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The Pardailhan Formation has yielded, close to Villeneuve-Minervois (Minervois nappe), a new fossil assemblage composed of ellipsocephalid, redlichiid, and abadiellid trilobites (Blayacina lineata nov. sp., Eoredlichia cf. noiri, and Granolenus midi and G. jagoi nov. sp., respectively), linguliformean brachiopods, bradoriids, chancelloriid sclerites, hyoliths, sponge, spicules, ichnofossils (Astropolichnus...
The solenopleurine trilobite genera Jincella and Liosolenopleura are revised herein. The species Jincella prantli, Jincella convexa nov. sp. and Liosolenopleura serventi occur in Languedocian (upper Middle Cambrian) rocks of the southern Montagne Noire (France), southwestern Sardinia (Italy), and the Pribram-Jince and Skryje areas (Czech Republic). The correlation of their first appearances permits...
The paper presents the first description and illustration of archaeocyaths and small shelly fossils from the lower member of the Lower Cambrian Lastours Formation (southern Montagne Noire). The outcrops of the Caunes-Minervois sheet thrust (Pardailhan nappe) represent alternation of relatively low-energy, shallow subtidal substrates (highly bioturbated mottled limestones), and reef flanks or inter-reef...
This paper describes the pattern of trilobite diversity throughout the Middle Cambrian in two fossiliferous basins of the western Gondwana margin: the Iberian Chains (northeastern Spain) and the Montagne Noire (southern France). The documented fluctuations of species diversity allow us to recognize: (1) a substantial extinction event recorded in latest Early Cambrian times (named Valdemiedes event),...
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