Abstract. Glacial meltwater from the western Antarctic Ice Sheet is
hypothesized to be an important source of cryospheric iron, fertilizing the
Southern Ocean, yet its trace-metal composition and factors that control its
dispersal remain poorly constrained. Here we characterize meltwater iron
sources in a heavily glaciated western Antarctic Peninsula (WAP) fjord.
Using dissolved and particulate ratios of manganese to iron in meltwaters,
porewaters, and seawater, we show that surface glacial melt and subglacial
plumes contribute to the seasonal cycle of iron and manganese within a fjord
still relatively unaffected by climate-change-induced glacial retreat.
Organic ligands derived from the phytoplankton bloom and the glaciers bind
dissolved iron and facilitate the solubilization of particulate iron
downstream. Using a numerical model, we show that buoyant plumes generated
by outflow from the subglacial hydrologic system, enriched in labile
particulate trace metals derived from a chemically modified crustal source,
can supply iron to the fjord euphotic zone through vertical mixing. We also show that
prolonged katabatic wind events enhance export of meltwater out of the
fjord. Thus, we identify an important atmosphere–ice–ocean coupling
intimately tied to coastal iron biogeochemistry and primary productivity
along the WAP.