The chemical microenvironment of the symbiotic planktonic foraminifer Orbulina universa

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Biological mechanisms supporting adaptation to ocean acidification in coastal ecosystems (2015, unknown): “During light-dark cycles the pH in the DBL of calcifying foraminifera and diatoms ranges from 8.0 to 9.1 (Köhler-Rink and Kühl 2005; Kühn and Raven 2008).”
Modelling planktic foraminifer growth and distribution using an ecophysiological multi-species approach (2011, background): “Photosynthesis also depends on light availability (L, µmole photon m−2 s−1) and reaches saturation for high light intensities (Jørgensen et al., 1985; Köhler-Rink and Kühl 2005; Spero and Parker, 1985).”