Input of easily available organic C and N stimulates microbial decomposition of soil organic matter in arctic permafrost soil
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文摘

We tested the response of decomposition in arctic soils to organic matter input.

Decomposition rates in organic topsoil were hardly affected by substrate additions.

Decomposition rates in mineral subsoil doubled after addition of organic C.

Decomposition rates of cryoturbated material doubled after addition of organic N.

Arctic C stocks might be diminished by increased C and N availability with warming.

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