Carbon is stored in the short term primarily through biological processes, such as photosynthesis, where plants absorb carbon dioxide and convert it into organic matter. This carbon can then be released back into the atmosphere through respiration or decomposition. In the long term, carbon is sequestered in geological formations, such as fossil fuels, coal, and sedimentary rocks, where it can remain for millions of years. Additionally, carbon can also be stored in soils and oceanic systems, contributing to longer-term carbon storage solutions.
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