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Molecular and geochemical perspectives on the influence of CO 2 on calcification in coral cell cultures
Author(s) -
Drake Jeana L.,
Schaller Morgan F.,
Mass Tali,
Godfrey Linda,
Fu Athena,
Sherrell Robert M.,
Rosenthal Yair,
Falkowski Paul G.
Publication year - 2018
Publication title -
limnology and oceanography
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.7
H-Index - 197
eISSN - 1939-5590
pISSN - 0024-3590
DOI - 10.1002/lno.10617
Subject(s) - stylophora pistillata , biomineralization , aragonite , seawater , calcification , coral , ocean acidification , chemistry , calcium carbonate , carbonate , biophysics , biology , calcite , biochemistry , mineralogy , ecology , medicine , paleontology , organic chemistry
Understanding the cellular and molecular responses of stony corals to ocean acidification is key to predicting their ability to calcify under projected high CO 2 conditions. Of specific interest are the links between biomineralization proteins and the precipitation of new calcium carbonate (CaCO 3 ), which potentially can provide a better understanding of the biomineralization process. We have assessed the effects of increased CO 2 on the calcification process in cell cultures of the stony coral, Stylophora pistillata , reared in nutrient‐enriched artificial seawater at four pCO 2 levels and two glucose concentrations. Dispersed S. pistillata cells grown at low (400 ppmV) and moderate (700 ppmV) pCO 2 re‐aggregate into proto‐polyps and precipitate CaCO 3 . When grown at pCO 2 levels of 1000 ppmV and 2000 ppmV, the cells up‐regulate genes for two highly acidic proteins as well as a carbonic anhydrase, but down‐regulate long term cadherin protein production and minimize proto‐polyp formation, and exhibit a significant decrease in measurable CaCO 3 precipitation. However, cell cultures precipitate CaCO 3 in all treatments, even at slightly undersaturated conditions (Ω aragonite < 0.95). Glucose addition does not influence either biomineralization gene expression or calcification rate. Measured δ 11 B of the mineral phase, as a proxy of the pH at the calcifying sites, is out of equilibrium with the ambient seawater medium surrounding the cells and proto‐polyps, suggesting pH is elevated in the micro‐environment of the precipitating mineral. Our results suggest that coral cells possess molecular mechanisms to help compensate for the effects of ocean acidification within the bounds projected in the coming century.