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Middle Triassic

Adapted from Wikipedia · Adventurer experience

A stunning view of Earth from space, captured by astronauts during the Apollo 17 mission.

The Middle Triassic is an important time in Earth's history. It is the second part of the Triassic period. The Middle Triassic lasted from about 246.7 million years ago to 237 million years ago. Before this time was the Early Triassic, and after it came the Late Triassic.

During the Middle Triassic, many changes happened on Earth. This time is split into two parts called the Anisian and Ladinian ages. Scientists study rocks and fossils to learn about life long ago.

In some places, like western Europe, rocks from this time are called Muschelkalk. In Australia, near Sydney, there are special rocks such as the Ashfield Shale and Bringelly Shale that contain fossils. These fossils help us understand what the world was like millions of years ago.

Middle Triassic life

Main page: Category:Middle Triassic life

After a big event that made many plants and animals disappear, life started to grow again during the Middle Triassic. Many different sea animals, like ichthyosaurs, sauropterygians, and ray-finned fish, began to appear. Also, many small creatures that do not have a backbone, such as molluscs, started to live in the oceans.

At this time, there were no flowering plants yet. Instead, plants like seed ferns and gymnosperms grew on land. The first very small dinosaur-like animals also began to show up.

Mixosaurus cornalianus was a sea animal that lived during this time.

Images

A natural rock formation showing layers of limestone, known as 'Schaumkalk,' found near Dörzbach.
A map showing how Earth looked 240 million years ago during the Ladinian Age.
An artist’s pencil drawing of Mixosaurus, an ancient ichthyosaur that lived in the Triassic period.
A diagram showing the layers of rock in the Williston Basin, helping us learn about Earth's history.

Related articles

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

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