Increasing precipitation (WET) speeds up litter decomposition, while decreasing precipitation (DRY) slows it down.
In arid regions litter decomposition is more sensitive to WET, while in humid regions it’s more sensitive to DRY.
A double asymmetric model best explains the litter decomposition-altered precipitation relationships.
Meta-analyses confirm that this asymmetrical effect between humid and arid regions is true globally.
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Time to 95% decomposition in WET and DRY relative to CK (mean, n = 3)
Dynamics and average moisture content of the surface soil (0-5 cm) in the treatments in A, the humid region and B, the arid region (mean or mean ± SD, n = 3)
Litter microbial biomass carbon (MBC, A) and nitrogen (MBN, B) concentrations in the treatments after two years of decomposition (mean ± 1.5 SD, n = 3)
Litter enzymatic activity (β-glucosidase, A; β-N-acetyl-glucosaminnidase, B and acid phosphatase, C) in the treatments after two years of decomposition (mean ± 1.5 SD, n = 3)
Responses of the rate of litter decomposition, soil moisture content, microbial biomass and enzymatic activity to the effect of increased (A) and decreased (B) precipitation as a percentage relative to the control from the meta-analysis