Chironomid-inferred temperatures (CI-T) ranging from the onset of the late-glacial to Early-Holocene has been reconstructed.
CI-T have been validated by cross-correlating with diatoms and pollen analyses.
Climate events such as, the GI-1e warming, the GS1 cooling and the early Holocene improvement have been recorded.
Cool regional conditions prevailed during the LGI and early-Holocene in the Aubrac region, which is always the case today due to temperature inversion processes and cool air stagnation in winter.