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Biogeochemical cycle

earth science Maturity 9-11 Next article →

Earth is a master at recycling everything it has.

Generalized biogeochemical cycle
Generalized biogeochemical cycle

Most matter does not just disappear from our planet. Instead, it moves through a series of steps called a biogeochemical cycle. These cycles move chemical elements between living things and the Earth. The living part of our world is called the biosphere. The non-living parts include the atmosphere, the lithosphere, and the hydrosphere.

90 mile beach
90 mile beach

These different areas work together to keep the planet running.

These cycles work by moving substances through different pathways. In the carbon cycle, plants take carbon dioxide from the air. They use a process called photosynthesis to turn it into food. This helps them grow and gives them energy.

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

When organisms breathe or die, carbon goes back into the air or soil. In the nitrogen cycle, tiny life forms perform nitrogen fixation. This turns nitrogen gas into forms that plants can actually use.

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

Water also moves in a constant cycle. It evaporates from the ocean to form clouds in the sky. Then, it falls back to the ground as precipitation.

Scientists study how these cycles move through the Earth. They look at how elements move between the living and non-living worlds. Much of this work focuses on important nutrients like carbon and nitrogen.

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

Some cycles move very quickly through the air and life. Other cycles, like the movement of minerals in rocks, are much slower. These slow changes happen in the lithosphere through weathering and erosion. Even volcanoes play a role by releasing matter from deep inside the Earth.

Many different elements take part in these global cycles. Carbon, nitrogen, hydrogen, and oxygen are some of the most common.

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

Phosphorus is used to make parts of cells, and sulfur helps shape proteins. There are also cycles for elements like calcium, iron, and mercury. These elements can stay in certain places for a very long time. These places are called geological reservoirs. Even the rock cycle is a type of large-scale cycle.

These cycles are all connected to each other. For example, moving water helps carry sulfur and phosphorus into rivers.

Rock cycle nps
Rock cycle nps

Tiny microorganisms are the most important drivers of these movements. Without these tiny life forms, many cycles would stop working. Human activities can also change how these cycles work. Burning fossil fuels or using too much fertilizer can disrupt the natural balance. This can lead to problems like climate change or pollution. Keeping these cycles healthy helps support all life on Earth.

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🖼️ 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
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