Temperature and soil C decomposition – synthesis of current knowledge and a way forward
(2011) In Global Change Biology 17(11). p.3392-3404- Abstract
- The response of soil organic matter (OM) decomposition to increasing temperature is a critical aspect of ecosystem responses to global change. The impacts of climate warming on decomposition dynamics have not been resolved due to apparently contradictory results from field and lab experiments, most of which has focused on labile carbon with short turnover times. But the majority of total soil carbon stocks are comprised of organic carbon with turnover times of decades to centuries. Understanding the response of these carbon pools to climate change is essential for forecasting longer-term changes in soil carbon storage. Herein, we briefly synthesize information from recent studies that have been conducted using a wide variety of approaches.... (More)
- The response of soil organic matter (OM) decomposition to increasing temperature is a critical aspect of ecosystem responses to global change. The impacts of climate warming on decomposition dynamics have not been resolved due to apparently contradictory results from field and lab experiments, most of which has focused on labile carbon with short turnover times. But the majority of total soil carbon stocks are comprised of organic carbon with turnover times of decades to centuries. Understanding the response of these carbon pools to climate change is essential for forecasting longer-term changes in soil carbon storage. Herein, we briefly synthesize information from recent studies that have been conducted using a wide variety of approaches. In our effort to understand research to-date, we derive a new conceptual model that explicitly identifies the processes controlling soil OM availability for decomposition and allows a more explicit description of the factors regulating OM decomposition under different circumstances. It explicitly defines resistance of soil OM to decomposition as being due either to its chemical conformation (quality) or its physico-chemical protection from decomposition. The former is embodied in the depolymerization process, the latter by adsorption/desorption and aggregate turnover. We hypothesize a strong role for variation in temperature sensitivity as a function of reaction rates for both. We conclude that important advances in understanding the temperature response of the processes that control substrate availability, depolymerization, microbial efficiency, and enzyme production will be needed to predict the fate of soil carbon stocks in a warmer world. (Less)
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https://lup.lub.lu.se/record/3808638
- author
- publishing date
- 2011
- type
- Contribution to journal
- publication status
- published
- subject
- keywords
- decomposition, experiments, new conceptual model, review, soil carbon, temperature sensitivity
- in
- Global Change Biology
- volume
- 17
- issue
- 11
- pages
- 3392 - 3404
- publisher
- Wiley-Blackwell
- external identifiers
-
- scopus:80053500787
- ISSN
- 1354-1013
- DOI
- 10.1111/j.1365-2486.2011.02496.x
- language
- English
- LU publication?
- no
- id
- 49f51604-fd2d-4eb6-a590-d9279133d348 (old id 3808638)
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- http://onlinelibrary.wiley.com/doi/10.1111/j.1365-2486.2011.02496.x/abstract
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@article{49f51604-fd2d-4eb6-a590-d9279133d348,
abstract = {{The response of soil organic matter (OM) decomposition to increasing temperature is a critical aspect of ecosystem responses to global change. The impacts of climate warming on decomposition dynamics have not been resolved due to apparently contradictory results from field and lab experiments, most of which has focused on labile carbon with short turnover times. But the majority of total soil carbon stocks are comprised of organic carbon with turnover times of decades to centuries. Understanding the response of these carbon pools to climate change is essential for forecasting longer-term changes in soil carbon storage. Herein, we briefly synthesize information from recent studies that have been conducted using a wide variety of approaches. In our effort to understand research to-date, we derive a new conceptual model that explicitly identifies the processes controlling soil OM availability for decomposition and allows a more explicit description of the factors regulating OM decomposition under different circumstances. It explicitly defines resistance of soil OM to decomposition as being due either to its chemical conformation (quality) or its physico-chemical protection from decomposition. The former is embodied in the depolymerization process, the latter by adsorption/desorption and aggregate turnover. We hypothesize a strong role for variation in temperature sensitivity as a function of reaction rates for both. We conclude that important advances in understanding the temperature response of the processes that control substrate availability, depolymerization, microbial efficiency, and enzyme production will be needed to predict the fate of soil carbon stocks in a warmer world.}},
author = {{Conant, Richard T. and Ågren, Göran I. and Birge, Hannah E. and Bradford, Mark A. and Davidson, Eric A. and Eliasson, Peter and Evans, Sarah E. and Frey, Serita D. and Giardina, Christian P. and Hopkins, Francesca and Hyvönen, Riita and Kirschbaum, Miko U. F. and Lavallee, Jocelyn M. and Leifeld, Jens and Parton, William J. and Steinweg, J. Megan and Wallenstein, Matthew D. and Wetterstedt, J. A. Martin and Ryan, Michael G.}},
issn = {{1354-1013}},
keywords = {{decomposition; experiments; new conceptual model; review; soil carbon; temperature sensitivity}},
language = {{eng}},
number = {{11}},
pages = {{3392--3404}},
publisher = {{Wiley-Blackwell}},
series = {{Global Change Biology}},
title = {{Temperature and soil C decomposition – synthesis of current knowledge and a way forward}},
url = {{http://dx.doi.org/10.1111/j.1365-2486.2011.02496.x}},
doi = {{10.1111/j.1365-2486.2011.02496.x}},
volume = {{17}},
year = {{2011}},
}