Carbon and Nitrogen Cycles
Carbon Cycle
All living organisms contain carbon, essential for life processes.
Carbon is cyclical, moving through different forms and reservoirs in the environment.
Once organisms die, carbon from their bodies is decomposed and returned to the ecosystem.
Decomposers like bacteria and fungi play a crucial role in breaking down dead matter.
Human activities such as burning fossil fuels release carbon into the atmosphere as carbon dioxide, contributing to climate change.
Key Concepts of the Nitrogen Cycle
Importance of Nitrogen:
Nitrogen is a vital component of molecules in living organisms, particularly in proteins and nucleic acids.
Forms of Nitrogen:
N: nitrogen gas in the atmosphere (78% of atmosphere).
NH₃: ammonia, a usable form for plants.
NO₃⁻ and NO₂⁻: nitrates and nitrites, forms that plants can absorb.
Processes in the Nitrogen Cycle:
Nitrogen Fixation:
Bacteria in soil and plant roots convert nitrogen gas into ammonia, nitrates, and nitrites.
Lightning can also convert nitrogen gas into these usable forms.
Denitrification:
Bacteria covert nitrates back into nitrogen gas, returning it to the atmosphere.
Uptake:
Plants absorb nitrogen from the ground through their roots, primarily in the form of nitrates.
Excretion:
Animals release nitrogen back into the environment through urine or feces (mostly as urea).
Feeding:
Animals obtain nitrogen by consuming plants or other animals.
Decomposition:
Breaks down dead organisms, releasing nitrogen back into the soil, making it available for reabsorption by plants.
This process is carried out by decomposers such as bacteria and fungi.
Human Impact:
Human-made fertilizers can enhance nitrogen levels in crops but can also lead to runoff and environmental concerns.
Overall Breakdown:
The nitrogen cycle comprises a series of processes that allows for the continuous use of nitrogen in different forms within ecosystems, emphasizing the connectedness of life and the environment.