Effects of Elevated CO2 on a Marine Antarctic Diatom
Boelen, P., van de Poll, W.H., van der Strate, H.J., Neven, I.A., Beardall, J. and Buma, A.G.J. 2011. Neither elevated nor reduced CO2 affects the photophysiological performance of the marine Antarctic diatom Chaetoceros brevis. Journal of Experimental Marine Biology and Ecology 406: 38-45.
According to the authors, no significant differences between the enhanced and reduced CO2 levels were found, with respect to either "growth, pigment content and composition, photosynthesis, photoprotection and RuBisCO activity," and so they concluded that "within the range tested, CO2 does not significantly affect the photophysiological performance of C. brevis." In these respects, they also note that their results "agree with other studies on marine diatoms showing little or no effect of elevated CO2 on growth (Burkhardt et al., 1999) or maximum rates of photosynthesis (Rost et al., 2003; Trimborn et al., 2009)," although they say that in still other studies "elevated CO2 concentrations enhanced growth rates (e.g., Riebesell et al., 1993; Clark and Flynn, 2000)," while adding that "a recent field study in the Southern Ocean (Tortell et al., 2008) showed an increase in phytoplankton productivity and the promotion of large chain-forming Chaetoceros species under elevated CO2."
In summing up the implications of their findings, the six scientists say their results suggest that "under saturating and limiting, as well as under dynamic and constant irradiance conditions, the marine Antarctic diatom C. brevis has the ability to adjust its cellular physiology in response to changing CO2 levels with minimal effects on growth and photosynthesis." And although this maintenance of the status quo could validly be considered to be a neutral response to elevated CO2, it could also be regarded as a positive finding, in light of the fact that climate alarmists generally contend that atmospheric CO2 enrichment will be bad for almost all oceanic life.
Burkhardt, S., Riebesell, U. and Zondervan, I. 1999. Effects of growth rate, CO2 concentration, and cell size on the stable carbon isotope fractionation in marine phytoplankton. Geochimica et Cosmochimica Acta 63: 3729-3741.
Clark, D.R. and Flynn, K.J. 2000. The relationship between the dissolved inorganic carbon concentration and growth rate in marine phytoplankton. Proceedings of the Royal Society of London Series B 267: 953-959.
Riebesell, U., Wolf-Gladrow, D.A. and Smetacek, V. 1993. Carbon-dioxide limitation of marine-phytoplankton growth-rates. Nature 361: 249-251.
Rost, B., Riebesell, U., Burkhardt, S. and Suitemeyer, D. 2003. Carbon acquisition of bloom-forming marine phytoplankton. Limnology and Oceanography 48: 55-67.
Tortell, P.D., Payne, C.D., Li, Y.Y., Trimborn, S., Rost, B., Smith, W.O, Riesselman, C., Dunbar, R.B., Sedwick, P. and DiTullio, G.R. 2008. CO2 sensitivity of Southern Ocean phytoplankton. Geophysical Research Letters 35: 10.1029/2007GL032583.
Trimborn, S., Wolf-Gladrow, D., Richter, K.U. and Rost, B. 2009. The effect of pCO2 on carbon acquisition and intracellular assimilation in four marine diatoms. Journal of Experimental Marine Biology and Ecology 376: 26-36.