Increasing temperatures are expected to increase decomposition rates in soils, potentially reducing ecosystem carbon storage. Research now indicates that — in a tropical montane forest — soil carbon stocks are unaffected by higher temperatures despite substantially increased rates of CO2 release from the soil.
This is a preview of subscription content, access via your institution
Relevant articles
Open Access articles citing this article.
-
Drivers of spatio-temporal changes in paddy soil pH in Jiangxi Province, China from 1980 to 2010
Scientific Reports Open Access 09 February 2018
-
Rising soil temperature in China and its potential ecological impact
Scientific Reports Open Access 21 October 2016
Access options
Subscribe to this journal
Receive 12 print issues and online access
$209.00 per year
only $17.42 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
Giardina, C. P., Litton, C. M., Crow, S. E. & Asner, G. P. Nature Clim. Change 4, 822–827 (2014).
Schmidt, M. et al. Nature 478, 49–56 (2011).
Torn, M. et al. Nature 389, 170–173 (1997).
Luo, Y., Hui, D. & Zhang, D. Ecology 87, 53–63 (2006).
Hassink, J. Plant Soil 191, 77–87 (1997).
Wiesmeier, M. et al. Glob. Change Biol. 20, 653–665 (2014).
Author information
Authors and Affiliations
Corresponding author
Rights and permissions
About this article
Cite this article
Hartley, I. Resisting climate change. Nature Clim Change 4, 760–761 (2014). https://doi.org/10.1038/nclimate2356
Published:
Issue Date:
DOI: https://doi.org/10.1038/nclimate2356
This article is cited by
-
Drivers of spatio-temporal changes in paddy soil pH in Jiangxi Province, China from 1980 to 2010
Scientific Reports (2018)
-
Rising soil temperature in China and its potential ecological impact
Scientific Reports (2016)