| one publication added to basket [223637] | 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, more
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| Keywords |
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]
Belgium, Couvin [Marine Regions]; Belgium, Viroinval [Marine Regions]
Marine/Coastal |
| Authors | | Top |
- Helsen, S.
- Bultynck, P., more
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| 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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