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Stratigraphie et systématique des Rugueux de la partie moyenne du Frasnien de Frasnes-lez-Couvin (Belgique). Stratigraphy and systematic palaeontology of the rugose corals from the middle part of the Frasnian at Frasnes-lez-Couvin (Belgium)
Coen-Aubert, M (1994). Stratigraphie et systématique des Rugueux de la partie moyenne du Frasnien de Frasnes-lez-Couvin (Belgique). Stratigraphy and systematic palaeontology of the rugose corals from the middle part of the Frasnian at Frasnes-lez-Couvin (Belgium). Bull. Kon. Belg. Inst. Natuurwet. Aardwet. = Bull. - Inst. r. sci. nat. Belg., Sci. Terre 64: 21-56
In: Bulletin van het Koninklijk Belgisch Instituut voor Natuurwetenschappen. Aardwetenschappen = Bulletin de l'Institut Royal des Sciences Naturelles de Belgique. Sciences de la Terre. KBIN: Brussel. ISSN 0374-6291, more
Peer reviewed article  
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Keywords
    Geological time > Phanerozoic > Paleozoic > Palaeozoic > Devonian > Devonian, Upper
    Geological time > Phanerozoic > Paleozoic > Palaeozoic > Devonian > Devonian, Upper > Frasnian
    Anthozoa [WoRMS]; Cnidaria [WoRMS]; Hexacorallia [WoRMS]; Rugosa † [WoRMS]
    Belgium, Couvin [Marine Regions]; Belgium, Frasnes; Belgium, Viroinval [Marine Regions]
    Marine/Coastal
Author keywords
    Rugose corals, Frasnian, Taxonomy, Stratigraphy, Ardenne, Rugueux, Frasnien, Taxinomie, Stratigraphie
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  • Coen-Aubert, M, more
Abstract
    Ten species belonging to the genera Hexagonaria GÜRICH, 1896, Aristophyllum BULVANKER, SPASSKY & KRAVTSOV, 1975, Phillipsastrea D'ORBIGNY, 1849, Frechastraea SCRUTTON, 1968, Scruttonia TCHEREPNINA, 1974, Peneckiella SOSHKINA, 1939 and Trapezophyllum ETHERIDGE. 1899 including T. roharti n. sp. are described and figured. This material comes mainly from the Boussu-en-Fagne Member and the Neuville Formation exposed at Frasnes, Boussu-en-Fagne and Nismes. The geological surveys emphasize interesting lateral facies variations close to the second and third levels of Frasnian bioherms. The correlations with the Philippeville Massif are also considered. The investigated fauna shows strong affinities with that from the Boulonnais in France and the Holy Cross Mountains in Poland.
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