Phytate (IP 6 ) is often the most common organic P compound particularly in agricultural soils. understanding the fate of inositol phosphate (IP x ) in the environment in terms of isomeric composition and concentration and assessing relative resistance to (or preference for) degradation is essential to estimate the potential role of IP x in generating inorganic P (P i ) as well as overall P cycling in the environment. In this study, we analyzed IP 6 degradation by four common phosphohydrolase enzymes (phytase from wheat [Triticum aestivum l.] and Aspergillus niger and acid phosphatase from wheat germ and potato [Solanum tuberosum l.]), with particular focus on degradation pathways, isomer kinetic decay rate, and isotope effects using a combination of high-performance ion chromatography, nuclear magnetic resonance, stable isotopes, and process-based modeling techniques. our results show that the degradation pathways are often distinct among enzymes. The process-based Bayesian inverse modeling was used to capture the trend and magnitude of the measured concentrations for each IP x isomer and to determine the decay constants. Furthermore, o isotope ratios (d 18 o P ) of released P i enabled the identification of isotopically identical phosphate moieties in phytate derived from natural sources. Distinctly different fractionation factors, degradation pathways, and kinetic decay rate coefficients among the enzymes studied could lead to potential discrimination and tracking of phytate sources and products as well as active enzymes present in the environment.Abbreviations: HPIC, high-performance ion chromatography; IP, inositol phosphate; NMR, nuclear magnetic resonance; P i , inorganic phosphorus; pNPP, para-nitrophenyl phosphate.I nositol phosphates are a group of organic P compounds widely present in the natural environment (Turner et al., 2002). Phytate (the salt of myo-inositol 1,2,3,4,5,6-hexakisphosphate or IP 6 ) is a P storage molecule in cereals and grains and represents between 60 and 80% of P in mature seeds (Raboy, 1997). Since it is reported that ?51 million tonnes of phytate is formed in commercially produced fruits and crop seeds every year (Lott et al., 2000), a good fraction of phytate in seeds and grains is released to the soil environment as plant residues and animal manures (Dao, 2007;Gerke, 2015). Phytate readily sorbs onto minerals or precipitates with soil cations and organic matter, and then accumulates to constitute an often dominant class of organic P (Celi and Barberis, 2007;Giles and Cade-Menun, 2014). Although sorption and precipitation immobilizes a large fraction of phytate in soil, there is a potential for its transfer to water bodies with soil particulates and colloids (Turner et al., 2002;Turner and Newman, 2005
Core Ideas• Phytate is degraded through distinct pathways for a particular enzyme.• oxygen isotope ratios of phosphate moieties in phytate are isotopically identical.• These findings bring new insights into tracking phytate sources in the environment.