Decomposition of leaf and root tissue of three perennial grass species grown at two levels of atmospheric CO2 and N supply

Leaf and root tissue of Lolium perenne L., Agrostis capillaris L. and Festu ca ovina L. grown under ambient (350 mu l l(-1) CO2) and elevated (700 mu l l(-1)) CO2 in a continuously C-14-labelled atmosphere and at two soil N le vels, were incubated at 14 degrees C for 222 days. Decomposition of leaf an d root tissue grown in the low N treatment was not affected by elevated [CO 2], whereas decomposition in the high N treatment was significantly reduced by 7% after 222 days. Despite the increased C/N ratio (g g(-1)) of tissue cultivated at elevated [CO2] when compared with the corresponding ambient t issue, there was no significant correlation between initial C/N ratio and C -14 respired. This finding suggests that the CO2-induced changes in decompo sition rates do not occur via CO2-induced changes in C/N ratios of plant ma terials. We combined the decomposition data with data on C-14 uptake and al location for the same plants, and give evidence that elevated [CO2] has the potential to increase soil C stores in grassland via increasing C uptake a nd shifting C allocation towards the roots, with an inherent slower decompo sition rate than the leaves. An overall increase of 15% in C-14 remaining a fter 222 days was estimated for the combined tissues, i.e., the whole plant s; the leaves made a much smaller contribution to the C remaining (+6%) tha n the roots (+26%). This shows the importance of clarifying the contributio n of roots and leaves with respect to the question whether grassland soils act as a sink or source for atmospheric CO2.