Geologia Croatica, Vol. 74 No. 3, 2021.
Izvorni znanstveni članak
https://doi.org/10.4154/gc.2021.15
Sedimentology and ichnology of the mid-Cretaceous succession of the Ouled Nail Mounts (Eastern Saharan Atlas, Algeria)
Mohammed Nadir Naimi
orcid.org/0000-0001-9787-262X
; Université Kasdi Merbah, Laboratoire de Géologie du Sahara, Ghardaïa Road, Ouargla, 30000, Algeria
Amine Cherif
; Université Kasdi Merbah, Laboratoire de Géologie du Sahara, Ghardaïa Road, Ouargla, 30000, Algeria
Sažetak
Shallow marine deposits characterize the upper Albian – lower Cenomanian deposits of Northern Algeria. In Djebel Azzeddine (Ouled Nail Mounts), the corresponding sediments have been subdivided into three distinctive units A to C. The first discovered ammonite fauna from the Bou Saada area allowed the attribution of a part of the mid-Cretaceous post-Continental Intercalaire deposits to the upper Albian. The ammonite-bearing level indicates a maximum flooding surface and could be correlated with similar levels from Northern Algeria. The studied succession is characterized by a low ichnodiversity containing eight ichnotaxa with abundant Thalassinoides, common Skolithos, and rare Gyrolithes, Oichnus, Planolites and cf. Tisoa. This ichnoassemblage is dominated by domichnion, fodinichnion and praedichnion trace fossils, and is attributed to the Skolithos and Glossifungites ichnofacies. These traces are produced mainly by decapod crustaceans, polychaetes and naticid gastropods. The sedimentological and ichnological data suggest shoreface to backshore environments with mixed tide/storm energy, and long subaerial exposures indicated by Lofer cyclothems in the lowermost part and dinosaur footprints in the upper part of the section.
Ključne riječi
Trace fossils; Transgression; Albian – Cenomanian; Ouled Nail Mounts; Algeria
Hrčak ID:
265323
URI
Datum izdavanja:
27.10.2021.
Posjeta: 795 *