The DOI matches its Crossref record; 35 of the 35 references it cites were found in a registry or an index.
Soil respiration under prolonged soil warming: are rate reductions caused by acclimation or substrate loss?
Abstract
The world's soils contain a large amount of carbon so that even a fractionally small loss or gain could have a quantitatively important feedback effect on net CO 2 emissions to the atmosphere. It is therefore important to fully understand the temperature dependence of soil‐carbon decomposition. Evidence from various observations can be used to quantify the temperature dependence of carbon efflux, but it is important to ensure that confounding factors, such as changing water relations or availability of readily decomposable substrate, are fully considered in inferring an underlying temperature response from observed response patterns. A number of recent findings from soil‐warming experiments have led to the suggestion that stimulation of soil‐carbon efflux by increasing temperature is only transitory before acclimation takes place and carbon efflux rates return to similar rates as before the increase in temperature. It is shown here that this response pattern can be explained through a simple two‐pool soil‐carbon model with no acclimation response needing to be invoked. The temporal pattern is, instead, due to depletion of readily decomposable substrate. It shows that findings of reduced respiration rate in soil‐warming experiments are consistent with unchanged high temperature sensitivity of organic carbon decomposition and affirms that there is, indeed, a danger of positive feedback between global warming and the release of soil organic carbon that can lead to further warming.
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Cites
THE VERTICAL DISTRIBUTION OF SOIL ORGANIC CARBON AND ITS RELATION TO CLIMATE AND VEGETATION
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Batjes, N. H. (2014) · European Journal of Soil Science · doi:10.1111/ejss.12114_2 · Cited by 2,550
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Self-citationSoil Warming and Carbon-Cycle Feedbacks to the Climate System
Melillo, J. M., Steudler, P. A., Aber, J. D., Newkirk, K., Lux, H., Bowles, F. P., Catricala, C., Magill, A., Ahrens, T., & Morrisseau, S. (2002) · Science · doi:10.1126/science.1074153 · Cited by 1,380
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AGE OF SOIL ORGANIC MATTER AND SOIL RESPIRATION: RADIOCARBON CONSTRAINTS ON BELOWGROUND C DYNAMICS
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Cited by
Temperature sensitivity of soil carbon decomposition and feedbacks to climate change
Davidson, E. A., & Janssens, I. A. (2006) · Nature · doi:10.1038/nature04514 · Cited by 6,919
Soil enzymes in a changing environment: Current knowledge and future directions
Burns, R. G., DeForest, J. L., Marxsen, J., Sinsabaugh, R. L., Stromberger, M. E., Wallenstein, M. D., Weintraub, M. N., & Zoppini, A. (2013) · Soil Biology and Biochemistry · doi:10.1016/j.soilbio.2012.11.009 · Cited by 2,552
Conant, R. T., Ryan, M. G., Ågren, G. I., Birge, H. E., Davidson, E. A., Eliasson, P. E., Evans, S. E., Frey, S. D., Giardina, C. P., Hopkins, F. M., et al. (2011) · Global Change Biology · doi:10.1111/j.1365-2486.2011.02496.x · Cited by 1,635
Self-citationHow strongly can forest management influence soil carbon sequestration?
Jandl, R., Lindner, M., Vesterdal, L., Bauwens, B., Baritz, R., Hagedorn, F., Johnson, D. W., Minkkinen, K., & Byrne, K. A. (2007) · Geoderma · doi:10.1016/j.geoderma.2006.09.003 · Cited by 1,458
Hyvönen, R., Ågren, G. I., Linder, S., Persson, T., Cotrufo, M. F., Ekblad, A., Freeman, M., Grelle, A., Janssens, I. A., Jarvis, P. G., et al. (2007) · New Phytologist · doi:10.1111/j.1469-8137.2007.01967.x · Cited by 688
Metadata
- Authors
- Kirschbaum, M. U. F.
- Venue
- Global Change Biology
- Publisher
- Wiley
- Published
- 2004-10-25
- Volume
- 10
- Issue
- 11
- Pages
- 1870-1877
- ISSN
- 1354-1013 (ISSN-L)
- 1365-2486
- OpenAlex
- W2156657148
- Cited by
- 377
- References
- 35
- FWCI
- 19.83
- Type
- journal article
- Language
- en
- Open access
- closed
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