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by cbkeller
1607 days ago
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That certainly doesn't help either! To some extent though, anthropogenic emissions are dangerous more for their rate than their absolute magnitude; in the long run, once we stop emitting, silicate weathering will take back over "soon enough" -- it's just that "soon enough" in this case means ~5 myr and probably a mass extinction later. The other one I forgot to mention is that the sun is a bit brighter now than it was 700 Myr ago (by perhaps a few percent). Go back another two or three billion years to the Archean and the difference would have been bigger -- to the point that we have some trouble explaining why there weren't a lot more snowballs back then [1] [1] https://en.wikipedia.org/wiki/Faint_young_Sun_paradox |
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