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Geological periodsMesoproterozoicProterozoic geochronology

Stenian

Adapted from Wikipedia · Explorer experience

A stunning view of Earth from space, taken by astronauts aboard the Apollo 17 mission. This famous photo shows our beautiful planet as a whole.

The Stenian Period

The Stenian Period was a long, long time ago — about 1.2 billion to 1 billion years before today! It was the last part of a big chunk of time called the Mesoproterozoic Era. Back then, Earth looked very different from today.

One of the biggest things that happened during the Stenian Period was that a giant group of land called a supercontinent named Rodinia came together. Imagine all the puzzle pieces of Earth fitting into one big shape! This big land was surrounded by a huge ocean called the Mirovian.

Scientists learned about this time by looking at special rocks and using dating tricks, because there are very few fossils from then. But they did find some very old tiny plants, like Bangiomorpha pubescens, which was one of the first living things that had boys and girls.

The Stenian name comes from an Ancient Greek word, stenós, meaning “narrow.” It refers to the narrow rock belts formed back then. Before this name was used, scientists called this time the Riphean age.

The world back then had less bright sunshine, more air made of carbon dioxide, and very little oxygen — quite different from our world today!

Images

A map showing how the Earth's continents may have looked around 1 billion years ago during the Stenian period.
A map showing the ancient landmass Proto-Rodinia as it may have looked 1 billion years ago.
Map showing the location of the Grenville orogenic belt in North America and Scotland.
A microscopic fossil of Bangiomorpha pubescens, one of the oldest known eukaryotic life forms, showing its cellular structure.
A colorful diagram showing the layers of rock in the Williston Basin, a large area under the ground in North America.

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

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