Fig. 4: Palaeobiogeography of Deinosuchus spp.

(A) Distribution of Deinosuchus riograndensis and D. schwimmeri3 during the Campanian around the Western Interior Seaway (WIS). (B) parsimony ancestral state reconstruction (equal branch length) of osmoregulation in Crocodylia and close relatives using presence/absence of salt glands, stable isotopes, and coastal marine occurrences as proxies11,13,14,15,17,35,36,37,38,39,40,42,44,120. The topology is from the present study except for ‘thoracosaurs’ for which we follow a more appropriate tip-dated work41. The analysis suggests potential plesiomorphic saltwater-tolerance for Deinosuchus and Crocodylia with early loss in Alligatoroidea. The distribution of Deinosuchus may be explained by dispersal across the WIS. Map is redrawn from118, early to late Campanian. Distribution of Deinosuchus spp. follows3,11,17 and references therein.