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
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.