The carbon cycle is the process through which carbon moves between the biotic (living organisms) and abiotic (non-living components) parts of an ecosystem. Below is an overview of how carbon moves through the various components you've listed, along with the relevant processes:
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CO₂ (Carbon Dioxide) in the Atmosphere
- Photosynthesis: Plants absorb CO₂ from the atmosphere and convert it into organic matter (glucose) using sunlight.
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Plants
- Absorption: Plants absorb CO₂ during photosynthesis, storing carbon in their biomass (stems, leaves, and roots).
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Animals
- Consumption: Animals consume plants (and other animals), taking in carbon in the organic material.
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Respiration:
- Both plants and animals release CO₂ back into the atmosphere through respiration as they convert glucose for energy.
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Ocean:
- CO₂ from the atmosphere can dissolve in ocean water.
- CaCO₂ Fixation: Marine organisms (like shellfish) use dissolved CO₂ in the water to form calcium carbonate (CaCO₂) for their shells.
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Shells:
- When marine organisms die, their shells can accumulate on the ocean floor and become part of sedimentary deposits.
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Fossils:
- Over geological time, shells and organic matter can be buried and converted into fossil fuels (coal, oil, natural gas) through heat and pressure in a process known as geologic storage.
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Human Use:
- Humans extract fossil fuels for energy and other uses, which releases stored carbon back into the atmosphere.
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Combustion:
- When fossil fuels are burned for energy (like in cars, factories, and power plants), CO₂ is released back into the atmosphere, completing the cycle.
Summary of Processes in the Carbon Cycle:
- Photosynthesis → Plants absorb CO₂ → Animals consume plants → Respiration → CO₂ released back into the atmosphere.
- From atmosphere to ocean → CaCO₂ Fixation in marine organisms → Shells → Fossils → Geologic Storage and human extraction → Combustion, releasing CO₂ back into the atmosphere.
This cycle is crucial to maintain the balance of carbon in the environment and is essential for life on Earth.