You’re conflating two different regimes of climate behavior. Pre industrial CO2 lagging temperature is entirely consistent with CO2’s role as both a feedback and a forcing, depending on context. During glacial-interglacial cycles, orbital changes initiated warming; as ice sheets partially melted, CO2 was released from oceans and permafrost, amplifying the warming. That’s why CO2 lagged initially. It was a feedback, not a trigger. The correlation appears because temperature drove CO2 at first, but the feedback amplified the signal, making subsequent warming stronger than the orbital forcing alone could explain. Ice core records consistently show this pattern.
Today’s situation is fundamentally different. We are injecting CO2 directly into the atmosphere at rates orders of magnitude faster than anything seen in the paleoclimate record. The initial trigger is anthropogenic, not orbital. The system still responds with feedbacks, but because the forcing is fast and global, CO2 now acts as the primary driver. That’s why incremental CO2 today matters: it’s no longer a slow feedback; it’s a rapid, externally imposed forcing that overwhelms the slow, background natural variability.
Past lag of CO2 = feedback. Present rapid rise = forcing. Both are consistent with physics, but context and rate determine which role dominates. The oxygen isotope curve shows feedbacks and natural variability, not a refutation of CO2 sensitivity today.