Plant Physiol. Illumina
HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
 QUICK SEARCH:   [advanced]


     


Plant Physiology 97:1439-1444 (1991)
© 1991 American Society of Plant Biologists

This Article
Right arrow Full Text (PDF)
Right arrow Alert me when this article is cited
Right arrow Alert me if a correction is posted
Services
Right arrow Email this article to a friend
Right arrow Similar articles in this journal
Right arrow Similar articles in Web of Science
Right arrow Similar articles in PubMed
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Right arrow reprints & permissions
Citing Articles
Right arrow Citing Articles via HighWire
Right arrow Citing Articles via CrossRef
Right arrow Citing Articles via Web of Science (36)
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Drechsler, Z.
Right arrow Articles by Beer, S.
Right arrow Search for Related Content
PubMed
Right arrow PubMed Citation
Right arrow Articles by Drechsler, Z.
Right arrow Articles by Beer, S.
Agricola
Right arrow Articles by Drechsler, Z.
Right arrow Articles by Beer, S.
Metabolism and Enzymology

Utilization of Inorganic Carbon by Ulva lactuca

Zivia Drechsler and Sven Beer

Department of Botany, Tel Aviv University, Tel Aviv 69978, Israel

Thalli discs of the marine macroalga Ulva lactuca were given inorganic carbon in the form of HCO3, and the progression of photosynthetic O2 evolution was followed and compared with predicted O2 evolution as based on calculated external formation of CO2 (extracellular carbonic anhydrase was not present in this species) and its carboxylation (according to the Km(CO2) of ribulose-1,5-bisphosphate carboxylase/oxygenase), at two different pHs, assuming a photosynthetic quotient of 1. The Km(inorganic carbon) was some 2.5 times lower at pH 5.6 than at the natural seawater pH of 8.2, whereas Vmax was similar under the two conditions, indicating that the unnaturally low pH per se had no adverse effect on U. lactuca's photosynthetic performance. These results, therefore, could be evaluated with regard to differential CO2 and HCO3 utilization. The photosynthetic performance observed at the lower pH largely followed that predicted, with a slight discrepancy probably reflecting a minor diffusion barrier to CO2 uptake. At pH 8.2, however, dehydration rates were too slow to supply CO2 for the measured photosynthetic response. Given the absence of external carbonic anhydrase activity, this finding supports the view that HCO3 transport provides higher than external concentrations of CO2 at the ribulose-1,5-bisphosphate carboxylase/oxygenase site. Uptake of HCO3 by U. lactuca was further indicated by the effects of potential inhibitors at pH 8.2. The alleged band 3 membrane anion exchange protein inhibitor 4,4'-diisothiocyanostilbene-2,2'disulphonate reduced photosynthetic rates only when HCO3 (but not CO2) could be the extracellular inorganic carbon form taken up. A similar, but less drastic, HCO3-competitive inhibition of photosynthesis was obtained with Kl and KNO3. It is suggested that, under ambient conditions, HCO3 is transported into cells at defined sites either via facilitated diffusion or active uptake, and that such transport is the basis for elevated internal [CO2] at the site of ribulose-1,5-bisphosphate carboxylase/oxygenase carboxylation.





This article has been cited by other articles:


Home page
J. Exp. Biol.Home page
P Furla, I Galgani, I Durand, and D Allemand
Sources and mechanisms of inorganic carbon transport for coral calcification and photosynthesis
J. Exp. Biol., January 11, 2000; 203(22): 3445 - 3457.
[Abstract] [PDF]




HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
ASPB Publications PLANT PHYSIOLOGY® THE PLANT CELL
Copyright © 1991 by the American Society of Plant Biologists