4.5 Article

Osteohistology and growth pattern of a large pterosaur from the Lower Cretaceous Romualdo Formation of the Araripe Basin, Northeastern Brazil

Journal

CRETACEOUS RESEARCH
Volume 118, Issue -, Pages -

Publisher

ACADEMIC PRESS LTD- ELSEVIER SCIENCE LTD
DOI: 10.1016/j.cretres.2020.104667

Keywords

Pterosauria; Anhangueridae; Ontogeny; Osteohistology; Araripe Basin; Cretaceous

Funding

  1. Conselho Nacional de Desenvolvimento Cientifico e Tecnologico e CNPq [420687/2016-5, 313461/2018-0, 458164/2014-3, 311715/2017-6, 140555/2013-7]
  2. Fundacao Cearense de Apoio ao Desenvolvimento Cientifico e Tecnologico - FUNCAP [BMD-0124-00302.01.01/19]
  3. Fundacao Carlos Chagas Filho de Amparoa Pesquisa do Estado do Rio de Janeiro -FAPERJ [E-26/202.905/2018]

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This study describes a pteranodontoid pterosaur with anhanguerid affinities, which comes from the Araripe Basin in Brazil. The specimen is large in size but considered to be immature. Its ontogenetic stage is established by comparing skeletal fusion and detailed osteohistological analyses.
A pteranodontoid pterosaur with anhanguerid affinities (MPSC R 1935) from the Romualdo Formation (Lower Cretaceous, Aptian), is described here and provides one of the few cases where the ontogenetic stage is established by comparison of skeletal fusion and detailed osteohistological analyses. The specimen comes from the Baixa Grande locality (Araripe Municipality - Ceara State) and is one of the few pterosaurs from the Araripe Basin with precise geographic and stratigraphic data. It consists of a left forelimb, comprising an incomplete humerus, metacarpal IV, pteroid and digits I, II, III, IV, including unguals. This specimen has an estimated maximized wingspan between 5.76 m and 5.84 m and a normal wingspan between 5.47 m and 5.54 m, and despite its large dimensions, is considered as an ontogenetically immature individual. Where observable, all bone elements are unfused, such as the extensor tendon process of the first phalanx and the carpal series. The absence of some microstructures such as bone resorption cavities, endosteal lamellae, an external fundamental system (EFS), and growth marks supports this interpretation. Potentially, this individual could have reached a gigantic wingspan, contributing to the hypothesis that such large flying reptiles might have been abundant during the Early Cretaceous of what is now the northeastern portion of Brazil. (C) 2020 Elsevier Ltd. All rights reserved.

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