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• W1567128788 abstract "The biosphere plays an important role in the global carbon cycle during Earth’s evolution starting from the Archaean to the far future. In particular it has a significant influence on the silicate rock weathering by amplifying the processes. Furthermore relatively inert organic carbon is built up from the decay of organic matter, which contributes 10–20% to the present surface reservoirs of carbon. The buildup of this storage of reduced carbon is complemented by the rise of oxygen in the atmosphere. The Cambrian explosion, that is, the occurrence of complex life 0.54 Gy ago, can be explained by interactions between the geosphere and biosphere. The Cambrian explosion was so rapid because of a positive feedback between the spread of biosphere, increased silicate weathering, and a consequent cooling of the climate. After the Cambrian explosion the environment itself has been actively changed by the biosphere maintaining the temperature conditions for its existence. The ultimate life span of the biosphere is defined by the extinction of prokaryotes in about 1.6 Gy because of CO 2 starvation." @default.
• W1567128788 created "2016-06-24" @default.
• W1567128788 creator A5054983337 @default.
• W1567128788 date "2008-01-01" @default.
• W1567128788 modified "2023-10-18" @default.
• W1567128788 title "Climate Change 2: Long-Term Dynamics" @default.
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• W1567128788 doi "https://doi.org/10.1016/b978-008045405-4.00725-4" @default.
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