Eon (geology)
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Eon Million Years Ago
Phanerozoic 542 mya to the present
Proterozoic 2500 mya – 542 mya
Archean 3600 mya – 2500 mya
Hadean Formation of Earth to 3600 mya

In general usage, an eon (sometimes spelled æon) is an arbitrarily designated period of time. Geologists and other scientific disciplines interested in earth history refer to an eon as the largest subdivision of time on the geologic time scale. For example, the Phanerozoic Eon, which is about 550 million years long, covers the period of time during which animals with hard shells that fossilize would have been abundant.

Contents

The Eonothem is a corresponding system of classification of stratigraphy, a subdiscipline of geology, the multi-discipline analysis and classification of the rock layers laid down over the time passing during the specific eon. Eon's and Eonthems usually have the same names as established by the International Commission on Stratigraphy (ICS), then ratified by the parent organization the International Union of Geological Sciences (IUGS).

An eon is composed of several geologic eras, which in turn are composed of geologic periods, which are composed of geologic epochs, and so forth. The finest subdivisions in the system are geologic stages (Faunal stages), from which experts can give the most accurate dating estimates.

Terminology

We are currently in the Phanerozoic Eon, the Cenozoic Era, the Quaternary Period, and the Holocene epoch. Formerly, only one eon existed besides the Phanerozoic: the Precambrian. More recently, the Hadean, Archean, and Proterozoic "eras" of Precambrian time have been considered eons by the parent body of the ICS, the International Union of Geological Sciences (IUGS). The geologic timescale in terms of eons, eras, and periods looks like this:

GSSA/GSSA calibration points

The International Commission on Stratigraphy has been since 1974 and is currently undertaking a world wide series of baseline comparisons and calibrations establishing basal Global Boundary Stratotype Section and Point (GSSP), a sort of benchmark in the rock layers calibrated region to region world wide. Whereas the ICS states that for Precambrian era and before (always earlier than 630 Mya, and many others before 542 Mya due to the spotty fossil record), similar reference points called Global Standard Stratigraphic Ages (GSSA), each used also in defining subdivisions are established by absolute age of the strata and related classification criteria. Global Standard and Selection GSSP and GSSA points will aid many disciplines going forward, and the calibration such data references enables has already benefited research dependent upon lithographic dating.

Greek root

The English word eon is derived from the Koine Greek word aion.

Although a proposal was made in 1957 to define an aeon to be a unit of time equal to one billion years (1 Ga), the idea was not approved as a unit of scientific measure and is seldom used for a specific period of time. Its more common usage is for any lengthy or indefinite period of time. The origin is from the Greek root "aion" for "age" or "life force." A similar Latin word "aevum" for age is still present in words such as longevity and medieval.[1]

See also

Multidiscipline comparison

e  h
Units in geochronology and stratigraphy
Chronostratigraphic
strata units of the
geologic record
Geochronological
units of the
geological time system
Main article: geologic time scale


Notes
Eonothem
Eon
4 total, largest spans of years
Erathem
Era
 12 total, roughly span multiples
of a hundred million years
System
Period
 Some familiar names, defined in
21 major divisions and 2 minor
Series
Epoch
48 units & each spanning
tens of millions of years
Stage
Age
100+ units & most all
spanning millions of years
Outside the heirarchy, units cross stage and age boundaries as needed
if the strata has good dating characteristics.
Chronozone Chron  only in more recent strata*
* Most and the most time specific time divisions[2]


Related other topics

External links

Notes and references

References

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