Taberia Fm
Type Locality and Naming
Joulia, 1959; Claret & Tempère, 1968.
References: Lessard, 1961; Claret & Tempère, 1968; Dars et al., 1971; Valsardieu, 1971; Termier et al., 1973; Fabre et al., 1983; Fabre, 2005.
Synonym: Grès d’Amesgueur (Joulia, 1959); Grès de Taberia (Claret & Tempère, 1968);
Lithology and Thickness
Coarse to fine sandstones locally gypsiferous, and lagoonal shales with rare bivalves (Valsardieu, 1971). Claret et al. (1968) state that except for a coarse-grained base, the sandstones are fine and intercalated with siltstones and shales with rare trace fossils Spirophyton (Fig. 1). Thickness: 80 – 150 m. On page 51 of Valsardieu (1971), it is stated a thickness of 80 m for this Formation in the area of Touaret town.
[Figure 1. Distribution of the Upper Devonian formations with Spirophyton trace fossil in the Sahara (Source: Termier et al., 1973).]
Relationships and Distribution
Lower contact
Underlain by the Akara Mbr of the Tin Séririne Fm
Upper contact
Overlain by the Farrazekat Fm
Regional extent
GeoJSON
Fossils
Rare trace fossils of Spirophyton (page 51 of Valsardieu, 1971).
Age
Depositional setting
Marine
Additional Information