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- W2894213435 abstract "Abstract The Khabt-el-Hajar Formation, very rich in bryozoans and echinoderms but relatively poor in other fossil groups, has provided a brachiopod association that allows an improvement in the stratigraphic correlation of this Moroccan eastern Anti-Atlas unit with those from the Upper Ordovician of SW Europe and the rest of the Anti-Atlas. The intermediate marly beds, with bryozoan and echinoderm patches, of the Khabt-el-Hajar Formation have yielded Streptis ? sp., Paucicrura catalanica and Drabovia sp. Of these, P. catalanica , the richest in the association and known up to now exclusively from the Catalonian Coastal Ranges in NE Spain, is dated as mid to late Katian (Ka2–Ka4), since it occurs in the La Mora Slates, correlatable with horizons of that age from Iberia, Sardinia or the Montagne Noire. The analysis of the stratigraphic and palaeobiogeographical ranges of the bryozoans from the same formation agrees with the correlation above. The quartzitic sandstones that underlie the Khabt-el-Hajar Formation in the surroundings of Erfoud have yielded a different brachiopod association, including Kiaeromena ? chouberti and Rostricellula termieri among other forms more poorly represented. K. ? chouberti allows its yielding horizon to be dated as mid Katian (Ka2) and supports the identification of the sandstone-dominated unit where it occurs as the Tiouririne Formation." @default.
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- W2894213435 date "2018-09-24" @default.
- W2894213435 modified "2023-10-14" @default.
- W2894213435 title "Brachiopods from the Upper Ordovician of Erfoud (eastern Anti-Atlas, Morocco) and the stratigraphic correlation of the bryozoan-rich Khabt-el Hajar Formation" @default.
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- W2894213435 doi "https://doi.org/10.1144/sp485.2" @default.
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