How does phosphorus cycle through ecosystems and why does it often limit growth?
Explain the phosphorus cycle and its role in limiting ecosystem productivity
A focused answer to the WACE Year 12 Earth and Environmental Science dot point on the phosphorus cycle. Covers weathering of phosphate rock, uptake and recycling, the lack of an atmospheric step, why phosphorus limits productivity, and human disruption through mining and fertiliser, with Australian context.
Reviewed by: AI editorial process; not yet individually human-reviewed
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What this dot point is asking
SCSA wants you to explain the phosphorus cycle and why it differs from the carbon and nitrogen cycles, and to connect it to productivity and human impact. The defining feature is that phosphorus has essentially no atmospheric reservoir, which makes it a sedimentary cycle and a common limiting nutrient.
A cycle without a gas phase
Carbon and nitrogen both have major atmospheric reservoirs and gaseous steps, which let them move quickly and globally. Phosphorus does not form a significant gas, so it is locked into a slow, mostly local cycle through rock, soil, water and organisms. This is the single most important contrast to draw.
Steps of the phosphorus cycle
- Weathering. Phosphorus is released slowly from phosphate-bearing rock as it weathers, freeing phosphate ions into soil and water.
- Uptake. Plants absorb dissolved phosphate and build it into molecules such as DNA, ATP and cell membranes; animals get phosphorus by eating plants.
- Recycling. Decomposers return phosphorus to the soil from dead organisms and waste, and this internal recycling supplies most of an ecosystem's phosphorus.
- Loss to sediment. Phosphate washed into water bodies settles into sediment, where it is effectively removed until uplift and weathering return it over millions of years.
Phosphorus and Australian soils
Many Australian landscapes are extremely old and have been weathered for a very long time, so much of their original phosphorus has been lost to leaching and sediment. Native ecosystems are adapted to low phosphorus, but agriculture on these soils usually requires added phosphate fertiliser, which is mined from phosphate rock, a finite resource.
Human disruption
- Mining phosphate rock transfers phosphorus from slow geological storage into the fast cycle, and the rock reserves are finite.
- Fertiliser runoff carries excess phosphate into rivers and lakes, where, with nitrogen, it drives eutrophication and algal blooms.
- Because the cycle is slow, phosphorus added to ecosystems is not quickly removed, so impacts persist.