There, the carbon was crushed and cooked until it was
eventually returned to the surface by the clashing plates.
This cold polar water
eventually returns to the surface in a variety of different ways.
When those stored molecules
eventually return to the surface, pH can be lowered due to respiration of ancient carbon, independent of atmospheric CO2.
Not exact matches
Atlantic
surface waters
eventually return northward
to the Labrador and Greenland seas in the North Atlantic.