Skip to main content
Publications | Persons | Institutes | Projects
[ report an error in this record ]basket (1): add | show Print this page

one publication added to basket [221953]
Warnantian
Poty, E.; Hance, L. (2006). Warnantian. Geol. Belg. 9(1-2): 139-144
In: Geologica Belgica. Geologica Belgica: Brussels . ISSN 1374-8505; e-ISSN 2034-1954, more
Peer reviewed article  

Available in  Authors 

Keywords
    Geological time > Phanerozoic > Paleozoic > Palaeozoic > Carboniferous > Mississippian, Middle > Visean
    Anthozoa [WoRMS]; Foraminifera [WoRMS]
    Belgium, Anhée [Marine Regions]
    Marine/Coastal
Author keywords
    Warnantian, Viséan, Carboniferous, Belgium, lithostratigraphy, biostratigraphy, palaeogeography

Authors  Top 
  • Poty, E., more
  • Hance, L.

Abstract
    The Warnantian Substage is about 8 to 12 Ma long and was defined as corresponding to the Cf6 Foraminifer Zone by Conil et al., 1977 (= MFZ13 to MFZ15 Zones of Devuyst & Hance (in Poty et al., in press). Its base is taken at the base of the Bonne River Formation (Fm); its top is defined by the base of the Namurian stage, but its upper part is almost completely missing in the Namur-Dinant Basin. The substage is covered by the RC7 and RC8 Coral Zones. It comprises the Bonne River and the Anhée Fms, which are mainly composed of shallowing-upward parasequences which were deposited by aggradation on the shelf, as suggested by their lateral regularity. It corresponds to the HST of the third-order sequence 8 (Thon-Samson Member of the Bonne River Fm) and to the third-order sequences 9 and 10 (Hance et al., 2001; Poty et al., 2002). The lower (MFZ13-MFZ14, RC7) and the upper Warnantian (MFZ15, RC8) can be correlated respectively with the British Asbian and Brigantian Substages.

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