Nepedia
Back to Discover
Advanced Reader
🌍

Biogeochemical cycle

earth science Maturity 9-11 Next article →

A biogeochemical cycle is the continuous movement and transformation of chemical elements and compounds. These substances move between living organisms and the Earth's physical environments. This process is vital because Earth's chemical composition is essentially fixed. Unlike energy, which enters from the Sun and leaves as heat, matter must be recycled.

Generalized biogeochemical cycle
Generalized biogeochemical cycle

This recycling allows life to persist using the same limited supply of atoms.

These cycles operate through two main compartments. The biotic compartment is the biosphere, which includes all living things. The abiotic compartments are the atmosphere (air), the hydrosphere (water), and the lithosphere (land).

90 mile beach
90 mile beach

Substances move through pathways connecting these areas. They may undergo chemical rearrangements during this journey. For example, a molecule might change its structure as it moves from a rock into a plant.

Microorganisms are the critical drivers of these global cycles. These tiny life forms carry out diverse metabolic processes. These processes are essential for cycling macronutrients and micronutrients through ecosystems. Without microorganisms, many of these essential cycles would simply not occur.

Role of marine organisms in biogeochemical cycling
Role of marine organisms in biogeochemical cycling

Their activity ensures that nutrients are available for all other life forms.

Different cycles move at different speeds. The carbon cycle is a major example. Plants absorb atmospheric carbon dioxide through photosynthesis. This process uses light energy to combine carbon with hydrogen and oxygen. This creates organic compounds used for energy and growth.

Simplified diagram of the global carbon cycle
Simplified diagram of the global carbon cycle

Carbon returns to the atmosphere through respiration and decomposition. It can also be stored in fossil fuels for long periods.

The nitrogen cycle follows a different path. Most nitrogen exists as gas in the atmosphere. Plants cannot use this gas directly. Instead, nitrogen fixation converts atmospheric nitrogen into usable forms like ammonia and nitrates. Other organisms then use these compounds. Eventually, nitrogen returns to the atmosphere through processes like denitrification.

The Nitrogen Cycle (1)
The Nitrogen Cycle (1)

This ensures the nitrogen supply remains balanced.

Water also moves through a constant cycle. Water evaporates from land and oceans to form clouds. This is called evaporation. The water then returns to the planet through precipitation.

Simplified budget of carbon flows in the ocean
Simplified budget of carbon flows in the ocean

Precipitation can seep into the ground to become groundwater. It can also become surface runoff that forms rivers and lakes. This water eventually carries dissolved organic matter and nutrients into the oceans.

Six elements are especially important for organic molecules. Carbon is found in all organic molecules. Nitrogen is a key component of proteins and nucleic acids. Hydrogen and oxygen are essential parts of water. Phosphorus is used to build biological membranes and nucleic acids. Sulfur is critical for the three-dimensional shape of proteins.

Rock cycle nps
Rock cycle nps

These elements cycle through various geological reservoirs, where they may remain sequestered for long periods.

All these cycles are deeply interconnected. For instance, the movement of water helps leach sulfur and phosphorus into rivers. These rivers then carry those nutrients into the oceans. However, human activities can disrupt these delicate balances. Burning fossil fuels and using large amounts of fertilizer can change how cycles function. These disruptions contribute to environmental issues like climate change and pollution.

490 words

Where will your curiosity go next?

Keep exploring at your chosen reading level.

🖼️ Images & Media (9)
File:Generalized biogeochemical cycle.jpg
Generalized biogeochemical cycle.jpg
File:The Nitrogen Cycle (1).png
The Nitrogen Cycle (1).png
File:90 mile beach.jpg
90 mile beach.jpg
File:Role of marine organisms in biogeochemical cycling.jpg
Role of marine organisms in...
File:Simple box model.png
Simple box model.png
File:Simplified budget of carbon flows in the ocean.png
Simplified budget of carbon flows in the ocean.png
File:Simplified diagram of the global carbon cycle.jpg
Simplified diagram of the global carbon cycle.jpg
File:Carbon cycle.jpg
Carbon cycle.jpg
File:Rock cycle nps.PNG
Rock cycle nps.PNG
More to explore

🔬 Go deeper

More advanced topics to explore

🪜 Step back

Simpler topics to build understanding

What is Nepedia?

A free, ad-free encyclopedia for children. Every article is written at five reading levels, so the same page works for a five-year-old and a fifteen-year-old — use the level switcher above to see this one change. No account needed to read.