“…Precipitation may occur abiogenically, but there are also numerous examples of extant microbes that are known to modify their surroundings causing phosphate minerals to form external to the cell, and other microbes that precipitate phosphate within or on their cell wall (Ehrlich, 1999). Most bio-phosphates are initially amorphous precursor species (Konhauser, Fyfe, Schultze-Lam, Ferris, & Beveridge, 1994) but crystalline phosphates, including the apatite minerals, also have been identified (e.g., Arning et al, 2009;Bailey et al, 2013;Beveridge, Meloche, Fyfe, & Murray, 1983;Beveridge & Fyfe, 1985;Benzerara, Yoon, et al, 2004;Benzerara, Menguy et al, 2004;Blakemore & Frankel, 1989;Brock & Schulz-Vogt, 2011;Ennever, Vogel, & Streckfuss, 1974;Goldhammer et al, 2010;González-Muñoz et al, 2010;Hirschler, Lucas, & Hubert, 1990;Konhauser et al, 1994;Lovley & Phillips, 1988;Macaskie, Empson, Cheetham, Grey, & Skarnulis, 1992;Rivadeneyra, Pérez-García, & Ramos-Cormenzana, 1992;Rivadeneyra, Martín-Algarra, Sánchez-Navas, & Martín-Ramos, 2006;Schulz & Schulz, 2005). However, the range of abiogenic and biogenic conditions for such bioprecipitation remains poorly understood (Rivadeneyra et al, 2006).…”