Leptolepis kremmeldorfensis ( Schroeder , 1956)

Schwarzhans, Werner & Keupp, Helmut, 2022, Early teleost otolith morphogenesis observed in the Jurassic of Franconia, Bavaria, southern Germany, Zitteliana 96, pp. 51-67 : 51

publication ID

https://dx.doi.org/10.3897/zitteliana.96.81737

publication LSID

lsid:zoobank.org:pub:CD8C70BA-0253-4540-8EFC-D430A12F6B35

persistent identifier

https://treatment.plazi.org/id/85B2B81D-ABE9-5707-AC20-0C56C70CC45B

treatment provided by

Zitteliana by Pensoft

scientific name

Leptolepis kremmeldorfensis ( Schroeder , 1956)
status

 

Leptolepis kremmeldorfensis ( Schroeder, 1956)

Plate 3, figs 1-8 View Plate 3

Otolithus kremmeldorfensis 1956 Otolithus kremmeldorfensis - Schröder: pl. 7, figs 34-35.

Otolithus amygdalinus 1956 Otolithus amygdalinus - Schröder: pl. 6, figs 4-6.

Otolithus bambergensis ?1956 Otolithus bambergensis - Schröder: pl. 6, fig. 19, pl. 7, fig. 20.

Otolithus franconicus ?1956 Otolithus franconicus - Schröder: pl. 7, figs 31-33.

Material.

11 specimens from Schröder’s collection from the late Toarcian to early Aalenian: holotype of Ot. kremmeldorfensis from Kremmeldorf (SNSB-BSPG 2022 III 35, Plate 3 View Plate 3 , fig. 1) and 1 paratype from Kremmeldorf (SNSB-BSPG 2022 III 36, Plate 3 View Plate 3 , fig. 2), holotype of Ot. amygdalinus from Kremmeldorf (SNSB-BSPG 2022 III 14, Plate 3 View Plate 3 , fig. 3) and 1 paratype from Kremmeldorf (SNSB-BSPG 2022 III 15), 1 paratype of Ot. bambergensis from Freiahorn (SNSB-BSPG 2022 III 10, Plate 3 View Plate 3 , fig. 4), holotype of Ot. franconicus from Kremmeldorf (SNSB-BSPG 2022 III 24, Plate 3 View Plate 3 , fig. 5) and 5 paratypes, with 4 from Kremmeldorf (SNSB-BSPG 2022 III 25, 27-29, Plate 3 View Plate 3 , fig. 6) and 1 from Freiahorn (SNSB-BSPG 2022 III 26).

Tentatively assigned specimens.

2 poorly preserved specimens from the late Pliensbachian of Buttenheim (SNSB-BSPG 2022 IV 15, Plate 3 View Plate 3 , figs 7-8).

Differential diagnosis.

Leptolepis kremmeldorfensis shares its otolith and sulcus proportions with the coeval L. curvisulcatus and differs in its flat, low, and relatively long postdorsal rim. However, small specimens below 1 mm in length, which have been described as Ot. bambergensis and Ot. franconcius , mostly show a more rounded postdorsal rim similar to the status in L. normandica . Therefore, they are only tentatively attributed and could in fact represent juveniles of any other Leptolepis species.

Discussion.

As with L. curvisulcatus , the validity of L. kremmeldorfensis should be regarded as provisional until larger otoliths have become available from the region and stratigraphic interval. Although a single larger otolith of nearly 3 mm in length, designated as Ot. amygdalinus by Schröder (1956), shares the characteristic shape of the postdorsal rim, it is otherwise too eroded to make a firm identification. Two poorly preserved specimens from the late Pliensbachian of Buttenheim are tentatively accounted for in L. kremmeldorfensis because of their relatively shallow and long postdorsal rim. If verified, it would extend the stratigraphic reach of the species significantly.