The Phosphorus Cycle
Phosphorus starts its journey when weathering breaks down phosphate rocks on land, releasing soluble phosphates into soil and water. This is where things get interesting - most plants are actually rubbish at absorbing phosphates on their own!
That's why plants team up with mycorrhizal fungi in brilliant symbiotic relationships. These fungi create vast underground networks that massively increase the surface area available for phosphate absorption. It's like having a supercharged root system that can hoover up nutrients much more effectively.
When organisms die, decomposition breaks down their phosphorylated proteins, releasing phosphates back into the environment. However, much of this phosphorus gets locked away in marine sediments through sedimentation, making it unavailable to living organisms for potentially millions of years.
Key Point: Phosphorus often becomes a limiting factor for biological processes because most phosphorus compounds have very low solubility, and unlike nitrogen or carbon, there's no atmospheric reservoir to draw from.