Station 869
Greater North Sea none
Geological Time: Quaternary Holocene recent
the washed raw material from which the forams are picked is provided by Dr.
lateral and apertural view, aperture not visible
The identification is based upon:
Gabel, B., 1971: Die Foraminiferen der Nordsee. Helgoländer wissenschaftliche Meeresuntersuchungen. 22.
65 pp. Plate 4, Fig. 31,32