Bioerosion: the other ocean acidification problem
Bioerosion of calcium carbonate is the natural counterpart of biogenic calcification. Both are affected by ocean acidification (OA). We summarize definitions and concepts in bioerosion research and knowledge in the context of OA, providing case examples and meta-analyses. Chemically mediated bioeros...
Published in: | ICES Journal of Marine Science |
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2017
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Online Access: | http://dx.doi.org/10.1093/icesjms/fsw254 http://academic.oup.com/icesjms/article-pdf/74/4/895/31246419/fsw254.pdf |
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croxfordunivpr:10.1093/icesjms/fsw254 2024-10-13T14:09:59+00:00 Bioerosion: the other ocean acidification problem Schönberg, Christine H. L. Fang, James K. H. Carreiro-Silva, Marina Tribollet, Aline Wisshak, Max Norkko, Joanna Research Council of Norway-funded Fundação para a Ciência e a Tecnologia 2017 http://dx.doi.org/10.1093/icesjms/fsw254 http://academic.oup.com/icesjms/article-pdf/74/4/895/31246419/fsw254.pdf en eng Oxford University Press (OUP) https://academic.oup.com/journals/pages/open_access/funder_policies/chorus/standard_publication_model ICES Journal of Marine Science volume 74, issue 4, page 895-925 ISSN 1054-3139 1095-9289 journal-article 2017 croxfordunivpr https://doi.org/10.1093/icesjms/fsw254 2024-09-17T04:29:23Z Bioerosion of calcium carbonate is the natural counterpart of biogenic calcification. Both are affected by ocean acidification (OA). We summarize definitions and concepts in bioerosion research and knowledge in the context of OA, providing case examples and meta-analyses. Chemically mediated bioerosion relies on energy demanding, biologically controlled undersaturation or acid regulation and increases with simulated OA, as does passive dissolution. Through substrate weakening both processes can indirectly enhance mechanical bioerosion, which is not directly affected by OA. The low attention and expert knowledge on bioerosion produced some ambiguous views and approaches, and limitations to experimental studies restricted opportunities to generalize. Comparability of various bioerosion and calcification rates remains difficult. Physiological responses of bioeroders or interactions of environmental factors are insufficiently studied. We stress the importance to foster and advance high quality bioerosion research as global trends suggest the following: (i) growing environmental change (eutrophication, coral mortality, OA) is expected to elevate bioerosion in the near future; (ii) changes harmful to calcifiers may not be as severe for bioeroders (e.g. warming); and (iii) factors facilitating bioerosion often reduce calcification rates (e.g. OA). The combined result means that the natural process bioerosion has itself become a “stress factor”” for reef health and resilience. Article in Journal/Newspaper Ocean acidification Oxford University Press ICES Journal of Marine Science 74 4 895 925 |
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Open Polar |
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Oxford University Press |
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croxfordunivpr |
language |
English |
description |
Bioerosion of calcium carbonate is the natural counterpart of biogenic calcification. Both are affected by ocean acidification (OA). We summarize definitions and concepts in bioerosion research and knowledge in the context of OA, providing case examples and meta-analyses. Chemically mediated bioerosion relies on energy demanding, biologically controlled undersaturation or acid regulation and increases with simulated OA, as does passive dissolution. Through substrate weakening both processes can indirectly enhance mechanical bioerosion, which is not directly affected by OA. The low attention and expert knowledge on bioerosion produced some ambiguous views and approaches, and limitations to experimental studies restricted opportunities to generalize. Comparability of various bioerosion and calcification rates remains difficult. Physiological responses of bioeroders or interactions of environmental factors are insufficiently studied. We stress the importance to foster and advance high quality bioerosion research as global trends suggest the following: (i) growing environmental change (eutrophication, coral mortality, OA) is expected to elevate bioerosion in the near future; (ii) changes harmful to calcifiers may not be as severe for bioeroders (e.g. warming); and (iii) factors facilitating bioerosion often reduce calcification rates (e.g. OA). The combined result means that the natural process bioerosion has itself become a “stress factor”” for reef health and resilience. |
author2 |
Norkko, Joanna Research Council of Norway-funded Fundação para a Ciência e a Tecnologia |
format |
Article in Journal/Newspaper |
author |
Schönberg, Christine H. L. Fang, James K. H. Carreiro-Silva, Marina Tribollet, Aline Wisshak, Max |
spellingShingle |
Schönberg, Christine H. L. Fang, James K. H. Carreiro-Silva, Marina Tribollet, Aline Wisshak, Max Bioerosion: the other ocean acidification problem |
author_facet |
Schönberg, Christine H. L. Fang, James K. H. Carreiro-Silva, Marina Tribollet, Aline Wisshak, Max |
author_sort |
Schönberg, Christine H. L. |
title |
Bioerosion: the other ocean acidification problem |
title_short |
Bioerosion: the other ocean acidification problem |
title_full |
Bioerosion: the other ocean acidification problem |
title_fullStr |
Bioerosion: the other ocean acidification problem |
title_full_unstemmed |
Bioerosion: the other ocean acidification problem |
title_sort |
bioerosion: the other ocean acidification problem |
publisher |
Oxford University Press (OUP) |
publishDate |
2017 |
url |
http://dx.doi.org/10.1093/icesjms/fsw254 http://academic.oup.com/icesjms/article-pdf/74/4/895/31246419/fsw254.pdf |
genre |
Ocean acidification |
genre_facet |
Ocean acidification |
op_source |
ICES Journal of Marine Science volume 74, issue 4, page 895-925 ISSN 1054-3139 1095-9289 |
op_rights |
https://academic.oup.com/journals/pages/open_access/funder_policies/chorus/standard_publication_model |
op_doi |
https://doi.org/10.1093/icesjms/fsw254 |
container_title |
ICES Journal of Marine Science |
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74 |
container_issue |
4 |
container_start_page |
895 |
op_container_end_page |
925 |
_version_ |
1812817096840577024 |