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Tetrapod tracks from the Middle/Late Triassic of the Ourika and Yagour basins (Morocco): new ichnotaxonomical data based on the Biron collection

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  • معلومة اضافية
    • Contributors:
      Biogéosciences UMR 6282 (BGS); Université de Bourgogne (UB)-Centre National de la Recherche Scientifique (CNRS); Université Cadi Ayyad Marrakech (UCA); Centre de Recherche en Paléontologie - Paris (CR2P); Muséum national d'Histoire naturelle (MNHN)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS); Géosciences Rennes (GR); Université de Rennes (UR)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire des Sciences de l'Univers de Rennes (OSUR); Université de Rennes (UR)-Institut national des sciences de l'Univers (INSU - CNRS)-Université de Rennes 2 (UR2)-Centre National de la Recherche Scientifique (CNRS)-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE)-Institut national des sciences de l'Univers (INSU - CNRS)-Université de Rennes 2 (UR2)-Centre National de la Recherche Scientifique (CNRS)-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE)-Centre National de la Recherche Scientifique (CNRS)
    • بيانات النشر:
      HAL CCSD
      Elsevier
    • الموضوع:
      2024
    • Collection:
      Université de Bourgogne (UB): HAL
    • نبذة مختصرة :
      International audience ; Palaeontological prospecting organized in the Ourika and Yagour basins (Marrakech High Atlas, Morocco) in the 1980's, have yielded abundant and exquisitely preserved tetrapod tracks, some of them preserving thinly detailed skin traces (Collection Biron, Cadi Ayyad, Marrakech, Morocco). Based on this material, diverse morphologies of tracks were described and six new ichnotaxa were erected. However, these trackways have never been reinvestigated in detail from an ichnotaxonomic point of view. Here, the Biron collection is reevaluated using modern photogrammetric imaging techniques. The fine-grained sandstone slabs bear trackways ascribed to Apatopus lineatus, Isochirotherium isp. and Rhynchosauroides isp. whose trackmakers are possible phytosaurs, crocodylian-stem archosaurs or non-crown-group archosauriforms and lepidosauromorphs/archosauromorphs, respectively. “Chirotherium atlensis”, “Enigmatopus atlensis”, “Hyloidichnus triasicus”, “Prochirotherium triasicum”, “Pseudochirotherium oukaimedensis” and “Rectilinetopus ourikensis” are considered as invalid. The palaeoichnological assemblage includes a mixture of Early to the Middle Triassic (Isochirotherium) and Late Triassic (Apatopus lineatus) tracks. This result corroborates the biostratigraphic data recently obtain from the base of the Oukaïmeden Sandstone Formation, suggesting a Middle-Late Triassic age. The living environment was a semi-arid alluvial plain with ponds and ephemeral rivers.
    • الرقم المعرف:
      10.1016/j.jafrearsci.2024.105202
    • الدخول الالكتروني :
      https://insu.hal.science/insu-04452136
      https://insu.hal.science/insu-04452136v1/document
      https://insu.hal.science/insu-04452136v1/file/Moreau%20et%20al%202024.pdf
      https://doi.org/10.1016/j.jafrearsci.2024.105202
    • Rights:
      http://creativecommons.org/licenses/by/ ; info:eu-repo/semantics/OpenAccess
    • الرقم المعرف:
      edsbas.633FB87F