Environmental parameters and carbonate chemistry for the five different treatments during the course of the experiment (mean ± SD).
- Frédéric Gazeau (346439)
- Jean-Pierre Gattuso (246587)
- Mervyn Greaves (346442)
- Henry Elderfield (346443)
- Jan Peene (346445)
- Carlo H. R. Heip (346446)
- Jack J. Middelburg (119295)
Publication date
February 2013
DOIAbstract
<p>The partial pressure of CO<sub>2</sub> (pCO<sub>2</sub>), dissolved inorganic carbon concentration (<i>C</i><sub>T</sub>) as well as the saturation state of seawater with respect to aragonite and calcite (Ω<sub>a</sub> and Ω<sub>c</sub> respectively) were computed from pH<sub>T</sub> and total alkalinity (<i>A</i><sub>T</sub>).</p><p>*: Ω<sub>a</sub> and Ω<sub>c</sub> were increased by addition of calcium (CaCl<sub>2</sub>-2H<sub>2</sub>O; ×2.6 <i>in situ</i> Ca<sup>2+</sup> concentrations).</p
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