Observations of the uptake of carbonyl sulfide (COS) by trees under elevated atmospheric carbon dioxide concentrations

• Main Authors: L. Sandoval-Soto, M. Kesselmeier, V. Schmitt, A. Wild, J. Kesselmeier
• Format: Article
• Language: English
• Published: Copernicus Publications 2012-08-01
• Series: Biogeosciences
• Online Access: http://www.biogeosciences.net/9/2935/2012/bg-9-2935-2012.pdf

Global change forces ecosystems to adapt to elevated atmospheric concentrations of carbon dioxide (CO<sub>2</sub>). We understand that carbonyl sulfide (COS), a trace gas which is involved in building up the stratospheric sulfate aerosol layer, is taken up by vegetation with the same triad of the enzymes which are metabolizing CO<sub>2</sub>, i.e. ribulose-1,5-bisphosphate carboxylase/oxygenase (Rubisco), phosphoenolpyruvate carboxylase (PEP-Co) and carbonic anhydrase (CA). Therefore, we discuss a physiological/biochemical acclimation of these enzymes affecting the sink strength of vegetation for COS. We investigated the acclimation of two European tree species, <i>Fagus sylvatica</i> and <i>Quercus ilex</i>, grown inside chambers under elevated CO<sub>2</sub>, and determined the exchange characteristics and the content of CA after a 1–2 yr period of acclimation from 350 ppm to 800 ppm CO<sub>2</sub>. We demonstrate that a compensation point, by definition, does not exist. Instead, we propose to discuss a point of uptake affinity (PUA). The results indicate that such a PUA, the CA activity and the deposition velocities may change and may cause a decrease of the COS uptake by plant ecosystems, at least as long as the enzyme acclimation to CO<sub>2</sub> is not surpassed by an increase of atmospheric COS. As a consequence, the atmospheric COS level may rise causing an increase of the radiative forcing in the troposphere. However, this increase is counterbalanced by the stronger input of this trace gas into the stratosphere causing a stronger energy reflection by the stratospheric sulfur aerosol into space (Brühl et al., 2012). These data are very preliminary but may trigger a discussion on COS uptake acclimation to foster measurements with modern analytical instruments.