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Microfossiles a paroi organique de l'ypresien inferieur a quenast
De Coninck, J (1986). Microfossiles a paroi organique de l'ypresien inferieur a quenast. Professional Paper. Geological Survey of Belgium, 1986/01(224). Geologische Dienst van België: Brussel. 59 pp., 3 figs., 2 tab., 5 pl. pp.
Part of: Professional Paper. Geological Survey of Belgium. Koninklijk Belgisch Instituut voor Natuurwetenschappen. Belgische Geologische Dienst: Bruxelles. ISSN 0378-0902, more
Peer reviewed article  

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Document type: Scientific report

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  • De Coninck, J, more

Abstract
    Twohundred and fortyeight species of organic walled micro- fossils, with among them seven new species, were found in the Sands of Oostende-ter-Streep, the Clay of leper, the Sands of Mons-en-Pevele and the Clay of Merelbeke in the Belgian basin. The assemblages of the marine Ypresian deposits are rich and totally different from the very poor assemblages of the lagunar Landenian deposits. About one fourth of the species have been found, each of them, in a limited part of the sequence. Their distribution allows us to correlate Ypresian deposits of several localities in the Belgian basin with those from the reference profile of Kallo with a precision of about five to ten metres.

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