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The Rhaetian is the latest age of the Triassic period or the uppermost stage of the Triassic system . It was preceded by the Norian and succeeded by the Hettangian . The base of the Rhaetian lacks a formal GSSP, though candidate sections include Steinbergkogel in Austria and Pignola-Abriola in Italy . The end of the Rhaetian is more well-defined. According to the current ICS system, the Rhaetian ended 201.3 ± 0.2 Ma .