User:Jtwsaddress42/Projects/Project 1/Parts/Part 1

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Stage I - Surface-Catalyzed Ignition of the Metabolism and Biosphere (4.6-3.85 bya)

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Stage I - Surface-Catalyzed Ignition of the Metabolism and Biosphere (4.6-3.85 bya)

Phase I - Gaia-Genesis (4.6-4.5 bya)

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 Earth/Moon 

 Moon 

 Stationary 

 Core 

 Metallic 

 Mesosphere 

 Lithosphere 

 Ionic 
 Geosphere 

 Cryosphere 

 Ice 
 Phase 
 Mobile 

 Liposphere 

 Nonpolar 

 Hydrosphere 

 Polar 

 Atmosphere 

 Gases 
 Phase 
 Earth 
Biosphere
 System 

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)

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 CS2,COS,CO2 
 FeS/H2S ⇒ FeS2 + 2 H+ + 2 e 
 FeS/H2S ⇒ FeS2 + H2O 

 Fe-S Clusters 

 Exergonic 
 R‑COSH + CO2 ⇒ R‑CO‑COSH 
 Thiols,Thials,Thiones 

 Thioacetal 
 Chemistry 

 Carbonyl [H] Rxns 
 α‑Ketoacids 

 Chemoautotrophic 
 RCC Core 

 Iron-Sulfur World 

 Autocatalytic Cycle 
 Thiocarboxylates 
 & Carbon Fixation 
 Chemoautotrophic 
 Ignition 

4.56 - 3.9 GYA 

Pyrite-Pyrrhotite
 
Hydrothermal "Black Smoker" vent

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)
    • H2S/(Fe,Ni,Co) Sulphides ⇒ Iron-Sulfur Clusters  
    • H-R-COS- + CO2 + FeS + 2 H2S ⇒ R=CSH-COS- + FeS2 + 2 H2O
  • Anionic Surface-anchored Thiocarboxylates anchored on a positively charged iron sulfide/pyrite surface - (Carboxypeds)
    • Polycarboxylic Acids possess enhanced surface-bonding and retention by the iron sulfide/pyrite surface
  • Pyrite-pulled Autocatalytic Proto-Reductive Citric Acid Cycle (RCC) ⇒ Chemoautotrophic Surface Metabolist (RCC Metabolic Core)
    • Thiols /(Thio)Aldehydes /(Thio)Ketones ↔ Thioenols /(Thio)Carboxylates / Alpha-Keto-Acids ↔ Alpha-Thioenol-Acids
    • Fatty Acids  
  • Surface-anchored Thio-analogs of Proto-coenzyme moieties
    • 2-mercaptoethanesulfonate ⇒ Coenzyme M  
    • ? ⇒ Lipoic Acid  
    • ? ⇒ Coenzyme Q  


Phase III - Thioester World & The Nitrogen Invasion

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 Nitrogen Invasion 
 Branch Pathways 
 FeS/H2S ⇒ FeS2 

 αKG ⇒ Glu (Acidic)

 OXO ⇒ Asp (Acidic)

 PYR ⇒ Ala (Neutral Non-polar)

 Reductive Amination 
 FeS/H2S ⇒ FeS2 

 Glu + Glu ⇔ αKG + Gln (Neutral Polar)

 Glu + Asp ⇔ αKG + Asn (Neutral Polar)

 Synthase Rxns 

 α-Ketoacids ⇔ α-Amino Acids

 Transanimase Rxns 
 AA Synthesis 

 Non-coded Polypeptides 

 Condensation Rxns 

 Biotin 

 Pyridoxal 

 Pantetheine 

 Proto-Thiamine 

 Proto‑Coenzymes 

 Thioester World 

 Chemoautotrophic 
 RCC Core
 
 Iron-Sulfur World 

Expanding the core - Heterochemistry and The Introduction of New Elements

  • Thioester World - Kinetically Inhibited High-energy Thioester intermediates as proto-bioenergetic transferase metabolites  
  • Nitrogen Invasion - Ammonium enters the system via Pyrite-pulled Nitrogen Fixation on Fe,V,Mo Sulphide surfaces  
  • Amino Acid Pathways  
  • GSH-GSSG Redox Buffer  
  • Surface-anchored Thio-analogs of Nitrogen containing Proto-coenzyme moieties
    • ? ⇒ Biotin  
    • ? ⇒ Coenzyme B  
    • ? ⇒ Flavin  
    • ? ⇒ Nicotinamide  
    • ? ⇒ Pantothenic Acid  
    • ? ⇒ Protoporphyrin IX  
    • ? ⇒ Pyridoxamine  ⇔ Pyridoxal  ⇔ Pyridoxine  
    • ? ⇒ Tetrahydrofolate  
    • ? ⇒ Thiamine  
  • Pyrimidines  
  • Purines  


Phase IV - Phosphoester World & The Bioenergetic Takeover (3.87 bya)

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 Phosphate Invasion 
 Peptides 

 Proto-Kinase Rxns 

 Carbohydrates 

 Proto-Neoglucogenesis 

 Phosphorylation 
 Rxns 

 Aminoglycan Pathways 

 Nucleoside Pathways 

  

 Nucleotide Coenzymes 

 Energy Carriers 

 Nucleic Acid Chemistry 

 Phosphoester World 

  
 Polymerization 
 Rxns 
 Bioenergetic 
 Transfer 
 Phosphoanhydride 
 Takeover 
 Thioester World 

Vivianite-Pyrite

Mesophily, Alkaline Earths & Phosphates

  • 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  
    • pH Buffer System: H2PO4-/HPO42-
  • Phosphorylation Pathways
  • Aldose & Ketose Pathways
  • PNPP
  • cyclicAminoacetals/purines
  • Surface-anchored protoNucleotides (protoNMP's)]
  • Reversible energy-storage carriers/NucleotidePolyphosphates (NDP's/NTP's)
  • NucleotideCoenzymes


Phase V - Nucleic Acid World

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Psychrophily, Coenzyme Handles, Polymerization

  • Nucleic Acid World -
  • Montmorillonite
  • Macromolecular Polymerization
  • Nucleozymes(Ligase/Nuclease/Polymerase/Replicase/AminoAcylNAsynthase/Kinase)
  • Surface-bound Amino Acid-anchored 3' AminoAcylNucleic Acids(Sb3ANA's)