Contrasting responses of DMS and DMSP to ocean acidification in Arctic waters
Increasing atmospheric CO 2 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 p CO 2 on the co...
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ftdoajarticles:oai:doaj.org/article:5bcdfebcadee46379dcb0b6279896ff4 2023-05-15T14:52:02+02:00 Contrasting responses of DMS and DMSP to ocean acidification in Arctic waters S. D. Archer S. A. Kimmance J. A. Stephens F. E. Hopkins R. G. J. Bellerby K. G. Schulz J. Piontek A. Engel 2013-03-01T00:00:00Z https://doi.org/10.5194/bg-10-1893-2013 https://doaj.org/article/5bcdfebcadee46379dcb0b6279896ff4 EN eng Copernicus Publications http://www.biogeosciences.net/10/1893/2013/bg-10-1893-2013.pdf https://doaj.org/toc/1726-4170 https://doaj.org/toc/1726-4189 doi:10.5194/bg-10-1893-2013 1726-4170 1726-4189 https://doaj.org/article/5bcdfebcadee46379dcb0b6279896ff4 Biogeosciences, Vol 10, Iss 3, Pp 1893-1908 (2013) Ecology QH540-549.5 Life QH501-531 Geology QE1-996.5 article 2013 ftdoajarticles https://doi.org/10.5194/bg-10-1893-2013 2022-12-30T22:15:44Z Increasing atmospheric CO 2 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 p CO 2 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 pH T 8.3 to 7.5, equivalent to p CO 2 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 p CO 2 , 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 p CO 2 . 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. Article in Journal/Newspaper Arctic Ocean acidification Phytoplankton Spitzbergen Directory of Open Access Journals: DOAJ Articles Arctic Biogeosciences 10 3 1893 1908 |
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Open Polar |
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Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
Ecology QH540-549.5 Life QH501-531 Geology QE1-996.5 |
spellingShingle |
Ecology QH540-549.5 Life QH501-531 Geology QE1-996.5 S. D. Archer S. A. Kimmance J. A. Stephens F. E. Hopkins R. G. J. Bellerby K. G. Schulz J. Piontek A. Engel Contrasting responses of DMS and DMSP to ocean acidification in Arctic waters |
topic_facet |
Ecology QH540-549.5 Life QH501-531 Geology QE1-996.5 |
description |
Increasing atmospheric CO 2 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 p CO 2 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 pH T 8.3 to 7.5, equivalent to p CO 2 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 p CO 2 , 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 p CO 2 . 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. |
format |
Article in Journal/Newspaper |
author |
S. D. Archer S. A. Kimmance J. A. Stephens F. E. Hopkins R. G. J. Bellerby K. G. Schulz J. Piontek A. Engel |
author_facet |
S. D. Archer S. A. Kimmance J. A. Stephens F. E. Hopkins R. G. J. Bellerby K. G. Schulz J. Piontek A. Engel |
author_sort |
S. D. Archer |
title |
Contrasting responses of DMS and DMSP to ocean acidification in Arctic waters |
title_short |
Contrasting responses of DMS and DMSP to ocean acidification in Arctic waters |
title_full |
Contrasting responses of DMS and DMSP to ocean acidification in Arctic waters |
title_fullStr |
Contrasting responses of DMS and DMSP to ocean acidification in Arctic waters |
title_full_unstemmed |
Contrasting responses of DMS and DMSP to ocean acidification in Arctic waters |
title_sort |
contrasting responses of dms and dmsp to ocean acidification in arctic waters |
publisher |
Copernicus Publications |
publishDate |
2013 |
url |
https://doi.org/10.5194/bg-10-1893-2013 https://doaj.org/article/5bcdfebcadee46379dcb0b6279896ff4 |
geographic |
Arctic |
geographic_facet |
Arctic |
genre |
Arctic Ocean acidification Phytoplankton Spitzbergen |
genre_facet |
Arctic Ocean acidification Phytoplankton Spitzbergen |
op_source |
Biogeosciences, Vol 10, Iss 3, Pp 1893-1908 (2013) |
op_relation |
http://www.biogeosciences.net/10/1893/2013/bg-10-1893-2013.pdf https://doaj.org/toc/1726-4170 https://doaj.org/toc/1726-4189 doi:10.5194/bg-10-1893-2013 1726-4170 1726-4189 https://doaj.org/article/5bcdfebcadee46379dcb0b6279896ff4 |
op_doi |
https://doi.org/10.5194/bg-10-1893-2013 |
container_title |
Biogeosciences |
container_volume |
10 |
container_issue |
3 |
container_start_page |
1893 |
op_container_end_page |
1908 |
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1766323155847086080 |