Sources of inorganic carbon for photosynthesis in a strain of Phaeodactylum tricornutum

Diatoms are an important functional group of marine phytoplankton because of their role ill the fixation of atmospheric carbon dioxide (CO2) and transfer of organic carbon to deep waters. Carbon-concentrating-mechanisms, such as active CO2 and bicarbonate (HCO(3) over bar) uptake and carbonic anhydrase activity, are believed to be essential to marine photosynthesis, because the main carbon-fixing enzyme, ribulose-1 5-bisphosphate carboxylase-oxygenase, is less than half saturated at normal seawater CO2 concentrations. On the basis of short-term inorganic C-14 uptake experiments, Tortell et al. (1997: Nature 390: 243-244) recently argued that marine diatoms are capable of HCO(3) over bar uptake. However, as discussed herein. the extent of HCO(3) over bar uptake cannot be assessed on the basis of these experiments. Using short-term (CO2)-C-14-disequilibrium experiments. we show that a clone of the marine diatom Phaeodactylum tricornutum takes up little or no HCO(3) over bar even under conditions of severe CO2 limitation. Predicting the response of the oceans to increased CO2 concentrations will require, among other things, a careful assessment of the extent to which marine algae take up HCO(3) over bar or CO2 Because the the plasinalernma of microalgae is gas permeable, all phytoplankton exchange CO2 with the growth medium. Experimental results that are merely consistent with HCO(3) over bar uptake are insufficient to prove that HCO(3) over bar Uptake is occurring. Our results are in accord with predictions based oil stable carbon isotopic fractionation data. Combining isotopic disequilibrium experiments with continuous growth Cultures and stable isotope fractionation experiments is a Powerful tool for understanding the response of oceanic primary producers to anthropogenic CO2 emissions as well as for interpreting paleoceanographic carbon isotope data.