Contrasting responses of DMS and DMSP to ocean acidification in Arctic waters

Increasing atmospheric CO2 is decreasing ocean pH most rapidly in colder regions such as the Arctic. As a component of the EPOCA pelagic mesocosm experiment off Spitzbergen in 2010, we examined the consequences of decreased pH and increased pCO2 on the concentrations of dimethylsulphide (DMS). DMS i...

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Published in:Biogeosciences
Main Authors: Archer, S D, Kimmance, S A, Stephens, J A, Hopkins, F E, Bellerby, R GJ, Schulz, Kai G, Piontek, J, Engel, A
Format: Article in Journal/Newspaper
Language:unknown
Published: ePublications@SCU 2012
Subjects:
Online Access:https://epubs.scu.edu.au/esm_pubs/1686
https://doi.org/10.5194/bg-10-1893-2013
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spelling ftsoutherncu:oai:epubs.scu.edu.au:esm_pubs-2699 2023-05-15T14:51:08+02:00 Contrasting responses of DMS and DMSP to ocean acidification in Arctic waters Archer, S D Kimmance, S A Stephens, J A Hopkins, F E Bellerby, R GJ Schulz, Kai G Piontek, J Engel, A 2012-01-01T08:00:00Z https://epubs.scu.edu.au/esm_pubs/1686 https://doi.org/10.5194/bg-10-1893-2013 unknown ePublications@SCU School of Environment, Science and Engineering Papers Environmental Sciences article 2012 ftsoutherncu https://doi.org/10.5194/bg-10-1893-2013 2019-08-06T12:52:07Z Increasing atmospheric CO2 is decreasing ocean pH most rapidly in colder regions such as the Arctic. As a component of the EPOCA 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 pH 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 most representative phase of the 30 d experiment were reduced by approximately 60% at the highest [H+] and by 35% at [H+] equivalent to 750 μatm pCO2, as predicted 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 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 Southern Cross University: epublications@SCU Arctic Biogeosciences 10 3 1893 1908
institution Open Polar
collection Southern Cross University: epublications@SCU
op_collection_id ftsoutherncu
language unknown
topic Environmental Sciences
spellingShingle Environmental Sciences
Archer, S D
Kimmance, S A
Stephens, J A
Hopkins, F E
Bellerby, R GJ
Schulz, Kai G
Piontek, J
Engel, A
Contrasting responses of DMS and DMSP to ocean acidification in Arctic waters
topic_facet Environmental Sciences
description Increasing atmospheric CO2 is decreasing ocean pH most rapidly in colder regions such as the Arctic. As a component of the EPOCA 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 pH 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 most representative phase of the 30 d experiment were reduced by approximately 60% at the highest [H+] and by 35% at [H+] equivalent to 750 μatm pCO2, as predicted 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 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 Archer, S D
Kimmance, S A
Stephens, J A
Hopkins, F E
Bellerby, R GJ
Schulz, Kai G
Piontek, J
Engel, A
author_facet Archer, S D
Kimmance, S A
Stephens, J A
Hopkins, F E
Bellerby, R GJ
Schulz, Kai G
Piontek, J
Engel, A
author_sort Archer, S D
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 ePublications@SCU
publishDate 2012
url https://epubs.scu.edu.au/esm_pubs/1686
https://doi.org/10.5194/bg-10-1893-2013
geographic Arctic
geographic_facet Arctic
genre Arctic
Ocean acidification
Phytoplankton
Spitzbergen
genre_facet Arctic
Ocean acidification
Phytoplankton
Spitzbergen
op_source School of Environment, Science and Engineering Papers
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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