Photosynthesis and calcification by Emiliania huxleyi (Prymnesiophyceae) as a function of inorganic carbon species

Citation
Et. Buitenhuis et al., Photosynthesis and calcification by Emiliania huxleyi (Prymnesiophyceae) as a function of inorganic carbon species, J PHYCOLOGY, 35(5), 1999, pp. 949-959
Citations number
33
Categorie Soggetti
Aquatic Sciences
Journal title
JOURNAL OF PHYCOLOGY
ISSN journal
00223646 → ACNP
Volume
35
Issue
5
Year of publication
1999
Pages
949 - 959
Database
ISI
SICI code
0022-3646(199910)35:5<949:PACBEH>2.0.ZU;2-4
Abstract
To test the possibility of inorganic carbon limitation of the marine unicel lular alga Emiliania huxleyi (Lohmann) Hay and Mohler, its carbon acquisiti on was measured as a function of the different chemical species of inorgani c carbon present in the medium. Because these different species are interde pendent and covary in any experiment in which the speciation is changed, a set of experiments was performed to produce a multidimensional carbon uptak e scheme for photosynthesis and calcification. This scheme shows that CO2 t hat is used for photosynthesis comes from two sources. The CO2 in seawater supports a modest rate of photosynthesis. The HCO3- is the major substrate for photosynthesis by intracellular production of CO2 (HCO3- + H+ --> CO2 H2O --> CH2O + O-2). This use of HCO3- is possible because of the simultan eous calcification using a second HCO3-, which provides the required proton (HCO3- + Ca2+ --> CaCO3 + H+). The HCO3- is the only substrate for calcifi cation. By distinguishing the two sources of CO2 used in photosynthesis, it was shown that E. huxleyi has a K-1/2 for external CO2 of "only" 1.9 +/- 0 .5 mu M (and a V-max of 2.4 +/- 0.1 pmol.cell(-1).d(-1)). Thus, in seawater that is in equilibrium with the atmosphere ([CO2] = 14 mu M, [HCO3-] = 192 0 mu M, at fCO(2) = 360 mu atm, pH = 8, T = 15 degrees C), photosynthesis i s 90% saturated with external CO2. Under the same conditions, the rate of p hotosynthesis is doubled by the calcification route of CO2 supply (from 2.1 to 4.5 pmol.cell(-1).d(-1)). However, photosynthesis is not fully saturate d, as calcification has a K-1/2 for HCO3- of 3256 +/- 1402 mu M and a V-max of 6.4 +/- 1.8 pmol.cell(-1).d(-1). The H+ that is produced during calcifi cation is used with an efficiency of 0.97 +/- 0.08, leading to the conclusi on that it is used intracellularly. A maximum efficiency of 0.88 can be exp ected, as NO3- uptake generates a H+ sink (OH- source) for the cell. The su ccess of E. huxleyi as a coccolithophorid may be related to the efficient c oupling between H+ generation in calcification and CO2 fixation in photosyn thesis.