Schreibersite on the early Earth:Scenarios for prebiotic phosphorylation

The mineral schreibersite,(Fe,Ni)P,provides a reactive source of phosphorus capable of forming phosphorylated molecules.These molecules may have been an important component of prebiotic chemistry,allowing their build-up and eventual commencement of autopoiesis.Discussed here are potential geochemical routes to providing schreibersite,as a potentially important prebiotic mineral,to the Hadean Earth.Two routes are identified:delivery of phosphides by meteoritic material and the reduction of phosphates to phosphides by high-temperature,low-redox conditions.About 1-10% of all crustal phosphorus is estimated to have been in schreibersite during the Hadean,making the long-term reaction of this mineral with organic-laden water plausible for many years.Ultimately,such conditions would have been conducive to the formation of life as we know it today.