biogeochemical cycle

This cycling of matter is known as the biogeochemical cycle.

This discovery has had an important impact on our current understanding of biogeochemical cycles.

Land plants are key components of the water cycle and several other biogeochemical cycles.

From this view, biogeochemical cycles are driven by radiant energy.

The sulfur cycle was the first of the biogeochemical cycles to be discovered.

Such biogeochemical cycles are important in geology because they affect many minerals.

As a result, the rates of carbon circulation in the biogeochemical cycle is decreased.

After death, the remains of an organism re-enter the biogeochemical cycle.

All chemical elements occurring in organisms are part of biogeochemical cycles.

These microbes play a vital role in biogeochemical cycles.

A key difference compared to other biogeochemical cycles is that because of its low molecular weight hydrogen can leave Earth's atmosphere.

Soil microorganisms act as both sinks and sources of available P in the biogeochemical cycle.

There is much overlap between the terms for biogeochemical cycle and nutrient cycle.

Responses of Society: What are the relationships between marine biogeochemical cycles, ecosystems, and the human system?

Throughout history, the Earth's atmosphere and biogeochemical cycles have been in a dynamic equilibrium with planetary ecosystems.

Winogradsky discovered various biogeochemical cycles and parts of these cycles.

Biogeochemical cycles including related aspects of marine chemistry and geochemistry also represent a central theme.

Beyond direct transformation of land area, humans have impacted the global biogeochemical cycles, leading to human caused change in even the most remote areas.

In addition to the practical applications, near-surface geophysics includes the study of biogeochemical cycles.

Changes in marine biogeochemical cycles and ecosystems due to global change will also have consequences for the broader Earth System.

Humans are altering the planet's biogeochemical cycles in a largely unregulated way with limited knowledge of the consequences.

Global biogeochemical cycles are critical to life, most notably those of water, oxygen, carbon, nitrogen and phosphorus.

Biogeochemical cycles always involve hot equilibrium states: a balance in the cycling of the element between compartments.

All agricultural systems are underpinned by the processes of energy flows and biogeochemical cycles which, when disrupted, bring about environmental degradation.

Understanding the sensitivity of these biogeochemical cycles to changing environmental condition will improve projections of the ocean's response to global change.