Poly- and perfluoroalkyl
substances are synthetic chemicals that
are widely present in the global environment including the Arctic.
However, little is known about how these chemicals (particularly perfluoroalkyl
acids, PFAA) enter the Arctic marine system and cycle between seawater
and sea ice compartments. To evaluate this, we analyzed sea ice, snow,
melt ponds, and near-surface seawater at two ice-covered stations
located north of the Barents Sea (81 °N) with the aim of investigating
PFAA dynamics in the late-season ice pack. Sea ice showed high concentrations
of PFAA particularly at the surface with snow-ice (the uppermost sea
ice layer strongly influenced by snow) comprising 26–62% of
the total PFAA burden. Low salinities (<2.5 ppt) and low δ
18
O
H20
values (<1‰ in snow and upper ice
layers) in sea ice revealed the strong influence of meteoric water
on sea ice, thus indicating a significant atmospheric source of PFAA
with subsequent transfer down the sea ice column in meltwater. Importantly,
the under-ice seawater (0.5 m depth) displayed some of the highest
concentrations notably for the long-chain PFAA (e.g., PFOA 928 ±
617 pg L
–1
), which were ≈3-fold higher than
those of deeper water (5 m depth) and ≈2-fold higher than those
recently measured in surface waters of the North Sea infuenced by
industrial inputs of PFAAs. The evidence provided here suggests that
meltwater arising early in the melt season from snow and other surface
ice floe components drives the higher PFAA concentrations observed
in under-ice seawater, which could in turn influence the timing and
extent of PFAA exposure for organisms at the base of the marine food
web.