Global Change Biology · 2005 · 154 citations · 38 references
AgricultureEcologySoil SciencesSoil BiogeochemistrySoil Organic MatterSoil ScienceOrganic Matter AccumulationPlant-soil InteractionsSoil Carbon FractionationSoil Enzyme ActivitySoil Nutrient CyclingSoil Organic Matter FractionsEnzyme ActivityFree Light Fraction Organic MatterLignin DegradationOccluded Light FractionOrganic Matter FractionationPhenol Oxidase ActivitySoil Organic Carbon FractionationSoil Organic Matter Effects On Nutrient Availability
Abstract Elevated CO 2 , N deposition and climate change can alter ecosystem‐level nutrient cycling both directly and indirectly. We explored the interactive effects of these environmental changes on extracellular enzyme activity and organic matter fractionation in soils of a California annual grassland. The activities of hydrolases (polysaccharide‐degrading enzymes and phosphatase) increased significantly in response to nitrate addition, which coincided with an increase in soluble C concentrations under ambient CO 2 . Water addition and elevated CO 2 had negative but nonadditive effects on the activities of these enzymes. In contrast, water addition resulted in an increase in the activities of lignin‐degrading enzymes (phenol oxidase and peroxidase), and a decrease in the free light fraction (FLF) of soil organic matter. Independent of treatment effects, lignin content in the FLF was negatively correlated with the quantity of FLF across all samples. Lignin concentrations were lower in the aggregate‐occluded light fraction (OLF) than the FLF, and there was no correlation between percent lignin and OLF quantity, which was consistent with the protection of soil organic matter in aggregates. Elevated CO 2 decreased the quantity of OLF and increased the OLF lignin concentration, however, which is consistent with increased degradation resulting from increased turnover of soil aggregates. Overall, these results suggest that the effects of N addition on hydrolase activity are offset by the interactive effects of water addition and elevated CO 2 , whereas water and elevated CO 2 may cause an increase in the breakdown of soil organic matter as a result of their effects on lignin‐degrading enzymes and soil aggregation, respectively.
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Organic matter and water‐stable aggregates in soils
J. M. Tisdall, JM Oades · Journal of Soil Science · 1982 · 6.2K citations
An enzymic 'latch' on a global carbon store
Chris Freeman, Nick Ostle, Hojeong Kang · Nature · 2001 · 1.3K citations