Varying Biological Activity and Wind Stress Affect the DMS Response during the SAGE Iron Enrichment Experiment

Surface dissolved dimethylsulfide (DMS) and depth-integrated dimethylsulfoniopropionate (DMSP) measurements were made from March to April 2004 during the SOLAS Air–Sea Gas Exchange Experiment (SAGE), a multiple iron enrichment experiment in subantarctic waters SE of New Zealand. During the first two...

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Main Authors: Graham Jones, Mike Harvey, Stacey King, Anke Schneider, Simon Wright, Darren Fortescue, Hilton Swan, Damien T. Maher
Format: Article
Language:English
Published: MDPI AG 2020-04-01
Series:Journal of Marine Science and Engineering
Subjects:
Online Access:https://www.mdpi.com/2077-1312/8/4/268
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author Graham Jones
Mike Harvey
Stacey King
Anke Schneider
Simon Wright
Darren Fortescue
Hilton Swan
Damien T. Maher
author_facet Graham Jones
Mike Harvey
Stacey King
Anke Schneider
Simon Wright
Darren Fortescue
Hilton Swan
Damien T. Maher
author_sort Graham Jones
collection DOAJ
description Surface dissolved dimethylsulfide (DMS) and depth-integrated dimethylsulfoniopropionate (DMSP) measurements were made from March to April 2004 during the SOLAS Air–Sea Gas Exchange Experiment (SAGE), a multiple iron enrichment experiment in subantarctic waters SE of New Zealand. During the first two iron enrichments, chl <i>a</i> and DMS production were constrained, but during the third enrichment, large pulses of DMS occurred in the fertilised IN patch, compared with the unfertilised OUT patch. During the third and fourth iron infusions, total chl <i>a</i> concentrations doubled from 0.52 to 1.02 µg/L. Hapto8s and prasinophytes accounted for 50%, and 20%, respectively, of total chl <i>a</i>. The large pulses of DMS during the third iron enrichment occurred during high dissolved DMSP concentrations and wind strength; changes in dinoflagellate, haptophyte, and cyanobacteria biomass; and increased microzooplankton grazing that exerted a top down control on phytoplankton production. A further fourth iron enrichment did cause surface waters to increase in DMS, but the effect was not as great as that recorded in the third enrichment. Differences in the biological response between SAGE and several other iron enrichment experiments were concluded to reflect microzooplankton grazing activities and the microbial loop dominance, resulting from mixing of the MLD during storm activity and high winds during iron enrichment.
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spelling doaj.art-a9ca8857c06a4867b1313038d4672d0d2023-11-19T21:08:42ZengMDPI AGJournal of Marine Science and Engineering2077-13122020-04-018426810.3390/jmse8040268Varying Biological Activity and Wind Stress Affect the DMS Response during the SAGE Iron Enrichment ExperimentGraham Jones0Mike Harvey1Stacey King2Anke Schneider3Simon Wright4Darren Fortescue5Hilton Swan6Damien T. Maher7Centre for Coastal Biogeochemistry, School of Environment, Science and Engineering, Southern Cross University, Lismore, NSW 2480, AustraliaNational Institute of Water and Atmospheric Research, Wellington 6241, New ZealandCentre for Coastal Biogeochemistry, School of Environment, Science and Engineering, Southern Cross University, Lismore, NSW 2480, AustraliaInstitute for Marine Chemistry, University of Oldenburg, 26122 Oldenburg, GermanyAustralian Antarctic Division and Antarctic Climate and Ecosystems CRC, Kingston, Tasmania 7050, AustraliaCentre for Coastal Biogeochemistry, School of Environment, Science and Engineering, Southern Cross University, Lismore, NSW 2480, AustraliaCentre for Coastal Biogeochemistry, School of Environment, Science and Engineering, Southern Cross University, Lismore, NSW 2480, AustraliaSouthern Cross Geoscience, Southern Cross University, Lismore, NSW 2480, AustraliaSurface dissolved dimethylsulfide (DMS) and depth-integrated dimethylsulfoniopropionate (DMSP) measurements were made from March to April 2004 during the SOLAS Air–Sea Gas Exchange Experiment (SAGE), a multiple iron enrichment experiment in subantarctic waters SE of New Zealand. During the first two iron enrichments, chl <i>a</i> and DMS production were constrained, but during the third enrichment, large pulses of DMS occurred in the fertilised IN patch, compared with the unfertilised OUT patch. During the third and fourth iron infusions, total chl <i>a</i> concentrations doubled from 0.52 to 1.02 µg/L. Hapto8s and prasinophytes accounted for 50%, and 20%, respectively, of total chl <i>a</i>. The large pulses of DMS during the third iron enrichment occurred during high dissolved DMSP concentrations and wind strength; changes in dinoflagellate, haptophyte, and cyanobacteria biomass; and increased microzooplankton grazing that exerted a top down control on phytoplankton production. A further fourth iron enrichment did cause surface waters to increase in DMS, but the effect was not as great as that recorded in the third enrichment. Differences in the biological response between SAGE and several other iron enrichment experiments were concluded to reflect microzooplankton grazing activities and the microbial loop dominance, resulting from mixing of the MLD during storm activity and high winds during iron enrichment.https://www.mdpi.com/2077-1312/8/4/268dimethylsulfideiron enrichmentsubantarcticmicrozooplankton grazing
spellingShingle Graham Jones
Mike Harvey
Stacey King
Anke Schneider
Simon Wright
Darren Fortescue
Hilton Swan
Damien T. Maher
Varying Biological Activity and Wind Stress Affect the DMS Response during the SAGE Iron Enrichment Experiment
Journal of Marine Science and Engineering
dimethylsulfide
iron enrichment
subantarctic
microzooplankton grazing
title Varying Biological Activity and Wind Stress Affect the DMS Response during the SAGE Iron Enrichment Experiment
title_full Varying Biological Activity and Wind Stress Affect the DMS Response during the SAGE Iron Enrichment Experiment
title_fullStr Varying Biological Activity and Wind Stress Affect the DMS Response during the SAGE Iron Enrichment Experiment
title_full_unstemmed Varying Biological Activity and Wind Stress Affect the DMS Response during the SAGE Iron Enrichment Experiment
title_short Varying Biological Activity and Wind Stress Affect the DMS Response during the SAGE Iron Enrichment Experiment
title_sort varying biological activity and wind stress affect the dms response during the sage iron enrichment experiment
topic dimethylsulfide
iron enrichment
subantarctic
microzooplankton grazing
url https://www.mdpi.com/2077-1312/8/4/268
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