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 (mya) to 2,500 mya. It contains the first sedimentary rocks, and the first fossil life forms, which were cyanobacteria, and acritarchs.
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. The large supercontinent Vaalbara formed in the Archaean. There were oceans already, before the Archaean. The atmosphere almost entirely lacked free oxygen, and instead, it was mostly methane and CO2.
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. Initially, this oxygen was absorbed by combining with iron ions in solution. Not until much later did oxygen build up in the atmosphere.
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References[change | change source]
- 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.