Silurian Period

443.8 – 419.2 million years ago · Paleozoic Era

The Silurian was a time of recovery after the end-Ordovician extinction. Warm seas returned, reefs rebuilt, and life made decisive steps onto land.

At a glance

Began
443.8 Ma
Ended
419.2 Ma
Duration
24.6 million years
Era
Paleozoic
Climate state
Greenhouse (warm, little or no polar ice)
Land above sea level (PaleoDEM)
~20.3%
Dinosaurs on our map
0

The world in the Silurian

Reconstructed elevation and shorelines at 430 Ma (PALEOMAP PaleoDEM, Scotese & Wright 2018). Greens and browns are land, blues are sea.

Open the interactive map at 430 Ma → Elevation view

What Earth was like

Laurentia and Baltica collided to form Laurussia (the "Old Red Sandstone continent"), raising the Caledonian mountains in what are now Scotland, Scandinavia and Greenland. Gondwana still dominated the southern hemisphere.

Climate

With the ice sheets melted, the Silurian was largely warm and stable, with high sea levels and extensive tropical reefs. Short cooler episodes occurred, but no major ice age.

Life

The first vascular plants, such as Cooksonia, appeared: small stems only a few centimeters tall. Millipedes and early arachnids followed them onto land. In the sea, jawed fish diversified and giant sea scorpions (eurypterids) became top predators.

Dinosaurs of the Silurian

There were no dinosaurs yet. The first dinosaurs appear in the Late Triassic, around 233 million years ago.

How it ended

The Silurian ended quietly compared with other periods, at 419.2 million years ago, with the start of the Devonian.

Key facts

Data: land and sea

Land above sea level, 540 Ma to today
20%30%40%540 Ma400 Ma300 Ma200 Ma100 Ma0 Ma

Across the Silurian, an average of 20.3% of Earth’s surface stood above reconstructed sea level (range 18.2–22.9%). Today the same model gives 31.8%.

Where this data comes from

These are scientific reconstructions, not observations. Uncertainty grows the further back in time you go. About & data sources

Related reading

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