In the late 1980's, the late John Martin advanced the idea that carbon uptake during plankton photosynthesis in many regions of the world's surface ocean was limited not by light or the major nutrients nitrogen and phosphorus, but rather by a lack of the trace metal iron. Correlations between dust input to the ocean (which is the major source of iron) and past climate changes and CO2 levels, led Martin's to exclaim "Give me half a tanker of iron and I'll give you the next ice age". Over the past decade, scientists have been looking at the ocean iron cycle in more detail to better understand these links. At the same time, in light of increasing greenhouse gas CO2, there has been commercial interest in fertilizing the ocean with iron as a possible mitigation strategy to reduce atmospheric CO2. Our group has been focused on the export of C, or flux of sinking particles that would be associated with waters either artificially enriched with iron, or such as might be found naturally in association with dust inputs or for example in melt waters surrounding Antarctica.
Charette, M. A. and K. O. Buesseler (2000). Does iron fertilization lead to rapid carbon export in the Southern Ocean? Geochemistry, Geophysics, Geosystems, 1, Paper 2000GC000069.
Buesseler, K.O., Boyd, P. W., (2003), Will Ocean Fertilization Work? Science, 300, 67-68. (Article available online: see reference #77).
Buesseler,
K.O., J.E. Andrews, S.M. Pike and M.A. Charette (2004). The effects of iron fertilization
on carbon sequestration in the Southern Ocean. Science, 304: 414-417.
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