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Nauru and nearby Ocean Island were important sources of phosphate for Australian and New Zealand fertilizer production and played an important role on both countries agriculture industries at the time of World War II.
Additionally, the δ18Op ranges of many phosphate sources overlap one another, making it very difficult to infer sources of phosphate.
The availability of economically viable sources of phosphate fertilizer is declining [ 5].
However, even with careful dietary modification, hidden sources of phosphate mean that dietary limitation of phosphate intake is difficult, and often remains an inadequate means of controlling hyperphosphataemia.
Patients were encouraged not to alter their eating habits during the study and protein intake was retrospectively estimated based on urea nitrogen levels; however, non-protein sources of phosphate would not necessarily be identified using this method.
Johnson et al. [ 47] and Lindsay et al. [ 48] speculated that this phosphate derived from dephosphorylation of CP and ATP, since these were the most likely sources of phosphate.
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Non-point sources of phosphates may include natural decomposition of rocks and minerals, agricultural runoff, erosion and direct input by animals/wildlife.
Non-point sources of phosphates may include: natural decomposition of rocks and minerals, agricultural runoff, erosion and direct input by animals/wildlife; whereas point sources may include: aquaculture activities and permitted industrial discharges.
The island's guano, a rich source of phosphate, has fertilised Australian and New Zealand farms for nearly a century.
Struvite is a good source of phosphate and it can be recovered from livestock waste such as cow urine.
Alternatively, during times of severe phosphate deprivation, the phosphate contained in bone mineral provides a source of phosphate for the metabolic needs of the organism.
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