Abstract
Investigations into Fe(II) cycling during two Southern Ocean mesoscale iron enrichment experiments, SOFeX and EIFeX, clearly show the importance of Fe(II) to iron speciation during these experiments. In both cases the added Fe(II) persisted significantly longer than its expected oxidation time indicating a significant Fe reduction process at work. During EIFeX diel studies showed a strong photochemically induced cycle in Fe(II) production in sunlit surface waters. Our results suggest that the photochemical cycling of iron may also be important in unfertilized waters of the Southern Ocean.
| Original language | English |
|---|---|
| Article number | L19606 |
| Journal | Geophysical Research Letters |
| Volume | 35 |
| Issue number | 19 |
| DOIs | |
| Publication status | Published - 16 Oct 2008 |
| Externally published | Yes |