the greatest likelihood of the presence of plutonium.

The

values given in Table 14, therefore, probably are maximum values
for each type of sample.

The ratios of

239,240

Pu

238

to

Pu.

approach 2:1 at Eniman I. and are about 15:1 in Bravo Crater.
Bikini I.

soils contained no detectable 2385

although they

.
.
.
239,240
contained the highest concentration of
Pu of the samples
analyzed.

The presence of 239,240, and 20755 in goatfish viscera

is consistent and probably results
:

.

._.

from direct ingestion of fine

.

particles of sediment during feeding.

The absence of

238

~—

.

Pu in

goatfish viscera as compared with the sediment merely reflects
a low concentration of this radionuclide,

below the

limits of

detection.

Although none of the 1969 samples were analyzed for the
X-ray emitter 6345,

this radionuclide was found in concentrations

of 80 d/m/g dry weight in Bravo Crater sediment collected in
1967

(Beasley and Held,

1969).

Nickel-63 is of particular interest

as a tracer since it has a half-life of 92 years.
.

the clam kidney accumulates

63__,

Ni,

'

as it does

60

r organism for the presence of
fore an indicato

Another long-lived radionuclide,

108m

Ag,

Co,

In addition,
:

and is there-

cegy
fier
stor
meiantn’sof OfEn
tnrt
63 Ni. Depa

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with a half-life

of approximately 100 years, has been identified for the first
time among the radionuclides at Bikini.

This radionuclide was

detected from the gamma-ray spectrum of the hepatopancreas of

9001392

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