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Titlebook: Living Earth; A Short History of L E. G. Nisbet Book 1991 Springer Netherlands 1991 atmosphere.coevolution.development.ecosystem.environmen

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楼主: 战神
发表于 2025-3-23 11:54:59 | 显示全部楼层
The Archaean planetname is taken from the Greek source to describe the beginning of the geological record and the pervasive influence of life on Earth. As yet we have no agreed definition of when the Hadean (the accretionary period), ended and the Archaean began. We could use the beginning of the geological record, at
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The surface of the Proterozoic Earth time of great but shadowy events. The dark beginnings were closing: the world was starting to take its modern shape. In the late Archaean, we see the biosphere in its medieval morning, dispelling the Dark Ages. Then, at some time in the Proterozoic the bacteria give rise to the eukaryotes, with the
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The birth of the eukaryotesrm the essential background to existence. The more obvious players on the stage today are the multi-celled plants and animals that have occupied the seas and colonized the continents, to form a complex, planet-wide, interdependent network of life. How did the change come about?
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The rule of the reptilesliar large carnivorous reptile is the crocodile. One of the diversions of geological field work in Africa is to sit hidden on a river bank, very still, and watch for what are locally called ‘flat dogs’ or, in deference to Western consumer tastes, ‘handbags’. The signs are obvious — little mounds of
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Humanitying of these precursors is the fossil of a single tooth that appears to have belonged to a very primitive representative of the line of vertebrates called primates. Humans are primates. The animal that owned the tooth is appropriately called ., after Purgatory Hill in the Hell Creek Formation.
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