Seasonal variability of the carbonate system and coccolithophore Emiliania huxleyi at a Scottish Coastal Observatory monitoring site
Seasonal variability of the carbonate system and coccolithophore Emiliania huxleyi at a Scottish Coastal Observatory monitoring site
Lack of information about carbonate chemistry in inshore waters is a ‘knowledge gap’ in assessing the impacts of changing carbonate chemistry on the marine environment. Assessing the response of calcifying phytoplankton to this changing carbonate chemistry requires a greater understanding of temporal variation. This study provides a description of the variability of carbonate parameters at a monitoring site in the eastern coast of Scotland. Four-years of monthly data were analysed to assess the diversity, abundance and morphometrics of coccolithophores in relation to carbonate chemistry and environmental variables. The seasonality in carbonate parameters reflected the seasonal cycle in phytoplankton activity, with higher total alkalinity concentrations and pH and lower dissolved inorganic carbon concentrations during the growing season. The dominant coccolithophore at the site was Emiliania huxleyi which showed a clear seasonal pattern, being more abundant in mid-summer when warmer and nutrient-depleted conditions restricted the annual diatom bloom. This study revealed the presence of three morphotypes of E. huxleyi, type A, type A overcalcified (type AO) and type B, which were seasonally distributed throughout the year. The less calcified form was mainly observed in spring while heavily calcified morphotypes overlapped during summer. Autumn and winter months were dominated by the most calcified form (type AO). These results indicate that the seasonal pattern of E. huxleyi morphotypes was not related to the carbonate concentration at the site. This study reflects the strong interannual variability in carbonate chemistry and the complexity associated with coccolithophore calcification, and highlights the need of long-term data to understand the potential impact of ocean acidification on calcifying phytoplankton.
302-314
León, Pablo
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Walsham, Pam
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Bresnan, Eileen
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Hartman, Susan E.
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Hughes, Sarah
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Mackenzie, Kevin
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Webster, Lynda
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León, Pablo
6700211d-ca0e-4cca-8a8e-83d5ca771f7b
Walsham, Pam
94e6c73c-a41a-4086-9f60-d7bf73e34f98
Bresnan, Eileen
672e0908-e604-4fa9-bbe0-8ad9ddefaf51
Hartman, Susan E.
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Hughes, Sarah
96f3da78-e010-42f7-a280-dacd343d17fb
Mackenzie, Kevin
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Webster, Lynda
7651b239-c316-456e-b221-53d277469369
León, Pablo, Walsham, Pam, Bresnan, Eileen, Hartman, Susan E., Hughes, Sarah, Mackenzie, Kevin and Webster, Lynda
(2018)
Seasonal variability of the carbonate system and coccolithophore Emiliania huxleyi at a Scottish Coastal Observatory monitoring site.
Estuarine, Coastal and Shelf Science, 202, .
(doi:10.1016/j.ecss.2018.01.011).
Abstract
Lack of information about carbonate chemistry in inshore waters is a ‘knowledge gap’ in assessing the impacts of changing carbonate chemistry on the marine environment. Assessing the response of calcifying phytoplankton to this changing carbonate chemistry requires a greater understanding of temporal variation. This study provides a description of the variability of carbonate parameters at a monitoring site in the eastern coast of Scotland. Four-years of monthly data were analysed to assess the diversity, abundance and morphometrics of coccolithophores in relation to carbonate chemistry and environmental variables. The seasonality in carbonate parameters reflected the seasonal cycle in phytoplankton activity, with higher total alkalinity concentrations and pH and lower dissolved inorganic carbon concentrations during the growing season. The dominant coccolithophore at the site was Emiliania huxleyi which showed a clear seasonal pattern, being more abundant in mid-summer when warmer and nutrient-depleted conditions restricted the annual diatom bloom. This study revealed the presence of three morphotypes of E. huxleyi, type A, type A overcalcified (type AO) and type B, which were seasonally distributed throughout the year. The less calcified form was mainly observed in spring while heavily calcified morphotypes overlapped during summer. Autumn and winter months were dominated by the most calcified form (type AO). These results indicate that the seasonal pattern of E. huxleyi morphotypes was not related to the carbonate concentration at the site. This study reflects the strong interannual variability in carbonate chemistry and the complexity associated with coccolithophore calcification, and highlights the need of long-term data to understand the potential impact of ocean acidification on calcifying phytoplankton.
Text
Hartman-2018-PiO-carbonate-shelf
- Accepted Manuscript
More information
Accepted/In Press date: 12 January 2018
e-pub ahead of print date: 5 March 2018
Identifiers
Local EPrints ID: 419809
URI: http://eprints.soton.ac.uk/id/eprint/419809
ISSN: 0272-7714
PURE UUID: 798bf454-21bf-46a9-b742-960a70c4b2f5
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Date deposited: 20 Apr 2018 16:30
Last modified: 16 Mar 2024 06:24
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Contributors
Author:
Pablo León
Author:
Pam Walsham
Author:
Eileen Bresnan
Author:
Susan E. Hartman
Author:
Sarah Hughes
Author:
Kevin Mackenzie
Author:
Lynda Webster
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