The largest time division, lasting billions of years
Era
A subdivision of an eon, scaling hundreds of millions of years
Period
A subdivision of an era, lasting tens of millions of years
Epoch
A subdivision of a period, lasting around several million years
The Geologic Time Scale is the stratigraphic history of the Earth
The Earth is at least 4.6 billion years old
Humans have only thrived at less than a percent of the Earth's existence
Geologic Time Scale subdivisions
Eons
Eras
Periods
Epochs
Precambrian Supereon
Contains three eons that highlight the significant events in the Earth's early life (about ⅞ of the Earth's history)
Hadean Eon: The Burning Earth
1. Formation of the moon
2. Formation of the Earth
3. Iron Catastrophe
4. Earth's magnetic field began
5. First solid continental crust formed
6. Bombardment events
7. Continents began to form
Archaean Eon: The First Rain
1. First rain fell
2. Microfossils indicate chemoautotrophs were first living organisms
3. First atmosphere formed
4. Extremophiles born
5. Carbon dissolved and utilised
6. Vaalbara supercontinent formed
Proterozoic Eon: The First Freezer
1. Tectonic plates formed
2. Prokaryotes formed symbiosis
3. First extinction
4. Photosynthetic and energy-converting organisms born
5. First Ice Age
6. First extinction of carbon-dependent prokaryotes
Phanerozoic Eon is an eighth of the whole history of the Earth
Paleozoic Era: When Life Booms Over
1. Rodinia supercontinent broke up and formed Pangaea
2. Plants became dominant land organisms
3. Animals began to live on land
Paleozoic Era Periods
Cambrian
Ordovician
Silurian
Devonian
Carboniferous
Permian
Cambrian Period marked the Cambrian Explosion, creating biodiversity
Ordovician Period saw the first extinction of eukaryotes
Silurian Period saw the evolution of the first freshwater fish
Devonian Period is known as the Age of the Fish
Carboniferous Period saw the development of tropical swamps and the first reptiles
Permian Period saw all separate continents form Pangaea
Carboniferous
Meaning "to carry", coal-bearing
Rocks dated in this period are varied
Rock types from the Carboniferous period
Limestone
Sandstone
Shale
Coal
Coal deposits dominate other rock deposits from the Carboniferous period
Average global temperatures were exceedingly high during the Carboniferous period
Tropical swamps were developed during the Carboniferous period
Lignin-laden plants and trees grew taller and became more numerous, including seed ferns, during the Carboniferous period
Amniotic eggs were developed during the Carboniferous period, allowing amphibians to go farther inland and become the dominant vertebrate
The first reptiles appeared during the Carboniferous period
Because of the cool global temperatures, rainforests collapsed and a third Ice Age came during the Carboniferous period
Permian Period
Named after the Russian region of Perm
All separate continents formed Pangaea during the Permian period
The major marker of the Permian period is the Ural mountains (where Perm itself is located)
Reptiles dominated the scene during the Permian period, with early dinosaurs such as Dimetrodon and Edaphosaurus evolving and dominating Pangaea
The first cone-bearing plants (true conifers and cycads) and the ginkgo (sometimes written as gingko) evolved and thrived in the new landscape of the Permian period
Near the end of the Permian period, Pangaea became drier, thus creating more deserts
More vertebrates dominated the scene during the Permian period, such as Scutosaurus and Gorgonopsids
Eventually, a third extinction came during the Permian period, which is known as The Great Dying
Mesozoic Era
Also known as the Age of Reptiles or Age of the Dinosaurs, it is the period where the Earth began to recover from its third extinction