Really interesting. Makes me think of Daisyworld and the Gaia Hypothesis. Daisyworld is a model Earth covered in black and white daisies, that either absorb or reflect light. In the model, black daisies need less light because they absorb more, increasing the Earth's heat absorption. White daisies absorb less so need more light, but also reflect more light back, increasing the surface albedo of the planet and lowerin…
We know that there are a number of homeostatic (self-regulating) processes that affect the proportion of CO2 in the atmosphere; if it wasn't homeostatic it would have drifted off to an extreme long ago. The key question is how well and how rapidly these mechanisms can respond to an increase in CO2 levels.
Take for example the great oxidation event happening 2.5 billion years ago. As oxygen excreting algae began to take over methane producing organisms, oxygen started to build up in the atmosphere - first slowly, as there were lots of stuff to oxidize, like methane and iron. Eventually, these naturals sinks were saturated and oxygen levels reached the critical toxic point for the other species, leading to a runaway die-off where more and more oxygen was released and methane - a strong green house gas - rapidly disappeared from the atmosphere. This shock was so massive it produced the 400 million year Huronian glaciation - a whole planet freeze unlike any since.
So I have full faith life on Earth will eventually restore the feedback loops and get the temperatures back in the sweet spot. I have less faith that this will happen soon, or that most species, humans included, can survive such a massive transition event.