Increasing temperatures stimulate the decomposition of soil organic matter in the short term. But a shift in microbial carbon allocation could mitigate this response over longer periods of time.
This is a preview of subscription content, access via your institution
Access options
Subscribe to this journal
Receive 12 print issues and online access
$259.00 per year
only $21.58 per issue
Buy this article
- Purchase on Springer Link
- Instant access to full article PDF
Prices may be subject to local taxes which are calculated during checkout
References
Schimel, D. S. Glob. Change Biol. 1, 77–91 (1995).
Kirschbaum, M. U. F. Soil Biol. Biochem. 38, 2510–2518 (2006).
Melillo, J. M. et al. Science 298, 2173–2176 (2002).
Eliasson, P. E. et al. Glob. Change Biol. 11, 167–181 (2005).
Allison, S. D., Wallenstein, M. D. & Bradford, M. A. Nature Geosci. 3, 336–340 (2010).
Kirschbaum, M. U. F. Glob. Change Biol. 10, 1870–1877 (2004).
Balser, T. C. & Wixon, D. L. Glob. Change Biol. 15, 2935–2949 (2009).
von Lützow, M. et al. Eur. J. Soil Sci. 57, 426–445 (2006).
Kemmitt, S. J. et al. Soil Biol. Biochem. 40, 61–73 (2008).
Author information
Authors and Affiliations
Rights and permissions
About this article
Cite this article
Ågren, G. Microbial mitigation. Nature Geosci 3, 303–304 (2010). https://doi.org/10.1038/ngeo857
Issue Date:
DOI: https://doi.org/10.1038/ngeo857
This article is cited by
-
Microorganisms and climate change: terrestrial feedbacks and mitigation options
Nature Reviews Microbiology (2010)