Similar response of labile and resistant soil organic matter pools to changes in temperature

By C. Fang, Pete Smith, J. Moncrieff, Jo U. Smith. Nature, 2005

787 citations recorded by the source corpus.

Subfields: Ecology, Global and Planetary Change, Soil Science

View Paper: https://www.semanticscholar.org/paper/515b878e61933da4200d7ef9ba38e282d37aaf7c

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Citations in the corpus

On the variability of respiration in terrestrial ecosystems: moving beyond Q10 (2006, background): “…questions regarding the temperature sensitivity of soil carbon pools with decadal turnover times (Giardina & Ryan, 2000; Davidson et al., 2000a; Fang et al., 2005; Knorr et al., 2005), the effects of permafrost melting and altered hydrologic budgets on organic matter decomposition at high…”
Microbial contributions to climate change through carbon cycle feedbacks (2008, background): “For example, other studies suggest that the temperature sensitivity of more recalcitrant substrates is similar (Fang et al., 2005; Conen et al., 2006) or less than (Luo et al.”
Methods for estimating temperature sensitivity of soil organic matter based on incubation data: A comparative evaluation (2015, methodology): “Therefore, there is an increasing concern on how temperature sensitivity (expressed as Q10, which measures the change in decay rates for a 10 K warming) depends on the SOM compounds and C qualities (Fang et al., 2005; Conant et al., 2008; Xu et al., 2012).”
Policy and technological constraints to implementation of greenhouse gas mitigation options in agriculture (2007, background): “, 2001) Increases in temperature could accelerate decomposition of soil organic matter, releasing stored soil C into the atmosphere (Knorr et al., 2005; Fang et al., 2005).”
Temperature sensitivity of soil carbon decomposition and feedbacks to climate change (2006, methodology): “Fang et al.(9) experimentally applied multiple cycles of varying temperature during a 108-day incubation and estimated the temperature sensitivity for each cycle.”
The likely impact of elevated [CO2], nitrogen deposition, increased temperature and management on carbon sequestration in temperate and boreal forest ecosystems: a literature review. (2007, background): “, 2005a) and others suggesting no effect (Giardina & Ryan, 2000; Fang et al., 2005); see Davidson & Janssens (2006) for a recent review.”
Bridging the gap between micro - and macro-scale perspectives on the role of microbial communities in global change ecology (2006, background): “The associated feedback from these changes has the potential to quickly increase or stabilize the increase in temperature (Luo et al. 2001; Fang et al. 2005; Knorr et al. 2005).”