Computing the carbonate chemistry of the coral calcifying medium and its response to ocean acidification

JOURNAL OF THEORETICAL BIOLOGY

卷:424

Article

Raybaud, Virginie^1,2,3,4  Tambutte, Sylvie^1,2  Ferrier-Pages, Christine^1,2  Reynaud, Stephanie^1,2  Venn, Alexander A.^1,2  Tambutte, Eric^1,2  Nival, Paul⁵  Allemand, Denis^1,2 

[1] Ctr Sci Monaco, Marine Biol Dept, 8 Quai Antoine 1er,MC98000, Monaco, Monaco

[2] Ctr Natl Rech Sci, Ctr Sci Monaco, Lab Int Associe BIOSENSIB 647, 8 Quai Antoine 1er,MC98000, Monaco, Monaco

[3] UPMC Univ Paris 06, Sorbonne Univ, CNRS UMS 829, Observ Oceanol Villefranche Sur Mer, F-06230 Villefranche Sur Mer, France

[4] Univ Cote Azur, CNRS, ECOMERS, Nice, France

[5] UPMC Univ Paris 06, Sorbonne Univ, CNRS UMR 7093, Lab Oceanol Villefranche, F-06230 Villefranche Sur Mer, France

关键词: Scleractinian corals;    Calcification;    Calcifying fluid;    Aragonite saturation state;    Ocean acidification;   

DOI  :  10.1016/j.jtbi.2017.04.028

来源: Elsevier

【 摘 要 】

Critical to determining vulnerability or resilience of reef corals to Ocean Acidification (OA) is a clearer understanding of the extent to which corals can control carbonate chemistry in their Extracellular Calcifying Medium (ECM) where the CaCO3 skeleton is produced. Here, we employ a mathematical framework to calculate ECM aragonite saturation state In. Omega(arag) ((ECM))) and carbonate system ion concentration using measurements of calcification rate, seawater characteristics (temperature, salinity and pH) and ECM pH (pH((ECM))). Our calculations of ECM carbonate chemistry at current -day seawater pH, indicate that Omega(arag).(ECM) ranges from similar to 10 to 38 (mean 20.41), i.e. about 5 to 6-fold higher than seawater. Accordingly, Dissolved Inorganic Carbon (DIC) and Total Alkalinity (TA) were calculated to be around 3 times higher in the ECM than in seawater. We also assessed the effects of acidification on ECM chemical properties of the coral Stylophora pistillata. At reduced seawater pH our calculations indicate that Omega(arag).((ECM)) remains almost constant.'DIC((Ecm)) and TA((Ecm)) gradually increase as seawater pH declines, reaching values about 5 to 6-fold higher than in seawater, respectively for DIC and TA. We propose that these ECM characteristics buffer the effect of acidification and explain why certain corals continue to produce CaCO3 even when seawater chemistry is less favourable. (C) 2017 Elsevier Ltd. All rights reserved.

【 授权许可】

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