• Source: Eoarchean

The Eoarchean (IPA: EE-oh-ar-KEE-ən; also spelled Eoarchaean) is the first era of the Archean Eon of the geologic record. It spans 431 million years, from the end of the Hadean Eon 4031 Mya to the start of the Paleoarchean Era 3600 Mya.
Some estimates place the beginnings of life on Earth in this era, while others place it earlier. Evidence of archaea and cyanobacteria date to 3500 Mya, comparatively shortly after the Eoarchean. At that time, the atmosphere was without oxygen and the pressure values ranged from 10 to 100 bar (around 10 to 100 times the atmospheric pressure today).




Chronology


The Eoarchean Era was formerly officially unnamed and informally referred to as the first part of the Early Archean Eon (which is now an obsolete name) alongside the Paleoarchean Era.
The International Commission on Stratigraphy now officially recognizes the Eoarchean Era as the
first part of the Archaean Eon, preceded by the Hadean Eon, during which the Earth is believed to have been essentially molten.
The Eoarchaean's lower boundary or starting point of 4.031 Gya (4031 million years ago) is officially recognized by the International Commission on Stratigraphy.
The name comes from two Greek words: eos (dawn) and Archaios (ancient). The first supercontinent candidate Vaalbara appeared around the end of this period at about 3,600 million years ago.




Geology



The beginning of the Eoarchean is characterized by heavy asteroid bombardment within the Inner Solar System: the Late Heavy Bombardment. The largest Eoarchean rock formation is the Isua Greenstone Belt on the south-west coast of Greenland, which dates from 3.8 billion years. The Acasta Gneiss within the Canadian Shield have been dated to be 4,031 Ma and are therefore the oldest preserved rock formations. In 2008, another rock formation was discovered in the Nuvvuagittuq Greenstone Belt in northern Québec, Canada, which has been dated to be 4,280 million years ago. These formations are presently under intense investigation. Oxygen isotope ratios show that the hydrological cycle had begun by the early Eoarchaean and possibly earlier. Carbonate precipitation (caused by heating of sea water by hydrothermal vents) acted as an important sink regulating the concentration of carbon dioxide in the atmosphere during this era.




Atmosphere


3,850 million years old apatite from Greenland shows evidence of Carbon-12 enrichment. This has sparked a debate whether there might have been photosynthetic life before 3.8 billion years ago.




Proposed subdivisions


Eoarchean Era — 4031–3600 Mya
Acastan Period — 4031–3810 Mya
Isuan Period — 3810–3600 Mya




See also


Precambrian Supereon (4600-539 Mya)
Hadean Eon (4600-4031 Mya)
Archean Eon (4031-2500 Mya)
Paleoarchean Era (3600-3200 Mya)
Mesoarchean Era (3200-2800 Mya)
Neoarchean Era (2800-2500 Mya)
Proterozoic Eon (2500-539 Mya)




References






Further reading


Egel, R.; Lankenau, D.-H.; Mulkidjanian, A. Y. (2011). Origins of Life: The Primal Self-Organization. Berlin Heidelberg: Springer-Verlag. doi:10.1007/978-3-642-21625-1. ISBN 978-3-642-21624-4.




External links


Media related to Eoarchean at Wikimedia Commons
Taxonconcept.stratigraphy.ne: A short fact sheet on the Eoarchean
Eoarchean (chronostratigraphy scale)

Kata Kunci Pencarian:

• Eoarkaikum
• Eoarchean
• Eoarchean geology
• EO
• Hadean
• Nuvvuagittuq Greenstone Belt
• Biodiversity
• Triassic
• Ur (continent)
• Plate tectonics
• Late Heavy Bombardment