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Coral reef calcification: carbonate, bicarbonate and proton flux under conditions of increasing ocean acidification.珊瑚礁钙化：海洋酸化条件下的碳酸盐、碳酸氢盐和质子通量。
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Coral calcifying fluid pH is modulated by seawater carbonate chemistry not solely seawater pH.珊瑚钙化液的pH值是由海水碳酸盐化学而非仅仅由海水pH值调节的。
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8
Effect of Ocean Acidification and pH Fluctuations on the Growth and Development of Coralline Algal Recruits, and an Associated Benthic Algal Assemblage.海洋酸化和pH值波动对珊瑚藻幼苗及相关底栖藻类群落生长和发育的影响
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Coral-algae metabolism and diurnal changes in the CO2-carbonate system of bulk sea water.珊瑚藻代谢与海水总体 CO2-碳酸盐体系的昼夜变化。
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Coral calcification under daily oxygen saturation and pH dynamics reveals the important role of oxygen.在日常氧饱和度和 pH 动态下的珊瑚钙化作用揭示了氧的重要作用。
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本文引用的文献

1
BEFORE OCEAN ACIDIFICATION: CALCIFIER CHEMISTRY LESSONS(1).海洋酸化之前：钙化生物化学课程(1)
J Phycol. 2012 Aug;48(4):840-3. doi: 10.1111/j.1529-8817.2012.01195.x. Epub 2012 Jun 21.
2
Impact of seawater acidification on pH at the tissue-skeleton interface and calcification in reef corals.海水酸化对珊瑚组织-骨骼界面 pH 值和钙化的影响。
Proc Natl Acad Sci U S A. 2013 Jan 29;110(5):1634-9. doi: 10.1073/pnas.1216153110. Epub 2012 Dec 31.
3
Coral reef calcifiers buffer their response to ocean acidification using both bicarbonate and carbonate.珊瑚礁钙化生物使用碳酸氢盐和碳酸盐来缓冲它们对海洋酸化的反应。
Proc Biol Sci. 2012 Dec 19;280(1753):20122374. doi: 10.1098/rspb.2012.2374. Print 2013 Feb 22.
4
The geological record of ocean acidification.海洋酸化的地质记录。
Science. 2012 Mar 2;335(6072):1058-63. doi: 10.1126/science.1208277.

珊瑚礁钙化：海洋酸化条件下的碳酸盐、碳酸氢盐和质子通量。

Coral reef calcification: carbonate, bicarbonate and proton flux under conditions of increasing ocean acidification.

机构信息

Hawaii Institute of Marine Biology, University of Hawaii, , PO Box 1346, Kaneohe, HI 96744, USA.

出版信息

Proc Biol Sci. 2013 Jun 12;280(1764):20130031. doi: 10.1098/rspb.2013.0031. Print 2013 Aug 7.

DOI:10.1098/rspb.2013.0031
PMID:23760863
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC3712411/
Abstract

Data on calcification rate of coral and crustose coralline algae were used to test the proton flux model of calcification. There was a significant correlation between calcification (G) and the ratio of dissolved inorganic carbon (DIC) to proton concentration ([DIC] : [H(+)] ratio). The ratio is tightly correlated with [CO3(2-)] and with aragonite saturation state (Ωa). An argument is presented that correlation does not prove cause and effect, and that Ωa and [CO3(2-)] have no basic physiological meaning on coral reefs other than a correlation with [DIC] : [H(+)] ratio, which is the driver of G.

摘要

珊瑚和有孔虫藻的钙化率数据被用来检验钙化的质子流模型。钙化（G）与溶解无机碳（DIC）与质子浓度的比值([DIC]：[H(+)] 比值)之间存在显著的相关性。该比值与[CO3(2-)]和霰石饱和度（Ωa）紧密相关。有人认为，相关性并不能证明因果关系，并且除了与[DIC]：[H(+)] 比值相关之外，Ωa 和[CO3(2-)]在珊瑚礁上没有基本的生理意义，而[DIC]：[H(+)] 比值是 G 的驱动力。