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  • Biogeochemical Cycling: How Organisms & Environment Exchange Nutrients
    The exchange of useful chemicals between organisms and their abiotic environment is an example of biogeochemical cycling.

    Here's why:

    * Bio refers to living organisms.

    * Geo refers to the Earth.

    * Chemical refers to the elements and compounds involved.

    Biogeochemical cycling describes the movement and transformation of chemical elements (like carbon, nitrogen, phosphorus, etc.) through the Earth's ecosystems. This includes:

    * Organisms taking in nutrients: Plants absorb nutrients from the soil and water. Animals obtain nutrients by consuming plants or other animals.

    * Organisms releasing nutrients: Plants and animals release waste products and eventually decompose, returning nutrients to the soil and water.

    * Abiotic processes: Geological processes like weathering and volcanic eruptions release nutrients into the environment. Physical processes like evaporation and precipitation also play a role.

    Examples:

    * Carbon Cycle: Plants absorb carbon dioxide from the atmosphere for photosynthesis. Animals consume plants (or other animals) and release carbon dioxide through respiration.

    * Nitrogen Cycle: Nitrogen gas from the atmosphere is converted into usable forms by bacteria in the soil. Plants absorb these forms and are consumed by animals.

    * Phosphorus Cycle: Phosphorus is released from rocks through weathering. Plants absorb phosphorus from the soil, and animals obtain it by eating plants.

    So, the exchange of useful chemicals is a fundamental part of how life on Earth sustains itself and interacts with the non-living environment.

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