New data on the glyptodontid Trachycalyptoides from the late miocene bolivian locality of Achiri

  1. F. Pujos 7
  2. L. R. González Ruiz 8
  3. T. J. Gaudin 6
  4. A. Boscaini 2
  5. M. A. Abello 4
  6. R. Andrade Flores 5
  7. M. Fernández-Monescillo 9
  8. B. Mamani Quispe 5
  9. L. Marivaux 1
  10. M. B. Prámparo 7
  11. P.-O. Antoine 1
  12. P. Münch 3
  1. 1 University of Montpellier
    info

    University of Montpellier

    Montpellier, Francia

    ROR https://ror.org/051escj72

  2. 2 Instituto de Ecología, Genética y Evolución de Buenos Aires
  3. 3 Géosciences Montpellier
  4. 4 Universidad Nacional de La Plata
    info

    Universidad Nacional de La Plata

    La Plata, Argentina

    ROR https://ror.org/01tjs6929

  5. 5 Museo Nacional de Historia Natural, Bolivia
  6. 6 University of Tennessee at Chattanooga
    info

    University of Tennessee at Chattanooga

    Chattanooga, Estados Unidos

    ROR https://ror.org/00nqb1v70

  7. 7 Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales
  8. 8 Universidad Nacional de la Patagonia San Juan Bosco
    info

    Universidad Nacional de la Patagonia San Juan Bosco

    Trelew, Argentina

    ROR https://ror.org/022g6pv04

  9. 9 Universidad Nacional de Córdoba
    info

    Universidad Nacional de Córdoba

    Córdoba, Argentina

    ROR https://ror.org/056tb7j80

Actas:
XII Congreso de Paleontología de la Asociación Paleontológica Argentina (CAPA),

Editorial: Asociación Paleontológica Argentina

Ano de publicación: 2021

Páxinas: 198

Tipo: Achega congreso

Resumo

Among armored xenarthrans, Glyptodontidae appears as one of the most peculiar and also characteristic groups of South American mammals that inhabited this continent since at least the early Eocene until the end of the Pleistocene. Their evolutionary history is particularly well documented in Patagonia, Central and North America, but less so in the tropics and central South America. In Bolivia during the Miocene epoch, this family is only recorded at the Laventan locality of Quebrada Honda, represented by cf. “Asterostemma”, “Propalaehoplophorus” andinus, and two sclerocalyptine species, the ?Colloncuran locality of Nazareno represented by “Propalaehoplophorus” and ?Neothoracophorus, occurring in Choquecota, and the late Mayoan–early Chasicoan localities of Chokorasi and Achiri by a single species, Trachycalyptoides achirense. The late Miocene vertebrate locality of Achiri discovered in the early 70’s by the French paleontologist Hoffstetter, was explored by severalteams during the subsequent decades. Its mammalian fauna is particularly diverse with more than 20 taxa, including metatherians (i.e., Borhyaenidium), notoungulates (e.g., Hoffstetterius), litopterns, rodents (e.g., Prolagostomus), as well as xenarthrans sloths (e.g., “Xyophorus”) and cingulates (e.g., Trachycalyptoides). rachycalyptoides was erected by Saint-André in 1996 on the basis on two dermal armors and caudal tubes, an incomplete skull, and a hemimandible. The abundantmaterial collected by our team during recent fieldwork, and the preliminary revision of the material housed in the museumsof La Paz and Paris, has allowed us to gather new information, specifically on the dentition, dorsal carapace, and caudal tubeon this peculiar glyptodontid. In Trachycalyptoides the presence of three lobes is well marked on certain upper and lowermolariforms, especially on the most posterior teeth (fourth to eighth molariforms), whereas their presence is doubtful onthe third teeth, and absent on the first and second teeth. The general structure of the osteoderms corresponds to apentagonal or hexagonal polygon with a “rosette” pattern (a central figure surrounded by peripheral figures) on the exposedsurface. The central and peripheral figures are elevated and separated by a sulcus. The subcircular central figure is slightlyconcave in the center. The peripheral figures are small and in a variable number according to region (ranging from 3–4 to12–15), with foramina at the intersection with the sulcus of the central figure. The caudal tube is conical and elongated andits apex is relatively acute. The ventral face is slightly convex and the dorsal face is flat. The distal portion of the tube isformed by two large right and left osteoderms. The latter are roughly quadrangular, rectangular proximally and quadratedistally. The osteoderms of the caudal tube lack peripheral figures. The molariforms, dorsal carapace, and caudal tube ofTrachycalyptoides show affinities with glyptodonts that have a simplified trilobate pattern in the anteriormost molariforms,a dorsal carapace formed by osteoderms with a “rosette” pattern, and a caudal tube formed by osteoderms withoutperipheral figures like Cochlops, Palaehoplophorus, Trachycalyptus, and Lomaphorus.