The extensive, predominantly siliciclastic deposits of the Upper Ordovician of the Tafilalt
have long been the subject of scientific investigation. In the past 25 years, intensified …

Cornute stylophorans are a minor, although typical, component of Middle–Late Ordovician
echinoderm assemblages adapted to soft siliciclastic substrates in high-latitude peri …

Abstract The Anti-Atlas contains a thick, volcanic-free Ordovician succession that originally
deposited in a passive-margin basin. Three main sedimentary packages are bounded by …

ABSTRACT The Late Ordovician Tafilalt Biota of the Moroccan Anti-Atlas includes a diverse
range of soft-bodied organisms, including palaeoscolecids, paropsonemid eldonioids …

Anomalocystitid mitrates represent one of the most diverse and long ranging clade of
stylophorans (Early Ordovician–Middle Devonian). Although they probably originated from a …

Exceptionally preserved fossils yield crucial information about the evolution of Life on Earth.
The Fezouata Biota from the Lower Ordovician of Morocco is a Konservat-Lagerstätte of …

In the western Tafilalt area, eastern Anti-Atlas (Morocco), solutan echinoderms are a major
faunal element of most echinoderm Lagerstätten occurring within the Lower Ktaoua …

Abstract The early Late Ordovician (Sandbian 1) representatives of the Tafilalt Biota in the
locality of Bou Nemrou (Jbel Tjarfaïouine) provide examples of fossil preservation in medium …

Abstract The late Ordovician Tafilalt Biota of Morocco is a recently discovered Konservat-
Lagerstätte that provides abundant paropsonemid eldonioids–resembling those from the …

Abstract Edrioasteroids from the Katian, Lower Ktaoua and Upper Tiouririne formations
provide new data on several previously described species and two new species of …