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Santonian - Campanian (Upper Cretaceous) inoceramids from the Houthalen mineshaft, NE Belgium
Walaszczyk, I.; Dhondt, A.V. (2005). Santonian - Campanian (Upper Cretaceous) inoceramids from the Houthalen mineshaft, NE Belgium. Bull. Kon. Belg. Inst. Natuurwet. Aardwet. = Bull. - Inst. r. sci. nat. Belg., Sci. Terre 75: 167-181
In: Bulletin van het Koninklijk Belgisch Instituut voor Natuurwetenschappen. Aardwetenschappen = Bulletin de l'Institut Royal des Sciences Naturelles de Belgique. Sciences de la Terre. KBIN: Brussel. ISSN 0374-6291, meer
Peer reviewed article  
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Trefwoorden
    Geological time > Phanerozoic > Geological time > Mesozoic > Cretaceous > Cretaceous, Upper > Campanian
    Geological time > Phanerozoic > Geological time > Mesozoic > Cretaceous > Cretaceous, Upper > Santonian
    Bivalvia [WoRMS]; Inoceramidae Giebel, 1852 † [WoRMS]
    Belgium, Houthalen
    Marien/Kust
Author keywords
    Inoceramids, Santonian, Campanian, biostratigraphy, Inoceramid zonation
Auteurs  Top 
  • Walaszczyk, I.
  • Dhondt, A.V.
Abstract
    The Santonian and Campanian inoceramids from the Houthalen mineshaft (Limburg, NE Belgium) are described. Four successive faunas were distinguished: the Sphenoceramus pachti fauna, dated for the Middle Santonian, the Sphenoceramus patootensiformis fauna, of the upper Upper Santonian - lower Lower Campanian, the Cordiceramus paraheberti fauna, possibly of the upper Lower Campanian, and the "Inoceramus" tenuilineatus fauna, characteristic for the middle Upper Campanian. The appearance of the latter fauna marks one of the main turnover events in the evolution of the Campanian inoceramids.
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