off West Africa Mauritania
Station 14910-2 (535m depth)
Geological Time: Quaternary Holocene recent
the washed raw material from which the forams are picked is provided by
visiting researcher at Senckenberg am Meer,
Abteilung Meeresforschung, Wilhelmshaven
View of a specimen of Unknown sp.
not identifiable, possibly Turborotalita
sp. (remark by M. Kucera
The identification is based upon:
Schiebel, R., Hemleben, C., 2017: Planktic Foraminifers in the Modern Ocean Plate , Fig.