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A geologic era is a subdivision of geologic time that divides an Eon into smaller buckets. The geologic time scale is a chronologic schema (or idealized Model) relating Stratigraphy to time that is used by Geologists and other The Phanerozoic Eon is divided into three such time frames: the Paleozoic, Mesozoic, and Cenozoic represent the major stages in the macroscopic fossil record. The Phanerozoic (occasionally Phanaerozoic) Eon is the current eon in the Geologic timescale, and the one during which abundant animal life has existed The Paleozoic or Palaeozoic Era (from the Greek palaio (παλαιο "old" and zoe (ζωη "life" meaning "ancient life" The Mesozoic Era is one of three geologic eras of the Phanerozoic eon. The Cenozoic (also Caenozoic or Cainozoic) Era (ˌsiːnəˈzoʊɪk/ /ˌsɛn- (meaning "new life" ( Greek ( kainos) "new" FOSSIL is a standard protocol for allowing serial communication for Telecommunications programs under the DOS Operating system. These eras are separated by catastrophic extinction boundaries, the P-T boundary between the Paleozoic and the Mesozoic and the K-T boundary between the Mesozoic and the Cenozoic. In Biology and Ecology, extinction is the cessation of existence of a Species or group of taxa. The Permian–Triassic (P–Tr extinction event, informally known as the Great Dying, was an Extinction event that occurred, and 70 percent of terrestrial The K-T boundary is a geological signature usually a thin band dated to 65 There is evidence that catastrophic meteorite impacts played a role in demarcating the differences between the eras. See also Impact crater An impact event is the Collision of a large Meteoroid, Asteroid or Comet (generically

The Hadean, Archean and Proterozoic eons were as a whole formerly called the Precambrian. The Hadean (ˈheɪdiən is the geologic eon before the Archean. The Proterozoic (ˌproʊtərəˈzoʊɪk is a geological eon representing a period before the first abundant complex life on Earth. The Precambrian ( Pre-Cambrian) is an informal name for the supereon comprising the eons of the Geologic timescale that came before the current This covered the four billion years of Earth history prior to the appearance of hard-shelled animals. More recently, however, those eons have been subdivided into eras of their own.

Era Time frame (Ma = million years ago)
Cenozoic 66 Ma to present day
Mesozoic 252 Ma–66 Ma
Paleozoic 542 Ma–252 Ma
Neoproterozoic 1000 Ma–542 Ma
Mesoproterozoic 1600 Ma–1000 Ma
Paleoproterozoic 2500 Ma–1600 Ma
Neoarchean 2800 Ma–2500 Ma
Mesoarchean 3200 Ma–2800 Ma
Paleoarchean 3600 Ma–3200 Ma
Eoarchean 3800 Ma (unofficial)–3600 Ma
Hadean Eon
not officially divided into eras
Formation of Earth to 3800 Ma
An era is a commonly used word for long period of time When used in science for example geology eras denote clearly defined periods of time of arbitrary but well defined Annum is one form of the Latin noun meaning Year, not a form normally used for derivatives in modern languages the accusative singular The Cenozoic (also Caenozoic or Cainozoic) Era (ˌsiːnəˈzoʊɪk/ /ˌsɛn- (meaning "new life" ( Greek ( kainos) "new" The Mesozoic Era is one of three geologic eras of the Phanerozoic eon. The Paleozoic or Palaeozoic Era (from the Greek palaio (παλαιο "old" and zoe (ζωη "life" meaning "ancient life" The Neoproterozoic Era is the unit of geologic time from 1000 to 542 +/- 0 The Mesoproterozoic Era is a geologic era that occurred between 1600 Ma and 1000 Ma (million years ago The Paleoproterozoic (ˌpeɪlɪoʊˌproʊtərəˈzoʊɪk also spelled Palaeoproterozoic) is the first of the three sub-divisions ( eras) of the The Neoarchean (ˌniːoʊɑrˈkiːən also spelled Neoarchaean) is a geologic era within the Archaean. The Mesoarchean (ˌmiːzoʊɑrˈkiːən also spelled Mesoarchaean) is a geologic era within the Archean, spanning 3200 Ma to 2800 The Paleoarchean (ˌpeɪlɪoʊɑrˈkiːən also spelled Palaeoarchaean) is a geologic era within the Archaean. In the Geologic record the Eoarchean Erathem (ˌiːoʊɑrˈkiːən also spelled Eoarchaean) and the Eoarchean era in the Geologic The Hadean (ˈheɪdiən is the geologic eon before the Archean. Modern geologists and Geophysicists consider the age of Earth to be around 4
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