Progyrolepis, Fritsch, 1895
publication ID |
https://doi.org/10.5852/cr-palevol2025v24a11 |
publication LSID |
urn:lsid:zoobank.org:pub:2C2F71B8-3C0A-4FB8-9262-E476BE6EDC9E |
DOI |
https://doi.org/10.5281/zenodo.15311263 |
persistent identifier |
https://treatment.plazi.org/id/038B87CF-9324-1158-526A-272BA7B4EA9B |
treatment provided by |
Felipe |
scientific name |
Progyrolepis |
status |
|
cf. Progyrolepis
( Fig. 4)
MATERIAL. — An isolated fulcral scale ( MHNT.PAL.2023.9.52 [ Fig. 4]) .
DESCRIPTION
The scale is isolated and lacks the most posterior part. It is 11 mm long and 5 mm wide as preserved. The scale is triangular in shape, with sculpted ridges running anteroposteriorly. A longitudinal groove runs through the middle of the scale, tapering off towards the anterior end.
COMPARISONS
Among the ichthyofauna of the Carboniferous-Permian basins of France, the morphology of MHNT.PAL.2023.9.52 most closely resembles the fulcral scales of Progyrolepis (e.g. Štamberg 2016a, 2018). The ridge scales of Progyrolepis have indeed a triangular shape with ornamentation consisting of prominent ridges arranged anteroposteriorly ( Poplin 1999; Štamberg 2018). MHNT.PAL.2023.9.52 does not resemble aeduellid nor amblypterid fulcral scales, which lack highly visible ornamentation (e.g. Dietze 1999; Poplin & Dutheil 2005). Ultimately, MHNT.PAL.2023.9.52 resembles the fulcral scales of Progyrolepis , with several identical specimens already reported from the Carboniferous-Permian of the Massif Central (e.g. Štamberg 2018: 268, fig. 22I; Štamberg & Steyer 2021: 159; fig. 10B). The preservation of MHNT.PAL.2023.9.52 does not allow a more precise systematic attribution, so we refer this specimen to cf. Progyrolepis .
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