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...
Published in: | Limnology and Oceanography |
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ASLO (Association for the Sciences of Limnology and Oceanography)
2021
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Online Access: | https://oceanrep.geomar.de/id/eprint/51384/ https://oceanrep.geomar.de/id/eprint/51384/1/lno.11669.pdf https://doi.org/10.1002/lno.11669 |
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ftoceanrep:oai:oceanrep.geomar.de:51384 2024-02-11T10:07:28+01:00 Growth response of calcifying marine epibionts to biogenic pH fluctuations and global ocean acidification scenarios Johnson, Mildred Hennigs, Laura Margarethe Sawall, Yvonne Pansch, Christian Wall, Marlene 2021-04-01 text https://oceanrep.geomar.de/id/eprint/51384/ https://oceanrep.geomar.de/id/eprint/51384/1/lno.11669.pdf https://doi.org/10.1002/lno.11669 en eng ASLO (Association for the Sciences of Limnology and Oceanography) Wiley https://oceanrep.geomar.de/id/eprint/51384/1/lno.11669.pdf Johnson, M. , Hennigs, L. M. , Sawall, Y. , Pansch, C. and Wall, M. (2021) Growth response of calcifying marine epibionts to biogenic pH fluctuations and global ocean acidification scenarios. Open Access Limnology and Oceanography, 66 (4). pp. 1125-1138. DOI 10.1002/lno.11669 <https://doi.org/10.1002/lno.11669>. doi:10.1002/lno.11669 cc_by_4.0 info:eu-repo/semantics/openAccess Article PeerReviewed 2021 ftoceanrep https://doi.org/10.1002/lno.11669 2024-01-15T00:22:57Z 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. Article in Journal/Newspaper Ocean acidification OceanRep (GEOMAR Helmholtz Centre für Ocean Research Kiel) Limnology and Oceanography 66 4 1125 1138 |
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Open Polar |
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OceanRep (GEOMAR Helmholtz Centre für Ocean Research Kiel) |
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ftoceanrep |
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. |
format |
Article in Journal/Newspaper |
author |
Johnson, Mildred Hennigs, Laura Margarethe Sawall, Yvonne Pansch, Christian Wall, Marlene |
spellingShingle |
Johnson, Mildred 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 Hennigs, Laura Margarethe Sawall, Yvonne Pansch, Christian Wall, Marlene |
author_sort |
Johnson, Mildred |
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 |
ASLO (Association for the Sciences of Limnology and Oceanography) |
publishDate |
2021 |
url |
https://oceanrep.geomar.de/id/eprint/51384/ https://oceanrep.geomar.de/id/eprint/51384/1/lno.11669.pdf https://doi.org/10.1002/lno.11669 |
genre |
Ocean acidification |
genre_facet |
Ocean acidification |
op_relation |
https://oceanrep.geomar.de/id/eprint/51384/1/lno.11669.pdf Johnson, M. , Hennigs, L. M. , Sawall, Y. , Pansch, C. and Wall, M. (2021) Growth response of calcifying marine epibionts to biogenic pH fluctuations and global ocean acidification scenarios. Open Access Limnology and Oceanography, 66 (4). pp. 1125-1138. DOI 10.1002/lno.11669 <https://doi.org/10.1002/lno.11669>. doi:10.1002/lno.11669 |
op_rights |
cc_by_4.0 info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/10.1002/lno.11669 |
container_title |
Limnology and Oceanography |
container_volume |
66 |
container_issue |
4 |
container_start_page |
1125 |
op_container_end_page |
1138 |
_version_ |
1790606036441235456 |