New oceanic crust forms at ridges, while oceanic plates descend into the mantle at subduction zones. Different assumptions about changing plate boundaries lead to futures in which the Atlantic closes or continues to widen.
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CO₂
280ppm
Temp
14.3°C
Sea
0m
O₂
21%
Annual surface temperature from CESM (T): a model estimate, not a direct observation of the past.
0 Ma: pre-industrial climate/CO₂; modern sea-level and O₂ references.