Biogeochemical Cycles
Biogeochemical cycles
Biogeochemical cycles are the natural pathways through which essential elements like carbon, nitrogen, and phosphorus circulate between the biotic (living) and abiotic (non-living) components of Earth.
- Biogeochemical cycles are natural processes that circulate and recycle the chemical elements essential for life through different spheres of the Earth.
- These cycles link the biotic environment (living organisms) with the abiotic environment (air, water, soil, rocks).
The key biogeochemical cycles include:
- Carbon cycle: involves the movement of carbon between the atmosphere, biosphere, hydrosphere, and lithosphere.
- Nitrogen cycle: focuses on nitrogen transformations through atmospheric, terrestrial, and aquatic systems.
- Phosphorus cycle: a sedimentary cycle involving movement from rocks to living organisms and back.
- Hydrological cycle: the movement of water through evaporation, condensation, precipitation, and runoff.
Key Spheres Involved in Biogeochemical Cycling
- Biosphere: all living organisms and their interactions.
- Lithosphere: the Earth’s crust and upper mantle; includes soils and rocks.
- Atmosphere: the layer of gases surrounding Earth, containing nitrogen, oxygen, CO₂, and trace gases.
- Hydrosphere: all forms of water on Earth, including oceans, rivers, lakes, groundwater, and atmospheric water vapour.
Role in Ecosystem Functioning
- Biogeochemical cycles ensure that key nutrients remain available to living organisms over time.
- Carbon is cycled through photosynthesis, feeding, respiration, and decomposition, maintaining a steady supply for biological molecules like carbohydrates, lipids, and proteins.
- Nitrogen is fixed by bacteria into forms plants can use, then recycled through food chains and decomposers.
- Phosphorus, often derived from weathering of rocks, cycles through soil, water, and organisms, supporting bone formation and DNA synthesis.
- Disruptions to these cycles can affect nutrient availability, impacting primary productivity, species interactions, and overall ecosystem resilience.
Human Impacts on Biogeochemical Cycles
- Human activities increasingly disrupt the natural balance of these cycles, often causing excess accumulation or depletion of elements in certain compartments, thereby affecting ecosystem sustainability.
- Major disruptions include:
- Burning fossil fuels → increases atmospheric CO₂, contributing to climate change.
- Deforestation → reduces carbon uptake and alters nutrient flows.
- Fertilizer overuse → disrupts nitrogen and phosphorus cycles, leading to eutrophication and water pollution.


