Utilization of inorganic carbon by the coccolithophorid Emiliania huxleyi (Lohmann) Kamptner

Inorganic carbon-dependent photosynthetic oxygen evolution was saturated at a photon flux density of 100 μmol m-2s-1for air-grown cells of a low calcifying strain of Emiliania huxleyi (Lohmann) Kamptner. Measurement of photosynthetic oxygen evolution at constant inorganic carbon concentration but va...

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Bibliographic Details
Published inThe New phytologist Vol. 120; no. 1; pp. 153 - 158
Main Authors Nimer, N.A, Dixon, G.K, Merrett, M.J
Format Journal Article
LanguageEnglish
Published Oxford, UK Cambridge University Press 1992
Blackwell Publishing Ltd
Blackwell
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Summary:Inorganic carbon-dependent photosynthetic oxygen evolution was saturated at a photon flux density of 100 μmol m-2s-1for air-grown cells of a low calcifying strain of Emiliania huxleyi (Lohmann) Kamptner. Measurement of photosynthetic oxygen evolution at constant inorganic carbon concentration but varying pH showed that exogenous bicarbonate was not a major carbon source for photosynthesis. At pH 8.0 the concentration of dissolved inorganic carbon (DIC) required for the half-maximal rate of photosynthetic O2evolution (K0.5[DIC]) was 2.86 mM; the rate of non-enzymic dehydration of HCO3 -greatly exceeding the rate of CO2fixation. Carbon dioxide uptake occurs by diffusive entry as shown by the K0.5[DIC] of 12.5 μM at pH 5.0. Bicarbonate uptake, measured by the silicone-oil-layer centrigual filtering technique, did not show Michaelis-Menten type kinetics. The electrical membrane potential difference was determined from the distribution of the lipophilic cation tetra[3H]phenylphosphonium (TPP+) between cells and the media. Cells grown at pH 8.0 exhibited a negative membrane potential (inside of cell relative to outside) of about -60 mV.
Bibliography:Dow Elano Europe, Letcombe Laboratory, Letcombe Regis, Oxon, OX12 9JT
ISSN:0028-646X
1469-8137
DOI:10.1111/j.1469-8137.1992.tb01068.x