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Plants in the biosphere take in carbon dioxide from the atmosphere during photosynthesis, releasing oxygen. This carbon is then transferred to the lithosphere through dead organic matter and geological processes such as weathering and erosion. Carbon also enters the hydrosphere through carbon dioxide dissolving in water and through the bodies of aquatic organisms. Carbon is then cycled back into the atmosphere through respiration, combustion, and volcanic activity. The diagram of Earth's carbon cycle demonstrates the interconnectedness and interdependence of the biosphere, lithosphere, atmosphere, and hydrosphere in maintaining the balance of carbon on our planet.

Plants play a crucial role in the carbon cycle by absorbing carbon dioxide during photosynthesis and releasing oxygen. Once the plants die, the carbon is transferred to the lithosphere through various geological processes like erosion and weathering. Additionally, carbon can enter the hydrosphere through dissolved carbon dioxide and aquatic organisms. The continuous cycle of carbon moving between the atmosphere, biosphere, lithosphere, and hydrosphere is illustrated in the Earth's carbon cycle diagram, showing the interconnectedness and balance of carbon on our planet.