During the 800,000 years prior to 1750, atmospheric CO2 varied from 180 ppm during glacial (cold) up to 300
ppm during interglacial (warm) periods.
During the last 800,000 years, CO2 fluctuated between about 180 ppm during ice ages and 280
ppm during interglacial warm periods.
Not exact matches
Before the industrial revolution, the natural level of atmospheric CO ₂
during warm
interglacials was around 280
ppm.
But
during these
interglacials the CO2 level was about 300
ppm, so I think the CO2 level had very little to do with the sea level rise.
Other processes must be responsible for the 40 - to 50 -
ppm pCO2 drawdown
during the initial transition from
interglacial to glacial conditions as well as for a comparable pCO2 increase
during the latter part of glacial terminatins.
Today, atmospheric CO2 is much higher; ~ 390
ppm and increasing by ~ 2
ppm yr - 1, giving a higher contribution to radiative forcing than would be expected
during the Last
Interglacial.
But the effect is limited: the six degrees temperature increases
during interglacials shows a 100
ppm increase in CO2.