Where: Figuig, Morocco (32.7° N, 3.1° W: paleocoordinates 27.1° N, 1.0° E)
• coordinate stated in text
When: Lower Anoual Member (Anoual Formation), Bathonian (168.3 - 166.1 Ma)
• The Guelb el Ahmar fauna is stratigraphically located in the upper part
•of the Anoual Formation... subdivided into a thick continental lower member, and a shallow marine carbonaceous upper member. The lithology and sedimentary structures of the lower member suggest a flooding plain and/or deltaic depositional environment. This is consistent with the large fossil trunks that are common in that unit. The fossiliferous levels yielding the Guelb el Ahmar (GEA) vertebrate fauna belong to the upper part of the lower member of the Anoual Fm. Sites GEA 3 and GEA 1 correspond to the same level of calcareous lacustrine limestones, which underlies site GEA 2.
Environment/lithology: fluvial-deltaic; lithified, calcareous limestone
Size classes: macrofossils, mesofossils
Collection methods: bulk, surface (in situ), mechanical, peroxide, sieve,
Primary reference: H. Haddoumi, R. Allain, S. Meslouh, G. Metais, M. Monbaron, D. Pons, J.-C. Rage, R. Vullo, S. Zouhri and E. Gheerbrant. 2016. Guelb el Ahmar (Bathonian, Anoual Syncline, eastern Morocco): first continental flora and fauna including mammals from the Middle Jurassic of Africa. Gondwana Research 29:290-319 [P. Barrett/T. Cleary]more details
Purpose of describing collection: general faunal/floral analysis
PaleoDB collection 176122: authorized by Paul Barrett, entered by Terri Cleary on 29.01.2016
Creative Commons license: CC BY (attribution)
Taxonomic list
Coelacanthimorpha | |
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Actinopteri | |
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Osteichthyes | |
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