Home Multi-Country Search About Admin Login
Cenozoic
Cretaceous
Jurassic
Triassic
Permian
Paleozoic


Compiled by: Jacques LeBlanc (2022), Stratigraphic Lexicon: The Sedimentary Formations of The Republic of Niger, Africa. Colnes Publishing (Tallin, Estonia), 365 pp. For more information see "About"

Search by
Select Region(s) to search
Hold Ctrl (Windows/Linux) or Command (Mac) to select multiple
Dibella Formation
Click to display on map of the Ancient World at:
Dibella Fm base reconstruction

Dibella Fm


Period: 
Cretaceous

Age Interval: 
Early Cretaceous (Aptian to Albian) (7c)


Province: 
East Niger Rift Basin - Termit Sub-basin

Type Locality and Naming

Faure, 1954, 1966; Faure et al., 1956.

References: Boureau, 1955; Furon, 1956, 1964; Faure, 1954, 1966; Faure et al., 1956; Fabre et al., 1983.

Synonym: Série de Dibella; Equivalent(s): Achegour Fm, Tiffa Fm, Tégama Gr, Téfidet Gr


Lithology and Thickness

Predominantly coarse sandstone with cross-bedded stratification underlined by gravel areas (Fig. 1). Towards the base, several conglomerate levels exist, which include quartz pebbles. The color of the sandstones is generally light. White, beige-pink, and especially gray dominate, often masked by a black patina. Silty levels play only a secondary role; they are reduced to inter-beds not exceeding a few decimeters. Its thickness is 150-200 m.

[Figure 1: Section of the Dibella Formation 3 km E-NE of the Dibella wells (Source: Faure, 1966, page 220)]


Lithology Pattern: 
Coarse-grained sandstone


Relationships and Distribution

Lower contact

Discordance onto the Precambrian basement (rubified granite)

Upper contact

Overlying unit is the Ezerza Fm

Regional extent


GeoJSON

{"type":"Feature","geometry":{"type":"MultiPolygon","coordinates":[[[[12.34,17.87],[12.62,17.27],[13.51,16],[14.35,15.19],[14.81,14.17],[14.71,14.97],[14.93,15.32],[14.66,15.36],[14.53,15.87],[13.19,17.56],[12.78,17.61],[12.67,17.92],[12.34,17.87]]]]}}

Fossils

Traces of plants (Podocarpites saharianum Boureau) and imprints of leaves of Dicotyledonous Angiosperms (Laurophyllum and Cinnamomoides) (Fig. 2). Faure (1966) states: “The shale levels with vertebrates of the Elrhas formation, known to the south and east of the Aïr, seem to be absent in the Dibella formation. Sedimentation may not have started there until after the period char­acterized by large lakes.”

[Figure 2: Drawings of Dicotyledonous Angiosperms [Podocarpites (?) saharianum (Aa, Ba, Ca); Laurophyllum gadilhei (Ad, Bb, Cb); Cinnamomoides faurei (Ab); Cinnamomoides tchadense (Ac)] leave imprints from the Dibella Fm (Boureau, 1955)]


Age 

Early Cretaceous (Aptian to Albian), just before the Cenomanian, Boureau, 1955.

Age Span: 

    Beginning stage: 
Aptian

    Fraction up in beginning stage: 
0.5

    Beginning date (Ma): 
117.30

    Ending stage: 
Albian

    Fraction up in the ending stage: 
1.0

    Ending date (Ma):  
100.50

Depositional setting

Continental


Depositional pattern:  


Additional Information


Compiler:  

Jacques LeBlanc (2022), Stratigraphic Lexicon: The Sedimentary Formations of The Republic of Niger, Africa. Colnes Publishing (Tallin, Estonia), 365 pp. https://doi.org/10.47909/978-9916-9760-6-7 (or via https://sites.google.com/site/leblancjacques)