Can sources of aquatic PO<sub>4sub> be traced using its stable oxygen isotope ratio?
Various PO<sub>4sub> sources within a catchment were analysed for their δ<sup>18sup>O<sub>PO4sub>.
River δ<sup>18sup>O<sub>PO4sub> indicated that rapid microbial cycling of PO<sub>4sub> was occurring.
This method appears inappropriate in systems where PO<sub>4sub> cycling is rapid.
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