IMIS

Publications | Institutes | Persons | Datasets | Projects | Maps
[ report an error in this record ]basket (0): add | show Print this page

Algues Givetiennes du bord sud du bassin de Dinant et des régions limitrophes
Mamet, B.; Preat, A. (1986). Algues Givetiennes du bord sud du bassin de Dinant et des régions limitrophes. Ann. Soc. Géol. Belg. (1968) 109(2): 431-454
In: Annales de la Société géologique de Belgique. Vaillant-Carmanne: Liège. ISSN 0037-9395, more
Peer reviewed article  

Available in  Authors 

Keywords
    Geological time > Phanerozoic > Paleozoic > Palaeozoic > Devonian > Devonian, Middle > Givetian
    Algae
    Belgium, Wallonia [Marine Regions]
    Marine/Coastal

Authors  Top 

Abstract
    The carbonate sedimentation of the Dinant Synclinorium givetian platform is controlled by moderate but steady subsidence. More than four hundred meters of shallow-water limestones were accumulated. Most of these are semi-restricted to restricted and are the lateral equivalents of bioconstructions. Carbonate production, mainly in the lagoons, is linked to algal proliferation. Forty-six genera are recognized among spongiostromids, porostromids. codiaceans, udoteaceans, phylloids?, dasyclads, solenoporids, coccoids, charophytes, umbellinids, calcispheres and incertae sedis. Bevocastria is the most prolific alga. Carbonate build-ups are erected by phylloids?, giant dasyclads and Sphaerocodium. The widespread occurrence of rudstone sheets is due to the scarcity of stabilizing solenoporids.

All data in the Integrated Marine Information System (IMIS) is subject to the VLIZ privacy policy Top | Authors