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. 2015 Mar 9;112(12):3752–3757. doi: 10.1073/pnas.1415123112

Fig. 3.

Fig. 3.

C response to decomposability of deep C in the fully forced C−N case. (A) Soil and litter C changes over the permafrost region. (B) Change in total ecosystem C as a function of varied Zτ parameter. (C) Change in vegetation C. Slight increase in vegetation between cases is due to enhanced N mineralization from deep soils.