Archaean
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The English used in this article may not be easy for everybody to understand. (June 2013) |
| Archaean Eon 4000 - 2500 million years ago |
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Scale:
Millions of years |
The Archaean (or Archean) eon is the geological period after the Hadean and before the Proterozoic. It is one of the four main time periods (eons) of Earth history.
The Archaean lasted from 4,000 million years ago to 2,500 mya.[1] It contains the first sedimentary rocks, and the first fossil life forms, which were cyanobacteria,[2] and acritarchs.[3]
Most of the rocks which survive are volcanic (igneous) and metamorphic in origin. Volcanic activity was everywhere. When the Archaean began, the Earth's heat flow was nearly three times higher than it is today. It was still twice the current level when the Archaean ended, 2,500 mya. This high level of heat flow may have made plate tectonics more vigorous than today. The question of when plate tectonics began is a major research area.[4] The large supercontinent Vaalbara formed in the Archaean. There were oceans already, before the Archaean. The atmosphere almost entirely lacked free oxygen, and instead, methane and CO2 were major constituents.
Fossil bacterial mats, called stromatolites, are found throughout the Archaean after about 3,500mya. These were formed by cyanobacteria, which used photosynthesis and gave off oxygen as a by-product.[5] Initially, this oxygen was absorbed by combining with iron ions in solution. Not until much later did oxygen accumulate in the atmosphere.[6]
Fossil raindrop marks have been found in the later Archaean, 2,700 mya.[7] The rocks were discovered in Ventersdorp in the North West Province of South Africa in the 1980s.
References[change]
- ↑ International Chronostratigraphic Chart. [1]
- ↑ Knoll, Andrew H. 2004. Life on a young planet: the first three billion years of evolution on Earth. Princeton, N.J. ISBN 0-691-12029-3
- ↑ Buick R. 2010. Early life: ancient acritarchs. Nature 463: 885–886. doi:10.1038/463885a. PMID 20164911.
- ↑ Stanley, Steven M. 1999. Earth system history. New York: Freeman. p297-301 ISBN 0-7167-2882-6
- ↑ Schopf J.W. 1992. Geology and paleobiology of the Archaean Earth, in Schopf J.W., and Klein C. The Proterozoic biosphere: a multidisciplinary study, Cambridge University Press. ISBN 0-521-36615-1
- ↑ see Great Oxygenation Event
- ↑ Amos, Jonathan 2012. Fossil raindrops probe ancient atmosphere. BBC News: Science & Environment. [2]
| Archaean Eon | |||
|---|---|---|---|
| Eoarchaean | Palaeoarchaean | Mesoarchaean | Neoarchaean |
| Precambrian (4.567 gya – 541 mya) | |
|---|---|
| In the left column are Eons, bold are Eras, not bold are Periods. gya = billion years ago, mya = million years ago | |
| Hadean (4.567 gya – 4 gya) | |
| Archaean (4 gya – 2.5 gya) | Eoarchaean (4 gya – 3.6 gya)
Palaeoarchaean (3.6 gya – 3.2 gya) |
| Proterozoic (4 gya – 2.5 gya) | Palaeoproterozoic (2.5 gya – 1.6 gya) Siderian (2.5 gya – 2.3 gya) Rhyacian (2.3 gya – 2.05 gya) Orosirian (2.05 gya – 1.8 gya) Statherian (1.8 gya – 1.6 gya)
Mesoproterozoic (1.6 gya – 1 gya) Calymmian (1.6 gya – 1.4 gya) Ectasian (1.4 gya – 1.2 gya) Stenian (1.2 gya – 1 gya) Neoproterozoic (1 gya - 541 mya) Tonian (1 gya – 850 mya) Cryogenian (850 mya – 635 mya) Ediacaran (635 mya – 541 mya) |
| Source | International Chronostratigraphic Chart 2013. International Commission on Stratigraphy, retrieved 8 April 2013. Divisions of geologic time – major chronostratigraphic and geochronologic units USGS, retrieved 8 April 2013. |
