Measuring gross and net calcification of a reef coral under ocean acidification conditions: methodological considerations

Ongoing ocean acidification (OA) is rapidly altering carbonate chemistry in the oceans. The projected changes will likely have deleterious consequences for coral reefs by negatively affecting their growth. Nonetheless, diverse responses of reef-building corals calcification to OA hinder our ability...

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Main Authors: Cohen, S., Fine, M.
Format: Text
Language:English
Published: 2018
Subjects:
Online Access:https://doi.org/10.5194/bgd-9-8241-2012
https://www.biogeosciences-discuss.net/bg-2012-238/
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spelling ftcopernicus:oai:publications.copernicus.org:bgd15794 2023-05-15T17:50:38+02:00 Measuring gross and net calcification of a reef coral under ocean acidification conditions: methodological considerations Cohen, S. Fine, M. 2018-09-26 application/pdf https://doi.org/10.5194/bgd-9-8241-2012 https://www.biogeosciences-discuss.net/bg-2012-238/ eng eng doi:10.5194/bgd-9-8241-2012 https://www.biogeosciences-discuss.net/bg-2012-238/ eISSN: 1726-4189 Text 2018 ftcopernicus https://doi.org/10.5194/bgd-9-8241-2012 2019-12-24T09:56:12Z Ongoing ocean acidification (OA) is rapidly altering carbonate chemistry in the oceans. The projected changes will likely have deleterious consequences for coral reefs by negatively affecting their growth. Nonetheless, diverse responses of reef-building corals calcification to OA hinder our ability to decipher reef susceptibility to elevated p CO 2 . Some of the inconsistencies between studies originate in measuring net calcification (NC), which does not always consider the proportions of the "real" (gross) calcification (GC) and gross dissolution in the observed response. Here we show that microcolonies of Stylophora pistillata (entirely covered by tissue), incubated under normal (8.2) and reduced (7.6) pH conditions for 16 months, survived and added new skeletal CaCO 3 , despite low (1.25) Ω arg conditions. Moreover, corals maintained their NC and GC rates under reduced (7.6) pH conditions and displayed positive NC rates at the low-end (7.3) pH treatment while bare coral skeleton underwent marked dissolution. Our findings suggest that S. pistillata may fall into the "low sensitivity" group with respect to OA and that their overlying tissue may be a key determinant in setting their tolerance to reduced pH by limiting dissolution and allowing them to calcify. This study is the first to measure GC and NC rates for a tropical scleractinian corals under OA conditions. We provide a detailed, realistic assessment of the problematic nature of previously accepted methods for measuring calcification (total alkalinity and 45 Ca). Text Ocean acidification Copernicus Publications: E-Journals
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description Ongoing ocean acidification (OA) is rapidly altering carbonate chemistry in the oceans. The projected changes will likely have deleterious consequences for coral reefs by negatively affecting their growth. Nonetheless, diverse responses of reef-building corals calcification to OA hinder our ability to decipher reef susceptibility to elevated p CO 2 . Some of the inconsistencies between studies originate in measuring net calcification (NC), which does not always consider the proportions of the "real" (gross) calcification (GC) and gross dissolution in the observed response. Here we show that microcolonies of Stylophora pistillata (entirely covered by tissue), incubated under normal (8.2) and reduced (7.6) pH conditions for 16 months, survived and added new skeletal CaCO 3 , despite low (1.25) Ω arg conditions. Moreover, corals maintained their NC and GC rates under reduced (7.6) pH conditions and displayed positive NC rates at the low-end (7.3) pH treatment while bare coral skeleton underwent marked dissolution. Our findings suggest that S. pistillata may fall into the "low sensitivity" group with respect to OA and that their overlying tissue may be a key determinant in setting their tolerance to reduced pH by limiting dissolution and allowing them to calcify. This study is the first to measure GC and NC rates for a tropical scleractinian corals under OA conditions. We provide a detailed, realistic assessment of the problematic nature of previously accepted methods for measuring calcification (total alkalinity and 45 Ca).
format Text
author Cohen, S.
Fine, M.
spellingShingle Cohen, S.
Fine, M.
Measuring gross and net calcification of a reef coral under ocean acidification conditions: methodological considerations
author_facet Cohen, S.
Fine, M.
author_sort Cohen, S.
title Measuring gross and net calcification of a reef coral under ocean acidification conditions: methodological considerations
title_short Measuring gross and net calcification of a reef coral under ocean acidification conditions: methodological considerations
title_full Measuring gross and net calcification of a reef coral under ocean acidification conditions: methodological considerations
title_fullStr Measuring gross and net calcification of a reef coral under ocean acidification conditions: methodological considerations
title_full_unstemmed Measuring gross and net calcification of a reef coral under ocean acidification conditions: methodological considerations
title_sort measuring gross and net calcification of a reef coral under ocean acidification conditions: methodological considerations
publishDate 2018
url https://doi.org/10.5194/bgd-9-8241-2012
https://www.biogeosciences-discuss.net/bg-2012-238/
genre Ocean acidification
genre_facet Ocean acidification
op_source eISSN: 1726-4189
op_relation doi:10.5194/bgd-9-8241-2012
https://www.biogeosciences-discuss.net/bg-2012-238/
op_doi https://doi.org/10.5194/bgd-9-8241-2012
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