The Hassi Nebech area of the SE Tafilalt (Tafilalt Basin, Anti-Atlas, Morocco) yielded the richest and most diverse late Givetian ammonoid fauna on a global scale. Above the distinctive regional "Lower Marker Bed" (Synpharciceras clavilobum Zone), abundant loosely collected limonitic specimens derive from hypoxic shales of the Taouzites taouzensis to Petteroceras errans zones. The ontogenetic morphometry and intraspecific variability of a total of 30 species representing five families, the Acanthoclymeniidae, Taouzitidae, Pharciceratidae, Petteroceratidae, and Tornoceratidae, are documented. New taxa are: Pseudoprobeloceras praecox n. sp., Scaturites minutus n. gen. n. sp., Darkaoceras velox n. sp., Pharciceras decoratum n. sp., Ph. fornix n. sp., Ph. subconstans n. sp., Ph. involutum n. sp., Lunupharciceras incisum n. sp., Transpharciceras procedens n. gen. n. sp., Stenopharciceras progressum n. sp., Pluripharciceras n. gen. (type species: Synpharciceras plurilobatum Petter, 1959), Plu. orbis n. sp., Synpharciceras frequens n. sp., Lobotornoceras bensaidi n. sp., Nebechoceras eccentricum n. gen. n. sp., and Phoenixites lenticulus n. sp.. The documentation of conch and particularly suture ontogeny and intraspecific variability necessitates a revised diagnosis for ten taxa. Manticoceras pontiformis Termier & Termier, 1950, Probeloceras costulatum Petter, 1959, and Pseudoprobeloceras nebechense BensaÒd, 1974 are regarded as subjective junior synonyms of Ps. pernai (Wedekind, 1918). Sandbergeroceras acutum Termier & Termier, 1950 is a subjective synonym of Taouzites taouzensis (Termier & Termier, 1950). Pharciceras applanatum BensaÒd, 1974 is transferred to Extropharciceras. Other forms (Ph. aff. tridens, Ph. cf. subconstans n. sp., Extropharciceras n. sp. 2, Ex. cf. arenicum, Ex. cf. applanatum, Synpharciceras sp., Plu. cf. plurilobatum) are described in open nomenclature. Fossil Record 16 (1) 2013, 5 -65 / DOI 10.1002 Additional supporting information may be found in the online version of this article at the publisher's web-site * Corresponding author are currently only ca. 20 named species for all of the late Givetian of the Rhenish Massive, the region with the next highest documented diversity.For a brief review of the palaeogeographic distribution ( Fig. 1) of pharciceratid faunas and of previous reports from the Anti-Atlas, the reader is referred to Bockwinkel et al. (2009). The late Givetian ammonoid zonation and conodont correlation within the Tafilalt region was summarized by Becker & House (2000a, 2000b and Aboussalam & Becker (2007
Locality and StratigraphyThe Hassi Nebech area in the south-eastern Tafilalt (Fig. 2) exposes an Early to Late Devonian succession in an elongated, ca. WNW-ESE striking band of low outcrop for several kilometres, starting ca. 19 km eastnortheast from Taouz. Following early records of pharciceratids in rather generalized faunal lists for the Erfoud region by Termier (1929) and Clariond (1934), it is the first North African locality from which a late Givetian goniatite ...