Soil organic carbon (SOC) decreases by 28% along the 3,994–5,120 m alpine gradient.
This decline is linked to trade-offs between ectomycorrhizal fungi and non-ligninolytic saprotrophs.
At higher elevations, ectomycorrhizal fungi dominate, linked to peroxidase activity and SOC turnover.
SOC fate is linked to trade-offs between fungal guilds along elevation gradients in alpine ecosystems.
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Information about the sampling sites
The changes in soil organic carbon (SOC) content along an elevational gradient
The changes in the relative abundance of fungal guilds along an elevational gradient.
Fungal community composition and its relationship with SOC content across an elevational gradient in alpine ecosystems
Main fungal predictors of SOC content
Relationships between fungal genera and SOC content (A) and soil fertility (B)
The relationships between environmental factors and fungal guild composition