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A review of the osteoderms of lizards (Reptilia: Squamata)

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  • Additional Information
    • Contributors:
      University of Guelph; Aarhus University Aarhus; University College of London London (UCL); Mécanismes Adaptatifs et Evolution (MECADEV); Muséum national d'Histoire naturelle (MNHN)-Centre National de la Recherche Scientifique (CNRS); Imperial College London
    • Publication Information:
      CCSD
      Wiley
    • Publication Date:
      2021
    • Collection:
      Muséum National d'Histoire Naturelle (MNHM): HAL
    • Abstract:
      International audience ; Osteoderms are mineralised structures consisting mainly of calcium phosphate and collagen. They form directly within the skin, with or without physical contact with the skeleton. Osteoderms, in some form, may be primitive for tetrapods as a whole, and are found in representatives of most major living lineages including turtles, crocodilians, lizards, armadillos, and some frogs, as well as extinct taxa ranging from early tetrapods to dinosaurs. However, their distribution in time and space raises questions about their evolution and homology in individual groups. Among lizards and their relatives, osteoderms may be completely absent; present only on the head or dorsum; or present all over the body in one of several arrangements, including non-overlapping mineralised clusters, a continuous covering of overlapping plates, or as spicular mineralisations that thicken with age. This diversity makes lizards an excellent focal group in which to study osteoderm structure, function, development and evolution. In the past, the focus of researchers was primarily on the histological structure and/or the gross anatomy of individual osteoderms in a limited sample of taxa. Those studies demonstrated that lizard osteoderms are sometimes two-layered structures, with a vitreous, avascular layer just below the epidermis and a deeper internal layer with abundant collagen within the deep dermis. However, there is considerable variation on this model, in terms of the arrangement of collagen fibres, presence of extra tissues, and/or a cancellous bone core bordered by cortices. Moreover, there is a lack of consensus on the contribution, if any, of osteoblasts in osteoderm development, despite research describing patterns of resorption and replacement that would suggest both osteoclast and osteoblast involvement. Key to this is information on development, but our understanding of the genetic and skeletogenic processes involved in osteoderm development and patterning remains minimal. The most common proposition for ...
    • Accession Number:
      10.1111/brv.12788
    • Online Access:
      https://hal.science/hal-03365407
      https://hal.science/hal-03365407v1/document
      https://hal.science/hal-03365407v1/file/Williams%20et%20al%202021%20Biol%20Rev.pdf
      https://doi.org/10.1111/brv.12788
    • Rights:
      info:eu-repo/semantics/OpenAccess
    • Accession Number:
      edsbas.7EB15D1C