Light‐dependent carbon isotope fractionation in the coccolithophorid Emiliania huxleyi

By B. Rost, I. Zondervan, U. Riebesell. 2002

151 citations recorded by the source corpus.

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Citations in the corpus

Nitrogen isotope fractionation in 12 species of marine phytoplankton during growth on nitrate (2003, background): “As with the even more extensive work on carbon isotope fractionation by marine phytoplankton, it is apparent that the mechanism of nitrogen isotope fractionation in phytoplankton is not a function of a simple process that can be related to 1 factor, such as cell size (Rost et al. 2002).”
The effect of pCO2 on carbon acquisition and intracellular assimilation in four marine diatoms (2009, background): “We conclude that the observed ε p values and the variation in response to the CO 2 supply can easily be explained by the operation of a classical CCM in the investigated species without invoking C 4 photosynthesis (e.g., Raven and Johnston, 1991; Rost et al., 2002; Trimborn et al., 2008).”
Carbon acquisition of bloom‐forming marine phytoplankton (2003, unknown): “huxleyi remains more or less constant over a wide range of CO2 concentrations, carbon fixation rate and carbon-specific growth rate are strongly CO2 dependent (Paasche et al. 1996; Rost et al. 2002), reflecting the low efficiency of its CCM.”
Zinc availability and alkaline phosphatase activity in Emiliania huxleyi: Implications for Zn‐P co‐limitation in the ocean (2006, background): “Dilute batch cultures, in which pH was kept nearly constant, have previously been used for studying carbon acquisition and calcification by coccolithophores at different CO2 levels (Burkhardt et al. 1999; Rost et al. 2002).”
Effect of CO2 concentration on the PIC/POC ratio in the coccolithophore Emiliania huxleyi grown under light-limiting conditions and different daylengths. (2002, background): “It is possible that a relationship between photosynthesis and calcification exists, but our data do not support the idea of a close coupling between these two processes under the conditions studied here for this high calcifying strain of E. huxleyi (see also Rost et al., 2002 ), as suggested in pre”
Coccolithophores and the biological pump: responses to environmental changes (2004, background): “A predominantly HCO3 - based calcification is indicated by the δ(13)C composition of the coccoliths, which is close to the δ(13)C of HCO3 - (Sikes and Wilbur 1982; Rost et al. 2002).”