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Biogeosciences, 10, 1893-1908, 2013
www.biogeosciences.net/10/1893/2013/
doi:10.5194/bg-10-1893-2013
© Author(s) 2013. This work is distributed
under the Creative Commons Attribution 3.0 License.
Contrasting responses of DMS and DMSP to ocean acidification in Arctic waters
S. D. Archer1,2, S. A. Kimmance1, J. A. Stephens1, F. E. Hopkins1, R. G. J. Bellerby3,4,5, K. G. Schulz6, J. Piontek6,7, and A. Engel6
1Plymouth Marine Laboratory, The Hoe, Plymouth, PL1 3DH, UK
2Bigelow Laboratory for Ocean Science, Maine 04575-0475, USA
3Norwegian Institute for Water Research, Bergen, Norway
4Bjerknes Centre for Climate Research, University of Bergen, Norway
5Geophysical Institute, University of Bergen, Bergen, Norway
6GEOMAR, Helmholtz Centre for Ocean Research, 24015 Kiel, Germany
7Alfred Wegener Institute, 27570 Bremerhaven, Germany

Abstract. Increasing atmospheric CO2 is decreasing ocean pH most rapidly in colder regions such as the Arctic. As a component of the EPOCA (European Project on Ocean Acidification) pelagic mesocosm experiment off Spitzbergen in 2010, we examined the consequences of decreased pH and increased pCO2 on the concentrations of dimethylsulphide (DMS). DMS is an important reactant and contributor to aerosol formation and growth in the Arctic troposphere. In the nine mesocosms with initial pHT 8.3 to 7.5, equivalent to pCO2 of 180 to 1420 μatm, highly significant but inverse responses to acidity (hydrogen ion concentration [H+]) occurred following nutrient addition. Compared to ambient [H+], average concentrations of DMS during the mid-phase of the 30 d experiment, when the influence of altered acidity was unambiguous, were reduced by approximately 60% at the highest [H+] and by 35% at [H+] equivalent to 750 μatm pCO2, as projected for 2100. In contrast, concentrations of dimethylsulphoniopropionate (DMSP), the precursor of DMS, were elevated by approximately 50% at the highest [H+] and by 30% at [H+] corresponding to 750 μatm pCO2. Measurements of the specific rate of synthesis of DMSP by phytoplankton indicate increased production at high [H+], in parallel to rates of inorganic carbon fixation. The elevated DMSP production at high [H+] was largely a consequence of increased dinoflagellate biomass and in particular, the increased abundance of the species Heterocapsa rotundata. We discuss both phytoplankton and bacterial processes that may explain the reduced ratios of DMS:DMSPt (total dimethylsulphoniopropionate) at higher [H+]. The experimental design of eight treatment levels provides comparatively robust empirical relationships of DMS and DMSP concentration, DMSP production and dinoflagellate biomass versus [H+] in Arctic waters.

Citation: Archer, S. D., Kimmance, S. A., Stephens, J. A., Hopkins, F. E., Bellerby, R. G. J., Schulz, K. G., Piontek, J., and Engel, A.: Contrasting responses of DMS and DMSP to ocean acidification in Arctic waters, Biogeosciences, 10, 1893-1908, doi:10.5194/bg-10-1893-2013, 2013.
 
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