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Phosphorus cycles through plants and animals much faster than it does through rocks and sediments. When animals and plants die, phosphates will return to the soils or oceans again during decay. After that, phosphorus will end up in sediments or rock formations again, remaining there for millions of years.
Together with nitrogen, arsenic, antimony, and bismuth, phosphorus is classified as a pnictogen. Phosphorus is an element essential to sustaining life largely through phosphates, compounds containing the phosphate ion, PO43?.
Particularly common in granitic pegmatites are the primary phosphates apatite [Ca5(F,Cl,OH)(PO4)3], triphylite [LiFePO4], lithiophilite [LiMnPO4], and the rare-earth phosphates monazite [(LaCe)(PO4)] and xenotime [Y(PO4)].
Organic phosphates are commonly found in the form of esters as nucleotides (e.g. AMP, ADP, and ATP) and in DNA and RNA.
Phosphates are compounds made of phosphorus and oxygen. The most common base phosphate unit is PO4. In simplified terms, phosphates can be derived as esters or salts of phosphoric acid.