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...

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Published in:ICES Journal of Marine Science
Main Authors: Schönberg, Christine H. L., Fang, James K. H., Carreiro-Silva, Marina, Tribollet, Aline, Wisshak, Max
Other Authors: Norkko, Joanna, Research Council of Norway-funded, Fundação para a Ciência e a Tecnologia
Format: Article in Journal/Newspaper
Language:English
Published: Oxford University Press (OUP) 2017
Subjects:
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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spelling 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
institution Open Polar
collection Oxford University Press
op_collection_id 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
container_volume 74
container_issue 4
container_start_page 895
op_container_end_page 925
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