After 30 + million years of cooling, 2 to 3 million years ago,
colder ocean waters eventually upwelled in the mid latitudes along the west coasts of major continents as well as along the equator.
Not exact matches
And around Antarctica, where even the surface
ocean water is already quite
cold and dense, some of that
water in the
ocean depths, which is also carbon rich,
eventually warmed enough so that it became less dense than the
water above it.
Through a complex interplay among the
ocean, ice shelves, and atmosphere, very
cold, dense
water builds up on the continental shelves and
eventually spills over their edges, mixing with surrounding
water and sinking to the sea floor.