Abstract. Globally, soil temperature to 1 m depth is predicted to be up to 4 ∘C warmer by the end of this century, with pronounced effects
expected in temperate forest regions. Increased soil temperatures will
potentially increase the release of carbon dioxide (CO2) from temperate forest soils,
resulting in important positive feedback on climate change. Dark CO2
fixation by microbes can recycle some of the released soil CO2, and
CO2 fixation rates are reported to increase under higher temperatures.
However, research on the influence of temperature on dark CO2 fixation
rates, particularly in comparison to the temperature sensitivity of
respiration in soils of temperate forest regions, is missing. To determine
the temperature sensitivity (Q10) of dark CO2 fixation and
respiration rates, we investigated soil profiles to 1 m depth from beech
(deciduous) and spruce (coniferous) forest plots of the Hummelshain forest,
Germany. We used 13C-CO2 labelling and incubations of soils at 4
and 14 ∘C to determine CO2 fixation and net soil respiration
rates and derived the Q10 values for both processes with depth. The
average Q10 for dark CO2 fixation rates normalized to soil dry
weight was 2.07 for beech and spruce profiles, and this was lower than the
measured average Q10 of net soil respiration rates with ∼2.98. Assuming these Q10 values, we extrapolated that net soil
respiration might increase 1.16 times more than CO2 fixation under a
projected 4 ∘C warming. In the beech soil, a proportionally
larger fraction of the label CO2 was fixed into soil organic carbon
than into microbial biomass compared to the spruce soil. This suggests
a primarily higher rate of microbial residue formation (i.e. turnover as
necromass or release of extracellular products). Despite a similar abundance
of the total bacterial community in the beech and spruce soils, the beech
soil also had a lower abundance of autotrophs, implying a higher proportion
of heterotrophs when compared to the spruce soil; hence this might partly explain
the higher rate of microbial residue formation in the beech soil.
Furthermore, higher temperatures in general lead to higher microbial
residues formed in both soils. Our findings suggest that in temperate forest
soils, CO2 fixation might be less responsive to future warming than net
soil respiration and could likely recycle less CO2 respired from
temperate forest soils in the future than it does now.