A geologic period is one of several subdivisions of geologic time enabling cross-referencing of rocks and geologic events from place to place.
The twelve currently recognised periods of the present eon - the Phanerozoic - are defined by the International Commission on Stratigraphy (ICS) by reference to the stratigraphy at particular locations around the world.
A consequence of this approach to the Phanerozoic periods is that the ages of their beginnings and ends can change from time to time as the absolute ages of the chosen rock sequences which define them is more precisely determined.
The suite of rocks (sedimentary, igneous or metamorphic) associated with a geologic period is known as a system, so for example the 'Jurassic System' of rocks was put in place during the 'Jurassic Period' (between around 200 and 145.5 million years ago).
In a steady effort ongoing since 1974, the International Commission on Stratigraphy has been working to correlate the world's local stratigraphic record into one uniform planet-wide benchmarked system.
American geologists have long considered the Mississippian and Pennsylvanian to be periods in their own right though the ICS now recognises them both as 'subperiods' of the Carboniferous Period recognised by European geologists. Cases like this in China, Russia and even New Zealand with other geological eras has slowed down the uniform organization of the stratigraphic record.
- Changes in recent years have included the abandonment of the former Tertiary Period in favour of the Paleogene and succeeding Neogene periods.
- The abandonment of the Quaternary period was also considered but it has been retained for continuity reasons.
- Even earlier in the history of the science, the Tertiary was considered to be an 'era' and its subdivisions (Pliocene, Miocene, Paleocene, Eocene, Oligocene, Miocene and Pliocene) were themselves referred to as 'periods' but they now enjoy the status of 'epochs' within the more recently erected Paleogene and Neogene periods.
|Phanerozoic||Cenozoic||Quaternary (Pleistocene/Holocene)||2.588 - 0|
|Neogene (Miocene/Pliocene)||23.03 - 2.588|
|Paleogene (Paleocene/Eocene/Oligocene)||65.0 - 23.03|
|Mesozoic||Cretaceous||145.5 - 65.0|
|Jurassic||201.3 - 145.0|
|Triassic||252.17 - 201.3|
|Paleozoic||Permian||298.9 - 252.17|
|Carboniferous (Mississippian/Pennsylvanian)||358.9 - 298.9|
|Devonian||419.2 - 358.9|
|Silurian||443.4 - 419.2|
|Ordovician||485.4 - 443.4|
|Cambrian||541.0 - 485.4|
|Proterozoic||Neoproterozoic||Ediacaran||635.0 - 541.0|
|Cryogenian||850 - 635|
|Tonian||1000 - 850|
|Mesoproterozoic||Stenian||1200 - 1000|
|Ectasian||1400 - 1200|
|Calymmian||1600 - 1400|
|Paleoproterozoic||Statherian||1800 - 1600|
|Orosirian||2050 - 1800|
|Rhyacian||2300 - 2050|
|Siderian||2500 - 2300|
Geology to Palaeobiology
- Cohen, K.M., Finney, S., Gibbard, P.L. (2013), International Chronostratigraphic Chart, International Commission on Stratigraphy.