Between 60 and 40 thousand years ago, during the middle of the last glacial, atmospheric CO2 levels hovered around 200 ppm โ half of todayโs concentration.
Tree remains dated to this period have been discovered 600-700 meters atop the modern treeline in the Russian Altai mountains.
This suggests surface air temperatures were between 2ยฐC and 3ยฐC warmer than today during this glacial period.
Tree trunks dating to the Early Holocene (between 10.6 and 6.2 thousand years ago) have been found about 350 meters higher than the modern treeline edge.
This suggests summer temperatures were between 2ยฐC and 2.5ยฐC warmer than today during the Early Holocene when CO2 concentrations ranged between about 250 and 270 ppm.
None of this paleoclimate treeline or temperature evidence correlates with a CO2-driven climate.
โSamples of wood having an age of 10.6โ6.2โฏcal ka BP were [the Early Holocene]found about 350โฏm higher than the present treeline. It seems that the summer temperature was 2.0โ2.5โฏยฐC higher and annual precipitation was double that of the present dayโ
โBuried wood trunks by a glacier gave ages between 60 and 28โฏcal ka BP and were found 600โ700โฏm higher than the present upper treeline. This evidences a distinctly elevated treeline during MIS 3a and c. With a correction for tectonics, we reconstructed the summer warming to have been between 2.1 and 3.0โฏยฐC [higher than today].โ