Prebiotic phosphorus chemistry reconsidered.
The available evidence indicates that the origin of life on Earth certainly occurred earlier than 3.5 billion years ago and perhaps substantially earlier. The time available for the chemical evolution which must have preceded this event is more difficult to estimate. Both endogenic and exogenic contributions to chemical evolution have been considered; i.e., from chemical reactions in a primitive atmosphere, or by introduction in the interiors of comets and/or meteorites. It is argued, however, that the phosphorus chemistry of Earth's earliest hydrosphere, whether primarily exogenic or endogenic in origin, was most likely dominated by compounds less oxidized than phosphoric acid and its esters. A scenario is presented for the early production of a suite of reactive phosphonic acid derivatives, the properties of which may have foreshadowed the later appearance of biophosphates.
Schwartz
A W
AW
Evolutionary Biology Research Group, University of Nijmegen, The Netherlands.
D001272:Atmosphere; D019418:Evolution, Chemical; D019110:Meteoroids; D063065:Organophosphonates / Q000737:chemistry*; D010720:Phosphines / Q000737:chemistry; D010721:Phosphinic Acids / Q000737:chemistry*; D017905:Phosphites / Q000737:chemistry; D010756:Phosphoric Acids / Q000737:chemistry; D010758:Phosphorus / Q000737:chemistry*; D017976:Phosphorus Acids / Q000737:chemistry*
D063065:Organophosphonates; D010720:Phosphines; D010721:Phosphinic Acids; D017905:Phosphites; D010756:Phosphoric Acids; D017976:Phosphorus Acids; D010758:Phosphorus