found at the cliffs of
Stohl North European Plain Germany
Geological Time: Paleogene Paleocene Selandian
Kerteminde Marl
the raw material was collected together with Stefan Polkowsky.
It was then cracked and forams picked and imaged by
glacial erratic rock
The identification is based upon:
Cushman, J., A., 1935: Upper Eocene foraminifera from the Southeastern United States Professional Papers U.S. Geological Survey, 181 Plate 5, Fig.
Main
Key to Species
About
Contact
