West African Craton - Snowball Earth

Snowball Earth

Proponents of the Snowball Earth theory claim that around 530 million years ago the Earth was going through an extremely cold period. The oceans were frozen to great depths, and their snow covering reflected the heat from the sun through cloudless skies. Only simple forms of life could survive in locations such as deep oceanic hydrothermal vents. At the end of this period the edges of the West African craton became highly active, throwing up a ring of volcanoes. The thermal activity was caused by excessive mantle heat that had built up below the craton, insulated by the lithosphere. The volcanic eruptions created a greenhouse effect on massive scale, melting the ice and releasing CO2 into the atmosphere. The climate quickly switched to one much warmer than today, resulting in the Cambrian explosion of life forms.

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