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iForest -Biogeosciences and Forestry
IntroductionForest ecosystems can be carbon sinks or sources depending on the balance between carbon input through photosynthesis and release from respiration (Saiz et al. 2006). In forest ecosystems, soil respiration (RS) can account for 30% to 80% of the whole ecosystem respiration (Davidson et al. 2000, Law et al. 2002, Davidson & Janssens 2006. Globally, RS is the second largest carbon exchange between the soil and atmosphere, and returns as much as 80 to 98 Pg C yr -1 back into the atmosphere (BondLamberty & Thomson 2010, Raich et al. 2002, which is more than 10 times the carbon release from fossil fuel combustion (IPCC 2007). Therefore, RS is one of the major contributors to the carbon balance, and small changes in RS rate could give rise to significant changes in atmospheric CO2 concentration, leading to feedbacks to climate change (Ryan & Law 2005). Although the significance of RS for carbon balance on a regional and even the global scale has been demonstrated, there is still much to understand about biotic or abiotic controllers of RS and its source components (Gomez-Casanovas et al. 2012). For example, partitioning RS is still challenging because of remarkable soil disturbances (Hanson et al. 2000, Tang et al. 2005. Spatial and temporal variability in RS are often reported due to high variations in forest types, stand ages and management practices (King et al. 2004, Tang & Baldocchi 2005, Saiz et al. 2006, Pang et al. 2013). This has limited our ability to accurately predict the responses of RS and carbon balance to current and future climate change (Ryan & Law 2005). Therefore, measuring RS in different forest types has been proven to be increasingly important to accurately predict global carbon cycles and its responses to climate change .RS is overwhelmingly comprised of rhizoshperic respiration (respiration from roots, mycorrhizae and microbial respiration in the rhizosphere) and heterotrophic respiration , indicating that the Moso bamboo forest studied is a significant carbon sink.