Leptolepis macrocephalus ( 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/71A2E839-B20B-523D-BA6D-3F93DB99997E

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Zitteliana by Pensoft

scientific name

Leptolepis macrocephalus ( Schroeder , 1956)
status

 

Leptolepis macrocephalus ( Schroeder, 1956)

Plate 3, figs 12-13 View Plate 3

Otolithus macrocephali 1956 Otolithus macrocephali - Schröder: pl. 7, fig. 40.

Otolithus guttaeformis 1956 Otolithus guttaeformis - Schröder: pl. 6, figs 15-16.

Material.

3 specimens from Schröder’s collection from the early Callovian of Pünzendorf: holotype of Ot. macrocephalus (emended spelling, SNSB-BSPG 2022 III 1, Plate 3 View Plate 3 , fig. 13), holotype of Ot. guttaeformis (SNSB-BSPG 2022 III 6, Plate 3 View Plate 3 , fig. 12) and 1 paratype (SNSB-BSPG 2022 III 7).

Differential diagnosis.

Leptolepis macrocephalus differs from the coeval L. inaequalis in its more compressed shape, which is exhibited by a deeper ventral rim and a more expanded postdorsal rim and is expressed in the OL:OH ratio of 1.35-1.4 (vs. 1.5). It shares with L. inaequalis completely flat inner and outer faces, features that distinguish both species from all other known Leptolepis otoliths.

Discussion.

Leptolepis macrocephalus and L. inaequalis form a small group of otoliths with a special trait of having flat inner and outer faces. They occur during the Callovian and possibly the early Oxfordian. Their attribution to the genus is therefore less certain than that of Leptolepis otoliths from the Early Jurassic (see above).