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Les Ostracodes de la partie supérieure de la formation de Teferguenite (Givétien) et de la formation de Marhouma (Givétien - Famennien) de la coupe du km 30 (Saoura, Sahara Algérien)
Casier, J.-G. (1985). Les Ostracodes de la partie supérieure de la formation de Teferguenite (Givétien) et de la formation de Marhouma (Givétien - Famennien) de la coupe du km 30 (Saoura, Sahara Algérien). Géobios 18(6): 833-846, 4 planches. dx.doi.org/10.1016/S0016-6995(85)80038-3
In: Géobios. Association Européenne de Paléontologie: Lyon. ISSN 0016-6995; e-ISSN 1777-5728, more
Peer reviewed article  

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Keywords
    Geological time > Phanerozoic > Paleozoic > Palaeozoic > Devonian > Devonian, Middle > Givetian
    Geological time > Phanerozoic > Paleozoic > Palaeozoic > Devonian > Devonian, Upper > Frasnian
    Ostracoda [WoRMS]
    Algeria [Marine Regions]
    Marine/Coastal
Author keywords
    Ostracods; New Metacopida (Tubulibairdia); Givetian; Frasnian; Famennian; Algerian Sahara; Biostratigraphy; Faunal Compositions; Paleoecology

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  • Casier, J.-G.

Abstract
    More than fifty ostracod species, twenty-two of which are Entomozoacea, have been identified in the upper part of the Teferguenite Formation and in the Marhouma Formation. The zonal sequence established on the Entomozoacea is applicable to the Frasnian and the Famennian of the Algerian Sahara; seven zones are recognized. One new species, Tubulibairdia marhoumaensis nov. sp., is described.

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