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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Published in:Biogeosciences
Main Authors: S. D. Archer, S. A. Kimmance, J. A. Stephens, F. E. Hopkins, R. G. J. Bellerby, K. G. Schulz, J. Piontek, A. Engel
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2013
Subjects:
Online Access:https://doi.org/10.5194/bg-10-1893-2013
https://doaj.org/article/5bcdfebcadee46379dcb0b6279896ff4
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spelling 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
institution Open Polar
collection 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
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