6533b7d9fe1ef96bd126d7af
RESEARCH PRODUCT
Preliminary report on new echinoderm Lagerstatten from the Upper Ordovician of the eastern Anti-Atlas, Morocco.
Bertrand LefebvreP. Van RoySamuel ZamoraAaron W. HunterElise NardinSerge Régnaultsubject
010506 paleontologyTaphonomybiologyPaleozoicRange (biology)LithologyStarfish010502 geochemistry & geophysicsbiology.organism_classification01 natural sciencesPaleontologyOPHIUROIDEAEchinodermOrdovicianAssemblage (archaeology)[SDU.STU.PG] Sciences of the Universe [physics]/Earth Sciences/Paleontology14. Life underwater[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/PaleontologyGeology[ SDU.STU.PG ] Sciences of the Universe [physics]/Earth Sciences/Paleontology0105 earth and related environmental sciencesdescription
8 pages (p.23-30); International audience; Four distinct echinoderm Lagerstatten have recently been discovered in the Upper Ordovician of the eastern Anti-Atlas, Morocco. They have yielded hundreds of exquisitely preserved specimens. Their taphonomy and associated lithology both suggest rapid, in situ burial. Here we discuss the diverse range of assemblages represented and their significance to the diversity of echinoderms in the Lower Palaeozoic. The oldest assemblage (Izegguirene Formation, lowermost Caradoc) is dominated by eocrinoids, large ophiuroids, and mitrate stylophorans associated with rare crinoids. It shows strong similarities with slightly older faunas described from the underlying Ouine-Inirne Formation (Llandeilian) in the Central Anti-Atlas. The second assemblage (lower part of the Lower Ktaoua Formation, lower-middle Caradoc) is composed of eocrinoids (Cardiocystites) and small ophiuroids (encrinasterid indet.). The third assemblage was collected in the upper part of the Lower Ktaoua Formation (lowermost Ashgill). This 'starfish' bed is dominated by ophiuroids and large solutes, associated with common diploporites and rhombiferans, and rare crinoids and mitrates. Finally, the youngest assemblage (lower part of Upper Tiouririne Formation, lower Ashgill) has yielded abundant remains of edrioasteroids and rhombiferans.
year | journal | country | edition | language |
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2006-08-07 |