Strict consensus tree obtained in the phylogenetic analysis and mapped against the stratigraphic ranges for each taxon. Black lines indicate temporal distribution based on type material. Gray lines indicate temporal distribution based on referred material. For simplicity, taxa are referred to full time bins (i.e., the entire Maastrichtian or the entire late Campanian).

 
 
  Part of: Spicher GE, Sertich JJW, Girard LC, Joyce WG, Lyson TR, Rollot Y (2023) A description of a Denazinemys nodosa specimen (Testudinata, Baenidae) from the Late Cretaceous Kaiparowits Formation of southern Utah. Fossil Record 26(2): 151-170. https://doi.org/10.3897/fr.26.102520