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.
CITATION STYLE
Wesselingh, F. P., Peters, W. J. M., & Munsterman, D. K. (2013). A brachiopod-dominated sea-floor assemblage from the Late Pliocene of the eastern Netherlands’. Geologie En Mijnbouw/Netherlands Journal of Geosciences, 92(2–3), 171–176. https://doi.org/10.1017/s0016774600000111
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