Ecological disturbance brought them to an end during the Edmontonian.[4] Relative sea levels fell very rapidly due to the Laramide orogeny.[4] Opportunistic generalist herbivores filled the vacated niches that were once filled by a diverse number of specialist forms.[4] The newly formed ecosystems tended to be dominated by a single herbivorous species each.[4] The new dominant herbivores were usually less ornamented and probably represent "survivors from indigenous lineages" rather than immigrants from other areas.[4] Gradually however "relict" dinosaurs such as protoceratopsids and sauropods began expanding into lower altitude areas as sea-levels fell.[4]
Cifelli, Richard L.; Eberle, Jaelyn J.; Lofgren, Donald L.; Lillegraven, Jason A.; Clemens, William A. (2012). "Mammalian Biochronology of the Latest Cretaceous". In Woodburne, Michael O. (ed.). Late Cretaceous and Cenozoic mammals of North America biostratigraphy and geochronology. New York: Columbia University Press. ISBN9780231503785.
Lehman, T. M., 2001, Late Cretaceous dinosaur provinciality: In: Mesozoic Vertebrate Life, edited by Tanke, D. H., and Carpenter, K., Indiana University Press, pp.310–328.
Lucas, Spencer G, ed. (1991). "Dinosaurs and Mesozoic biochronology". Modern Geology. 16: 127–138. Reprinted in Halstead, L.B. (1991). Dinosaur studies: commemorating the 150th anniversary of Richard Owen's Dinosauria. Philadelphia: Gordon and Breach. ISBN9782881248337.