The Givetian at Oufrane, ca. 5.5 km N of Sidi-El-
    Mehdaoui, has been visited, as most of the Dra Valley
    sections, by H. HOLLARD (see charts in 1981) but no
    detailed stratigraphic data have ever been pubhshed.
    BENSAID (1974) emphasized Oufrane as an important
    locality for goniatites, partly as type locality for new
    species, but did not include a measured section.  He
    illustrated well preserved specimens which in current
    taxonomy fall in the following species:
    Agoniatites costulatus (his pl. 1, figs 7-8)
    Wedekindella lata (his pl. 2, figs 7, 7a, the holotype)
    "Phoenixites " n. sp. 1 (his pl. 5,      fig. 7, figured as
    Tornoceras cf simplex)
    Maenioceras terebratum terebratum (his pl. 1, figs 12, 12a)
    Afromaenioceras sulcatostriatum (his pl. 2, figs 2, 3, 3a, the
    holotype, 8, 8a, 9, 9a)
    Mzerrebites juvenocostatus (his pl. 3, figs 2, 2a, figs 4-4b,
    figured as Hoeninghausia (Koenenites) cf lamellosa, pl. 4,
    fig. 5, pl. 6, figs 1, la, 12)
    Pharciceras aff. amplexum (his pl. 4, figs   8, 8a, figured as
    Ph. tridens)