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Sources of inorganic carbon for photosynthesis in a strain of Phaeodactylum tricornutum
Author(s) -
Cassar Nicolas,
Laws Edward A.,
Popp Brian N.,
Bidigare Robert R.
Publication year - 2002
Publication title -
limnology and oceanography
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.7
H-Index - 197
eISSN - 1939-5590
pISSN - 0024-3590
DOI - 10.4319/lo.2002.47.4.1192
Subject(s) - phaeodactylum tricornutum , phytoplankton , photosynthesis , total inorganic carbon , algae , carbon dioxide , carbon fixation , bicarbonate , environmental chemistry , autotroph , chemistry , seawater , photobioreactor , rubisco , ribulose , fractionation , botany , biology , ecology , nutrient , biomass (ecology) , chromatography , bacteria , genetics , organic chemistry
Diatoms are an important functional group of marine phytoplankton because of their role in the fixation of atmospheric carbon dioxide (CO 2 ) and transfer of organic carbon to deep waters. Carbon‐concentrating‐mechanisms, such as active CO 2 and bicarbonate (HCO 3 − ) 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 CO 2 2 concentrations. On the basis of short‐term inorganic 14 C uptake experiments, Tortell et al. (1997; Nature 390: 243–244) recently argued that marine diatoms are capable of HCO 3 − uptake. However, as discussed herein, the extent of HCO 3 − uptake cannot be assessed on the basis of these experiments. Using short‐term 14 CO 2 ‐disequilibrium experiments, we show that a clone of the marine diatom Phaeodactylum tricornutum takes up little or no HCO 3 − even under conditions of severe CO 2 2 limitation. Predicting the response of the oceans to increased CO 2 concentrations will require, among other things, a careful assessment of the extent to which marine algae take up HCO 3 − or CO 2 . Because the plasmalemma of microalgae is gas permeable, all phytoplankton exchange CO 2 with the growth medium. Experimental results that are merely consistent with HCO 3 − uptake are insufficient to prove that HCO 3 − 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 CO 2 emissions as well as for interpreting paleoceanographic carbon isotope data.