Unusual lizard fossil from the Miocene of Nebraska and a minimum age for cnemidophorine teiids

A Palaeogene stem crotaphytid (Aciprion formosum) and the phylogenetic affinities of early fossil pleurodontan iguanians

Pleurodonta is an ancient, diverse clade of iguanian lizard distributed primarily in the Western Hemisphere. Although the clade is a frequent subject of systematic research, phylogenetic resolution among the major pleurodontan clades is elusive. That uncertainty has complicated the interpretations of many fossil pleurodontans. I describe a fossil skull of a pleurodontan lizard from the Palaeogene of Wyoming that was previously allocated to the puzzling taxon Aciprion formosum, and provide an updated morphological matrix for iguanian lizards. Phylogenetic analyses using Bayesian inference demonstrate that the fossil skull is the oldest and first definitive stem member of Crotaphytidae (collared and leopard lizards), establishing the presence of that clade in North America during the Palaeogene. I also discuss new or revised hypotheses for the relationships of several early pleurodontans. In particular, I examine potential evidence for crown-Pleurodonta in the Cretaceous of Mongolia (Polrussia), stem Pleurodonta in the Cretaceous of North America (Magnuviator) and a stem anole in the Eocene of North America (Afairiguana). I suggest that the placement of the fossil crotaphytid is stable to the uncertain phylogeny of Pleurodonta, but recognize the dynamic nature of fossil diagnosis and the potential for updated systematic hypotheses for the other fossils analysed here.

Morphometric analyses of the vertebrae of Ambystoma (Tschudi, 1838) and the implications for identification of fossil salamanders

Ambystoma (Tschudi, 1838) represents a speciose clade of salamanders that are found across much of North America. Fossils referred to Ambystoma are reported from early Cenozoic deposits and are common in Quaternary fossil deposits. Most fossils identified as Ambystoma are isolated vertebrae. Both quantitative and qualitative characters were reported as being useful for identifying fossilized vertebrae of Ambystoma below the genus level. However, there is limited information on intraspecific variation in those characters and previous studies noted intracolumnar variation which affects the utility of those characters for fossil identification. A lack of understanding of variation in modern species of Ambystoma casts uncertainty on our ability to identify fossil vertebrae confidently. We aimed to document intraspecific and intracolumnar variation in vertebral morphology among species of Ambystoma and examine the implications for fossil identification. We assembled one of the largest skeletal datasets for Ambystoma and took linear measurements on 15 species. We used 2D geometric morphometric analyses to characterize atlantal shape variation in Ambystoma. We apply those morphometric data in a case study where we identify fossil vertebrae from Hall's Cave, a Quaternary fossil locality in central Texas. We found patterns of intraspecific and intracolumnar variation that have substantial implications for fossil identification. Classification accuracies for species and clades within Ambystoma varied considerably. Overall classification accuracies based on size adjusted measurements and 2D geometric morphometric landmarks were lower compared to classifications from non-size adjusted linear measurements and were similar to accuracies based on size adjusted linear measurements. We identified fossil vertebrae from our case study as likely belonging to the tiger salamander clade within Ambystoma, but found that some fossils with lower classification probabilities are of uncertain identity. We discuss biogeographic implications for our fossil identifications and comment on challenges and next steps for advancing our understanding of morphological variation in Ambystoma.