4.1 Article

Brazilian Permian Dvinosaurs (Amphibia, Temnospondyli): Revised Description and Phylogeny

Journal

JOURNAL OF VERTEBRATE PALEONTOLOGY
Volume 41, Issue 1, Pages -

Publisher

TAYLOR & FRANCIS INC
DOI: 10.1080/02724634.2021.1893181

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Funding

  1. Negaunee Foundation
  2. Grainger Foundation
  3. Field Museum of Natural History
  4. Conselho Nacional para a Ciencia e Tecnologia [CNPq 401848.2010-8, 456608/2014-1]
  5. National Geographic Committee for Research and Exploration [9601-14]
  6. Universidad de Buenos Aires Ciencia y Tecnica [UBACyT 20020170100643]
  7. Sofja Kovalevskaja Award of the Alexander von Humboldt Foundation
  8. Natural History Museum of London

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Recently discovered temnospondyl fossils from the Cisuralian Pedra de Fogo Formation in northeastern Brazil indicate a diverse assemblage of aquatic tetrapods, including Timonya anneae and Procuhy nazariensis. A new phylogenetic analysis reveals that Timonya represents an early branch within the 'short-snouted' dvinosaurs, and the dvinosaurs from the Pedra de Fogo Formation show close relationships with Cisuralian taxa from the North American southwest. This suggests a strong paleogeographic connection between these regions in the late Paleozoic, while also highlighting the presence of unique endemic taxa in the Pedra de Fogo Formation.
Recently collected temnospondyl fossils from the Cisuralian Pedra de Fogo Formation (north-eastern Brazil) indicate a diverse assemblage of aquatic tetrapods, including the dvinosaurs Timonya anneae and Procuhy nazariensis. Here we present revised diagnoses for these species and detailed descriptions of their holotypes. Timonya anneae is distinguished from all other dvinosaurs by several cranial characters including: combined width of both parietals less than interorbital width; presence of a groove-like internal carotid artery foramen; and presence of an ossified opisthotic. In the mandible, T. anneae presents two parasymphyseal fossae on each side of the mandibular symphysis to accommodate palatal fangs and a well-developed postglenoid area. Procuhy nazariensis, mostly preserved as a mold of the skull table and mandible, is diagnosed by the presence of the anteriormost extension of the squamosal posterior to parietal midlength; pineal foramen posterior to the midlength of the parietal; supratemporal exposed on the posterior border of the skull table; and presence of postglenoid process of the surangular separated from the retroarticular process of the articular by the mandibular sulcus. A new inclusive phylogeny of Temnospondyli indicates that Dvinosauria consists of the Trimerorhachidae (including Procuhy as the sister-taxon of Trimerorhachis) and the 'short-snouted' dvinosaurs, with Timonya as an early-diverging representative of the latter clade. The Pedra de Fogo dvinosaurs show close relationships with Cisuralian taxa from the North American southwest, reinforcing close paleogeographic connections between these regions in the late Paleozoic, but represent endemic taxa, corroborating the pattern suggested by the plant fossil record.

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