Ben Creisler
New reptile papers:
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Crocodylians evolved a high variety of rostral morphologies during their evolutionary history, highlighting the strong links between morphological plasticity and environmental and ecological parameters. Two Late Cretaceous alligatoroids, the mesorostrine Leidyosuchus canadensis Lambe, 1907, and the brevirostrine Stangerochampsa mccabei Wu et al., 1996, from Alberta, Canada, preserve a large groove-shaped recess on the posterior part of the maxilla that has not been documented in other alligatoroids. Despite the potential phylogenetic and paleoecological significance of this neurovascular feature, internal and endocranial structures remain under-explored among stem alligatoroids. The endocranial morphology, including the paratympanic sinus system of Leidyosuchus canadensis and Stangerochampsa mccabei, was compared to those of extant crocodylians and of the extinct alligatoroid Diplocynodon ratelii based on computed tomography data. The Cretaceous alligatoroids share endocranial features, such as a posteroventral neurovascular projection of the labiolateral canal that connects to the groove-like recess at the posterior edge of the maxilla and a paratympanic sinus system most similar to those of small-bodied and young extant crocodylians, suggesting that these pedomorphic features may reflect the ancestral crocodylian condition. Future phylogenetic studies should consider internal and endocranial characters alike to improve our understanding on the relationships among crocodylians.
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Roy Ebel, Jane Melville & J Scott Keogh (2026)
Lizards in chain mail: reconstructing the enigmatic past of dermal armour in squamate reptiles
Biological Journal of the Linnean Society 147(1): blaf129
doi:
https://doi.org/10.1093/biolinnean/blaf129https://academic.oup.com/biolinnean/article/147/1/blaf129/8422532Osteoderms, bone plates in the skin, occur widely but inconsistently throughout the tetrapod tree of life. Their evolutionary history remains poorly understood. Squamate reptiles (lizards and snakes) represent an ideal study system. It is often assumed that different squamate lineages acquired their osteoderms independently. However, this had yet to be tested. Covering 320 Myr of reptile evolution, we present here an ancestral character state reconstruction for the phenotypic osteoderm expression in 643 taxa of all major squamate crown-groups, including 70 extinct and outgroup representatives. Osteoderms were largely acquired in a series of events during the Late Jurassic and Early Cretaceous. Subsequent rate deceleration and absence of reversions ultimately led towards a state of evolutionary stability. As an exception, we reconstructed the loss of osteoderms in the varanid stem-lineage, and secondary re-acquisitions in Australopapuan varanids during an acquisition series in the Miocene. We discuss how lifestyle, locomotion, and biogeographical history may have driven these events. Foremost, we demonstrate that squamate osteoderm expression is the product of multiple independent acquisitions. This solidifies the foundation for future discussions on the underlying evolutionary mechanisms. Our findings also contribute towards a better understanding of the selective pressures and evolutionary trajectories that shaped present-day reptile biodiversity.
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Caroline D’Ávila Burgardt, Karine Pohlmann, Arielli Fabrício Machado, Mateus A. Costa Santos, João L. Meira & Felipe L. Pinheiro (2026)
A peculiar procolophonid lower jaw from the Sanga do Cabral Formation (Lower Triassic, Brazil)
Historical Biology (advance online publication)
doi:
https://doi.org/10.1080/08912963.2025.2608698https://www.tandfonline.com/doi/full/10.1080/08912963.2025.2608698In Brazil, the Lower Triassic is represented by the Sanga do Cabral Formation, known for its fragmented fossil tetrapods. However, in the last decade, some outcrops have revealed well-preserved remains, providing information about the first Triassic faunas of Western Gondwana. The Sanga do Cabral Formation fauna includes temnospondyls, procolophonids, and archosauromorphs. In this study, we describe a new procolophonid left hemimandible (UNIPAMPA 916) from the Sanga do Cabral Formation. The specimen differs from previously reported species for the site (Procolophon trigoniceps and Oryporan insolitus) in dental morphology, indicating a still hidden diversity of these parareptiles for the Brazilian Lower Triassic. The presence of a new procolophonoid morphotype for the Sanga do Cabral Formation underlines the importance of the Brazilian fossil record for understanding the recovery of ecosystems after the End-Permian Mass Extinction.