CO-dependent carbon isotope fractionation in dinoflagellates relates to their inorganic carbon fluxes.

Carbon isotope fractionation (ε) between the inorganic carbon source and organic matter has been proposed to be a function of CO. To understand the CO-dependency of ε and species-specific differences therein, inorganic carbon fluxes in the four dinoflagellate species and have been measured by means of membrane-inlet mass spectrometry. In-vivo assays were carried out at different CO concentrations, representing a range of CO from 180 to 1200 μatm. The relative bicarbonate contribution (i.e. the ratio of bicarbonate uptake to total inorganic carbon uptake) and leakage (i.e. the ratio of CO efflux to total inorganic carbon uptake) varied from 0.2 to 0.5 and 0.4 to 0.7, respectively, and differed significantly between species. These ratios were fed into a single-compartment model, and ε values were calculated and compared to carbon isotope fractionation measured under the same conditions. For all investigated species, modeled and measured ε values were comparable () and/or showed similar trends with CO (). Offsets are attributed to biases in inorganic flux measurements, an overestimated fractionation factor for the CO-fixing enzyme RubisCO, or the fact that intracellular inorganic carbon fluxes were not taken into account in the model. This study demonstrates that CO-dependency in ε can largely be explained by the inorganic carbon fluxes of the individual dinoflagellates.