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楼主: FERN
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https://doi.org/10.1057/9781137402561cient forms, but gave impetus to development of biochemical pathways that could use simple inorganic energy sources such as molecular hydrogen, or direct support of biochemical synthesis using sunlight. Pigments originally useful in protecting simple cells from the destructive effects of solar radia
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https://doi.org/10.1007/978-3-030-46582-7s global expansion. The need for carbon dioxide might initially have been met by such CO. as was contained in the atmosphere and dissolved in the oceans. When this was consumed, all photosynthesizers had to depend on new CO. produced by geologic process, such as subduction of organic sediments follo
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Danielle Mariann Dove,Sarah E. Maierest examples (the so-called Ediacaran fauna) are known from fossils of soft-bodied organisms in late Precambrian rocks. The fossil record of these creatures is good enough to indicate the existence of an ecosystem with a variety of types, and examples are known from around the world, suggesting wide
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Irregulars: Sherlockian Youth as Outsiders,veloped the capability of producing hard body parts, of either organic or mineral material. The Cambrian Explosion that led off the Phanerozoic saw the sudden (geologically speaking) appearance of virtually all of the basic body types seen in modern animals, including arthropods and vertebrates. The
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https://doi.org/10.1007/978-3-030-31911-3w the emergence of flying reptiles and birds, and the return of some land reptiles to an aquatic existence. These were generally gradual changes leading to a progressively more complex global ecosystem. This was suddenly ended at the end of the Cretaceous Period about 65 million years ago in yet ano
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