Global Change Biology · 2022 · 28 citations · 100 references
AgricultureEarth SciencesSoil SciencesSoil BiogeochemistrySoil ChemistrySoil ScienceOrganic Matter TurnoverPlant-soil InteractionsSoil Carbon ChemistrySoil Fauna EcologySoil Organic Matter ChemistrySoil Organic Matter FractionsCarbon Cycling DynamicsForest Soil FaunaLitter RemovalSoil Carbon StocksSoil Community DynamicsSoil Microbial TurnoverSoil Organic CarbonSoil Organic Carbon Turnover
Forest ecosystems are important global soil carbon (C) reservoirs, but their capacity to sequester C is susceptible to climate change factors that alter the quantity and quality of C inputs. To better understand forest soil C responses to altered C inputs, we integrated three molecular composition published data sets of soil organic matter (SOM) and soil microbial communities for mineral soils after 20 years of detrital input and removal treatments in two deciduous forests: Bousson Forest (BF), Harvard Forest (HF), and a coniferous forest: H.J. Andrews Forest (HJA). Soil C turnover times were estimated from radiocarbon measurements and compared with the molecular-level data (based on nuclear magnetic resonance and specific analysis of plant- and microbial-derived compounds) to better understand how ecosystem properties control soil C biogeochemistry and dynamics. Doubled aboveground litter additions did not increase soil C for any of the forests studied likely due to long-term soil priming. The degree of SOM decomposition was higher for bacteria-dominated sites with higher nitrogen (N) availability while lower for the N-poor coniferous forest. Litter exclusions significantly decreased soil C, increased SOM decomposition state, and led to the adaptation of the microbial communities to changes in available substrates. Finally, although aboveground litter determined soil C dynamics and its molecular composition in the coniferous forest (HJA), belowground litter appeared to be more influential in broadleaf deciduous forests (BH and HF). This synthesis demonstrates that inherent ecosystem properties regulate how soil C dynamics change with litter manipulations at the molecular-level. Across the forests studied, 20 years of litter additions did not enhance soil C content, whereas litter reductions negatively impacted soil C concentrations. These results indicate that soil C biogeochemistry at these temperate forests is highly sensitive to changes in litter deposition, which are a product of environmental change drivers.
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IntCal13 and Marine13 Radiocarbon Age Calibration Curves 0–50,000 Years cal BP
Radiocarbon · 2010 · 10K citations · Full text
M. Francesca Cotrufo, Matthew D. Wallenstein, Claudia M. Boot et al. · Global Change Biology · 2012 · 3.3K citations · Full text
Agriculture, Ecology, Soil Sciences +17