found in waters off
Sitka
Crawfish Inlet, from about 21m waterdepth
Pacific off Alaska USA
Geological Time: Quaternary Holocene recent
the specimen is photographed with the SEM VEGA3 TESCAN at Senckenberg am Meer by
Michael Hesemann and collected by
detail of wall
The identification is based upon:
, : Cushman, J.A. (1925). Recent Foraminifera from British Columbia. Contr. Cushman Lab. Foram. Res. 1: 38-47. Plate , Fig.