Ichnodisparity has been recently introduced as a concept to assess the variability of
morphologic plans in biogenic structures, revealing major innovations in body plan …

Bioturbation at all scales, which tends to replace the primary fabric of a sediment by the
ichnofabric (the overall fabric of a sediment that has been bioturbated), is now recognised as …

This book provides readers with a well-balanced blend of high-quality photographs, figures
and accompanying texts on the identification of trace fossils, both in core and in outcrop …

The taxonomic treatment of trace fossils needs a uniform approach, independent of the
ethologic groups concerned. To this aim, trace fossils are rigorously defined with regard to …

The Mickwitzia sandstone, south-central Sweden, consists of about 10 m of Lower Cambrian
clastic sediments deposited in an epicontinental setting. An in formal, lithologically based …

After taxonomic revision, trace fossils show a similarly explosive diversification in the
Ediacaran–Cambrian transition as metazoan body fossils. In shallow-marine deposits of …

The increase in trace fossil diversity across the Neoproterozoic-Cambrian boundary often is
presented in terms of tabulations of ichnogenera. However, a clearer picture of the increase …

The behaviour of the iconic ichnogenus Chondrites is re-evaluated based on review of
existing literature and analysis of novel data (macroscopic, thin section and ESEM-EDX …

Several concepts pertaining to the dramatic changes that occurred during the Cambrian
have been proposed, namely the Agronomic Revolution (AR), the Cambrian Substrate …

Rhizocorallium is one of the oldest known trace fossils, with wide distribution through the
Phanerozoic and all over the world. Originally introduced from the epicontinental Triassic of …