Trilobites, as we know them from their fossilized remains, existed in the Palaeozoic only and became extinct at the end of the Permian, some 250 million years before our time. The reasons for their evolutionary defeat are not entirely clear. There are strong indications (some scientists talk of evidence) that early trilobites or their immediate ancestors may have existed in the late Precambrian already, but we have not yet found fossilized remains of these animals. This may be due to the fact that early trilobites may have had a soft, non-calcified exoskeleton that hardly stood a chance of getting preserved. More information can be found here.
The Palaeozoic, like all other geologic eras, is sub-divided into periods and epochs. Here is a simplified breakdown of the geologic eras as is currently accepted.
Please bear in mind that this information is subject to constant change, as improving knowledge leads to corrective amendments of this chart pretty much every year. Time spans may shrink or grow, start dates may climb and fall on our time ladder, the treacherous steps of which being but slippery marks. The datings shown in our chart are, to a large extent, in accordance with the findings of the International Subcommission on Global Stratigraphy as published in 2004. This document can be downloaded in our Document-Section as a PDF-file.
The Geologic Eras |
Supereon / Eon / Era
| Period
| Epoch
| Start, years ago
|
Cenozoic

Mastodon longirostris
Tertiary / Pliocene
| Quaternary | Holocene (Alluvium)
Pleistocene (Dilluvium) |
1,8 million
|
Tertiary | Pliocene
Miocene
Oligocene
Eocene
Paleocene |
66 million
|
Mesozoic

Ammonite Perisphinctes.
Upper Jurassic (Malm)
| Cretaceous | Upper Cretaceous
Lower Cretaceous |
146 million
|
Jurassic | Upper Jurassic
Middle Jurassic
Lower Jurassic |
200 million
|
Triassic | Upper Triassic
Middle Triassic
Lower Triassic |
251 million
|
Palaeozoic

Odontochile
Middle Devonian

Cambropallas
Lower Cambrian
| Permian | Lopingian
Guadalupian
Cisuralian |
299 million
|
Carboniferous | Pennsylvanian
Mississippian |
359 million
|
Devonian | Upper Devonian
Middle Devonian
Lower Devonian |
416 million
|
Silurian | Pridoli
Ludlow
Wenlock
Llandovery
|
444 million
|
Ordovician | Upper Ordovician
Middle Ordovician
Lower Ordovician |
488 million
|
Cambrian | Furongian
Middle Cambrian
Lower Cambrian |
542 million
|
[Precambrian] - [Proterozoic]
Neoproterozoic
Mesoproterozoic
Paleoproterozoic

Eukarionts Chuaria sp.
Cryogenian
| Ediacaran
Cryogenian
Tonian | undefined | 1000 million |
Stenian
Ectasian
Calymmian |
undefined |
1600 million |
Statherian
Orosirian
Rhyacian
Siderian |
undefined |
2500 million |
[Precambrian]
Archean
Hadean
| undefined | undefined | > 3600 million |
Hereafter you can find a more detailed breakdown of the Palaeozoic. This chart shows the international chronostratigraphic units of the Palaeozoic, as approved by the ICS and ratified by the IUGS (2004).
International Stratigraphic Chart International Commission on Stratigraphy |
Period | Epoch | Stage | Start, years ago |
Permian  Kathwaia sp. | Lopingian | Changhsingian | 254 million |
Wuchiapingian | 260 million |
Guadalupian | Capitanian | 266 million |
Wordian | 268 million |
Roadian | 271 million |
Cisuralian | Kungurian | 276 million |
Artinskian | 284 million |
Sakmarian | 295 million |
Asselian | 299 million |
Carboniferous  Cummingella belisama | Pennsylvanian | Upper | Gzhelian | 304 million |
Kasimovian | 307 million |
Middle | Moscovian | 312 million |
Lower | Bashkirian | 318 million |
Mississippian | Upper | Serpukhovian | 326 million |
Middle | Visean | 345 million |
Lower | Tournaisian | 359 million |
Devonian  Drotops megalomanicus | Upper | Famennian | 375 million |
Frasnian | 385 million |
Middle | Givetian | 392 million |
Eifelian | 398 million |
Lower | Emsian | 407 million |
Pragian | 411 million |
Lochkovian | 416 million |
Silurian  Dalmanites limulurus | Pridoli | undefined | 419 million |
Ludlow | Ludfordian | 421 million |
Gorstian | 423 million |
Wenlock | Homerian | 426 million |
Sheinwoodian | 428 million |
Llandovery | Telychian | 436 million |
Aeronian | 439 million |
Rhuddanian | 444 million |
Ordovician  Isotelus "mafritzae" | Upper | Himantian | 446 million |
undefined | 456 million |
undefined | 461 million |
Middle | Darriwilian | 468 million |
undefined | 472 million |
Lower | undefined | 479 million |
Tremadocian | 488 million |
Cambrian  Cedaria minor | Furongian | undefined | undefined |
Paibian | 501 million |
Middle | undefined | undefined |
undefined | 513 million |
Lower | undefined | undefined |
undefined | 542 million |
Sometimes you may come across different descriptions for the very same subdivisions in stratigraphic charts. For example, some charts list the Middle Devonian as a "Series" while others list it as an "Epoch". The reason for that can be found in two different approaches used: One is based on chronostratigraphy, the other on geochronology. While the first refers to subdivisions based on the age of rock strata in relation to time, the latter determines the absolute age of rocks by various methods like radiometry and the like. To quote from Wikipedia:
"It is important not to confuse geochronologic and chronostratigraphic units. Geochronological units are periods of time, thus it is correct to say that Tyrannosaurus rex lived during the the Late Cretaceous Epoch. Chronostratigraphic units are geological material, so it is also correct to say that fossils of the genus Tyrannosaurus have been found in the Upper Cretaceous Series. In the same way, it is entirely possible to go and visit an Upper Cretaceous Series deposit - such as the Egyptian mangrove deposit where the Tyrannosaurus fossils were found - but it is naturally impossible to visit the Late Cretaceous Epoch as that is a period of time."
Equivalents of chronostratigraphic and geochronologic units
| Chronostratigraphic division |
|
Geochronologic division |
Eonothem (Phanerozoic, Proterozoic, Archean) | < equates > | Eon - Eonothem (Phanerozoic, Proterozoic, Archean) |
Erathem (Cenozoic, Mesozoic, Paleozoic) | < equates > | Era - Erathem (Cenozoic, Mesozoic, Paleozoic) |
System (Ordovician) | < equates > | Period - System (Ordovician) |
Series (Middle) | < equates > | Epoch - Series (Middle) |
Stage (Caradocian) | < equates > | Age - Stage (Caradocian) |
© Images of Perisphinctes, Odontochile and Cambropallas on this page courtesy of PaleoDirect, exclusive provider of trilobite images in support of this web site.
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