A meta-analysis of the temporal dynamics of priming soil carbon decomposition by fresh carbon inputs across ecosystems. (October 2016)

• Record Type: Journal Article
• Authors: Luo, Zhongkui; Wang, Enli; Sun, Osbert J.
• Is Part Of: Soil biology and biochemistry. Volume 101(2016)
• Page Start: 96
• Page End: 103
• Publication Date: 2016-10
• Subjects: Carbon turnover -- Carbon isotopes -- Carbon modelling -- Data assimilation -- Priming effect -- Review -- Substrate quality -- Stoichiometry; Soil biochemistry -- Periodicals; Soil biology -- Periodicals; Sols -- Biochimie -- Périodiques; Sols -- Biologie -- Périodiques; Sols -- Microbiologie -- Périodiques; Bodembiologie; Biochemie; 631.46
• DOI: 10.1016/j.soilbio.2016.07.011
• Languages: English
• ISSNs: 0038-0717

Abstract

Abstract: Priming of soil organic matter decomposition by fresh carbon inputs is a key ecological process determining soil carbon (C) and nutrient cycling in terrestrial ecosystems. Although this priming effect (PE) has been studied under various environmental conditions, the conclusions are inconsistent across space and time and the underlying mechanisms unclear. We used a meta-analysis with extensive datasets of CO2 effluxes from soils with 13 C or 14 C labelled fresh C inputs and without fresh C inputs under various soil conditions to synthesize and assess the temporal dynamics of the PE. The results indicated that the PE declined in 20 days on average from 67 − 21 + 26 % (95% confidence interval) immediately following the fresh C inputs to less than 7.6 − 1.8 + 2.0 % and remained relatively stable thereafter. We also assessed the variability of the temporal dynamics of the PE in the collected datasets and the underlying drivers. The results showed that the magnitude of PE at a specific time (i.e., the instantaneous PE after the fresh C inputs) was significantly and positively correlated with the instantaneous quantity of remaining fresh C. Under the same quantity of remaining fresh C, the PE varied significantly across ecosystems (in the order of grasslands < farmlands < forests < other ecosystems such as lake beds and volcanic soils), but, contrary to our expectation, the PE was independent of the quality of the added fresh C. We found that the PE experienced a faster decrease in soils with higher clay and moisture contents. These results describe the temporal dynamics of PE and the underlying drivers, underpinning the robust predictions of PE dynamics and their impact on soil C and nutrient balances. Highlights: The datasets from 171 experiments were used to assess the temporal PE dynamics. The average PE declines from 67% to <10% in 20 days after fresh C inputs. The quantity not the quality of fresh C significantly affects the PE temporal dynamics. The PE varies significantly across ecosystems under certain fresh C inputs. The PE decreases faster with time in soils with higher clay and moisture content.