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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"

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Elrhaz Formation
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Elrhaz Fm base reconstruction

Elrhaz Fm


Period: 
Cretaceous

Age Interval: 
Lower Cretaceous (Aptian?) (1)


Province: 
Iullemmeden Basin

Type Locality and Naming

Faure, 1954; the town of Elrhaz. The Type Section of the lower and middle Members is taken on the cliff along the eastern side of the Zelic kori. The Type Section of the upper Member is taken from a cliff south of Elrhaz (Fabre (1983)). Gadoufaoua Paleontological site. Group: Tégama Gr.

References: Faure, 1966; Taquet, 1976; Buffetaut & Taquet, 1977; Buffetaut & Taquet, 1979; de Lapparent de Broin, 1980; Taquet, 1982; Galton & Taquet, 1982; Fabre et al., 1983; Sereno et al., 1994, 1998; Taquet & Russell, 1998, 1999; Wenz, 1999; Sereno et al., 2001; de Lapparent de Broin, 2002; Blackburn & Sereno, 2002; Sereno et al., 2003; Rogers et al., 2005; Sereno & Brusatte, 2008; Sereno & Larsson, 2009; Le Loeuff et al., 2010, 2012; Sereno & ElShafie, 2013; Web-05. Group: Tégama Gr.

Synonym: El Rhas, El Rhaz. The upper part of the Girmaga Formation and lower part of the Mohra Formation of Molinas (1965). Equivalent(s): Tagrezou Fm (part of the Téfidet Gr) in Téfidet Sub-Basin.


Lithology and Thickness

The Elrhaz Formation is composed almost exclusively of cross-bedded medium-grained fluvial sandstones of low relief. Three Members are distinguished: two clay Members framing a sandier median Member. The lower and middle Members in the Type Section show black, purple, or red clays and black limestones with vertebrate bones overlain by coarse sandstone with cross-bedded and oblique stratifications, sometimes containing barite nodules. Cu (malachite) and U indices are also present in these layers. The upper Member in the Type Section is shaly and calcareous and very rich in large vertebrates, crocodiles and dinosaurians. At the Type Section, a little more than 80 m (can reach 120 m in the southeast). The formation thins towards the NE, where the limestone slabs at the top of the formation meet with the paleo reliefs of the Precambrian.


Lithology Pattern: 


Relationships and Distribution

Lower contact

Underlying Unit is the coarse sandstones of Tazolé Fm with silicified wood

Upper contact

Overlying unit is the Echkar Fm.

Regional extent


GeoJSON

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Fossils

Fish (bony fish), hybodont shark), crocodiles (Anatosuchus minor, Sarcosuchus imperator, Stolokrosuchus lapparenti, Araripesuchus wegeneri (Fig. 2)), turtles (Laganemys tenerensis) (Fig. 1), Platycheloides cf. nyasae and dinosaurians (the abelisaurid Kryptops palaios, the carcharodontosaurid Eocarcharia dinops, the spinosaurid theropods Baryonyx, Suchomimus tenerensis and Cristatusaurus lapparenti, the diplodocoid sauropod Nigersaurus taqueti (Rogers et al., 2005), the ornithopods Ouranosaurus nigeriensis, Valdosaurus nigeriensis and the iguanodon Lurdusaurus arenatus), pterosaurs (left humerus of Tapejaridae, a partial wing of Anhangueridae), freshwater bivalves.

[Figure 1. Turtle skull of Laganemys tenerensis in left lateral (top), dorsal (left) and ventral (right) views found in Gadoufaoua paleontological site (Source: Sereno & ElShafie, 2013).]

[Figure 2. Top: Skull of crocodilian Anatosuchus minor in dorsal view; length about 12 cm (Source: Sereno et al., 2003). Bottom: Flesh reconstruction of the crocodilian Anatosuchus minor (top) and Araripesuchus wegeneri (bottom) (Source: Sereno & Larsson, 2009).]


Age 

Lower Cretaceous (Aptian?). The exact age of the Elrhaz Formation is not so apparent: it was considered Barremian to Late Albian by Taquet (1976), who suggested an Aptian age, an opinion mainly followed by subsequent authors, although Taquet’s suggestion was based on the referral to the Aptian by Busson (1967) of an isolated ornithopod tooth found in Tunisia by Lapparent. It has since been demonstrated that this iguanodontid tooth (found in the Oum ed Diab Member of the Ain Guettar Fm, a few meters below the Cenomanian marine deposits) was more likely Albian after the discovery of am­monites in the vicinity. However, iguanodontid teeth are also known in the older Douiret Fm of Tunisia. Thus, Taquet’s main argument for an Aptian age seems weaker, and his ‘Barremian to Albian’ interval for the Elrhaz Formation is likely, although an older age (or an Aptian age) is not impossible as the lower part of the formation is not stratigraphically constrained (LeLoeuff et al., 2010; 2012). On the other hand, Sereno et al. (2009, 2013) consider it Aptian-Albian based on fossil interpretation and local stratigraphic observations. Since there has not yet been a consensus regarding the age of the Elrhaz Formation, it is decided here to stay with the status quo and keep assigning the unit to the Aptian, but with some reservation.

Age Span: 

    Beginning stage: 
Aptian

    Fraction up in beginning stage: 
0.65

    Beginning date (Ma): 
116.07

    Ending stage: 
Aptian

    Fraction up in the ending stage: 
1.0

    Ending date (Ma):  
113.20

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)