E vestigiis palaeontologicis constat exstinctiones specierum permultarum in fine periodus Cretaceae accidisse, ut puta omnium dinosauriorum, pterosauriorum, mosasauriorum, hippuritidorum et ammonearum.[6]
↑"La troisième, qui correspond à ce qu'on a déja appelé formation de la craie, sera désigné par le nom de terrain crétacé: Ioannes Iulianus d'Omalius d'Halloy, "Observations sur un essai de carte géologique de la France, des Pays-Bas, et des contrées voisines" in Annales des mines vol. 7 (1822) p. 353 sqq. (vide p. 373 apud Google Books).
↑De historia nominis definitionisque vide: Mary Grace Wilmarth, The Geologic Time Classification of the United States Geological Survey Compared With Other Classifications, accompanied by the original definitions of era, period and epoch terms (United States Geological Survey Bulletin 769. Vasingtoniae: U.S. Government Printing Office, 1925) (p. 56 apud Google Books).
↑N. MacLeod et alii (1997), The Cretaceous–Tertiary biotic transition. Journal of the Geological Society, London, 154: 265–292 lege hic[nexus deficit]
Bibliographia
Graham, Alan. 2011. "The age and diversification of terrestrial New World ecosystems through Cretaceous and Cenozoic time." American Journal of Botany 98 (3): 336-351 JSTOR
Skinner, Brian J.; Porter, Stephen C. (1995). The Dynamic Earth: An Introduction to Physical Geology (tertia ed.). Novi Eboraci: John Wiley & Sons. ISBN0-471-60618-9.
Stanley, Steven M. (1999). Earth System History. Novi Eboraci: W. H. Freeman and Company. ISBN0-7167-2882-6.
Wesener, Thomas et Leif Moritz. 2018. "Checklist of the Myriapoda in Cretaceous Burmese amber and a correction of the Myriapoda identified]." Check List 14: 1131–40. Editio interratialis.