Elrhaz Formation: Difference between revisions
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| age = [[Aptian]]-[[Albian]] ~{{fossilrange|112}} |
| age = [[Aptian]]-[[Albian]] ~{{fossilrange|112}} |
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| period = Aptian |
| period = Aptian |
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| prilithology = |
| prilithology = [[Sandstone]] |
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| otherlithology = |
| otherlithology = |
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[[Category:Albian Stage]] |
[[Category:Albian Stage]] |
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[[Category:Aptian Stage]] |
[[Category:Aptian Stage]] |
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[[Category:Sandstone formations]] |
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[[Category:Fluvial deposits]] |
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[[Category:Cretaceous paleontological sites of Africa]] |
[[Category:Cretaceous paleontological sites of Africa]] |
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Revision as of 18:11, 17 August 2018
| Elrhaz Formation | |
|---|---|
| Stratigraphic range: Aptian-Albian ~ | |
 Outcrops of the formation | |
| Type | Geological formation |
| Unit of | Tegama Group |
| Underlies | Echkar Formation |
| Overlies | Tazolé Formation |
| Lithology | |
| Primary | Sandstone |
| Location | |
| Region | Africa |
| Country |  Niger |
The Elrhaz Formation is a geological formation in Niger, central Africa.
Its strata date back to the Early Cretaceous (late Aptian-early Albian stages, about 112 million years ago). Dinosaur remains are among the fossils that have been recovered from the formation, alongside those of multiple species of crocodyliformes.
Gadoufaoua
Gadoufaoua (Touareg for “the place where camels fear to go”) is a site within the Elrhaz formation (16°50′N 9°25′E / 16.833°N 9.417°E ) in the Tenere desert of Niger known for its extensive fossil graveyard. It is where remains of Sarcosuchus imperator, popularly known as SuperCroc, were found (by Paul Sereno in 1997, for example), including vertebrae, limb bones, armor plates, jaws, and a nearly complete 6-foot (1.8 m) skull.
Gadoufaoua is very hot and dry. However, it is supposed that millions of years ago, Gadoufaoua had trees, plants and wide rivers. The river covered the remains of dead animals, the fossilized remains of which were protected by the drying rivers over millions of years.[1]
Vertebrate paleofauna
Crocodyliformes
| Crocodyliformes reported from the Elrhaz Formation | ||||
|---|---|---|---|---|
| Genus | Species | Material | Notes | Images |
|
A. wegeneri[2] |
"nearly complete skull" - Sereno & Larsson (1999) |
Pseudonim. Dog-Croc |  | |
|
A. minor[2] |
"nearly complete skull" - Sereno & Larsson (1999) |
Pseudonim. Duck-Croc |  | |
| Sarcosuchus[3] | S. imperator | "partial skeletons, numerous skulls" |  | |
Ornithischians
| Ornithischians reported from the Elrhaz Formation | |||||
|---|---|---|---|---|---|
| Genus | Species | Stratigraphic position | Material | Notes | Images |
|
L. arenatus[2] |
"Partial skull, fragmentary postcranial skeleton."[4] |
 | |||
|
O. nigeriensis[2] |
"Skull and poscrania, second skeleton."[5] |
 | |||
|
E. nigeriensis[2] |
"Femora."[6] |
A Dryosaurid | |||
Theropods
| Theropods reported from the Elrhaz Formation | |||||
|---|---|---|---|---|---|
| Genus | Species | Stratigraphic position | Material | Notes | Images |
| Afromimus | A. tenerensis | "caudal vertebrae, chevrons and portions of the right hind limb"[7] | An Noasaurid | ||
|
E. dinops[8] |
"Partial skull and postcranial remains."[9] |
Carcharodontosaurid |  | ||
|
S. tenerensis[2] |
Partial skull and associated skeleton.[10] |
A second, possible spinosaurid found in the formation, Cristatusaurus, is considered either a separate species or a synonym to Suchomimus[11] |  | ||
|
K. palaios[2] |
Postcranial skeleton and partial skull.[12] |
Abelisaurid |  | ||
Sauropods
| Sauropods reported from Elrhaz Formation | |||
|---|---|---|---|
| Genus | Species | Material | Images |
| Nigersaurus | N. taqueti | The limited understanding of the genus was the result of poor preservation of its remains, which arises from the delicate and highly pneumatic construction of the skull and skeleton, in turn causing disarticulation of the fossils. Some of the skull fossils were so thin that a strong light beam was visible through them. Therefore, no intact skulls or articulated skeletons have been found, and these specimens represent the most complete known rebbachisaurid remains. |  |
See also
Footnotes
- ^ SCIENCE IN THE NEWS - Nov. 13: Digest - 12 November 2001 Voice of America
- ^ a b c d e f g h i j k l m n o "68.1 Departement D'Agedez, Niger; 1. Elrhaz Formation," in Weishampel, et al. (2004). Page 572.
- ^ Sereno, P. C.; Larsson, H. C.; Sidor, C. A.; Gado, B. (2001-11-16). "The giant crocodyliform Sarcosuchus from the Cretaceous of Africa". Science. 294 (5546): 1516–1519. doi:10.1126/science.1066521. ISSN 0036-8075. PMID 11679634.
- ^ "Table 19.1," in Weishampel, et al. (2004). Page 416.
- ^ "Table 19.1," in Weishampel, et al. (2004). Page 417.
- ^ "Table 19.1," in Weishampel, et al. (2004). Page 415.
- ^ Sereno, P. (2017). "Early Cretaceous ornithomimosaurs (Dinosauria: Coelurosauria) from Africa". Ameghiniana. 54 (5): 576–616. doi:10.5710/AMGH.23.10.2017.3155.
- ^ Sereno, Paul C.; and Brusatte, Stephen L. (2008). "Basal abelisaurid and carcharodontosaurid theropods from the Lower Cretaceous Elrhaz Formation of Niger" (pdf). Acta Palaeontologica Polonica 53 (1): 15–46. doi:10.4202/app.2008.0102.
- ^ "Table 4.1," in Weishampel, et al. (2004). Page 73.
- ^ "Table 4.1," in Weishampel, et al. (2004). Page 72.
- ^ Rauhut, O.W.M. (2003). "The interrelationships and evolution of basal theropod dinosaurs". Special Papers in Palaeontology 69: 1-213.
- ^ "Table 4.1," in Weishampel, et al. (2008). Page 72.
References
- Weishampel, David B.; Dodson, Peter; and Osmólska, Halszka (eds.): The Dinosauria, 2nd, Berkeley: University of California Press. 861 pp. ISBN 0-520-24209-2.