Archean Eon oor Spaans
Archean Eon
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Arcaico
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archean eon
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eón Arcaico
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Archean eon
en
the time from 3,800 million years to 2,500 million years ago; earth's crust formed; unicellular organisms are earliest forms of life
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eón Arcaico
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voorbeelde
Advanced filtering
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No species existed in the Archean eon.
Artículo # (antiguo artículoLiterature Literature
The geologic record of the Proterozoic Eon is more complete than that for the preceding Archean Eon.
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(Presents more occurrences of detrital pyrite and uraninite during the Archean Eon.)
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During the Archean eon the Earth had little oxygen in its rocks, air, and water.
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Most of the rocks of the Archean Eon are dark basalts and its organisms are the bacteria.
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Gaia, the living system, was born at the very beginning of the Archean Eon, about 4,000 million years ago.
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The presence of pillow lavas in the oldest preserved volcanic sequences on the planet, the Isua and Barberton greenstone belts, confirms the presence of large bodies of water on the Earth's surface early in the Archean Eon.
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It includes three eons, the Hadean, Archean, and Proterozoic.
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Though commonly used, the Hadean is not a formal eon and no lower bound for the Archean and Eoarchean have been agreed upon.
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Current evidence suggests that the last universal common ancestor lived during the early Archean eon, perhaps roughly 3.5 Ga or earlier.
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Current phylogenetic evidence suggests that the last universal ancestor (LUA) lived during the early Archean eon, perhaps 3.5 Ga or earlier.
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Current phylogenetic evidence suggests that the last universal common ancestor (LUCA) lived during the early Archean eon, perhaps 3.5 Ga or earlier.
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Biological nitrogen fixation (BNF, performed by the organisms called diazotrophs) is a very old process that probably originated in the Archean eon when the primitive atmosphere lacked oxygen.
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This closeness to the Moon caused that, in the Archean Eon (approximately between 3900 and 2500 million years ago) the tidal forces were higher than the ones nowadays.
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The Archean Eon (/ɑːrˈkiːən/, also spelled Archaean) is a geologic eon, 4,000 to 2,500 million years ago (4 to 2.5 billion years), that followed the Hadean Eon and preceded the Proterozoic Eon.
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In contrast to the deep-water deposits of the Archean, the Proterozoic features many strata that were laid down in extensive shallow epicontinental seas; furthermore, many of those rocks are less metamorphosed than are Archean ones, and many are unaltered.[4]:315 Studies of these rocks have shown that the eon continued the massive continental accretion that had begun late in the Archean Eon.
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Though oxygen is believed to have been released by photosynthesis as far back as Archean Eon, it could not build up to any significant degree until mineral sinks of unoxidized sulfur and iron had been filled. Until roughly 2.3 billion years ago, oxygen was probably only 1% to 2% of its current level.[5]:323 The Banded iron formations, which provide most of the world's iron ore, are one mark of that mineral sink process.
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Since the origin of our planet, geologists have divided time into different divisions of millions of years: the eons (Archean, Proterozoic and Phanerozoic), which in turn are divided into different eras.
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^ Though commonly used, the Hadean is not a formal eon[35] and no lower bound for the Archean and Eoarchean have been agreed upon.
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In contrast to the deep-water deposits of the Archean, the Proterozoic features many strata that were laid down in extensive shallow epicontinental seas; furthermore, many of these rocks are less metamorphosed than Archean-age ones, and plenty are unaltered.[4]:315 Study of these rocks shows that the eon continued the massive continental accretion that had begun late in the Archean, as well as featured the first definitive supercontinent cycles and wholly modern orogenic activity.[4]:315–18, 329–32
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In contrast to the deep-water deposits of the Archean, the Proterozoic features many strata that were laid down in extensive, shallow epicontinental seas; furthermore, many of these rocks are less metamorphosed than Archean-age ones, and plenty are in fact unaltered.[13]p315 Study of these rocks show that the eon featured rapid continental accretion (unique to the Proterozoic), supercontinent cycles, and wholly-modern orogenic activity.[13]p315/8; 329/32
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Although the first continents formed during this eon, rock of this age makes up only 7% of the present world's cratons; even allowing for erosion and destruction of past formations, evidence suggests that continental crust equivalent to only 5-40% of the amount formed during the Archean.[7]
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Although the first continents formed during this eon, rock of this age makes up only 7% of the world's current cratons; even allowing for erosion and destruction of past formations, evidence suggests that continental crust equivalent to only 5-40% of the present amount formed during the Archean.[7]
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23 sinne gevind in 4 ms. Hulle kom uit baie bronne en word nie nagegaan nie.