Geologic timescale
The geologic timescale is used by geologists and other scientists to describe the timing and relationships between events that have occured during the history of the Earth. The table of geologic periods presented here is in accordance with the dates and nomenclature proposed by the International Commission on Stratigraphy, and uses the standard color codes of the United States Geologic Survey.
The Earth is thought by geologists to be about 4570 million years old. The geologic or "deep" time of Earth's past has been organized into various periods according to events which took place in each period.
Table of contents |
Table of geologic time
| Eon | Era | Period1 | Series/ Epoch | Major Events | End, Million Years Ago2 | |
|---|---|---|---|---|---|---|
| Phanerozoic | Cenozoic | Neogene3 | Holocene | End of recent glaciation and rise of modern civilization | Ongoing | |
| Pleistocene | Flourishing and then extinction of many large mammals (Pleistocene megafauna); Evolution of fully modern humans | 0.011430 ± 0.00013 | ||||
| Pliocene | Intensification of present ice age. Cool and dry climate; Australopithecines appear, many of the existing genera of mammals, and recent molluscs appear | 1.806 ± 0.005 * | ||||
| Miocene | Moderate climate; Mountain building in northern hemisphere; Modern mammal and bird families became recognizable. Horses and mastodonts diverse. Grasses become ubiquitous. | 5.332 ± 0.005 * | ||||
| Paleogene3 | Oligocene | Warm climate; Rapid evolution and diversification of fauna, especially mammals. Major evolution and dispersal of modern types of angiosperms | 23.03 ± 0.05 * | |||
| Eocene | Archaic mammals (e.g. Creodonts, Condylarths, Uintatheres, etc) flourish and continue to develop during the epoch. Appearance of several "modern" mammal families. Primitive whales diversify. First grasses. Reglaciation of Antartica; start of current ice age. | 33.9 ± 0.1 * | ||||
| Paleocene | Climate tropical. Modern plants; Mammals diversify into a number of primitive lineages following the extinction of the dinosaurs. First large mammals (upto bear or small hippo size) | 55.8 ± 0.2 * | ||||
| Mesozoic | Cretaceous | Upper/Late | Flowering plants appear, along with new types of insects. More modern teleost fish begin to appear. Ammonites, belemites, rudists, and sponges common. Many new types of dinosaurs (e.g. Tyrannosaurs, Titanosaurs, duck bills, and horned dinosaurs) evolve on land, as do modern crodilians; and mosasaurs and modern sharks appear in the sea. Primitive birds gradually replace pterosaurs. Monotremes, marsupials and placental mammals appear. Break up of Gondwana. | 65.5 ± 0.3 * | ||
| Lower/Early | 99.6 ± 0.9 * | |||||
| Jurassic | Upper/Late | Gymnosperms and ferns common. Many types of dinosaurs, such as sauropods, carnosaurs, and stegosaurs. Mammals common but small. First birds and lizards. Ichthyosaurs and plesiosaurs diverse. Ammonites and belemites abundant. Breakup of Pangea into Gondwana and Laurasia | 145.5 ± 4.0 | |||
| Middle | 161.2 ± 4.0 | |||||
| Lower/Early | 175.6 ± 2.0 * | |||||
| Triassic | Upper/Late | Archosaurs dominant and diverse on land; cynodonts become smaller and more mammal-like. Many large aquatic amphibians. Ichthyosaurs and ceratites common in the seas. First dinosaurs, mammals, teleosts, and crocodylia. | 199.6 ± 0.6 | |||
| Middle | 228.0 ± 2.0 | |||||
| Lower/Early | 245.0 ± 1.5 | |||||
| Paleozoic | Permian | Lopingian | Landmass unites in the supercontinent of Pangea. Synapsid reptiles become common (Pelycosaurs and Therapsids), amphibians also remain common. Carboniferous flora replaced by gymnosperms in the middle of the period. Beetles and flies evolve. Marine life flourishes in the warm shallow reefs. End of Permo-carboniferous ice age. At the end of the period the Permian extinction event- 95% of life on Earth becomes extinct | 251.0 ± 0.4 * | ||
| Guadalupian | 260.4 ± 0.7 * | |||||
| Cisuralian | 270.6 ± 0.7 * | |||||
| Carbon- iferous4 | Pennsyl- vanian | Upper/Late | Winged insects appear and are abundant, some growing to large size. Amphibians common and diverse. First reptiles, coal forests (Lepidodendron, Sigillaria, Calamites, Cordaites, etc), very high atmospheric oxygen content. | 299.0 ± 0.8 * | ||
| Middle | 306.5 ± 1.0 | |||||
| Lower/Early | 311.7 ± 1.1 | |||||
| Missis- sippian | Upper/Late | Large primitive trees, first land vertebrates, brackish water and amphibious eurypterids; rhizodonts dominant fresh-water predators. In the seas primitive sharks common and very diverse, echinoderms (especially crinoids and blastoids) abundant, brachiopods (Productida, Spriferida, etc) very common; trilobites and nautiloids in decline. Glaciation in East Gondwana. | 318.1 ± 1.3 * | |||
| Middle | 326.4 ± 1.6 | |||||
| Lower/Early | 345.3 ± 2.1 | |||||
| Devonian | Upper/Late | First clubmosses and horsetails appear, progymnosperms (first seed bearing plants) appear, first trees (Archaeopteris). First Amphibians (but still aquatic). In the sea strophomenid and atrypid brachiopods, rugose and tabulate corals, and crinoids abundant; ammonoids and coleoids appear; jawed fish (Placoderms, lobe-finned and ray-finned fish, and early sharks) important life in the sea. "Old Red Continent" (Euramerica) | 359.2 ± 2.5 * | |||
| Middle | 385.3 ± 2.6 * | |||||
| Lower/Early | 397.5 ± 2.7 * | |||||
| Silurian | Pridoli | First vascular land plants, millipedes and arthropleurids, first jawed fish, sea-scorpians reach large size, tabulate and rugose corals and brachiopods very common; trilobites and molluscs diverse. Graptolites not as varied. | 416.0 ± 2.8 * | |||
| Ludlow | 418.7 ± 2.7 * | |||||
| Wenlock | 422.9 ± 2.5 * | |||||
| Llandovery | 428.2 ± 2.3 * | |||||
| Ordovician | Upper/Late | Invertebrates dominant; they include brachiopods (Orthida, Strophomenida, etc), bivalves, nautiloids, trilobites, bryozoa, many types of echinoderms (cystoids, crinoids, starfish, etc), graptolites, and other taxa. Conodonts were primitive planktonic vertebrates that appear at the start of the Ordovician. Ice age at the end of the period. First land plants appear. | 443.7 ± 1.5 * | |||
| Middle | 460.9 ± 1.6 * | |||||
| Lower/Early | 471.8 ± 1.6 | |||||
| Cambrian | Furongian | Major diversification of life in the Cambrian Explosion; more than half of modern animal phyla appear, along with a number of extinct and problematic forms. Trilobites, Priapulida, sponges, inarticulate brachiopods, anomalocarids, and many other forms common. | 488.3 ± 1.7 * | |||
| Middle | 501.0 ± 2.0 * | |||||
| Lower/Early | 513.0 ± 2.0 | |||||
| Proterozoic5 | Neo- proterozoic | Ediacaran | First multi-celled animals | 542.0 ± 1.0 * | ||
| Cryogenian | Possible snowball Earth period, Rodinia begins to break up | 630 +5/-30 * | ||||
| Tonian | First acritarch radiation | 850 6 | ||||
| Meso- proterozoic | Stennian | Formation of Rodinia | 1000 6 | |||
| Ectasian | 1200 6 | |||||
| Calymmian | 1400 6 | |||||
| Paleo- proterozoic | Statherian | First complex single-celled life | 1600 6 | |||
| Orosirian | Transition to oxygen atmosphere | 1800 6 | ||||
| Rhyacian | 2050 6 | |||||
| Siderian | 2300 6 | |||||
| Archaean5 | Neoarchean | Stabilization of most modern cratons, possible mantle overturn event | 2500 6 | |||
| Mesoarchean | First stromatolites | 2800 6 | ||||
| Paleoarchean | First known oxygen producing bacteria | 3200 6 | ||||
| Eoarchean | Simple single-celled life | 3600 6 | ||||
| Hadean5,7 | 4100 MYA – Oldest known rock; 4400 MYA – Oldest known mineral; 4570 MYA – Formation of Earth | 3800 | ||||
- Paleontologists often refer to faunal stages rather than geologic Periods. The stage nomenclature is quite complex. See Harland for an excellent time ordered list of faunal stages.
- Dates are slightly uncertain with differences of a few percent between various sources being common. This is largely due to uncertainties in radiometric dating and the problem that deposits suitable for radiometric dating seldom occur exactly at the places in the geologic column where they would be most useful. The dates and errors quoted above are according to the International Commission on Stratigraphy 2004 time scale. Dates labeled with a * indicate boundaries where a Global Boundary Stratotype Section and Point has been internationally agreed upon.
- Historically, the Cenozoic has been divided up into the Quaternary and Tertiary sub-eras, as well as the Neogene and Paleogene periods. However, the International Commission on Stratigraphy has recently decided to stop endorsing the terms Quaternary and Tertiary as part of the formal nomenclature.
- In North America, the Carboniferous is subdivided into Mississippian and Pennsylvanian Periods.
- The Proterozoic, Archean and Hadean are often collectively referred to as Precambrian Time, and sometimes also as the Cryptozoic.
- Defined by absolute age (Global Standard Stratigraphic Age).
- Though commonly used, the Hadean is not a formal eon and no lower bound for the Eoarchean has been agreed upon. The Hadean has also sometimes been called the Priscoan.
Graphical timeline
<timeline> ImageSize = width:800 height:100 PlotArea = left:65 right:15 bottom:20 top:5 AlignBars = justify
Colors =
id:epoch value:rgb(0.7,0.7,1) # light blue id:period value:rgb(1,0.7,0.7) # light red id:era value:rgb(1,1,0.7) # light yellow id:eon value:rgb(1,0.7,1) # light purple id:black value:black
Period = from:-4567.17 till:0 TimeAxis = orientation:horizontal ScaleMajor = unit:year increment:500 start:-4500 ScaleMinor = unit:year increment:100 start:-4500
Define $markred = text:"*" textcolor:red shift:(0,3) fontsize:10
PlotData=
align:center textcolor:black fontsize:8 mark:(line,black) width:25 shift:(0,-5)
bar:eon color:eon
at: 0 align:right $markred at: -542 align:left $markred from: -542 till: 0 text:Phanerozoic from:-2500 till: -542 text:Proterozoic from:-3800 till: -2500 text:Archaean from: start till: -3800 text:Hadean
bar:era color:era
from: -65.5 till: 0 text:C~z shift:(0,1.5) from: -251 till: -65.5 text:Meso~zoic shift:(0,1.5) from: -542 till: -251 text:Paleo~zoic shift:(0,1.5) from: -1000 till: -542 text:Neoprote-~rozoic shift:(0,1.8) from:-1600 till: -1000 text:Mesoproterozoic from:-2500 till: -1600 text:Paleoproterozoic from:-2800 till: -2500 text:Neo-~archean shift:(0,1.5) from:-3200 till: -2800 text:Meso-~archean shift:(0,1.5) from:-3600 till: -3200 text:Paleo-~archean shift:(0,1.5) fontsize:7 from:-3800 till: -3600 text:Eo-~arch-~ean shift:(0,2) from:start till: -3800
bar:period color:period
fontsize:6 from: -23.03 till: 0 from: -65.5 till: -23.03 from: -145.5 till: -65.5 from: -199.6 till: -145.5 from: -251 till: -199.6 from: -299 till: -251 from: -359.2 till: -299 from: -416 till: -359.2 from: -443.7 till: -416 from: -488.3 till: -443.7 from: -542 till: -488.3
from: -630 till: -542 text:Ed. from: -850 till: -630 text:Cryo-~genian from: -1000 till: -850 text:Ton-~ian from: -1200 till: -1000 text:Sten-~nian from: -1400 till: -1200 text:Ect-~asian from: -1600 till: -1400 text:Calym-~mian from: -1800 till: -1600 text:Stath-~erian from: -2050 till: -1800 text:Oro-~sirian from: -2300 till: -2050 text:Rhy-~acian from: -2500 till: -2300 text:Sid-~erian from: start till: -2500
</timeline>
<timeline> ImageSize = width:800 height:100 PlotArea = left:65 right:15 bottom:20 top:5 AlignBars = justify
Colors =
id:epoch value:rgb(0.7,0.7,1) # light blue id:period value:rgb(1,0.7,0.7) # light red id:era value:rgb(1,1,0.7) # light yellow id:eon value:rgb(1,0.7,1) # light purple id:filler value:gray(0.8) # background bar id:black value:black
Period = from:-542 till:0 TimeAxis = orientation:horizontal ScaleMajor = unit:year increment:100 start:-500 ScaleMinor = unit:year increment:10 start:-540
Define $markred = text:"*" textcolor:red shift:(0,3) fontsize:10 Define $markgreen = text:"*" textcolor:green shift:(0,3) fontsize:10
PlotData=
align:center textcolor:black fontsize:8 mark:(line,black) width:25 shift:(0,-5)
bar:eon color:eon at: 0 align:right $markred at: -542 align:left $markred from: -542 till: 0 text:Phanerozoic bar:era color:era at: 0 align:right $markgreen at: -65.5 align:left $markgreen from: -65.5 till: 0 text:Cenozoic from: -251 till: -65.5 text:Mesozoic from: -542 till: -251 text:Paleozoic
bar:period color:period fontsize:8 from: -23.03 till: 0 text:Neo-~gene shift:(0,0.5) from: -65.5 till: -23.03 text:Paleo-~gene shift:(0,0.5) from: -145.5 till: -65.5 text:Cretaceous from: -199.6 till: -145.5 text:Jurassic from: -251 till: -199.6 text:Triassic from: -299 till: -251 text:Permian from: -359.2 till: -299 text:Carboniferous from: -416 till: -359.2 text:Devonian from: -443.7 till: -416 text:Sil-~urian shift:(0,0.5); from: -488.3 till: -443.7 text:Ordovician from: -542 till: -488.3 text:Cambrian
</timeline>
<timeline> ImageSize = width:800 height:100 PlotArea = left:65 right:15 bottom:20 top:5 AlignBars = justify
Colors =
id:epoch value:rgb(0.7,0.7,1) # light blue id:period value:rgb(1,0.7,0.7) # light red id:era value:rgb(1,1,0.7) # light yellow id:eon value:rgb(1,0.7,1) # light purple id:black value:black
Period = from:-65.5 till:0 TimeAxis = orientation:horizontal ScaleMajor = unit:year increment:10 start:-60 ScaleMinor = unit:year increment:1 start:-65
Define $markgreen = text:"*" textcolor:green shift:(0,3) fontsize:10
PlotData=
align:center textcolor:black fontsize:8 mark:(line,black) width:25 shift:(0,-5)
bar:era color:era at: 0 align:right $markgreen at: start align:left $markgreen from:start till: 0 text:Cenozoic
bar:period color:period from: -23.03 till: 0 text:Neogene from:start till: -23.03 text:Paleogene
bar:epoch color:epoch from: -0.1 till: 0 from: -1.806 till: -0.1 text:P from: -5.332 till: -1.806 text:Plio-~cene shift:(0,1) fontsize:6 from:-23.03 till: -5.332 text:Miocene from:-33.9 till:-23.03 text:Oligocene from:-55.8 till:-33.9 text:Eocene from:start till:-55.8 text:Paleocene
</timeline>
References
See also
- Age of the Earth
- Fossils and the geological timescale
- Cosmological timeline
- Lunar geologic timescale
- Martian geologic timescale
- Anthropocene
- Logarithmic timeline
External link
Categories: Graphical timelines | Earth sciences | Geology | Geochronology | Geologic timescale