Abstract Apatite is the primary phosphate mineral in the Earth’s crust and is present in a range of intrusive and extrusive igneous rocks, typically at minor to trace quantities. Similarly, apatite is a stable phase in many equilibrium crystallization experiments conducted with phosphorus-bearing starting compositions. We leverage this experimental stability to produce a large compilation of apatite-saturated liquid compositions, supplemented by additional apatite trace element and volatile partitioning and explicit apatite solubility experiments, as well as analyses of natural rhyolitic glasses. Using this compilation, we calibrate two new, independent models: for apatite saturation temperature as a function of melt P 2 O 5 and SiO 2 contents and aluminum saturation index (ASI; molar Al/(2Ca + Na + K)); and for melt P 2 O 5 contents at apatite saturation as a function of temperature, melt SiO 2 contents and ASI. The first model reproduces apatite saturation temperatures with an accuracy of ~ 32 °C, significantly outperforming existing apatite saturation models as well as recent zircon saturation thermometers. The second model reproduces melt P 2 O 5 contents at apatite saturation by better than a factor of two across four orders of magnitude. Our new calibrations show that, within uncertainty, apatite stability does not differ regardless of the specific volatile species present (H 2 O, F or Cl) or on the quantity of H 2 O dissolved in the melt. Further, we find that apatite stability is not sensitive to pressures at least in the range of 1 atm to 2 GPa. This model accurately describes the saturation of apatite in a wide range of liquids, including metaluminous liquids, moderately alkaline liquids, and most peraluminous liquids. Experimental and natural peraluminous liquids with unusually high P 2 O 5 contents that are not well described by our model contain CaO:P 2 O 5 ratios below apatite stoichiometry (‘perphosphorous melts’), indicating that apatite saturation in these liquids is at minimum jointly controlled by CaO and P 2 O 5 contents.
Klein et al. (Thu,) studied this question.