Station 14910-2 (535m depth)
off West Africa Mauritania
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
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.
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