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Late campanian belemnite faunas from Liège - Limburg (Ne Belgium, se Netherlands)
Keutgen, N; Jagt, J.W.M. (1998). Late campanian belemnite faunas from Liège - Limburg (Ne Belgium, se Netherlands). Professional Paper. Geological Survey of Belgium, 1998/02(287). Geologische Dienst van België: Brussel. 32 pp., 9 figs., 8 tab., 1 pl. pp.
Deel van: Professional Paper. Geological Survey of Belgium. Belgische Geologische Dienst: Brussel. ISSN 0378-0902, meer
Peer reviewed article  
Beschikbaar in  Auteurs 
Documenttype: Wetenschappelijk rapport
Trefwoorden
    British Isles, England, Norfolk
    Geological time > Phanerozoic > Geological time > Mesozoic > Cretaceous > Cretaceous, Upper > Campanian
    Germany, Schleswig-Holstein
    Netherlands, Limburg (Province)
    Ammonoida † [WoRMS]; Asterozoa [WoRMS]; Coleoidea [WoRMS]; Crinoidea [WoRMS]; Echinoidea [WoRMS]
    Limburg [Marine Regions]; Luik (Provincie) [Marine Regions]; Norfolk [Marine Regions]; Schleswig-Holstein [Marine Regions]
    Marien/Kust
Author keywords
    Cretaceous, Campanian, belemnites, paleontology, taxonomy, stratigraphie correlations, Belgium, The Netherlands
Auteurs  Top 
  • Keutgen, N
  • Jagt, J.W.M.
Abstract
    Late Campanian belemnite faunas from the Zeven Wegen and Beutenaken members of the Gulpen Formation in Liège-Limburg (NE Belgium, SE Netherlands) include five (sub)species of the genus Belemnitella d'Orbigny, 1840, viz. B. mucronata (von Schlottheim, 1813), B. woodi Christensen, 1995, B. minor I Jeletzky, 1951, B. minor II Christensen, 1995 and B. najdini Kongiel, 1962, which are described herein. CHRISTENSEN’S (1995, 1996) concept of B. minor is followed, with respect to the holotype. On the basis of these belemnite data more detailed zonal subdivisions of the Zeven Wegen and Beutenaken members are proposed. These allow correlations to be made with Late Campanian strata in Norfolk (SE England) and at Lägerdorf-Kronsmoor (NW Germany). Key taxa amongst echinoids, crinoids, asteroids and ammonites from the Zeven Wegen and Beutenaken members corroborate zonations and correlations based on belemnites.
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