tt ME Bete Ek 2 sheila! Salibaile wn sete, et ABSTRACT Radiochemical separations were made on plankton samples collected in and west of the Eniwetok Proving Ground in Sep- tember 1956. Ion exchange resin column and precipitation technicues were used. Fisston products, mainly Zr?9-Nb25 and Cel44-prl44, contributed an average of 29 per cent of the total radioactivity. The remaining 71 per cent of the activity was contributed by the non-fission radioisotopes zn©5, Co57,58,60, Fe55 and Mn?+, Radioactive zinc, cobalt, and tron accounted for averages of 24, 26 and 21 per cent respectively of the total radioactivity. in trace amounts. Variations Mn>4 was present in ratio of occurrence for the different non-fission products with change in geographi- cal location was observed. Relatively high levels of gn©5 were centered in the area near Bikini and Eniwetok Atolls. The area of high levels of radioactive cobalt and iron in comparison to gn©5 was located approximately 480 miles west and slightly north of Eniwetok Atoll.

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