettler B, Menkveld-Gfeller U (2022) Die Gastropoden aus der Korallenrifffazies der St-Ursanne-Formation (mittleres Oxfordien) des Schweizer Jura. 3. Die Unterklasse Caenogastropoda Cox, 1960. Revue de Paléobiologie 40: 29–84.
  • Gründel J, Keupp H, Lang F (2015) Die Arten der Unterklasse Neritimorpha Koken, 1896 (Gastropoda) aus der Korallenfazies des oberen Kimmeridgiums (oberer Jura) von Saal bei Kelheim und dem Gebiet Nattheim (Süddeutschland). Zitteliana A 55: 77–106.
  • Gründel J, Keupp H, Lang F (2017) Die Arten der Patellogastropoda und Vetigastropoda (Gastropoda) aus den Korallenriffen des oberen Kimmeridgiums (oberer Jura) von Saal bei Kelheim und dem Gebiet Nattheim (Süddeutschland). Zitteliana 89: 171–228.
  • Gründel J, Keupp H, Lang F (2019) Arten der Unterklasse Caenogastropoda aus der Korallenfazies des oberen Kimmeridgiums (Ober-Jura) von Saal bei Kelheim und dem Gebiet Nattheim (Süddeutschland). Zitteliana 93: 97–142.
  • Gründel J, Keupp H, Lang F, Nützel A (2022) Late Jurassic (Upper Kimmeridgian) Heterobranchia (Gastropoda) of the coral-facies of Saal near Kelheim and the viciniy of Nattheim (Germany) Zitteliana 96: 179–221. https://doi.org/10.3897/zitteliana.96.e84187
  • Guirand M, Ogérien LF (1865) Quelques fossiles nouveaux du Corallien du Jura. Travaux de la Société d’Émulation du Jura, für 1865: 369–394.
  • Guzhov AV (2004) Jurassic Gastropods of European Russia (Orders Cerithiiformes, Bucciniformes, and Epitoniiformes). Paleontological Journal 38: 457–562.
  • Haber G (1932) Gastropoda, Amphineura et Scaphopoda jurassica. In: W. Quenstedt (ed.): Fossilium Catalogus. I, Animalia; pars 53. Junk, Berlin, 304 pp.
  • Hägele G (1997) Juraschnecken. Fossilien, Sonderband 11: 1–144.
  • Haszprunar G (1988) On the origin and evolution of major gastropods groups, with special reference to the Streptoneura. Journal of Molluscan Studies 54: 367–441. https://doi.org/10.1093/mollus/54.4.367
  • Hébert M, Eudes-Deslongchamps E (1860) : Mémoire sur les fossiles de Montreuil-Bellay (Maine-et-Loire), 1re partie. Céphalopodes et Gastéropodes. Bulletin de le Société Linnéenne de Normandie 5: 153–240.
  • Janicke V (1966) Die Gastropoden und Scaphopoden der Neuburger Bankkalke (Mittel-Tithon). Palaeontographica A 126: 35–69.
  • Joukowsky ME, Favre J (1913) Monographie géologique et paléontologique du Salève (Hte-Savoie, France) Mémoires de la Société de Physique et d’Histoire naturelle de Gèneve 37: 295–523.
  • Karapunar B, Nützel A (2021) Slit-band gastropods (Pleurotomariida) from the Upper Triassic St. Cassian Formation and their diversity dynamics in the Triassic. Zootaxa 5042(1): 1–165. https://doi.org/10.11646/zootaxa.5042.1.1
  • Kase T (1984) Early Cretaceous marine and brackish-water Gastropoda from Japan. National Science Museum, Tokyo, 199 pp.
  • Kase T (1988) Reinterpretation of Brunonia annulata (Yokoyama) as an Early Cretaceous carinariid mesogastropod (Mollusca). Journal of Paleontology 62: 766–771.
  • Knight JB, Cox LR, Keen AM, Smith AG, Batten RL, Yochelson EL, Ludbrook NH, Robertson R, Yonge CM, Moore RC (1960) Treatise on Invertebrate Paleontology, Part I, Mollusca 1. University of Kansas Press, Lawrence, KS, 351 pp.
  • Koken E (1896) Die Gastropoden der Trias um Hallstatt. Jahrbuch der königlich-kaiserlichen geologischen Reichsanstalt 46: 37–126.
  • Kollmann HA (1979) Gastropoden aus den Losensteiner Schichten der Umgebung von Losenstein (Oberösterreich). 3. Teil: Cerithiacea (Mesogastropoda). Annalen des Naturhistorischen Museums Wien 82: 11–51.
  • Kollmann HA (2005) Révision critique de la Paléontologie Française d’Alcide d’Orbigny, vol. 3. Gastropodes crétacés. Backhuys Publishers, Leiden, 239 pp.
  • Kollmann HA (2014) The extinct Nerineoidea and Acteonelloidea (Heterobranchia, Gastropoda): a palaeobiological approach. Geodiversitas 36: 349–383. https://doi.org/10.5252/g2014n3a2
  • Kuhn O (1939) Beiträge zur Fauna des Oxford und Kimmeridge in Nordbayern. Neues Jahrbuch für Geologie und Paläontologie Abteilung B, Beilagen-Band 80: 464–497.
  • Lamarck JBPA de, Monet de (1799) Prodrome d’une nouvelle classification des coquilles. Mémoires de la Société Histoire Naturelle des Paris 1: 63–91.
  • Lindberg DR (1986) Radular evolution in the Patellogastropoda. American Malacological Bulletin 4(1): 115.
  • Linné C (1758) Systema naturae, ed. 10 reformata 1. Holmiae.
  • Loriol P de (1881) Monographie paléontologique des Couches de la zone à Ammonites tenuilobatus (Badener Schichten) d’Oberbuchsitten et de Wangen (Soleure). – Mémoires de la Société Paléontologique Suisse 7: 1–60 and 8: 61–120.
  • Loriol P de, Bourgeat AE (1886–1888) Études sur les mollusques des couches coralligènes de Valfin (Jura). Mémoires de la Société Paléontologique Suisse 13–15: 1–369.
  • Loriol P de, Koby E (1889–1892) Études sur les mollusques des couches coralligènes inférieures du Jura Bernois. Mémoires Société paléontologiques de Suisse 16–19: 1–419.
  • Loriol P de, Koby E (1894) Étude sur les mollusques du Rauracien inférieur du Jura Bernois. Mémoires Societé paléontologiques de Suisse 21: 1–129.
  • Loriol P de, Koby E (1895) Étude sur les mollusques du Rauracien superieur du Jura Bernois. 1e supplément. Mémoires Société paléontologiques de Suisse 22: 1–51.
  • Loriol P de, Lambert J (1893) Description des Mollusques et Brachiopodes des couches séquaniennes de Tonnerre (Yonne). Mémoires Société paléontologiques de Suisse 20: 1–213.
  • Loriol P de, Pellat E (1874) Monographie paléontologique et géologique des étages de la formation Jurassique des environs de Boulogne-sur-Mer (Pt. 1). Mémoires de la Société de Physique et d’Histoire Naturelle de Genève 1823: 261–407.
  • Loriol P de, Royer E, Tombeck H (1872) Monographie paléontologique et géologique des étages supérieurs de la formation jurassique du département de la Haute-Marne. Mémoires de la Société Linnéenne de Normandie 15 and 16: 1–542.
  • Lovén SL (1847) Malacozoology. Konglia Vetenskaps-Akademiens Förhandlingar: 175–199.
  • Lycett J (1848) Notes on the distribution of the fossil conchology of the Oolite formations in thevicinity of Minchinhampton, Gloucestershire. The Annals and Magazine of Natural History (2) 2: 248–259. https://doi.org/10.1080/03745485809494703
  • Maire V (1926) Les Gastropodes du Jurassique supérieur graylois (fin). Bulletin de la Société, grayloise d’émulation, Gray 19: 85–173.
  • Mandl GW, Dulai A, Schlögl J, Siblik M, Szabó J, Szente I, Vörös A (2010) First results on stratigraphy and faunal content of the Jurassic between Bad Mitterndorf and Toplitzsee (Salzkammergut, Austria). Abhandlungen der Geologischen Bundesanstalt 65: 77–34.
  • Martill DM, Etches S (2020) Fossils of the Kimmeridge Clay Formation (Volume 1). Palaeontological Association Field Guide to Fossils 16, 436 pp.
  • Matheron P (1842) Sur le genre Itieria. Bulletin de la Société Géologique de France 13: 493–495.
  • Monari S, Gatto R (2013) Pleurotomaria Defrance, 1826 (Gastropoda, Mollusca) from the Lower Bajocian (Middle Jurassic) sediments of Luxembourg, with considerations on its systematic, evolution and palaeobiogeographical history. Palaeontology 56: 751–781. https://doi.org/10.1111/pala.12014
  • Monari S, Gatto R, Valentini M (2017) Vetigastropoda and Neritimorpha from the Lower Bajocian of Luxembourg and palaeobiogeography of Aalenian-Bajocian (Middle Jurassic) Gastropoda of western Europe. Journal of Systematic Palaeontology 16(6): 449–492. https://doi.org/10.1080/14772019.2017.1312578
  • Morris J, Lycett J (1851–1855) A monograph of the Mollusca from the Great Oolite, chiefly from Minchinhampton and the coast of Yorkshire. Palaeontographical Society London 1851: 1–130; 1853: 1–80; 1855: 81–147. https://doi.org/10.1080/02693445.1853.12088369
  • Münster G von (1841) Beschreibung und Abbildung der in den Kalkmergelschichten von St. Cassian gefundenen Versteinerungen. In: Wissmann HL, Münster G zu, Braun KF (Eds) Beiträge zur Geologie und Petrefacten-Kunde des südöstlichen Tirol’s vorzüglich der Schichten von St. Cassian. Buchner, Bayreuth, 25–152.
  • Münster G von (1844) See Goldfuss A (1826–1844).
  • Munt MC (2020) see Martill DM, Etches S (2020).
  • Nützel A, Kaim A (2014) Diversity, palaeoecology and systematics of a marine fossil assemblage from the Late Triassic Cassian Formation at Settsass Scharte, N Italy. Paläontologische Zeitschrift 88: 405–431. https://doi.org/10.1007/s12542-013-0205-1
  • Ooster WA, Fischer-Ooster C de (1869) Pétrifications remarcables des Alpines suisses: le Corallien de Wimmis. 1. Band. H. Georg, Genf and Basel, 16 pp.
  • Orbigny A d’ (1841) Description de quelques espèces de Mollusques fossiles de France. Revue zoologique par la Société Cuvierienne 4: 318–319.
  • Orbigny A d’ (1842–1843) . Paléontologie française. Description zoologique et géologique de tous les animaux Mollusques et Rayonnés fossiles de France. Terrains crétacés. Tome 2. Paris, 456 pp.
  • Orbigny A d’ (1850) Prodrome de Paléontologie stratigraphique universelle des animaux mollusques et rayonnés, volume 1. Masson, Paris, IX + 394 pp.
  • Orbigny A d’ (1851–1860) Paléontologie française, terrains jurassiques. Tom II, Gastéropodes. Masson, Paris, 621 pp.
  • Pčelintsev VF (1926) Jurskaja fauna doliny Kubani bliz stanicy Krasnogorskoj. Trudy Geologičeskogo Muzeja Akademii Nauk SSSR 1: 77–114.
  • Pčelintsev VF (1927) Fauna jury i nižnego mela Kryma i Kavkasa. Mémoires du Comité géologique, nouvelle série 17xc: 1–320.
  • Pčelintsev VF (1960) see Pčelintsev VF, Korobkov IA (1960).
  • Pčelintsev VF (1965) Murčisoniata Mezozoja gornogo Kryma. Akademia Nauk SSSR, Izdatelstvo Nauka, Moskva-Leningrad, 215 pp.
  • Pčelintsev VF, Korobkov IA (1960) Osnovy paleontologii. Molljuski-Brjuchonogie, Moskva, 360 pp.
  • Peters KF (1855) Die Nerineen des oberen Jura in Österreich. Sitzungsberichte der mathematisch-naturwissenschftlichen Classe der kaiserlichen Akademie der Wissenschaften 16: 336–366.
  • Pictet JF, Campiche G (1861–1864) Descripion des fossiles du terrain Crétacé des environs de Sainte Croix. In: Pictet JF (1858–1872) Matériaux pour la Paléontologie Suisse sér. 3, 2: 1–752.
  • Piette E (1855) Observations sur les étages inférieurs du terrain jurassique dans les départements des Ardennes et de l’Aisne. Bulletin de la Société géologique de France (2) 12: 1083–1122.
  • Piette E (1860) Sur un nouveau genre de gastéropodes. Bulletin de la Société géologique de France (2) 18: 14–16.
  • Piette E (1864–1891) Paléontologie française, terrains jurassiques. Tome III. Gastéropodes. Masson, Paris, 535 pp. (1864): 1–48, 1866: 49–96, 1867: 97–144, 1869: 145–192, 1876: 193–336, 1882: 337–400, 1891: 401–535.
  • Piette E (1875) Sur plusieurs genres nouveaux on peu connus de gastéropodes. Association française pour l’avancemement des sciences - Compte rendu de la 3e session - Lille 1874. Association française pour l’avancemement des sciences, Paris, 360–366.
  • Quenstedt FA (1852) Handbuch der Petrefaktenkunde. 1. Auflage, 792 pp., Tübingen (Laupp).
  • Quenstedt FA (1856–1858) Der Jura. 1. Lfg. (1856): 1–208, pl. 1–24; 2. Lfg. (1856): 209–368, pl. 24–48, 1 Profiltafel (Lias); 3. Lfg. (1857): 369–576, pl. 49–72, 1 Profiltafel (Brauner Jura); 4. Lfg. (1857): I–IV + 577–842, pl. 73–100, 1 Profiltafel (Weißer Jura). Laupp and Siebeck, Tübingen. https://doi.org/10.1002/prac.18570720161
  • Quenstedt FA (1881–1884) Petrefaktenkunde Deutschlands. Erste Abteilung, Band 7: Gasteropoden. Fues´s, Leipzig, 867 pp.
  • Reiner W (1968) Callovian gastropods from Hamakhtesh Hagadol (southern Israel). Israel Journal of Earth Sciences 17: 171–198.
  • Riedel F (2000) Ursprung und Evolution der „höheren“ Caenogastropoda. Berliner geowissenschaftliche Abhandlungen E 32: 1–240.
  • Rolle F (1861) Über einige neue oder wenig bekannte Mollusken-Arten aus Sekundär-Ablagerungen. Sitzungsberichte der Kaiserlichen Akademie der Wissenschaften, Mathematisch-Naturwissenschaftliche Classe 42: 261–279.
  • Salvini-Plawen L von (1980) A reconsideration of systematics in the Mollusca (phylogeny and higher classification). Malacologia 19: 249–278.
  • Schlosser M (1882) Die Fauna des Kelheimer Diceras-Kalkes. I. Vertebrata, Crustacea, Cephalopoda und Gastropoda. Palaeontographica 28: 41–110.
  • Sieberer K (1907) Die Pleurotomarien des schwäbischen Jura. Palaeontographica 54: 1–68.
  • Sowerby J (1812–1822) The mineral conchology of Great Britain. 1 (1812), 234 S., pl. 1–9, (1813): pl. 10–44, (1814): pl. 45–78, (1815): pl. 79–102; 2 (1815): 251 S., pl. 103–114, (1816): pl. 115–150, (1817): pl. 151–186, (1818): pl. 187–203; 3 (1818): 194 S., pl. 204–221, (1819): pl. 222–253, (1820): pl. 254–271, (1821): pl. 272–306; 4 (1821): 114 S., pl. 307–318, (1822): pl. 319–383. Meridith, London.
  • Sowerby J de C (1823–1846) The mineral conchology of Great Britain. 4 (1823): S. 115–160, pl. 384–407; 5 (1823): 168 S., pl. 408–443; (1824): pl. 444–485; (1825): pl. 486–503; 6 (1826): 250 S, pl. 504–545; (1827): pl. 546–580; (1828): pl. 581–597; (1829): pl. 598–609; 7 (1840): 80 S., pl. 610–618; (1841): pl. 619–623; (1843): pl. 624–628; (1844): pl. 629–643; (1846): pl. 644–648. Meridith, London.
  • Stahl CF (1824) Uebersicht über die Versteinerungen Württembergs und dem gegenwärtigen Standpunkt der Petrefaktenkunde. Correspondenzblatt des Königlich-Württembergischen Landwirtschaftlichen Vereins 6: 1–91.
  • Stefano G di (1884) Sopra altri fossili del Titonio inferiore di Sicilia. Giornale di Scienze Naturali ed Economichi 16: 8–37.
  • Stoliczka F (1867–1868) Cretaceous fauna of Southern India. 2. The Gastropoda. Memoirs of the geological Survey of India Palaeontologica Indica 5: 1–498.
  • Szabó J (2010) see Mandl GW et al. (2010).
  • Terquem O (1855) Paléontologie de l’étage inferieur de la formation liassique de la province de Luxembourg, Grand-Duché (Hollande) et de Hettange du département de la Moselle. Mémoires de la Société géologique de France (2) 5: 219–343.
  • Thurman J (1832) Essai sur le soulèvements jurassiques du Porrentruy: déscription géognostique de la série jurassique et théorie orographique du soulèvement. Mémoires de la Société du muséum d’histoire naturelle de Strasbourg 1: 1–84.
  • Thurmann J, Étallon A (1861–1864) Lethea bruntrutana ou études paléontologiques et stratigraphiques sur le Jura bernois et en particulier les environs de Porrentruy. Neue Denkschrift der allgemeinen Switzerlanderischen Gesellschaft für die Naturwissenschaften 18–20: 1–500.
  • Verrill AE (1884) Second catalogue of Mollusca recently added to the fauna of the New England coast and the adjacent part of the Atlantic, consisting mostly of deep-sea species, with notes on others previously recorded. Transactions of the Connecticut Academy of Arts and Sciences 6: 139–194. https://doi.org/10.5962/bhl.part.7412
  • Voltz PL (1836) Über das fossile genus Nerinea. Neues Jahrbuch für Mineralogie, Geognosie, Geologie und Petrefaktenkunde 4: 359–543.
  • Wade B (1917) New and little known Gastropoda from the Upper Cretaceous of Tennessee. Proceedings of the Academy of Natural Sciences of Philadelphia 69: 280–304.
  • Wenz W (1938–1944) Gastropoda. Teil I: Allgemeiner Teil und Prosobranchia. In: Schindewolf OH „Handbuch der Paläozoologie“ Band 6. Bornträger, Berlin, 1639 pp. 1938: 1–480, 1939: 481–720, 1940: 721–960, 1941: 961–1200, 1943: 1201–1506, 1944: 1507–1639.
  • Werner W, Nützel A, Nose M (2017) Fossilien aus dem Oberjura von Saal – Die Sammlung Jürgen Sylla. Freunde der Bayerischen Staatssammlung für Paläontologie und Historische Geologie München e.V., Jahresbericht 2016 und Mitteilungen, 28–37.
  • Werner S (2019) Oberjura-Schnecken mit Farbmustererhaltung. Der Steinkern 37: 12–25.
  • Wieczorek J (1979) Upper Jurassic nerineacean gastropods from the Holy Cross Mts. (Poland). Acta Palaeontologica Polonica 24: 299–350.
  • Wieczorek J (1998) Nerineaceans from the Ernstbrunn Limestone (Tithonian, Austria). Annalen des Naturhistorischen Museums Wien 99A: 311–329.
  • Yin TH (1931) Étude de la Faune du Tithonique Coralligène du Gard et de l’Hérault. Travaux du laboratoire de Géologie de la faculté des sciences de Lyon 17, Mémoire 14: 1–191.
  • Zeuschner L (1849, 1850) Geognostische Beschreibungen des Nerineenkalkes von Inwald und Roczyny. Naturwissenschaftliche Abhandlungen Wien, 3(1850): 133–146.
  • Zieten CH von (1830–1833) Die Versteinerungen Württembergs. Verlag & Lithographie der Expedition des Werkes unserer Zeit, Stuttgart, 102 pp. [72 pls]
  • Zittel K (1873) Die Gastropoden der Stramberger Schichten. Palaeontographica, Supplement 2/1: 194–373.
login to comment