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Ocean Acidification and Marine Trace Gas Emissions
Frances E. Hopkins, Suzanne M. Turner, Philip D. Nightingale, Michael Steinke, Dorothee Bakker, Peter S. Liss and Michael L. Bender
Proceedings of the National Academy of Sciences of the United States of America
Vol. 107, No. 2 (Jan. 12, 2010), pp. 760-765
Published by: National Academy of Sciences
Stable URL: http://www.jstor.org/stable/40535844
Page Count: 6
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The oceanic uptake of man-made CO₂ emissions is resulting in a measureable decrease in the pH of the surface oceans, a process which is predicted to have severe consequences for marine biological and biogeochemical processes [Caldeira K, Wickett ME (2003) Nature 425: 365; The Royal Society (2005) Policy Document 12/05 (Royal Society, London)]. Here, we describe results showing how a doubling of current atmospheric CO₂ affects the production of a suite of atmospherically important marine trace gases, Two CO₂ treatments were used during a mesocosm CO₂ perturbation experiment in a Norwegian fjord (present day:~380 ppmv and year 2100:~750 ppmv), and phytoplankton blooms were stimulated by the addition of nutrients. Seawater trace gas concentrations were monitored over the growth and decline of the blooms, revealing that concentrations of methyl iodide and dimethylsulfide were significantly reduced under high CO₂. Additionally, large reductions in concentrations of other iodocarbons were observed. The response of bromocarbons to high CO₂ was less clear cut. Further research is now required to understand how ocean acidification might impact on global marine trace gas fluxes and how these impacts might feed through to changes in the earth's future climate and atmospheric chemistry.
Proceedings of the National Academy of Sciences of the United States of America © 2010 National Academy of Sciences