Planetary Accretion, Bombardment, and Equilibration
Formation of the Heliosphere and planetary solar system (4.6-4.5 bya)
Accretion of Earths Primordial Geosphere and Atmosphere
Initial atmosphere of H2, He, CH4, N2, NH3, H2O, Metallic Vapors, Noble Gases. Rapid loss of lighter non-polar gases. Gradual accumulation of volcanic outgassing - CO, CO2, H2O, H2S
Low abiotic concentrations of molecular oxygen scavenge electrons from other elements resulting in the formation of oxides and an anaerobic environment.
H2O, CO, CO2, P2O5
Na2O, K2O
MgO, CaO, Al2O3, SiO2, TiO2
FeO, Fe2O3, Fe3O4
Collisional Lunar Event and extraterrestrial bombardment (4.5-3.9 bya)
Last impactor large enough to completely boil off Earths oceans. and the first "prebiotic broths", strikes. Large impactors are still capable of boiling the Earths Oceans periodically, but the Great Bombardment is waning and the primary solvent base of the ocean is established permanently.
The Ten Million Year Rain - The Condensation of Atmospheric Water Vapors and establishment of the hydrosphere.
The final "Prebiotic Soup" of organic and inorganic constituents in a mineral-rich aqueous broth cooked by geological and atomospheric processes surge through the fissures of the Earths crust and mantle and then work their way back to the surface. This solution becomes increasingly dilute as water continues to condense out of the atmosphere and enters the hydrosphere. Non-polar substances partition from aqueous phase and give rise to prebiotic liposphere.
Establishment of permanent oceans/beginning of dynamic equilibration of the Geosphere/Hydrosphere (3.9 bya) - [Mantle-Crustal-Atmospheric Redox Couple, Na+,K+,Cl- osmolality]
Fe2+ and H2S abundant in seawater precipitates Iron Sulfide.
Primordial upwelling of inorganic and abiotic thiorganic molecules from hydrothermal and volcanic sources flow over precipitated Iron Sulfide chimney/vent systems in a continuous flux.
Substantial seawater concentrations of Ca2+,Mg2+ limits free/soluble phosphate. Phosphate is sequestered as precipitates of Mg, Ca, Fe, and other metals.
Phase II - Iron-Sulfur World & The Chemoautotrophic Ignition (3.9 bya)
Hyperbarometric Hyperthermophily/Thermophily, Transition Metals, Organosulfur, and Carboxylate Surface-bonders
Iron-Sulfur World - Thio-organic Chemistry occurring on the Iron Sulfide/Pyrite surface of a Hydrothermal Vent System generating sulfur-analogs of the primary metabolites from inorganic monomers CS, CO, CS2, COS, CO2, H2S, H2O, HCN
Iron Sulfide conversion to Pyrite serves as a kinetically inhibited source of energetic electrons for the reduction of inorganic carbon to organic carbon (Geoenergetic)
Phosphorus Invasion - the system encounters Ferrous Phosphate (Vivianite) and polyphosphate surfaces still under a flux of H2S and pyrite formation, enabling phosphate to enter the metabolism
Polyanionic surface-bonded phosphates anchor organic moieties on a positively charged pyrite surface (Phosphorypeds)
Phosphoesters provide a means to couple phosphoanhydride energy stores to their organic moieties