Progyrolepis Fritsch 1895

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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Publication Details

Journal
Zenodo (CERN European Organization for Nuclear Research)
Published
2025-04-16
DOI
https://doi.org/10.5281/zenodo.15311262
Primary Topic
Paleopathology and ancient diseases
Type
article
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article

Progyrolepis Fritsch 1895

Zenodo (CERN European Organization for Nuclear Research)
Paleopathology and ancient diseases
article

Progyrolepis Fritsch 1895

article en

Abstract

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.

Zenodo (CERN European Organization for Nuclear Research)
Centre National de la Recherche Scientifique (FR), Museum für Naturkunde (DE), Université Toulouse III - Paul Sabatier (FR), Université Fédérale de Toulouse Midi-Pyrénées (FR), East Bohemian Museum (CZ), Muséum national d'Histoire naturelle (FR), Géosciences Environnement Toulouse (FR), Structure et Instabilité des Génomes (FR)
Openalex Percentile: Top 52%
Paleopathology and ancient diseases
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Progyrolepis Fritsch 1895 · Zenodo (CERN European Organization for Nuclear Research) (2025) | TGRS Research Map | TGRS