Scientists link Earth's missing billion years of rock record to deep mantle processes

Researchers Santosh Dhungana and Nicolas Flament modelled the formation and breakup of ancient supercontinents to test how the Great Unconformity formed. They argue it is a surface result of deep mantle-driven geodynamic processes that reshaped global landscapes and sediment flow. The article also covers octopus squeezing behaviour and a proposal that a British Iron Age ruler named Verica was a woman, but neither has any security relevance.

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