“…were previously reported to solubilize PR by producing Ca-chelators or siderophores [ 78 ]. In addition to organic acid secretion and H + dissolving mechanisms, P may be liberated from P i minerals by the synthesis of chelators (e.g., Ca, Al, and Fe-chelators) in PSB, PSA, and blue green algae ( Figure 2 ) [ 78 , 81 , 87 , 88 ]. Since PR and other primary P i minerals are mainly insoluble hydroxyapatite, or Ca, Al, and Fe/phosphate, the siderophores and chelators could form chelates with Ca, Al, and Fe, resulting in the release of P originally bound by these metals [ 81 ].…”