https://en.wikipedia.org/wiki/Hyperoxia
This was a screenshot I took months ago while watching a Geology Hub upload on YT. It was a lightbulb moment for my understanding of mass extinction events, (the largest was 250ma). I’ve referenced this multiple times, so thought I might share. Perhaps you find it as interesting as I do.
That also makes me wonder how we do our studies on other planets and if there is a category for “not habitable, but it could be”
We can just barely sometimes tell the difference between a small neptune, a large earth, an ocean planets, a coteless ocean planet, and a hycean planet. Trying to guage not just habitability but also terraformability is a ways off yet.
We can start with size and surface temperature though. We’re not going to survive on a gas giant, and anything with a four digit temperature is right out.
Or similarly, “not habitable, but it could have been”. Subtle difference between the two.