Rapid Response to Experimental Warming of a Microbial Community Inhabiting High Arctic Patterned Ground Soil.

Increases in soil temperature of 0.4 °C were also recorded in chambers during autumn (SON; T value 3.47, p = 0.018), but OTCs only had a marginally significant effect on soil temperature in winter (DJF; p = 0.069, T value = −2.78; Figure 2 b).

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Despite the highly significant increase in CO 2 efflux rate from warmed soil, the measured effluxes from unchambered and chambered soils (0.081 and 0.117 μmol CO 2 m −2 s −1 , respectively) were lower than those from other vegetated High Arctic soils (0.2–3.0 μmol CO 2 m −2 s −1 ; [ 47 , 48 , 49 ]).

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