WOLFGANG KUHNT. Benthic foraminiferal assemblages from eight clay-layers within a relatively thick section of the lowermost Paleocene (planktonic foraminifera P0 Zone) at the Geulhemmerberg, SE Netherlands, were examined for changes in abundance and species composition. . Netherlands Journal of Geosciences, v. 75, p. 163-172, 1 Jan. 1996.