Redox history of the Earth's interior since approximately 3900 Ma: implications for prebiotic molecules

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Redox history of the Earth's interior since approximately 3900 Ma: implications for prebiotic molecules is …
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scholarly articleQ13442814

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P6179Dimensions Publication ID1008178700
P356DOI10.1023/A:1011895600380
P698PubMed publication ID11599174

P2093author name stringDelano JW
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Evidence in pre-2.2 Ga paleosols for the early evolution of atmospheric oxygen and terrestrial biotaQ47813138
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Evidence from detrital zircons for the existence of continental crust and oceans on the Earth 4.4 Gyr agoQ22122386
Initiation of clement surface conditions on the earliest EarthQ24619616
Primordial carbonylated iron-sulfur compounds and the synthesis of pyruvateQ28144509
Microfossils of the Early Archean Apex chert: new evidence of the antiquity of lifeQ28215389
Evidence for life on Earth before 3,800 million years agoQ28295460
Chemical events on the primitive EarthQ28776804
A production of amino acids under possible primitive earth conditionsQ29616231
Energetics and kinetics of the prebiotic synthesis of simple organic acids and amino acids with the FeS-H2S/FeS2 redox couple as reductantQ33541361
Oxygen-isotope evidence from ancient zircons for liquid water at the Earth's surface 4,300 Myr ago.Q33934396
Earth's early atmosphereQ34089375
Impact frustration of the origin of lifeQ34089395
Annihilation of ecosystems by large asteroid impacts on the early EarthQ34089402
Endogenous production, exogenous delivery and impact-shock synthesis of organic molecules: an inventory for the origins of lifeQ34089538
Mantle redox evolution and the oxidation state of the Archean atmosphereQ34517442
A thermodynamic assessment of the potential synthesis of condensed hydrocarbons during cooling and dilution of volcanic gasesQ38497435
P433issue4-5
P407language of work or nameEnglishQ1860
P304page(s)311-341
P577publication date2001-08-01
P1433published inOrigins of Life and Evolution of BiospheresQ2153690
P1476titleRedox history of the Earth's interior since approximately 3900 Ma: implications for prebiotic molecules
P478volume31

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cites work (P2860)
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