Hurdiid radiodont frontal appendages from the Fezouata Shale
The Early Ordovician (~480 million-year-old) Fezouata Shale Formation of Morocco is a critical source of evidence for the unfolding Great Ordovician Biodiversification Event, the largest radiation in animal diversity during the Paleozoic. The Fezouata Shale preserves abundant remains of ancient […]