repoman
Contributor
He left this part out of his Ordovician post:
This has important implications for the climate system, since chemical weathering of silicate rocks such as granite results in a drawdown of atmospheric CO2 and may therefore lead to global cooling. During the weathering process CO2 dissolves in water as acid, and is then transported to the ocean where the carbon is buried as carbonate rock.
I have looked at this in the past and it seems complicated. When there is a lot on carbon dioxide in the air and water (in whichever form) then past a certain point too much causes some of the ocean floor carbonate to dissolve? Lots of stuff involving the effects of depth as well.
having a hard time wrapping my head around this:
https://en.wikipedia.org/wiki/Carbonate_compensation_depth