Late Devonian Ichnofossil Lagerstätte of the Eastern Anti-Atlas, Morocco

A rich ichno-assemblage is known from the Upper Devonian (Famennian) Aoufilal Formation of the eastern Anti-Atlas in Morocco. Despite its high diversity, only a few trace fossils have been properly described until now. In addition to fish-produced ichnotaxon Undichna detected earlier, resting and walking trace fossils of aquatic arthropods (Rusophycus and Diplichnites), walking trackways and feeding areas of eurypterids (Palmichnium), and rosette-type crustacean or polychaetan feeding burrows (Asterichnus) are described here. All the traces are preserved in positive hyporeliefs on the lower bedding surfaces of a reddish-brown fine-grained sandstone accumulated under shallow-marine conditions. A high diversity, excellent preservation and frozen state of the paleocommunity despite the absence of body fossils allow us to rate the Aoufilal ichno-assemblage as an ichnofossil Lagerstätte.

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Publication Details

Journal
Paleontological Journal
Published
2025-12-01
DOI
https://doi.org/10.1134/s0031030125600453
Primary Topic
Geological formations and processes
Type
article
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article

Late Devonian Ichnofossil Lagerstätte of the Eastern Anti-Atlas, Morocco

Ya. A. Shurupova, A. Yu. Zhuravlev, J. V. Shuvalova
Paleontological Journal
Geological formations and processes
article

Late Devonian Ichnofossil Lagerstätte of the Eastern Anti-Atlas, Morocco

Ya. A. Shurupova, A. Yu. Zhuravlev, J. V. Shuvalova
article en

Abstract

A rich ichno-assemblage is known from the Upper Devonian (Famennian) Aoufilal Formation of the eastern Anti-Atlas in Morocco. Despite its high diversity, only a few trace fossils have been properly described until now. In addition to fish-produced ichnotaxon Undichna detected earlier, resting and walking trace fossils of aquatic arthropods (Rusophycus and Diplichnites), walking trackways and feeding areas of eurypterids (Palmichnium), and rosette-type crustacean or polychaetan feeding burrows (Asterichnus) are described here. All the traces are preserved in positive hyporeliefs on the lower bedding surfaces of a reddish-brown fine-grained sandstone accumulated under shallow-marine conditions. A high diversity, excellent preservation and frozen state of the paleocommunity despite the absence of body fossils allow us to rate the Aoufilal ichno-assemblage as an ichnofossil Lagerstätte.

Paleontological JournalVol. 59(8)
Lomonosov Moscow State University (RU), Institute of Paleontology A A Borisyak (RU), Moscow State University (TJ)
Life below water
Openalex Percentile: Top 27%
Geological formations and processes
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