Physics
Scientific paper
May 1999
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1999georl..26.1477a&link_type=abstract
Geophysical Research Letters, Volume 26, Issue 10, p. 1477-1480
Physics
10
Global Change: Remote Sensing, Oceanography: Physical: Air/Sea Interactions, Oceanography: General: Diurnal, Seasonal, And Annual Cycles
Scientific paper
While anthropogenic emissions have dramatically elevated lead concentrations in the North Atlantic troposphere and surface waters by orders of magnitude above natural levels [Murozumi et al., 1969; Schaule and Patterson, 1983; Boyle et al., 1986], it has been assumed that the relatively low lead levels in North Atlantic abyssal waters are not yet contaminated [Schaule and Patterson, 1981; Flegal and Patterson, 1983]. That misperception is redressed by the following stable lead isotopic composition data which reveal the advective transport of industrial lead into those deep basin waters through the formation of North Atlantic Deep Water (NADW). Additionally, spatial gradients in the isotopic signatures of anthropogenic lead within the North Atlantic abyss appear to serve as transient tracers of contaminant penetration rates.
Alleman Laurent Y.
Church Thomas M.
Flegal Russell A.
Hamelin Bernard
Veron A. J.
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