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Neoproterozoic Era

geochronology
Also known as: Late Proterozoic Era

Quick Summary

The Neoproterozoic Era is the most recent of the three periods of the Proterozoic Eon, spanning from 1 billion to 541 million years ago. It followed the Mesoproterozoic Era and preceded the Cambrian Period. This era is characterized by significant geological and biological developments.1

Key Features of the Neoproterozoic Era:

  • Geological Activity: Earth's landmasses were consolidated into the supercontinent Rodinia at the beginning of the preceding era, but near the end of the Neoproterozoic, this supercontinent began to break apart.2
  • Atmospheric Changes: The atmosphere was largely devoid of oxygen during this time, though concentrations began to rise, increasing to about 1 percent of present-day levels between 900 million and 800 million years ago.2
  • Biological Evolution: The earliest ancestors of green algae and seaweed appeared as unicellular and primitive multicellular forms. These organisms survived glaciations and later diversified.2

The Neoproterozoic Era is subdivided into the Tonian, Cryogenian, and Ediacaran periods, with the Tonian being the earliest. Due to the scarcity of fossils, Precambrian time is primarily subdivided using isotopic age dating rather than fossil records.21

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