Decomposition of soil organic matter could be an important positive feedback to climate change. Geochemical properties of soils can help determine what fraction of soil carbon may be protected from climate-induced decomposition.
This is a preview of subscription content, access via your institution
Relevant articles
Open Access articles citing this article.
-
Developing a molecular picture of soil organic matter–mineral interactions by quantifying organo–mineral binding
Nature Communications Open Access 30 August 2017
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
Doetterl, S. et al. Nature Geosci. 8, 780–783 (2015).
Schlesinger, W. H. & Bernhardt, E. S. Biogeochemistry: An Analysis of Global Change (Elsevier, 2013).
Davidson, E. A. & Janssens, I. Nature 440, 165–173 (2006).
Sollins, P. et al. Biogeochemistry 96, 209–231 (2009).
Todd-Brown, K. E. O. et al. Biogeosciences 10, 1717–1736 (2013).
Author information
Authors and Affiliations
Corresponding author
Rights and permissions
About this article
Cite this article
Davidson, E. Soil carbon in a beer can. Nature Geosci 8, 748–749 (2015). https://doi.org/10.1038/ngeo2522
Published:
Issue Date:
DOI: https://doi.org/10.1038/ngeo2522
This article is cited by
-
Predicting Soil Organic Carbon Mineralization Rates Using δ13C, Assessed by Near-Infrared Spectroscopy, in Depth Profiles Under Permanent Grassland Along a Latitudinal Transect in Chile
Journal of Soil Science and Plant Nutrition (2022)
-
Developing a molecular picture of soil organic matter–mineral interactions by quantifying organo–mineral binding
Nature Communications (2017)