Why might abundant shallow (epicontinental) seas have contributed cooling to the global climate?
A) More sunlight would have reflected off the shallow sea floor and directly back into space.
B) Shallow-water marine life forms would have consumed more methane, a greenhouse gas.
C) Extensive growth of corals and creatures that grew hard skeletal parts would have removed the greenhouse gas carbon dioxide from the ocean-atmosphere system.
D) More iron oxides would have precipitated out of the shallow waters, creating banded-iron formations (BIFs) , which are a greenhouse rock.
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