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Particle export during the Southern Ocean Iron Experiment (SOFeX)
Author(s) -
Buesseler K. O.,
Andrews J. E.,
Pike S. M.,
Charette M. A.,
Goldson L. E.,
Brzezinski M. A.,
Lance V. P.
Publication year - 2005
Publication title -
limnology and oceanography
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.7
H-Index - 197
eISSN - 1939-5590
pISSN - 0024-3590
DOI - 10.4319/lo.2005.50.1.0311
Subject(s) - flux (metallurgy) , iron fertilization , oceanography , environmental science , mixed layer , latitude , particle (ecology) , particulates , silicate , polar front , atmospheric sciences , biogenic silica , geology , chemistry , phytoplankton , nutrient , diatom , organic chemistry , geodesy
We studied the effect of iron addition on particle export in the Southern Ocean by measuring changes in the distribution of thorium‐234 during a 4‐week iron (Fe) enrichment experiment conducted in the high‐silicate highnitrate waters just south of the Southern Antarctic Circumpolar Current Front at 172.5°W. Decreases in 234 Th activity with time in the fertilized mixed layer (0–50 m) exceeded those in unfertilized waters, indicating enhanced export of 234 Th on sinking particles after Fe enrichment. The addition of Fe also affected export below the fertilized patch by increasing the efficiency of particle export through the 100‐m depth horizon. Extensive temporal and vertical Lagrangian sampling allowed us to make a detailed examination of the 234 Th flux model, which was used to quantify the fluxes of particulate organic carbon (POC) and biogenic silica (bSiO 2 ). Iron addition increased the flux of both POC and bSiO 2 out of the mixed layer by about 300%. The flux at 100 m increased by more than 700% and 600% for POC and bSiO 2 , respectively. The absolute magnitude of the POC and bSiO 2 fluxes were not large relative to natural blooms at these latitudes or to those found in association with the termination of blooms in other ocean regions. Our results support the hypothesis that Fe addition leads directly to significant particle export and sequestration of C in the deep ocean. This is a key link between ocean Fe inputs and past changes in atmospheric CO 2 and climate.