Geologic Time Basics
Life & Extinction
Paleozoic & Mesozoic
Dinosaurs & Later Eras
Cenozoic & Beyond
100

This is the longest unit of geologic time.

Eon

100

When organisms cannot adapt to rapid environmental changes, this usually happens to them.

They become extinct

100

This is the oldest era of the Phanerozoic eon.

Paleozoic Era

100

These are the three periods of the Mesozoic Era.

Triassic, Jurassic, and Cretaceous

100

These are the two periods of the Cenozoic Era.

Tertiary and Quaternary

200

This geologic time unit is a subdivision of an era.

Period

200

This term describes the extinction of many species in a relatively short period of time.

Mass extinction

200

This era is often called the “Age of Invertebrates” in its early part.

Early Paleozoic

200

During the Mesozoic, this process broke up Pangaea and eventually led to the formation of the Atlantic Ocean

The breakup of Pangaea

200

This is the most recent epoch of the Cenozoic Era.

Holocene

300

This term describes a sudden appearance of many new, complex life-forms in the fossil record at the start of the Paleozoic.

The Cambrian explosion

300

Iridium found in a global clay layer is evidence for this event that likely caused the extinction of the dinosaurs.

A meteorite impact

300

 This nickname is given to the Middle Paleozoic because of the dominance of fish.

Age of Fishes

300

Dinosaurs are distinguished from present-day reptiles because they walked with their legs in this position relative to their hips.

Legs directly below their hips (upright posture)

300

During the Pleistocene ice age, sea level dropped because of this.

Glaciers trapped large amounts of water

400

This type of isolation occurs when a population is separated by a physical barrier such as a mountain range or ocean.

Geographic isolation

400

These were the first life-forms on Earth.

Unicellular organisms

400

This supercontinent formed during the Late Paleozoic.

Pangaea

400

These marine reptiles of the Mesozoic had small heads, long necks, and flippers.

Plesiosaurs

400

These are large mammals that lived during the Cenozoic, many of which went extinct at the end of the Pleistocene.

Mega-mammals

500

The geologic time scale is primarily based on this evidence recorded in rock layers.

The fossil record

500

These Paleozoic animals are significant because they were the first organisms to have hard body parts preserved in the fossil record.

Trilobites

500

This combination of events—formation of Pangaea, volcanic eruptions, and possibly a meteorite impact—caused the largest mass extinction at the end of the Paleozoic.

The Permian mass extinction

500

This era, beginning about 65.5 million years ago, is known as the “Age of Mammals.”

Cenozoic Era

500

According to scientists, this is the primary cause of present-day global warming.

Human use of fossil fuels

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