Most other major nutrients such as phosphorus, potassium, magnesium, iron, and calcium enter terrestrial communities through the weathering of bedrock. These nutrients lack a volatile gaseous state. Consequently, they cycle through the biosphere differently from carbon, nitrogen, and sulfur, all of which sometimes occur as volatile gases. Of the nonvolatile nutrients, phosphorus is the one that most often limits plant growth, especially in aquatic environments.

Phosphorus and the other nonvolatile elements move unidirectionally from land, through aquatic environments, into ocean sediments. Most phosphorus cycling occurs between the surface and depths of the ocean. When near the surface, phosphorus is taken up by the plankton and passed through the food chain. It cycles back to the ocean bottom as individuals die and fall to the ocean floor, releasing assimilated phosphorus. Much of this element gradually accumulates in the ocean sediment as particulate phosphorus and is eventually brought back to the surface only through ocean upwelling and tectonic activity. The ocean sediments are therefore by far the greatest reservoirs of phosphorus.

In terrestrial ecosystems, much of the available phosphorus moves in a closed cycle between living organisms and the organic debris in the soil. Phosphate (PO₄³⁻) is the only important inorganic form involved in this cycle. Microorganisms in the soil break down litter and other organic matter, thereby releasing phosphate, which is then taken up by plants and released again when they die and decompose. Soils differ in the amount of phosphorus they contain, and in some phosphorus-poor soils almost all the available phosphorus resides in living organisms and organic debris. In some tropical forests, such as those in parts of Brazil, so much of the phosphorus is contained in living organisms that the clearing of forests eliminates most of this element. As a result, the plant communities cannot recover, and crops cannot be grown.

The addition of phosphorus to soils poor in this nutrient and the use of phosphorus-rich detergents have had a great impact on the phosphorus cycle in many ecosystems. Runoff from agricultural fields and the emptying of sewage has introduced so much extra phosphorus to rivers and lakes that populations of plants and microorganisms have grown explosively, sometimes creating a solid mat that extends over the surface of the water. This growth increases the amount of organic debris in the water, which can lead to a decrease in the available oxygen, resulting in suffocation of fish and other animals.

The hydrologic cycle

A portion of the biogeochemical cycle of all elements involves time spent cycling through the hydrosphere. Water itself cycles within the biosphere. (For a detailed discussion of the hydrologic cycle see hydrosphere: The hydrologic cycle.) Unlike the cycles of the other major nutrients, however, the hydrologic, or water, cycle would continue in some form even in the absence of living organisms. Most of Earth’s water is in its core, in the sedimentary rocks near its surface, and in the ocean. A minute percentage of the water, however, continually cycles through the atmosphere, oceans, and terrestrial environments mainly by the processes of evaporation and precipitation.

This part of the hydrologic cycle is driven by solar energy. Water evaporates from both the aquatic and terrestrial environments as it is heated by the Sun’s energy. The rates of evaporation and precipitation depend on solar energy, as do the patterns of circulation of moisture in the air and currents in the ocean. Evaporation exceeds precipitation over the oceans, and this water vapour is transported by the wind over land, where it returns to the land through precipitation. The water falling onto terrestrial environments seeps into the ground or runs off into lakes and streams and eventually empties into the oceans, carrying with it many of the other major nutrients. Water also reenters the atmosphere through the evaporative loss of water by plants (transpiration).

Links among the cycles

Although the overall pattern of cycling of all the major elements is now known, there is still much to learn about the relative importance of the different stages of each cycle. For example, there is considerable debate concerning which ecosystems act as the major sources of carbon for the atmosphere and which act as sinks by accumulating more carbon than they release. The ways in which the different cycles interact with one another also must be minutely studied. It has been discovered that sulfur availability influences the rate of nitrogen accumulation in plants and nitrogen availability influences phosphorus uptake. All three elements are thought to influence the rate of carbon accumulation by plants. As a result, changes in any one of these nutrient cycles influence the other cycles as well.

The effects that disruptions in these cycles may have within the biosphere are not clearly understood. Natural geologic phenomena, such as ice ages and major periods of volcanic activity, have repeatedly disturbed these cycles throughout Earth history. Many human activities may have impacts of similar scope. Deforestation, the burning of fossil fuels, and increased fertilization are disturbing these cycles. These anthropogenic disturbances have increased atmospheric levels of carbon dioxide (Figure 4), decreased ozone (O₃) levels, and undermined the natural equilibrium of streams and lakes by excessive nutrient enrichment from sewage, fertilizers, and factory waste (cultural eutrophication). Gleaning more information about the biogeochemical cycles and their interactions has become increasingly important now that the effects of human activities are becoming more apparent.

Another potential effect that may result from human intrusions in the environment is global warming. Carbon dioxide in the atmosphere has the ability to act as an insulator, preventing some of Earth’s heat, absorbed from solar radiation, from escaping back into space. This process, known as the greenhouse effect, is suspected of being enhanced by rising levels of atmospheric carbon dioxide (Figure 4), which have resulted in part from the combustion of fossil fuels and the clearing and burning of tropical forests. This increase in atmospheric carbon dioxide and other so-called greenhouse gases could raise the overall global temperature, causing the polar ice caps to melt, sea levels to rise, and Earth’s precipitation to be redistributed.

The complexity and interconnectedness of each of the biogeochemical cycles make it difficult to pinpoint how any one human activity is altering the cycles; nevertheless, the majority of those who study these fluctuations agree that this is happening. Disagreements generally concern the extent to which various activities affect particular cycles and what the long-term consequences of these disturbances will be.