Ma and 20.43 ± 0.05 Ma (million years ago) during the Early Miocene. It was a dry, cooling period.[5] The Aquitanian succeeds the Chattian (the youngest age of the Oligocene) and precedes the Burdigalian
.
The Aquitanian Age overlaps with the
Waitakian
Ages from various regional timescales.
Stratigraphic definition
The Aquitanian Stage was named after the Aquitaine region in France and was introduced in scientific literature by Swiss stratigrapher Karl Mayer-Eymar in 1858.
The base of the Aquitanian (also the base of the Miocene
GSSP for the Aquitanian Stage lies in the Lemme-Carrosio section near the small village of Carrosio (north of Genoa) in northern Italy.[6]
The top of the Aquitanian Stage (the base of the Burdigalian) is at the first appearance of
Mayer-Eymar, K.; 1858: Versuch einer neuen Klassifikation der Tertiär-Gebilde Europa’s, Verhandlungen der Schweizerischen Naturforschenden Gesellschaft 17–19 (August 1857), p. 70–71 & 165–199. (in German)
Steininger, F.F.; Aubry, M.P.; Berggren, W.A.; Biolzi, M.; Borsetti, A.M.; Cartlidge, J.E.; Cati, F.; Corfield, R.; Gelati, R.; Iaccarino, S.; Napoleone, C.; Ottner, F.; Rogl, F.; Roetzel, R.; Spezzaferri, S.; Tateo, F.; Villa, G. & Zevenboom, D.; 1997: The Global Stratotype Section and Point (GSSP) for the base of the Neogene, Episodes 20(1), p. 23-28.