Response of Acropora digitifera to ocean acidification: constraints from δ11B, Sr, Mg, and Ba compositions of aragonitic skeletons cultured under variable seawater pH

• Published in: Coral reefs 2015-12, Vol.34 (4), p.1139-1149
• Main Authors: Tanaka, Kentaro, Holcomb, Michael, Takahashi, Asami, Kurihara, Haruko, Asami, Ryuji, Shinjo, Ryuichi, Sowa, Kohki, Rankenburg, Kai, Watanabe, Tsuyoshi, McCulloch, Malcolm
• Format: Article
• Language: English
• Subjects: Biomedical and Life Sciences; Freshwater & Marine Ecology; Life Sciences; Oceanography
• ISSN: 0722-4028; 1432-0975
• DOI: 10.1007/s00338-015-1319-6

The response of Acropora digitifera to ocean acidification is determined using geochemical proxy measurements of the skeletal composition of A. digitifera cultured under a range of pH levels. We show that the chemical composition (δ 11 B, Sr/Ca, Mg/Ca, and Ba/Ca) of the coral skeletons can provide quantitative constraints on the effects of seawater pH on the pH in the calcification fluid (pH CF ) and the mechanisms controlling the incorporation of trace elements into coral aragonite. With the decline of seawater pH, the skeletal δ 11 B value decreased, while the Sr/Ca ratio showed an increasing trend. The relationship between Mg/Ca and Ba/Ca versus seawater pH was not significant. Inter-colony variation of δ 11 B was insignificant, although inter-colony variation was observed for Ba/Ca. The decreasing trend of pH CF calculated from δ 11 B was from ~8.5, 8.4, and 8.3 for seawater pH of ~8.1, 7.8, and 7.4, respectively. Model calculations based on Sr/Ca and pH CF suggest that upregulation of pH CF occurs via exchange of H + with Ca 2+ with kinetic effects (Rayleigh fractionation), reducing Sr/Ca relative to inorganic deposition of aragonite from seawater. We show that it is possible to constrain the overall carbonate chemistry of the calcifying fluid with estimates of the carbonate saturation of the calcifying fluid ( Ω CF ) being derived from skeletal Sr/Ca and pH CF (from δ 11 B). These estimates suggest that the aragonite saturation state of the calcifying fluid Ω CF is elevated by a factor of 5–10 relative to ambient seawater under all treatment conditions.