Aerobic carbon dioxide production data of permafrost-affected soils of the northeast Siberian polygonal tundra under different temperature treatments

We aerobically incubated soil samples from a polygon center (P3, 72° 22.5 N, 126° 29.4 E) on Samoylov, Northeast Siberia for 150 days. We used three soil layers ((i) surface active layer, (ii) bottom active layer, (iii) permafrost) and three different temperatures ((i) 1°C, (ii) 4°C, (iii) 8°C). For each sample we used 4 aliquots. CO2 production was measured via gas chromatography.