S65142B
Greater North Sea Sweden
Geological Time: Quaternary Holocene recent
the specimen was picked and photographed with the Vega3 Tescan SEM of Senckenberg am Meer by Michael Hesemann, the raw material was provided and the identification was done by Dr.
with attached diatoms
The identification is based upon:
, : Weiss, L. (1954). Foraminifera and origin of the Gardiners clay (Pleistocene), eastern Long Island, New York. United States Geological Survey Professional Papers. 254- G: 143-163. Plate , Fig.