Geologic time scale
Geologic time scale uses the principles and techniques of geology to work out the geological history of the Earth. It looks at the processes which change the Earth's surface and rocks under the surface.
Geologists use stratigraphy and paleontology to find out the sequence of the events, and show the plants and animals which lived at different times in the past. They worked out the sequence of rock layers. Then the discovery of radioactivity and the invention of radiometric dating techniques gave a way to get the ages of the layers (strata).
We now know the timing of important events that have happened during the history of Earth. The Earth is about 4.567 billion (4,567 million) years old. The geological or deep time of Earth's past has been organized into various units. Boundaries on the time scale are usually marked by major geological or palaeontological events, such as mass extinctions. For example, the boundary between the Cretaceous period and the Palaeogene period is defined by the Cretaceous–Tertiary extinction event. This marked the end of the dinosaurs and of many marine species.
Prospecting for energy sources and valuable minerals depends on understanding the geological history of an area. Such knowledge can also help lessen the hazards of earthquakes and volcanoes.
The largest defined unit of time is the supereon composed of Eons. Eons are divided into Eras, which are in turn divided into Periods, Epochs and Stages. At the same time paleontologists define a system of faunal stages, of varying lengths, based on the kinds of animal fossils found there. In many cases, such faunal stages have been adopted in building the geological nomenclature, though in general there are far more recognized faunal stages than defined geological time units.
Geologists tend to talk in terms of Upper/Late, Lower/Early and Middle parts of periods and other units, such as "Upper Jurassic", and "Middle Cambrian". Upper, Middle, and Lower are terms applied to the rocks themselves, as in "Upper Jurassic sandstone," while Late, Middle, and Early are applied to time, as in "Early Jurassic deposition" or "fossils of Early Jurassic age." The adjectives are capitalized when the subdivision is formally recognized, and lower case when not; thus "early Miocene" but "Early Jurassic."
Because geologic units occurring at the same time but from different parts of the world can often look different and contain different fossils, there are many examples where the same period was historically given different names in different locales. For example, in North America the Lower Cambrian is called the Waucoban series that is then subdivided into zones based on trilobites. The same timespan is split into Tommotian, Atdabanian and Botomian stages in East Asia and Siberia. A key aspect of the work of the International Commission on Stratigraphy is to reconcile this conflicting terminology and define universal horizons (time division) that can be used around the world.
Table of geologic timeEdit
The following table summarizes the major events and characteristics of the periods of time making up the geologic time scale. As above, this time scale is based on the International Commission on Stratigraphy. The height of each table entry does not correspond to the duration of each subdivision of time. (not shown to scale)
|Phanerozoic||Cainozoic||Quaternary||Holocene||Rise of human population; Last ice age ends||11,700|
|Pleistocene||Ice ages and warmer periods; extinction of many large mammals; evolution of fully modern humans||2.588 million|
|Tertiary||Neogene||Pliocene||Climate cools further; Australopithecine hominins evolve||5.333 million|
|Miocene||Earth has many forests; animals flourish but later temperatures start to cool||23.03 million|
|Palaeogene||Oligocene||The continents move into their current places||33.9 million|
|Eocene||The Himalayas are formed as India moves into Asia||56 million|
|Palaeocene||India reaches Asia; mammals evolve into new groups; birds survive extinction||66 million|
|Mesozoic||Cretaceous||Upper Cretaceous||Dinosaurs become extinct in K/T extinction event.||100.5 million|
|Lower Cretaceous||Dinosaurs continue to flourish; marsupial and placental mammals appear; first flowering plants||145 million|
|Jurassic||Upper Jurassic||Dinosaurs dominate on land; first birds, early mammals; conifers, cycads and other seed plants. Supercontinent Pangaea begins to break up||163.5 million|
|Middle Jurassic||174.1 million|
|Lower Jurassic||201.3 million|
|Triassic||Upper Triassic||First dinosaurs; pterosaurs; ichthyosaurs; plesiosaurs; turtles; egg-laying mammals||237 million|
|Middle Triassic||247.2 million|
|Lower Triassic||252.17 million|
|Palaeozoic||Permian||P/Tr extinction event – 95% of species become extinct. Supercontinent Pangaea forms.||298.9 million|
|Carboniferous||Pennsylvanian||Tropical climate: abundant insects, first synapsids and reptiles; coal forests||323.2 million|
|Mississippian||Large primitive trees||358.9 million|
|Devonian||Age of fish; first amphibia; clubmosses and horsetails appear; progymnosperms (first seed bearing plants) appear||419.2 million|
|Silurian||First land plant fossils||443.4 million|
|Ordovician||Invertebrates dominant||485.4 million|
|Cambrian||Major diversification of life in the Cambrian adaptive radiation||541 million|
|Proterozoic||Neoproterozoic2||Ediacaran||First multi-celled animals||635 million|
|Cryogenian||Possible Snowball Earth period||720 million|
|Tonian||Supercontinent Rodinia breaks up||1 billion|
|Mesoproterozoic||Stenian||The supercontinent Rodinia forms||1.2 billion|
|Ectasian||First sexually reproducing organism||1.4 billion|
|Calymmian||The supercontinent of Columbia breaks up||1,6 billion|
|Palaeoproterozoic||Statherian||Formation of the Columbia (supercontinent) happens during this period||1.8 billion|
|Orosirian||First complex single-celled life||2.05 billion|
|Rhyacian||Replacement of CO2 by oxygen triggers the Huronian glaciation in this period||2.3 billion|
|Siderian||The breakup of the supercontinent Kenorland occurs||2.5 billion|
|Archaean||Neoarchaean||The supercontinent Kenorland forms||2.8 billion|
|Mesoarchaean||The supercontinet Ur is from this era||3.2 billion|
|Palaeoarchaean||Bacteria build stromatolites||3.6 billion|
|Eoarchaean||1st supercontinet Vaalbara existed during this era||4 billion|
|Hadean||Formation of Earth 4.6 billion years ago; formation of Moon 4.5 bya||4.54 billion (~4.6 bya)|
References and footnotesEdit
- ↑ Levin, Harold 2003. The Earth through time, Hoboken, New Jersey: Wiley, p.2
- GSA: Geologic Time Scale
- CHRONOS Archived 1998-12-05 at the Wayback Machine
- National Museum of Natural History - Geologic Time Archived 2005-11-11 at the Wayback Machine
- Geological Time Systems Archived 2008-07-23 at the Wayback Machine - Information model for the geologic time scale
- Exploring Time Archived 2015-02-21 at the Wayback Machine from Planck Time to the lifespan of the universe