Erathem

Source: Wikipedia, the free encyclopedia.
Eras mapped into Eons
Eras in the Phanerozoic Eon[1][2]
Geologic Era Span of Years Notes:
Cenozoic present – 065.5 (+/- 0.3) Mya many
GSSP
points
Mesozoic 065.5 (+/- 0.3) Mya – 251.0 (+/- 0.4) Mya many
GSSP
points
Paleozoic 251.0 (+/- 0.4) Mya – 542.0 (+/- 1.0) Mya mostly
GSSP
points
Eras in the Proterozoic Eon
542.0 (+/- 1.0) Mya – 2500 Mya[1][2]
Neoproterozoic 542.0 (+/- 1.0) Mya – 1000 Mya few
GSSP
points
Mesoproterozoic 1000 Mya – 1600 Mya all
GSSA
points
Paleoproterozoic 1600 Mya – 2500 Mya all
GSSA
points
Eras in the
Billion years – rocks older than 3.6 Billion years[1][2]
Neoarchean 2500 Mya – 2800 Mya (only
GSSA
points)
Mesoarchean 2800 Mya – 3200 Mya
Paleoarchean 3200 Mya – 3600 Mya
Eoarchean 3600 Mya – 4000 Mya Earth's crust solidifies
ca 3800 Mya[3]
Note: Rocks older than ca. 2500 Mya old are rare due to tectonic activity recycling the Earth's crust.

In

geologic timescale
.

It can therefore be used as a

microbial fossils in Australia are dated to this figure).[3] The atmosphere was a mix of noxious and poisonous gases (methane, ammonia, sulfur compounds, etc.[3] – a so-called reducing atmosphere[4] lacking much free oxygen
which was bound up in compounds).

These simple organisms,

fossil record
which specialists use to demarcate times early in planet earth's history in various disciplines.

Erathems are not often used in practice. While they are subdivisions of

systems
, dating experts prefer the finer resolution of smaller spans of time when evaluating strata.

Erathems have the same names as their corresponding eras. The Phanerozoic eonothem can thus be divided into Cenozoic, Mesozoic, and Paleozoic erathems. Similarly, the Proterozoic eonothem is divided youngest to oldest into the Neoproterozoic, Mesoproterozoic and Paleoproterozoic erathems, and the Archean eon and eonothem are divided similarly into the Neoarchean, Mesoarchean, Paleoarchean and the Eoarchean, for which a lower (oldest) limit is undefined.[1][2]

See also

Multidiscipline comparison

Units in geochronology and stratigraphy[5]
Segments of rock (strata) in chronostratigraphy Time spans in geochronology Notes to
geochronological units
Eonothem Eon 4 total, half a billion years or more
Erathem Era 10 defined, several hundred million years
System Period 22 defined, tens to ~one hundred million years
Series Epoch 34 defined, tens of millions of years
Stage Age 99 defined, millions of years
Chronozone
Chron
subdivision of an age, not used by the ICS timescale

Related other topics

Notes

  1. ^ a b c d International Commission on Stratigraphy, by Gabi Ogg. "International Stratigraphic Chart" (PDF). Archived from the original (PDF) on 2008-05-29. Retrieved 2008-06-17.
  2. ^ a b c d F.M. Gradstein, J.G. Ogg, A.G. Smith, et al., "A Geologic Time Scale", (2004; Cambridge University Press).
  3. ^ a b c d "Rockman's Geologic Time Chart". Retrieved 2008-06-17.
  4. ^ basis for the Miller–Urey experiment
  5. ^ Cohen, K.M.; Finney, S.; Gibbard, P.L. (2015), International Chronostratigraphic Chart (PDF), International Commission on Stratigraphy.

References

External links