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Breakup of Ancient Supercontinent Tied to Rise of Complex Life, New Study Finds

Deep-time modeling of plate motions and carbon fluxes points to cooler climates that enabled oxygenated shallow seas.

Overview

  • The peer-reviewed research, published October 27 in Earth and Planetary Science Letters, was led by the University of Sydney’s EarthByte Group with collaborators from the University of Adelaide.
  • Computer simulations reconstructing 1.8 billion years of plate history place the fragmentation of Nuna at roughly 1.46 billion years ago.
  • The model shows continental shelves expanded to about 130,000 kilometers, creating extensive stable shallow-water habitats suited to early eukaryotes.
  • Shortened subduction zones reduced volcanic CO2 outgassing while geological carbon storage increased, cooling the planet and promoting marine oxygenation.
  • The timing aligns with the oldest fossil eukaryotes near 1.05 billion years ago, supporting a testable reinterpretation of the so-called Boring Billion as dynamic rather than static.