Ocean acidification with (de)eutrophication will alter future phytoplankton growth and succession

Human activity causes ocean acidification (OA) though the dissolution of anthropogenically generated CO2 into seawater, and eutrophication through the addition of inorganic nutrients. Eutrophication increases the phytoplankton biomass that can be supported during a bloom, and the resultant uptake of...

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Published in:Proceedings of the Royal Society B: Biological Sciences
Main Authors: Flynn, Kevin J., Clark, Darren R., Mitra, Aditee, Fabian, Heiner, Hansen, Per J., Glibert, Patricia M., Wheeler, Glen L., Stoecke, Diane K., Blackford, Jerry C., Brownlee, Colin
Format: Article in Journal/Newspaper
Language:English
Published: Royal Society, The 2015
Subjects:
Online Access:https://orca.cardiff.ac.uk/id/eprint/129691/
https://doi.org/10.1098/rspb.2014.2604
https://orca.cardiff.ac.uk/id/eprint/129691/1/rspb.2014.2604.pdf
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spelling ftunivcardiff:oai:https://orca.cardiff.ac.uk:129691 2023-06-11T04:15:35+02:00 Ocean acidification with (de)eutrophication will alter future phytoplankton growth and succession Flynn, Kevin J. Clark, Darren R. Mitra, Aditee Fabian, Heiner Hansen, Per J. Glibert, Patricia M. Wheeler, Glen L. Stoecke, Diane K. Blackford, Jerry C. Brownlee, Colin 2015-04-07 application/pdf https://orca.cardiff.ac.uk/id/eprint/129691/ https://doi.org/10.1098/rspb.2014.2604 https://orca.cardiff.ac.uk/id/eprint/129691/1/rspb.2014.2604.pdf en eng Royal Society, The https://orca.cardiff.ac.uk/id/eprint/129691/1/rspb.2014.2604.pdf Flynn, Kevin J., Clark, Darren R., Mitra, Aditee https://orca.cardiff.ac.uk/view/cardiffauthors/A2537465T.html orcid:0000-0001-5572-9331 orcid:0000-0001-5572-9331, Fabian, Heiner, Hansen, Per J., Glibert, Patricia M., Wheeler, Glen L., Stoecke, Diane K., Blackford, Jerry C. and Brownlee, Colin 2015. Ocean acidification with (de)eutrophication will alter future phytoplankton growth and succession. Proceedings of the Royal Society B: Biological Sciences 282 (1804) , 20142604. 10.1098/rspb.2014.2604 https://doi.org/10.1098/rspb.2014.2604 file https://orca.cardiff.ac.uk/id/eprint/129691/1/rspb.2014.2604.pdf doi:10.1098/rspb.2014.2604 cc_by Article PeerReviewed 2015 ftunivcardiff https://doi.org/10.1098/rspb.2014.2604 2023-05-04T22:36:16Z Human activity causes ocean acidification (OA) though the dissolution of anthropogenically generated CO2 into seawater, and eutrophication through the addition of inorganic nutrients. Eutrophication increases the phytoplankton biomass that can be supported during a bloom, and the resultant uptake of dissolved inorganic carbon during photosynthesis increases water-column pH (bloom-induced basification). This increased pH can adversely affect plankton growth. With OA, basification commences at a lower pH. Using experimental analyses of the growth of three contrasting phytoplankton under different pH scenarios, coupled with mathematical models describing growth and death as functions of pH and nutrient status, we show how different conditions of pH modify the scope for competitive interactions between phytoplankton species. We then use the models previously configured against experimental data to explore how the commencement of bloom-induced basification at lower pH with OA, and operating against a background of changing patterns in nutrient loads, may modify phytoplankton growth and competition. We conclude that OA and changed nutrient supply into shelf seas with eutrophication or de-eutrophication (the latter owing to pollution control) has clear scope to alter phytoplankton succession, thus affecting future trophic dynamics and impacting both biogeochemical cycling and fisheries. Article in Journal/Newspaper Ocean acidification Cardiff University: ORCA (Online Research @ Cardiff) Proceedings of the Royal Society B: Biological Sciences 282 1804 20142604
institution Open Polar
collection Cardiff University: ORCA (Online Research @ Cardiff)
op_collection_id ftunivcardiff
language English
description Human activity causes ocean acidification (OA) though the dissolution of anthropogenically generated CO2 into seawater, and eutrophication through the addition of inorganic nutrients. Eutrophication increases the phytoplankton biomass that can be supported during a bloom, and the resultant uptake of dissolved inorganic carbon during photosynthesis increases water-column pH (bloom-induced basification). This increased pH can adversely affect plankton growth. With OA, basification commences at a lower pH. Using experimental analyses of the growth of three contrasting phytoplankton under different pH scenarios, coupled with mathematical models describing growth and death as functions of pH and nutrient status, we show how different conditions of pH modify the scope for competitive interactions between phytoplankton species. We then use the models previously configured against experimental data to explore how the commencement of bloom-induced basification at lower pH with OA, and operating against a background of changing patterns in nutrient loads, may modify phytoplankton growth and competition. We conclude that OA and changed nutrient supply into shelf seas with eutrophication or de-eutrophication (the latter owing to pollution control) has clear scope to alter phytoplankton succession, thus affecting future trophic dynamics and impacting both biogeochemical cycling and fisheries.
format Article in Journal/Newspaper
author Flynn, Kevin J.
Clark, Darren R.
Mitra, Aditee
Fabian, Heiner
Hansen, Per J.
Glibert, Patricia M.
Wheeler, Glen L.
Stoecke, Diane K.
Blackford, Jerry C.
Brownlee, Colin
spellingShingle Flynn, Kevin J.
Clark, Darren R.
Mitra, Aditee
Fabian, Heiner
Hansen, Per J.
Glibert, Patricia M.
Wheeler, Glen L.
Stoecke, Diane K.
Blackford, Jerry C.
Brownlee, Colin
Ocean acidification with (de)eutrophication will alter future phytoplankton growth and succession
author_facet Flynn, Kevin J.
Clark, Darren R.
Mitra, Aditee
Fabian, Heiner
Hansen, Per J.
Glibert, Patricia M.
Wheeler, Glen L.
Stoecke, Diane K.
Blackford, Jerry C.
Brownlee, Colin
author_sort Flynn, Kevin J.
title Ocean acidification with (de)eutrophication will alter future phytoplankton growth and succession
title_short Ocean acidification with (de)eutrophication will alter future phytoplankton growth and succession
title_full Ocean acidification with (de)eutrophication will alter future phytoplankton growth and succession
title_fullStr Ocean acidification with (de)eutrophication will alter future phytoplankton growth and succession
title_full_unstemmed Ocean acidification with (de)eutrophication will alter future phytoplankton growth and succession
title_sort ocean acidification with (de)eutrophication will alter future phytoplankton growth and succession
publisher Royal Society, The
publishDate 2015
url https://orca.cardiff.ac.uk/id/eprint/129691/
https://doi.org/10.1098/rspb.2014.2604
https://orca.cardiff.ac.uk/id/eprint/129691/1/rspb.2014.2604.pdf
genre Ocean acidification
genre_facet Ocean acidification
op_relation https://orca.cardiff.ac.uk/id/eprint/129691/1/rspb.2014.2604.pdf
Flynn, Kevin J., Clark, Darren R., Mitra, Aditee https://orca.cardiff.ac.uk/view/cardiffauthors/A2537465T.html orcid:0000-0001-5572-9331 orcid:0000-0001-5572-9331, Fabian, Heiner, Hansen, Per J., Glibert, Patricia M., Wheeler, Glen L., Stoecke, Diane K., Blackford, Jerry C. and Brownlee, Colin 2015. Ocean acidification with (de)eutrophication will alter future phytoplankton growth and succession. Proceedings of the Royal Society B: Biological Sciences 282 (1804) , 20142604. 10.1098/rspb.2014.2604 https://doi.org/10.1098/rspb.2014.2604 file https://orca.cardiff.ac.uk/id/eprint/129691/1/rspb.2014.2604.pdf
doi:10.1098/rspb.2014.2604
op_rights cc_by
op_doi https://doi.org/10.1098/rspb.2014.2604
container_title Proceedings of the Royal Society B: Biological Sciences
container_volume 282
container_issue 1804
container_start_page 20142604
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