Long-term sensitivity of soil carbon turnover to warming

By S. W. Simpson, Jay Quade, P. Renne, Robert F. Butler, W. C. McIntosh, Naomi Levin, M. Domínguez‐Rodrigo, Michael J. Rogers. Nature, 2005

1,295 citations recorded by the source corpus.

Subfields: Global and Planetary Change

View Paper: https://www.semanticscholar.org/paper/7acce308406dc49c60cd57313ca65fdcda1143cb

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Citations in the corpus

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).”
Thermal adaptation of soil microbial respiration to elevated temperature. (2008, methodology): “recently been applied (e.g. Oechel et al. 2000; Luo et al. 2001; Kirschbaum 2004; Knorr et al. 2005) in a general sense to define adjustments in respiration that result from temperature-induced changes in microbial individuals, populations and ⁄ or communities.”
Microbial contributions to climate change through carbon cycle feedbacks (2008, background): “, 2005), which is consistent with kinetic theory which indicates greater temperature sensitivity for decomposition of recalcitrant carbon pools (Knorr et al., 2005).”
Temperature sensitivity of soil carbon decomposition and feedbacks to climate change (2006, background): “In contrast, Knorr et al. 10 came to a conclusion consistent with kinetic theory when they fitted data from a laboratory soil incubation experiment 56 to a multi-pool soil C model.”
Soils and climate change: potential impacts on carbon stocks and greenhouse gas emissions, and future research for Australian agriculture (2012, positive): “Knorr et al. (2005) also showed that the relative temperature sensitivity of SOC fractions increased as the stability of the SOC fraction against biological attack increased.”
Consistent temperature dependence of respiration across ecosystems contrasting in thermal history (2012, background): “…limitation, driven by either differential temperature dependencies of mineralisation of labile and recalcitrant soil carbon pools (Kirschbaum, 2004; Knorr et al., 2005), or limitation of plant respiration by the supply rate of reduced substrates from photosynthesis (Dewar et al., 1999; Atkin &…”
Differential Growth Responses of Soil Bacterial Taxa to Carbon Substrates of Varying Chemical Recalcitrance (2011, background): “This together with the fact that soil C pools are heterogeneous and vary in chemical recalcitrance and turnover times (Dixon et al., 1994; Lichtfouse et al., 1995; Knorr et al., 2005) suggests that specialization on C substrates may contribute to the high phylogenetic diversity observed in soils.”
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, neutral): “The temperature response of litter at later stages of decomposition and of SOM is debatable, with some studies suggesting increasing sensitivity with decreasing quality (Ågren & Bosatta, 2002; Fierer et al., 2005; Knorr et al., 2005a) and others suggesting no effect (Giardina & Ryan, 2000; Fang et a”
Past and future polar amplification of climate change: climate model intercomparisons and ice-core constraints (2006, background): “…Research, Royal Netherlands Meteorological Institute (KNMI), P.O. Box 201, 3730 AE De Bilt, The Netherlands F. Wolk Institut d’Astronomie et de Géophysique G. Lemaı̂tre, Université catholique de Louvain, Chemin du cyclotron, 2, 1348 Louvain-la-Neuve, Belgium Y. Yu LASG, Institute of…”
Biological enhancement of soil carbonate precipitation: passive removal of atmospheric CO2 (2008, background): “Recent work has shown that in general the organic carbon content of UK soils may be decreasing with time (Jones et al., 2005; Knorr et al., 2005), adding concern that weathering and erosion are removing soil carbon increasingly in response to climate change.”
The Temperature Dependence of the Carbon Cycle in Aquatic Ecosystems (2010, background): “In terrestrial ecosystems, the potential for strong positive feedbacks between warming and carbon sequestration through temperature-induced enhancement of microbial respiration is well established (Davidson and Janssens, 2006; Knorr et al. , 2005).”
Thermal acclimation of organic matter decomposition in an artificial forest soil is related to shifts in microbial community structure (2014, background): “On the other hand, it has also been suggested that the temperature sensitivity of SOM decomposition increases with increasing molecular complexity of substrates (Knorr et al., 2005; Davidson and Janssens, 2006; Hartley and Ineson, 2008; Craine et al., 2010; Conant et al., 2011).”
Synergistic effects of water temperature and dissolved nutrients on litter decomposition and associated fungi (2011, background): “, 2000; MEA, 2005), which might have profound effects in the carbon cycle (Clark, 2004; Knorr et al., 2005; Cornelissen et al., 2007).”