OCEANS:
Dis-Crediting Ocean Fertilization
Sallie W. Chisholm,* Paul G. Falkowski, John J. Cullen
Episodic phytoplankton blooms are part of the natural cycle of production and regeneration in ocean ecosystems. There is growing interest in using iron fertilization to produce massive phytoplankton blooms in parts of the ocean where they do not now occur. The goal is to transfer carbon from the atmosphere to the deep sea (see also the Perspective by Seibel and Walsh in this issue of Science) and trade it in the emerging carbon credit market. In their Policy Forum, Chisholm, Falkowski, and Cullen warn that iron fertilization would be extremely difficult to validate and would significantly alter oceanic food webs and biogeochemical cycles.
S. W. Chisholm is in the Department of Civil and Environmental Engineering, MIT, Cambridge, MA 02139, USA. P. Falkowski is in the Department of Geology, Rutgers University, New Brunswick, NJ 08901, USA. J. J. Cullen is in the Department of Oceanography, Dalhousie University, Halifax, NS B3H 4J1, Canada.
*To whom correspondence should be addressed. E-mail: chisholm{at}mit.edu