Also known as Moradi Fauna, outskirts of Arlit
Where: Agadez, Niger (18.8° N, 7.2° E: paleocoordinates 16.6° S, 8.2° E)
• coordinate estimated from map
• small collection-level geographic resolution
When: Moradi Formation (Izégouandane Group), Changhsingian (254.2 - 252.2 Ma)
• "The locality lies within the upper strata of the Moradi Formation, approximately 25 m below an unconformity at the base of the Téloua 1 Formation [...] The age of the Moradi Formation is poorly constrained, but paleontological evidence indicates a Late Permian age (Taquet, 1972; de Ricqlès and Taquet, 1982). This is based mainly on the presence of the Triassic ichnotaxon Chirotherium in the overlying Téloua 1 Formation (Ginsburg et al., 1966), and on the presence of pareiasaurs and captorhinids in the Moradi Formation, all other known Gondwanan captorhinids also being of supposedly Late Permian age (Modesto and Smith, 2001)." (Damiani, 2006)
• group of beds-level stratigraphic resolution
Environment/lithology: "floodplain"; red mudstone and conglomerate
Size class: macrofossils
Preservation: mold/impression, trace
Collected in 2003, 2006
Primary reference: R. M. H. Smith, C. A. Sidor, N. J. Tabor and J. S. Steyer. 2015. Sedimentology and vertebrate taphonomy of the Moradi Formation of northern Niger: A Permian wet desert in the tropics of Pangaea. Palaeogeography, Palaeoclimatology, Palaeoecology 440:128-141 [A. Dunhill/B. Allen]more details
Purpose of describing collection: taxonomic analysis
PaleoDB collection 199774: authorized by Alex Dunhill, entered by Bethany Allen on 14.02.2019
Creative Commons license: CC BY (attribution)
Taxonomic list
Amphibia | |
Limnopus sp. Marsh 1894 tetrapod | |
Reptilia | |
cf. Pachypes sp. Leonardi et al. 1975 parareptile | |
Dromopus sp. Marsh 1894 reptile | |
Hyloidichnus sp. Gilmore 1927 eureptile |