Hg has been measured using ultraclean procedures in snow deposited in
central Greenland from 1949 to 1989. Concentrations range from less th
an or equal to 0.05 to 2.0 pg/g (mean : 0.43 pg/g), i.e. values which
are orders of magnitude lower than those obtained in earlier studies.
It indicates that earlier data were plagued by major contamination pro
blems. Combined estimated contributions from natural Hg sources cannot
explain Hg concentrations observed in the snow. It suggests that Hg d
eposition to the Greenland ice sheet is now significantly influenced b
y anthropogenic inputs from North America, Asia and Europe linked espe
cially to coal burning and solid waste incineration. Although our data
suggest that Hg concentrations were higher in snow dated from the lat
e 1940s to the mid 1960s than in more recent snow, further studies are
needed to clearly assess Hg temporal trends.