Santonian
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]
Stratigraphic definition
The Santonian Stage was established by French geologist Henri Coquand in 1857. It is named after the city of Saintes in the region of Saintonge , where the original type locality is located.[ 7]
The base of the Santonian Stage is defined by the appearance of the inoceramid bivalve Cladoceramus undulatoplicatus . The GSSP (official reference profile) for the base of the Santonian Stage is located near Olazagutia , Spain; it was ratified by the Subcommission on Cretaceous Stratigraphy in 2012.[ 7] The Santonian's top (the base of the Campanian Stage) is informally marked by the extinction of the crinoid Marsupites testudinarius .[ 8] A GSSP for the top of the Santonian was ratified in October 2022 in Bottaccione, Gubbio , Italy .[ 3]
Subdivision
The Santonian is sometimes subdivided into Lower, Middle and Upper Substages. In the Tethys domain the Santonian is coeval with a single ammonite biozone : that of Placenticeras polyopsis . Biostratigraphy based on inoceramids, nanoplankton or forams is more detailed.
References
Notes
^ 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 c 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)
^ a b Gradstein, F.M.; Ogg, J.G.; Schmitz, M.D.; Ogg, G.M., eds. (2020). Geologic Time Scale 2020 . Elsevier. p. 1038. ISBN 978-0-12-824360-2 .
^ Gradstein, F.M.; Ogg, J.G.; Schmitz, M.D.; Ogg, G.M., eds. (2020). Geologic Time Scale 2020 . Elsevier. p. 1040. ISBN 978-0-12-824360-2 .
Literature
External links