Journal
SOIL BIOLOGY & BIOCHEMISTRY
Volume 42, Issue 2, Pages 373-375Publisher
PERGAMON-ELSEVIER SCIENCE LTD
DOI: 10.1016/j.soilbio.2009.10.024
Keywords
Soil organic carbon; Warming; Grassland; Microbial respiration; Temperature sensitivity
Categories
Funding
- NSF [DEB-0816629]
- Research Experience for Undergraduates
- Direct For Biological Sciences
- Division Of Environmental Biology [0816629] Funding Source: National Science Foundation
- Direct For Biological Sciences
- Div Of Biological Infrastructure [0851835] Funding Source: National Science Foundation
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We examined landscape-level variation in temperature sensitivity of labile SOC across 71 sites at a central North American grassland. The observed range in activation energy of decomposition (E-a), an index of temperature sensitivity, was as great at the landscape scale as has been observed at the continental scale. E-a was lower for soils with more labile C, consistent with the 'Carbon quality-temperature' hypothesis. Soil pH explained 67% of the variation in E-a. Although there are strong environmental correlates with the E-a of SOC decomposition at landscape scales, the amount of variation within landscapes could confound regional-to global-scale predictions of the response of soil C to warming. (C) 2009 Elsevier Ltd. All rights reserved.
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