The boundary for the Eifelian-Givetian Stage Global Stratotype Section and Point (GSSP) in the Middle Devonian has been ratified by the ICS and the IUGS and is placed in a section at Jebel Mech Irdane in the Tafilalt of Morocco. The position of the boundary was selected bx the Subconvnission on Devonian Stratigraphy in 1992 to coincide with the level at which Polygnathus pseudo-foliatus changes to Polygnathus hemiansatus as described herein. The boundaiy corresponds closely with the base of the goniatite Maenioceras Stufe used as a Middle Devonian division, and with the entry of the dacryoconarid Nowakia otomari. Although spores are not described from the section owing to thermal modification, the level is thought to lie below the appearance of Geminospora lemurata the entiy of which has been widely used elsewhere in spore-bearing regions as a guide to the Givetian. Comments are made on the relations of the GSSP level to the associated Kacdk or otomari Event.
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