Winter advection of iron can explain the summer phytoplankton bloom that extends 1000 km downstream of the Kerguelen Plateau in the Southern Ocean

Mongin, M., Abraham, E., & Trull, T. (2009). Winter advection of iron can explain the summer phytoplankton bloom that extends 1000 km downstream of the Kerguelen Plateau in the Southern Ocean. Journal of Marine Research, 67, 225–237. doi:10.1357/002224009789051218