Synthesis of iron fertilization experiments: From the Iron Age in the Age of Enlightenment
University of Groningen · Royal Netherlands Institute for Sea Research · +26 more institutions
Abstract
Comparison of eight iron experiments shows that maximum Chl a , the maximum DIC removal, and the overall DIC/Fe efficiency all scale inversely with depth of the wind mixed layer (WML) defining the light environment. Moreover, lateral patch dilution, sea surface irradiance, temperature, and grazing play additional roles. The Southern Ocean experiments were most influenced by very deep WMLs. In contrast, light conditions were most favorable during SEEDS and SERIES as well as during IronEx‐2. The two extreme experiments, EisenEx and SEEDS, can be linked via EisenEx bottle incubations with shallower simulated WML depth. Large diatoms always benefit the most from Fe addition, where a remarkably small group of…
Citation impact
- FWCI
- 52.91
- Percentile
- 100%
- References
- 125
Authors
34- HJH. J. W. de BaarCorresponding
University of Groningen, Royal Netherlands Institute for Sea Research
- PWPhilip W. Boyd
National Institute of Water and Atmospheric Research, University of Otago
- KHKenneth H. Coale
Moss Landing Marine Laboratories
- MRMichael R. Landry
Scripps Institution of Oceanography, University of California San Diego
- ATAtsushi Tsuda
The University of Tokyo
Topics & keywords
- Dissolved organic carbon
- Diatom
- Seawater
- Mixed layer
- Iron fertilization
- Chlorophyll a
- Phytoplankton
- Oceanography
- Life below water