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Conodonts and megafauna from two sections at Nismes and Mariembourg (Frasnian of the Southern Flank of the Dinant Synclinorium, Belgium)
Helsen, S.; Bultynck, P. (1992). Conodonts and megafauna from two sections at Nismes and Mariembourg (Frasnian of the Southern Flank of the Dinant Synclinorium, Belgium). Ann. Soc. géol. Belg. (1968) 115(1): 145-157
In: Annales de la Société géologique de Belgique. Vaillant-Carmanne: Liège. ISSN 0037-9395
Peer reviewed article  
Beschikbaar in  Auteurs 
Trefwoorden
    Geological time > Phanerozoic > Paleozoic > Palaeozoic > Devonian
    Geological time > Phanerozoic > Paleozoic > Palaeozoic > Devonian > Devonian, Upper
    Geological time > Phanerozoic > Paleozoic > Palaeozoic > Devonian > Devonian, Upper > Frasnian
    Anthozoa [WoRMS]; Bivalvia [WoRMS]; Brachiopoda [WoRMS]; Bryozoa [WoRMS]; Cephalopoda [WoRMS]; Conodonta; Echinodermata [WoRMS]; Gastropoda [WoRMS]
    Couvin [Marine Regions]; Viroinval [Marine Regions]
    Marien/Kust
Auteurs  Top 
  • Helsen, S.
  • Bultynck, P.
Abstract
    Both conodonts and megafaunal associations have been examined from two Frasnian sections at Nismes and Mariembourg (Dinant Synclinorium, Belgium). The recognition of the Late hassi?, the jamieae, and the Early rhenana Conodont Zones (= Ancyrognathus triangularis (Ziegler, 1962) and Lower Palmatolepis gigas Zones (Ziegler, 1971)) makes it possible to situate both sections in the middle and upper part of the Frasnian. From the base towards the top of the Nismes section there is a deepening of the environment. This can be documented by the conodont biofacies, the megafaunal associations and some lithological characteristics.
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