Cretaceous Period

145 – 66 million years ago · Mesozoic Era

The Cretaceous is the longest period of the Phanerozoic. It saw the greatest diversity of dinosaurs, the rise of flowering plants, and one of the most famous endings in Earth history.

At a glance

Began
145 Ma
Ended
66 Ma
Duration
79 million years
Era
Mesozoic
Climate state
Greenhouse (warm, little or no polar ice)
Land above sea level (PaleoDEM)
~32.5%
Dinosaurs on our map
9

The world in the Cretaceous

Reconstructed elevation and shorelines at 90 Ma (PALEOMAP PaleoDEM, Scotese & Wright 2018). Greens and browns are land, blues are sea.

Open the interactive map at 90 Ma → Elevation view Show dinosaurs on the map

What Earth was like

The continents moved toward their modern shapes. South America separated from Africa, opening the South Atlantic, and India broke away from Gondwana and raced north. Sea levels were exceptionally high: the Western Interior Seaway split North America in two, and shallow seas covered much of Europe and North Africa.

Climate

A hot greenhouse world. Carbon dioxide was several times today’s level, the poles were largely ice-free, and forests grew near the poles. Chalk from tiny plankton accumulated in warm seas, giving the period its name (creta, Latin for chalk).

Life

Flowering plants spread and diversified alongside pollinating insects. Dinosaurs reached their peak: Iguanodon and Spinosaurus earlier on, then Triceratops, Ankylosaurus, Velociraptor, Parasaurolophus and Tyrannosaurus rex. Mosasaurs ruled the seas and pterosaurs such as Quetzalcoatlus soared overhead.

Dinosaurs of the Cretaceous

These genera from our map lived during the Cretaceous. Bars show each genus’s accepted time range within the period.

IguanodonSpinosaurusParasaurolophusVelociraptorEdmontosaurusPachycephalosaurusTyrannosaurus rexAnkylosaurusTriceratops145 Ma106 Ma66 Ma
Ranges are consensus stratigraphic ranges; fossil counts from the Paleobiology Database.

Silhouettes via PhyloPic: Iguanodon — Tasman Dixon, CC0 1.0 (PhyloPic) · Spinosaurus — Alessio Ciaffi, CC BY 4.0 (PhyloPic) · Parasaurolophus — Richard Rich, CC0 1.0 (PhyloPic) · Velociraptor — Itai Fein, CC0 1.0 (PhyloPic) · Edmontosaurus — Ivan Iofrida, CC BY 4.0 (PhyloPic) · Pachycephalosaurus — Emily Willoughby, CC BY-SA 3.0 (PhyloPic) · Tyrannosaurus — Fred Wierum, CC BY 4.0 (PhyloPic) · Ankylosaurus — Itai Fein, CC0 1.0 (PhyloPic) · Triceratops — Jagged Fang Designs, CC0 1.0 (PhyloPic)

How it ended

At 66 million years ago an asteroid about 10 km wide struck Chicxulub, Mexico, while the Deccan Traps erupted in India. Around three quarters of species, including all non-avian dinosaurs, went extinct.

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 Cretaceous, an average of 32.5% of Earth’s surface stood above reconstructed sea level (range 27.5–36.8%). 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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