Warming prevents the elevated CO2-induced reduction in available soil nitrogen in a temperate, perennial grassland
Article first published online: 31 JAN 2008
DOI: 10.1111/j.1365-2486.2008.01558.x
© 2008 The Authors
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How to Cite
HOVENDEN, M. J., NEWTON, P. C. D., CARRAN, R. A., THEOBALD, P., WILLS, K. E., VANDER SCHOOR, J. K., WILLIAMS, A. L. and OSANAI, Y. (2008), Warming prevents the elevated CO2-induced reduction in available soil nitrogen in a temperate, perennial grassland. Global Change Biology, 14: 1018–1024. doi: 10.1111/j.1365-2486.2008.01558.x
Publication History
- Issue published online: 31 JAN 2008
- Article first published online: 31 JAN 2008
- Received 30 July 2007; revised version received 13 November 2007 and accepted 19 November 2007
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Keywords:
- biogeochemistry;
- elevated CO2;
- FACE;
- progressive nitrogen limitation;
- warming
Abstract
Rising atmospheric carbon dioxide concentration ([CO2]) has the potential to stimulate ecosystem productivity and sink strength, reducing the effects of carbon (C) emissions on climate. In terrestrial ecosystems, increasing [CO2] can reduce soil nitrogen (N) availability to plants, preventing the stimulation of ecosystem C assimilation; a process known as progressive N limitation. Using ion exchange membranes to assess the availability of dissolved organic N, ammonium and nitrate, we found that CO2 enrichment in an Australian, temperate, perennial grassland did not increase plant productivity, but did reduce soil N availability, mostly by reducing nitrate availability. Importantly, the addition of 2 °C warming prevented this effect while warming without CO2 enrichment did not significantly affect N availability. These findings indicate that warming could play an important role in the impact of [CO2] on ecosystem N cycling, potentially overturning CO2-induced effects in some ecosystems.

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