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


Journal Article

Diatoms are an important functional group of marine phytoplankton because of their role in the fixation of atmospheric carbon dioxide (CO2) and transfer of organic carbon to deep waters. Carbon-concentrating-mechanisms, such as active CO2 and bicarbonate (HCO3 -) 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 14C uptake experiments, Tortell et al. (1997; Nature 390: 243-244) recently argued that marine diatoms are capable of HCO3 - uptake. However, as discussed herein, the extent of HCO3 - uptake cannot be assessed on the basis of these experiments. Using short-term 14CO2-disequilibrium experiments, we show that a clone of the marine diatom Phaeodactylum tricornutum takes up little or no HCO3 - 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 HCO3 - or CO2. Because the plasmalemma of microalgae is gas permeable, all phytoplankton exchange CO2 with the growth medium. Experimental results that are merely consistent with HCO3 - uptake are insufficient to prove that HCO3 - uptake is occurring. Our results are in accord with predictions based on 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.

Full Text

Duke Authors

Cited Authors

  • Cassar, N; Laws, EA; Popp, BN; Bidigare, RR

Published Date

  • 2002

Published In

  • Limnology and Oceanography

Volume / Issue

  • 47 / 4

Start / End Page

  • 1192 - 1197