"Ocean acidification in response to rising atmospheric CO2 partial pressures is widely expected to reduce calcification by marine organisms. From the mid-Mesozoic, coccolithophores have been major calcium carbonate producers in the world's oceans, today accounting for about a third of the total marine CaCO3 production. Here, we present laboratory evidence that calcification and net primary production in the coccolithophore species Emiliania huxleyi are significantly increased by high CO2 partial pressures. Field evidence from the deep ocean is consistent with these laboratory conclusions, indicating that over the past 220 years there
has been a 40% increase in average coccolith mass. Our findings show that coccolithophores are already responding and will probably continue to respond to rising atmospheric CO2 partial pressures, which has important implications for biogeochemical modeling of future oceans and climate."
Phytoplankton Calcification in a High-CO2 World
Impact of Coccolith Formation on the Carbon Cycle
Thomas J. Goreau
Global Coral Reef Alliance, Cambridge, MA 02139, USA
The Research Article "Phytoplankton calcification in a high-CO2 world" (M. D. Iglesias-Rodriguez et al., 18 April 2008, p. 336) presents data from lab cultures showing that coccolithophorids produce more limestone skeleton under a high CO2 environment. This contradicts widespread claims that increasing CO2 in seawater will cause them to dissolve, assuming the internal milieu is the same as the external one, which is not true for any known organism.
Their results are no surprise. In the carbon balance model of coccolith formation (1), based on models of coral calcification (2, 3), photosynthesis removes CO2, increasing internal pH. This promotes calcification as a mechanism of pH homeostasis, obviating the need for metabolically-costly alkalinity efflux or proton influx. If this is the dominant mode of pH regulation, the photosynthesis to calcification ratio must be close to 1, as found in corals and calcareous algae, including coccolithophores (4). Any factor increasing photosynthesis leads to equal increases in calcification. Non-photosynthesizing deep-sea corals and mollusks (except Tridacnids), must generate alkalinity through costly proton and bicarbonate pumping, but their internal milieu is also greatly different than surrounding water. Deep sea ahermatypic corals have no problem growing skeletons in water undersaturated in skeletal solubility, and are hardly threatened by decreasing ocean pH (5), although this should increase the metabolic energy they must expend.
A serious caveat is that Iglesias-Rodriguez et al.'s cultures were grown under high "nutrient-replete conditions" (nitrate 100 micromolar, phosphate 6.24 micromolar). Only when nutrients are in excess can phytoplankton be CO2 limited and increase growth rates when CO2 rises. These conditions are extremely abnormal in surface waters, other than sewage plumes or the most intense upwelling events. Coccolithophores should not show such responses in most ocean waters. This is reminiscent of the "CO2 fertilization effect" that predicts plants should grow faster as CO2 rises, as found in highly fertilized greenhouse plants, but not during normal nutrient-limited plant growth. Experiments with elevated CO2 under natural nutrient levels are needed to assess the real-world carbon cycle implications.
Thomas J. Goreau
Global Coral Reef Alliance, 37 Pleasant Street, Cambridge, MA 02139, USA.
References
1. E. Paasche, Phys. Plant. Suppl. 3, 1 (1964).
2. T. F. Goreau, Biol. Bull. 116, 59 (1959).
3. T. F. Goreau, Annals New York Academy of Sciences 109, 127 (1963).
4. T. J. Goreau, Proc. 3d. Int. Coral Reef Symp. 2, 395 (1977).
5. M. Fine, D. Tchernov, Science 315, 1811 (2007).
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Published 20 October 2008