Molecular Mechanisms Underlying Calcification in Coccolithophores

By Luke C. M. Mackinder, Glen L. Wheeler, D. Schroeder, U. Riebesell, C. Brownlee. 2010

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Environmental controls on coccolithophore calcification (2012, background): “The intracellular calcification by coccolithophores (Mackinder et al. 2010, 2011) involves the supply of inorganic carbon to the coccolith-forming vesicle involving influx of HCO3− at the plasmalemma (Paasche 1964, Buitenhuis et al. 1999; cf. Maberly 1992).”
Effects of CO2 and their modulation by light in the life‐cycle stages of the coccolithophore Emiliania huxleyi (2012, background): “An increased proton (H+) concentration may impair transport processes, such as the uptake of inorganic carbon (Ci) or calcium ions (Ca2+), being dependent on electrochemical membrane potentials (Mackinder et al. 2010; Taylor et al. 2011).”
Distinguishing between the effects of ocean acidification and ocean carbonation in the coccolithophore Emiliania huxleyi (2011, background): “The removal of H+ is relatively easy at high seawater pH since the electrochemical gradient between inand outside the cell is comparatively large (Mackinder et al. 2010).”
The Omega Myth: What Really Drives Lower Calcification Rates in an Acidifying Ocean (2016, background): “, 1996) or coccolithophores (Mackinder et al., 2010).”