MadSci Network: Earth Sciences |
The short answer is that land plants and marine phytoplankton (algae) contribute _all_ of the oxygen to the atmosphere. Before the evolution of photosynthesis (the biological process which generates oxygen), there was essentially no oxygen in the earth’s atmosphere. About 2 Billion years ago photosynthesis evolved but it wasn’t until about 430 million years ago that oxygen rose to near current levels (21% of the atmosphere). In any given year, respiration, oxidation and combustion only consume a small fraction of the oxygen that has built up in the atmosphere (less than 1 part out of 2500), which is balanced by the generation of “fresh” oxygen by photosynthesis. Roughly half the oxygen generated each year comes from land plants and half from phytoplankton. A full budget for oxygen in the atmosphere (just like a budget for a business, it tracks where all of the oxygen is stored and “spent”) can be found in the article: What atmospheric oxygen measurements can tell us about the global carbon cycle by RF Keeling and others in the March 1993 issue of Global Biogeochemical Cycles.
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