Acclimatization of soil respiration to warming in a tall grass prairie

By Yiqi Luo, S. Wan, D. Hui, L. Wallace. Nature, 2001

1,245 citations recorded by the source corpus.

Subfields: Forestry, Global and Planetary Change, Soil Science

View Paper: https://www.semanticscholar.org/paper/fc050aa14944621fa9816a7b719003c141a1bbdd

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Citations in the corpus

Linking the global carbon cycle to individual metabolism (2005, methodology): “(b) Standardized fluxes of CO2 from soils measured over multiple seasons in the field [compilation in Lloyd & Taylor (1994) supplemented with data in Boone et al. (1998); Keith et al. (1997); Luo et al. (2001) ].”
The microbial aspect of climate change (2016, background): “…between 1.4 and 5.8 C by 2100 (World Meteorological Organization Web site), and predictions state that a surge of worldwide temperature by 2 C would increase soil carbon release by 106 kg (10 petagrams) CO2 and other greenhouse gases (Raich and Potter 1995; Luo et al. 2001; Pendall et al. 2004).”
Adaptation of soil microbial communities to temperature: comparison of fungi and bacteria in a laboratory experiment (2009, result): “Similar results, seen in soil, where the magnitude of the initial respiration response declined over time when a soil was exposed to increased temperature, were initially also interpreted as thermal acclimation of the soil microorganisms (e.g. Luo et al., 2001).”
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).”
Integrating microbial ecology into ecosystem models: challenges and priorities (2012, background): “However, in field-based studies, warming-induced increases in soil respiration rates can be short-lived, returning to pre-warming levels within a decade or so (Jarvis and Linder 2000; Luo et al. 2001; Melillo et al. 2002; Oechel et al. 2000; Rustad et al. 2001).”
Microbial responses to a changing environment: implications for the future functioning of terrestrial ecosystems (2011, background): “Although some microorganisms may physiologically acclimate to warmer soil temperatures by lowering respiration rates (Luo et al. 2001; Bradford et al. 2008), others do not (Kirchbaum 2006; Malcolm et al. 2009; Vanhala et al. 2010).”
Microbial mediation of carbon-cycle feedbacks to climate warming (2012, background): “On the basis of our previous studies related to above-ground plant community dynamics and ecosystem processe”
Root respiration in temperate mountain grasslands differing in land use (2006, background): “There is substantial evidence on grassland soil C fluxes under changing climate scenarios, such as rising temperatures (e.g. Luo et al., 2001; Edwards et al., 2004; Zhang et al., 2005), elevated CO2 (e.g. Hungate et al., 1997; Niklaus et al., 2001; Gill et al., 2002; Pendall et al., 2003) and…”
Temperature sensitivity of soil organic matter decomposition—what do we know? (2009, background): “The decay rate of the labile SOM is very temperaturesensitive, but not the decay rate of stable SOM (Bradford et al. 2008; Eliasson et al. 2005; Liski et al. 1999; Luo et al. 2001; Melillo et al. 2002; Oechel et al. 2000; Trumbore et al. 1996).”
Acclimation to temperature and temperature sensitivity of metabolism by ectomycorrhizal fungi (2008, background): “…values found for roots in a variety of plant species (Pregitzer et al., 2000 and references therein) and to values found for decomposer microorganisms (Luo et al., 2001; Janssens & Pilegaard, 2003) with some exceptions noted in the literature (Larigauderie & Körner, 1995; Davidson et al., 1998).”
Microbial contributions to climate change through carbon cycle feedbacks (2008, background): “, 1999), and whether short-term increases in carbon mineralization—which are commonly observed in warming experiments in the field (Luo et al., 2001; Melillo et al., 2002)—will be sustained due to depletion of substrate availability and acclimation of soil microbial communities to higher temperature”
Response of mycorrhizal, rhizosphere and soil basal respiration to temperature and photosynthesis in a barley field (2007, background): “Such seasonal Q10 changes have been already observed in a number of studies (Luo et al., 2001; Xu and Qi, 2001; Janssens and Pilegaard, 2003).”