their assignment shifting around between several different geologic formations before finally being settled as its own unit of the Chubut Group, dating to the Maastrichtian. Additionally, Secernosaurus specifically had a very uncertain geologic provenance. Resultingly, the ecosystem Secernosaurus would've lived in was not strongly understood historically. A 2016 paper by Casal A. Gabriel and colleagues studied the climatic conditions of the region more in depth, finding evidence of climate change across geologic time. Fluvial systems and evidence of a floodplain environment were recognized, but the geologically lower parts of the formation also showed evidence of semi-arid conditions, large gypsum deposits, and desiccation cracks, indicating intense aridization of the region compared to the very humid climate of the Bajo Barreal Formation's ecosystem that preceded Lago Colhué Huapi Formation. However, palynological data indicates that during the upper deposits of the formation at the very end of the Cretaceous and into the Danian age of the Paleocene, the climate become more mild once again and returned to a balance wet and dry season. It is from this uppermost part of the formation that Secernosaurus it from. More recent discoveries of hadrosaur remains from other localities, which could belong to Secernosaurus might extend the range within the formation hadrosaurs are found in. Currently, however, they have not been research in depth. Secernosaurus is not the only dinosaur known from Lago Colhué Huapi. Remains of the sauropods Elaltitan lilloi, Argyrosaurus superbus and Aeolosaurus colhuehuapensis, as well as unidentified sauropod remains found in 2010, have been discovered in the formation. Very fragmentary remains of dromaeosaurid and megaraptoran theropods have also been discovered, as is expected from other formations from a similar time and place. The enigmatic ornithischian dinosaur Notoceratops, based on a lost fragmentary specimen originally considered to belong to a ceratopsian but now debated between that identity and that of a hadrosaur. Finally, scant fossils of chelonians, crocodyliformes, and dipnoid fish have also been found. Palaeobiogeography Secernosaurus lived in what is now Patagonia during the Maastrichtian age of the Cretaceous period. It was one of the few hadrosaurs to live in South America. Their presence in South America is likely to represent a dispersal event from North America during the Campanian, when the proto-Antilles may have formed an island chain that allowed land vertebrates to cross between the two continents. The arrival of hadrosaurids in South America may have caused the decline of the native