found in the Gardiner Clays on Long Island
East Coast USA
Geological Time: Quaternary Pleistocene
holotype
View of a specimen of Cribroelphidium albiumbilicatum (Weiss, 1954)
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.
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