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Great Oxidation Event

Adapted from Wikipedia Β· Explorer experience

A massive 2.1-billion-year-old banded ironstone rock on display at the National Museum of Mineralogy and Geology in Dresden, Germany.

The Great Oxidation Event

The Great Oxidation Event was a very important time for our planet. It happened a long time ago, between 2.46 billion and 2.06 billion years ago. During this time, the air and water around Earth started to fill with oxygen. This oxygen came from tiny plants called cyanobacteria. They made oxygen as they used sunlight to grow, a process called photosynthesis.

Before this event, Earth's air was very different. It had lots of nitrogen and carbon dioxide, but almost no oxygen. The tiny plants changed everything by making oxygen over many years. This new oxygen helped change the planet so that more complex life could grow and thrive later on.

Scientists learn about this event by looking at very old rocks. These rocks tell a story of how the air and water changed. For example, special layers of rock called banded iron formations show us that oxygen was building up. These rocks stopped forming after the Great Oxidation Event because there was too much oxygen in the water.

The Great Oxidation Event is very important because oxygen later became a key part of the air we breathe today. It helped make our world ready for many different kinds of life to live and grow.

Images

A scientific timeline showing how life on Earth has changed from the Precambrian era to today.
A diagram showing the timeline of Earth's ice ages with annotated periods.

This article is a child-friendly adaptation of the Wikipedia article on Great Oxidation Event, available under CC BY-SA 4.0.

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