Due
to the nuclear testing in the 20th century, a considerable
amount of anthropogenic transuranic isotopes (237Np, 239, 240Pu, and 241Am) was produced, spread,
and deposited in the natural environment including Antarctica. Here,
activities of 239+240Pu, 237Np, and 241Am in Antarctic marine sediments are determined by ICP-SF-MS, ranging
from 0.008 to 0.293 Bq/kg for 239+240Pu, from 0.057 to
0.926 mBq/kg for 237Np, and from 0.027 to 0.277 Bq/kg for 241Am. The dominant source of 237Np, 239, 240Pu, and 241Am in the study marine sediments is global
fallout. 240Pu/239Pu atom ratio is measured
to be 0.179 ± 0.010 (n = 17) on average, which
is consistent with the global fallout of the nuclear weapons tests.
Average 237Np/239Pu atom ratio for global fallout
is suggested as 0.221 (n = 58), which may be used
as a new characteristic index to indicate the current source of Np
in a certain region. Due to the different fractionations of Pu and
Am by seawater and the enrichment efficiency of marine particles, 241Am/239+240Pu activity ratios in these samples
(mean, 2.037 ± 0.040; n = 17) are much higher
than global fallout. In addition, 237Np/239Pu
atom ratio and 241Am/239+240Pu activity ratio
are found to be positively correlated with the sampling depth. Furthermore,
the correlation between organic matter and eight heavy metals with
transuranic activities is revealed. The cold climate, latitude, and
sediment properties have an important influence on the distributions
of Np, Pu, and Am in these marine sediments of Antarctic.