Growth response of calcifying marine epibionts to biogenic pH fluctuations and global ocean acidification scenarios

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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Main Authors: Johnson, Mildred Jessica, Hennigs, Laura Margarethe, Sawall, Yvonne, Pansch, Christian, Wall, Marlene
Format: Text
Language:English
Published: John Wiley & Sons, Inc. 2020
Subjects:
Online Access:https://dx.doi.org/10.23689/fidgeo-4067
https://e-docs.geo-leo.de/handle/11858/8407
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spelling ftdatacite:10.23689/fidgeo-4067 2023-05-15T17:50:42+02:00 Growth response of calcifying marine epibionts to biogenic pH fluctuations and global ocean acidification scenarios Johnson, Mildred Jessica Hennigs, Laura Margarethe Sawall, Yvonne Pansch, Christian Wall, Marlene 2020 https://dx.doi.org/10.23689/fidgeo-4067 https://e-docs.geo-leo.de/handle/11858/8407 en eng John Wiley & Sons, Inc. Text Article article-journal ScholarlyArticle 2020 ftdatacite https://doi.org/10.23689/fidgeo-4067 2021-11-05T12:55:41Z 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. : Deutsche Forschungsgemeinschaft http://dx.doi.org/10.13039/501100001659 Text Ocean acidification DataCite Metadata Store (German National Library of Science and Technology)
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language English
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. : Deutsche Forschungsgemeinschaft http://dx.doi.org/10.13039/501100001659
format Text
author Johnson, Mildred Jessica
Hennigs, Laura Margarethe
Sawall, Yvonne
Pansch, Christian
Wall, Marlene
spellingShingle Johnson, Mildred Jessica
Hennigs, Laura Margarethe
Sawall, Yvonne
Pansch, Christian
Wall, Marlene
Growth response of calcifying marine epibionts to biogenic pH fluctuations and global ocean acidification scenarios
author_facet Johnson, Mildred Jessica
Hennigs, Laura Margarethe
Sawall, Yvonne
Pansch, Christian
Wall, Marlene
author_sort Johnson, Mildred Jessica
title Growth response of calcifying marine epibionts to biogenic pH fluctuations and global ocean acidification scenarios
title_short Growth response of calcifying marine epibionts to biogenic pH fluctuations and global ocean acidification scenarios
title_full Growth response of calcifying marine epibionts to biogenic pH fluctuations and global ocean acidification scenarios
title_fullStr Growth response of calcifying marine epibionts to biogenic pH fluctuations and global ocean acidification scenarios
title_full_unstemmed Growth response of calcifying marine epibionts to biogenic pH fluctuations and global ocean acidification scenarios
title_sort growth response of calcifying marine epibionts to biogenic ph fluctuations and global ocean acidification scenarios
publisher John Wiley & Sons, Inc.
publishDate 2020
url https://dx.doi.org/10.23689/fidgeo-4067
https://e-docs.geo-leo.de/handle/11858/8407
genre Ocean acidification
genre_facet Ocean acidification
op_doi https://doi.org/10.23689/fidgeo-4067
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