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- W1623136437 endingPage "555" @default.
- W1623136437 startingPage "515" @default.
- W1623136437 abstract "Molecular oxygen (O 2 ) is generated and consumed by a wide span of biological and abiotic processes. Chief among these are photosynthesis and respiration, but on geologic timescales, burial and weathering of redox-active elements such as carbon and sulfur exert strong controls on atmospheric O 2 concentrations. The global cycling of O 2 is controlled by a coupled system of physical, chemical, and most importantly, biological processes acting on and in the Earth's surface. Large inroads have been made toward understanding the processes that control the concentration of atmospheric O 2 , especially regarding O 2 as a component of coupled biogeochemical cycles of many elements, including carbon, sulfur, nitrogen, phosphorus, iron, and others. Numerical models of sedimentary rock abundance and of the isotope systematics of the surficial cycles of carbon and sulfur provide useful insights into the evolution of atmospheric O 2 through time. At the same time, advances in isotope geochemistry and geobiology contribute to an ever more detailed understanding of the geologic history of atmospheric O 2 from the early Earth through the Phanerozoic." @default.
- W1623136437 created "2016-06-24" @default.
- W1623136437 creator A5034012904 @default.
- W1623136437 date "2003-01-01" @default.
- W1623136437 modified "2023-10-18" @default.
- W1623136437 title "The Global Oxygen Cycle" @default.
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