Effects of elevated CO2 on shell 13C and 18O content and growth rates in the clam Scapharca broughtonii. (15th August 2018)

• Record Type: Journal Article
• Authors: Nishida, Kozue; Hayashi, Masahiro; Yamamoto, Yuzo; Irie, Takahiro; Watanabe, Yusuke; Kishida, Chiho; Nojiri, Yukihiro; Sato, Mizuho; Ishimura, Toyoho; Suzuki, Atsushi
• Is Part Of: Geochimica et cosmochimica acta. Volume 235(2018)
• Page Start: 246
• Page End: 261
• Publication Date: 2018-08-15
• Subjects: Ocean acidification -- Stable isotopes -- Bivalve -- Kinetic isotope effect -- Calcification; Geochemistry -- Periodicals; Meteorites -- Periodicals; Géochimie -- Périodiques; Météorites -- Périodiques; Geochemie; Astrochemie; Electronic journals; 551.905
• DOI: 10.1016/j.gca.2018.05.030
• Languages: English
• ISSNs: 0016-7037

Abstract

Abstract: The effects of elevated CO2 levels on growth and stable carbon and oxygen isotope compositions (δ 13 C and δ 18 O) of aragonitic shells were experimentally evaluated by rearing the bloody clam, Scapharca broughtonii, at two different temperatures and at six different p CO2 levels (17 °C: 269, 382, 550, 757, 939, and 1114 µatm; 25 °C: 332, 463, 653, 872, 1137, and 1337 μatm). Ambient CO2 levels did not much affect shell growth rates. Mass spectrometric analysis of the outer shell layer indicated a negative correlation between seawater pH and shell δ 18 O (equivalently, a positive correlation between seawater p CO2 and shell δ 18 O) at both temperatures (regression slopes: −0.70‰ ± 0.14‰/pH unit at 17 °C; −0.36‰ ± 0.17‰/pH unit at 25 °C). A positive correlation was observed between seawater pH and shell δ 13 C at both temperatures, but the regression slopes were less steep than those between seawater pH and the δ 13 C of seawater DIC. As CO2 levels rose (and pH dropped to about 7.6), shell δ 18 O and δ 13 C increased relative to ambient dissolved inorganic carbon (DIC). Both approached apparent isotopic equilibrium in acidified waters. Shell δ 18 O was below that of the ambient mix of bicarbonate and carbonate ions, and usually below apparent isotopic equilibrium with water. Kinetic discrimination against heavy isotopes during CO2 hydration and hydroxylation reactions may contribute to this isotopic "enlightenment", and elevated ambient CO2 may "wash out" this effect. Our findings thus generally support models of calcification physiology and shell isotopic content, and have implications for isotopic paleontology.