A brachiopod-dominated sea-floor assemblage from the Late Pliocene of the eastern Netherlands

A sea-floor assemblage from hardened sandstone boulders in which lingulid brachiopods predominate is recorded from the Oosterhout Formation near Balgoy (province of Gelderland, the Netherlands). Dinoflagellate cysts indicate a late Early-Late Pliocene (late Zanclean-Piacenzian) age of these boulders...

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Bibliographic Details
Published inGeologie en mijnbouw Vol. 92; no. 2-3; pp. 171 - 176
Main Authors Wesselingh, F.P., Peters, W.J.M., Munsterman, D.K.
Format Journal Article
LanguageEnglish
Published Cambridge, UK Cambridge University Press 01.09.2013
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Summary:A sea-floor assemblage from hardened sandstone boulders in which lingulid brachiopods predominate is recorded from the Oosterhout Formation near Balgoy (province of Gelderland, the Netherlands). Dinoflagellate cysts indicate a late Early-Late Pliocene (late Zanclean-Piacenzian) age of these boulders; the entire assemblage is indicative of clear marine waters near storm wave base along the southeastern margin of the North Sea Basin at the time. A possible commensal relationship between the lingulid brachiopods and the gastropod Calyptraea chinensis is implied.
ISSN:0016-7746
1573-9708
DOI:10.1017/S0016774600000111