“…aulacophore in extended position, with slightly ajar cover plates; Lefebvre et al 2022a, b) and also of ophiuroids literally 'frozen in the act' of capturing, and presumably feeding on, young individuals of eocrinoids (Lefebvre et al 2008) Comprising representatives of ten distinct classes (Asteroidea, Coronoidea, Crinoidea, Diploporita, Edrioasteroidea, Eocrinoidea, Ophiuroidea, Rhombifera, Soluta, and Stylophora), the Tafilalt Biota yielded not only one of the best preserved, but also one of the most diverse Late Ordovician echinoderm faunas from the Mediterranean Province. Although their composition varies from locality to locality, possibly reflecting subtle differences in environmental conditions, such as hydrodynamics and bathymetry, starfish beds from the eastern and western Tafilalt yielded comparable Sandbian-early Katian assemblages generally dominated by ophiuroids, solutans and/or stylophorans, with sometimes locally abundant edrioasteroids, eocrinoids and/or rhombiferans, and more occasional occurrences of asteroids, coronoids, diploporites and/or crinoids (Lefebvre et al 2007(Lefebvre et al , 2008(Lefebvre et al , 2010(Lefebvre et al , 2022aNardin 2007;Régnault 2007;Hunter et al 2010;Sumrall & Zamora 2011Nardin & Régnault 2015;Botting 2018;, 2019Nohejlová & Lefebvre 2021). These assemblages display strong palaeobiogeographical affinities with coeval faunas from Bohemia (Czech Republic) and, to a lesser extent, with the Armorican Massif (France) and the Iberian Peninsula (Portugal and Spain).…”