Seawater carbonate chemistry and growth response of calcifying marine epibionts

In coastal marine environments, physical and biological forces can cause dynamic pH fluctuations from microscale (diffusive boundary layer [DBL]) up to ecosystem‐scale (benthic boundary layer [BBL]). In the face of ocean acidification (OA), such natural pH variations may modulate an organism's...

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Bibliographic Details
Main Authors: Johnson, Mildred Jessica, Hennigs, Laura Margarethe, Sawall, Yvonne, Pansch, Christian, Wall, Marlene
Format: Dataset
Language:English
Published: PANGAEA 2021
Subjects:
pH
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.929951
https://doi.org/10.1594/PANGAEA.929951
id ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.929951
record_format openpolar
institution Open Polar
collection PANGAEA - Data Publisher for Earth & Environmental Science
op_collection_id ftpangaea
language English
topic Alkalinity
total
standard deviation
Animalia
Aragonite saturation state
Arthropoda
Balanus improvisus
Baltic Sea
Benthic animals
Benthos
Bicarbonate ion
Bryozoa
Calcite saturation state
Calculated using seacarb
Calculated using seacarb after Nisumaa et al. (2010)
Carbon
inorganic
dissolved
Carbonate ion
Carbonate system computation flag
Carbon dioxide
Coast and continental shelf
Containers and aquaria (20-1000 L or < 1 m**2)
Electra pilosa
Experiment duration
Fugacity of carbon dioxide (water) at sea surface temperature (wet air)
Growth
Growth/Morphology
Growth efficency
Growth rate
Laboratory experiment
OA-ICC
Ocean Acidification International Coordination Centre
Other
Partial pressure of carbon dioxide
Partial pressure of carbon dioxide (water) at sea surface temperature (wet air)
pH
Position
Registration number of species
spellingShingle Alkalinity
total
standard deviation
Animalia
Aragonite saturation state
Arthropoda
Balanus improvisus
Baltic Sea
Benthic animals
Benthos
Bicarbonate ion
Bryozoa
Calcite saturation state
Calculated using seacarb
Calculated using seacarb after Nisumaa et al. (2010)
Carbon
inorganic
dissolved
Carbonate ion
Carbonate system computation flag
Carbon dioxide
Coast and continental shelf
Containers and aquaria (20-1000 L or < 1 m**2)
Electra pilosa
Experiment duration
Fugacity of carbon dioxide (water) at sea surface temperature (wet air)
Growth
Growth/Morphology
Growth efficency
Growth rate
Laboratory experiment
OA-ICC
Ocean Acidification International Coordination Centre
Other
Partial pressure of carbon dioxide
Partial pressure of carbon dioxide (water) at sea surface temperature (wet air)
pH
Position
Registration number of species
Johnson, Mildred Jessica
Hennigs, Laura Margarethe
Sawall, Yvonne
Pansch, Christian
Wall, Marlene
Seawater carbonate chemistry and growth response of calcifying marine epibionts
topic_facet Alkalinity
total
standard deviation
Animalia
Aragonite saturation state
Arthropoda
Balanus improvisus
Baltic Sea
Benthic animals
Benthos
Bicarbonate ion
Bryozoa
Calcite saturation state
Calculated using seacarb
Calculated using seacarb after Nisumaa et al. (2010)
Carbon
inorganic
dissolved
Carbonate ion
Carbonate system computation flag
Carbon dioxide
Coast and continental shelf
Containers and aquaria (20-1000 L or < 1 m**2)
Electra pilosa
Experiment duration
Fugacity of carbon dioxide (water) at sea surface temperature (wet air)
Growth
Growth/Morphology
Growth efficency
Growth rate
Laboratory experiment
OA-ICC
Ocean Acidification International Coordination Centre
Other
Partial pressure of carbon dioxide
Partial pressure of carbon dioxide (water) at sea surface temperature (wet air)
pH
Position
Registration number of species
description In coastal marine environments, physical and biological forces can cause dynamic pH fluctuations from microscale (diffusive boundary layer [DBL]) up to ecosystem‐scale (benthic boundary layer [BBL]). In the face of ocean acidification (OA), such natural pH variations may modulate an organism's response to OA by providing temporal refugia. We investigated the effect of pH fluctuations, generated by the brown alga Fucus serratus' biological activity, on the calcifying epibionts Balanus improvisus and Electra pilosa under OA. For this, both epibionts were grown on inactive and biologically active surfaces and exposed to (1) constant pH scenarios under ambient (pH 8.1) or OA conditions (pH 7.7), or (2) oscillating pH scenarios mimicking BBL conditions at ambient (pH 7.7–8.6) or OA scenarios (pH 7.4–8.2). Furthermore, all treatment combinations were tested at 10°C and 15°C. Against our expectations, OA treatments did not affect epibiont growth under constant or fluctuating (BBL) pH conditions, indicating rather high robustness against predicted OA scenarios. Furthermore, epibiont growth was hampered and not fostered on active surfaces (fluctuating DBL conditions), indicating that fluctuating pH conditions of the DBL with elevated daytime pH do not necessarily provide temporal refugia from OA. In contrast, results indicate that factors other than pH may play larger roles for epibiont growth on macrophytes (e.g., surface characteristics, macrophyte antifouling defense, or dynamics of oxygen and nutrient concentrations). Warming enhanced epibiont growth rates significantly, independently of OA, indicating no synergistic effects of pH treatments and temperature within their natural temperature range.
format Dataset
author Johnson, Mildred Jessica
Hennigs, Laura Margarethe
Sawall, Yvonne
Pansch, Christian
Wall, Marlene
author_facet Johnson, Mildred Jessica
Hennigs, Laura Margarethe
Sawall, Yvonne
Pansch, Christian
Wall, Marlene
author_sort Johnson, Mildred Jessica
title Seawater carbonate chemistry and growth response of calcifying marine epibionts
title_short Seawater carbonate chemistry and growth response of calcifying marine epibionts
title_full Seawater carbonate chemistry and growth response of calcifying marine epibionts
title_fullStr Seawater carbonate chemistry and growth response of calcifying marine epibionts
title_full_unstemmed Seawater carbonate chemistry and growth response of calcifying marine epibionts
title_sort seawater carbonate chemistry and growth response of calcifying marine epibionts
publisher PANGAEA
publishDate 2021
url https://doi.pangaea.de/10.1594/PANGAEA.929951
https://doi.org/10.1594/PANGAEA.929951
genre Ocean acidification
genre_facet Ocean acidification
op_relation Johnson, Mildred Jessica; Hennigs, Laura Margarethe; Sawall, Yvonne; Pansch, Christian; Wall, Marlene (2020): Growth response of calcifying marine epibionts to biogenic pH fluctuations and global ocean acidification scenarios. Limnology and Oceanography, 9999, 1-14, https://doi.org/10.1002/lno.11669
Johnson, Mildred Jessica; Hennigs, Laura Margarethe; Pansch, Christian; Wall, Marlene (2020): Growth response of the barnacle Balanus improvisus and the bryozoan Electra pilosa from Kiel Fjord to biogenic pH fluctuations and global ocean acidification scenarios. PANGAEA, https://doi.pangaea.de/10.1594/PANGAEA.917864
Gattuso, Jean-Pierre; Epitalon, Jean-Marie; Lavigne, Héloïse; Orr, James (2021): seacarb: seawater carbonate chemistry with R. R package version 3.2.16. https://cran.r-project.org/web/packages/seacarb/index.html
https://doi.pangaea.de/10.1594/PANGAEA.929951
https://doi.org/10.1594/PANGAEA.929951
op_rights CC-BY-4.0: Creative Commons Attribution 4.0 International
Access constraints: unrestricted
info:eu-repo/semantics/openAccess
op_rightsnorm CC-BY
op_doi https://doi.org/10.1594/PANGAEA.929951
https://doi.org/10.1002/lno.11669
_version_ 1766158147733422080
spelling ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.929951 2023-05-15T17:51:07+02:00 Seawater carbonate chemistry and growth response of calcifying marine epibionts Johnson, Mildred Jessica Hennigs, Laura Margarethe Sawall, Yvonne Pansch, Christian Wall, Marlene 2021-04-01 text/tab-separated-values, 86045 data points https://doi.pangaea.de/10.1594/PANGAEA.929951 https://doi.org/10.1594/PANGAEA.929951 en eng PANGAEA Johnson, Mildred Jessica; Hennigs, Laura Margarethe; Sawall, Yvonne; Pansch, Christian; Wall, Marlene (2020): Growth response of calcifying marine epibionts to biogenic pH fluctuations and global ocean acidification scenarios. Limnology and Oceanography, 9999, 1-14, https://doi.org/10.1002/lno.11669 Johnson, Mildred Jessica; Hennigs, Laura Margarethe; Pansch, Christian; Wall, Marlene (2020): Growth response of the barnacle Balanus improvisus and the bryozoan Electra pilosa from Kiel Fjord to biogenic pH fluctuations and global ocean acidification scenarios. PANGAEA, https://doi.pangaea.de/10.1594/PANGAEA.917864 Gattuso, Jean-Pierre; Epitalon, Jean-Marie; Lavigne, Héloïse; Orr, James (2021): seacarb: seawater carbonate chemistry with R. R package version 3.2.16. https://cran.r-project.org/web/packages/seacarb/index.html https://doi.pangaea.de/10.1594/PANGAEA.929951 https://doi.org/10.1594/PANGAEA.929951 CC-BY-4.0: Creative Commons Attribution 4.0 International Access constraints: unrestricted info:eu-repo/semantics/openAccess CC-BY Alkalinity total standard deviation Animalia Aragonite saturation state Arthropoda Balanus improvisus Baltic Sea Benthic animals Benthos Bicarbonate ion Bryozoa Calcite saturation state Calculated using seacarb Calculated using seacarb after Nisumaa et al. (2010) Carbon inorganic dissolved Carbonate ion Carbonate system computation flag Carbon dioxide Coast and continental shelf Containers and aquaria (20-1000 L or < 1 m**2) Electra pilosa Experiment duration Fugacity of carbon dioxide (water) at sea surface temperature (wet air) Growth Growth/Morphology Growth efficency Growth rate Laboratory experiment OA-ICC Ocean Acidification International Coordination Centre Other Partial pressure of carbon dioxide Partial pressure of carbon dioxide (water) at sea surface temperature (wet air) pH Position Registration number of species Dataset 2021 ftpangaea https://doi.org/10.1594/PANGAEA.929951 https://doi.org/10.1002/lno.11669 2023-01-20T09:14:44Z In coastal marine environments, physical and biological forces can cause dynamic pH fluctuations from microscale (diffusive boundary layer [DBL]) up to ecosystem‐scale (benthic boundary layer [BBL]). In the face of ocean acidification (OA), such natural pH variations may modulate an organism's response to OA by providing temporal refugia. We investigated the effect of pH fluctuations, generated by the brown alga Fucus serratus' biological activity, on the calcifying epibionts Balanus improvisus and Electra pilosa under OA. For this, both epibionts were grown on inactive and biologically active surfaces and exposed to (1) constant pH scenarios under ambient (pH 8.1) or OA conditions (pH 7.7), or (2) oscillating pH scenarios mimicking BBL conditions at ambient (pH 7.7–8.6) or OA scenarios (pH 7.4–8.2). Furthermore, all treatment combinations were tested at 10°C and 15°C. Against our expectations, OA treatments did not affect epibiont growth under constant or fluctuating (BBL) pH conditions, indicating rather high robustness against predicted OA scenarios. Furthermore, epibiont growth was hampered and not fostered on active surfaces (fluctuating DBL conditions), indicating that fluctuating pH conditions of the DBL with elevated daytime pH do not necessarily provide temporal refugia from OA. In contrast, results indicate that factors other than pH may play larger roles for epibiont growth on macrophytes (e.g., surface characteristics, macrophyte antifouling defense, or dynamics of oxygen and nutrient concentrations). Warming enhanced epibiont growth rates significantly, independently of OA, indicating no synergistic effects of pH treatments and temperature within their natural temperature range. Dataset Ocean acidification PANGAEA - Data Publisher for Earth & Environmental Science