Abstract <p>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 <i>Undichna</i> detected earlier, resting and walking trace fossils of aquatic arthropods (<i>Rusophycus</i> and <i>Diplichnites</i>), walking trackways and feeding areas of eurypterids (<i>Palmichnium</i>), and rosette-type crustacean or polychaetan feeding burrows (<i>Asterichnus</i>) 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.</p>

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

  • Ya. A. Shurupova,
  • J. V. Shuvalova,
  • A. Yu. Zhuravlev

摘要

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.