Carbon does not move through the carbon cycle in isolation; it is continually exchanged between different reservoirs, including the atmosphere, oceans, soil, and living organisms. Human activities, such as burning fossil fuels and deforestation, can disrupt these natural processes by increasing atmospheric carbon levels. Additionally, certain forms of carbon, such as fossilized organic matter, can remain locked in geological formations for millions of years, effectively removing them from the active carbon cycle. Thus, carbon's movement is influenced by both natural processes and human impact.
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