Fourth age of the Late Cretaceous epoch
The Santonian is an age in the geologic timescale or a chronostratigraphic stage. It is a subdivision of the Late Cretaceous Epoch or Upper Cretaceous Series. It spans the time between 86.3 ± 0.7 mya (million years ago) and 83.6 ± 0.7 mya. The Santonian is preceded by the Coniacian and is followed by the Campanian.[6]
- ^ International Commission on Stratigraphy. "ICS - Chart/Time Scale". www.stratigraphy.org.
- ^ Lamolda, M.; Paul, C.; Peryt, D.; Pons, J. (March 2014). "The Global Boundary Stratotype and Section Point (GSSP) for the base of the Santonian Stage, "Cantera de Margas", Olazagutia, northern Spain". Episodes. 37 (1): 2–13. doi:10.18814/epiiugs/2014/v37i1/001. Retrieved 24 December 2020.
- ^ a b Jarvis, Ian; et al. (2023). "Carbon isotopes, palynology and stratigraphy of the Santonian–Campanian boundary: The GSSP auxiliary sections, Seaford Head (England) and Bocieniec (Poland), and correlation between the Boreal and Tethyan realms". Cretaceous Research. 143: 105415. Bibcode:2023CrRes.14305415J. doi:10.1016/j.cretres.2022.105415. hdl:10871/133015. S2CID 253436620.
- ^ Gale, Andy; Batenburg, Sietske; Coccioni, Rodolfo; Dubicka, Zofia; Erba, Elisabetta; Falzoni, Francesca; Haggart, Jim; Hasegawa, Takishi; Ifrim, Christina; Jarvis, Ian; Jenkyns, Hugh; Jurowska, Agata; Kennedy, Jim; Maron, Matteo; Muttoni, Giovanni; Pearce, Martin; Petrizzo, Maria Rose; Premoli-Silva, Isabella; Thibault, Nicolas; Voigt, Silke; Wagreich, Michael; Walaszczyk, Irek (1 February 2023). "The Global Boundary Stratotype Section and Point (GSSP) of the Campanian Stage at Bottaccione (Gubbio, Italy) and its Auxiliary Sections: Seaford Head (UK), Bocieniec (Poland), Postalm (Austria), Smoky Hill, Kansas (U.S.A), Tepayac (Mexico)". Episodes. 46 (3): 6. doi:10.18814/epiiugs/2022/022048. hdl:2434/968946. S2CID 256539746. Retrieved 27 March 2023.
- ^ "Campanian GSSP Ratified by IUGS". Subcommission on Cretaceous Stratigraphy. International Commission on Stratigraphy. Retrieved 14 January 2023.
- ^ Gradstein et al. (2004)