title: Serpentinite and the dawn of life.
abstract: Submarine hydrothermal vents above serpentinite produce chemical potential gradients of aqueous and ionic hydrogen, thus providing a very attractive venue for the origin of life. This environment was most favourable before Earth's massive CO(2) atmosphere was subducted into the mantle, which occurred tens to approximately 100 Myr after the moon-forming impact; thermophile to clement conditions persisted for several million years while atmospheric pCO(2) dropped from approximately 25 bar to below 1 bar. The ocean was weakly acid (pH ∼ 6), and a large pH gradient existed for nascent life with pH 9-11 fluids venting from serpentinite on the seafloor. Total CO(2) in water was significant so the vent environment was not carbon limited. Biologically important phosphate and Fe(II) were somewhat soluble during this period, which occurred well before the earliest record of preserved surface rocks approximately 3.8 billion years ago (Ga) when photosynthetic life teemed on the Earth and the oceanic pH was the modern value of approximately 8. Serpentinite existed by 3.9 Ga, but older rocks that might retain evidence of its presence have not been found. Earth's sequesters extensive evidence of Archaean and younger subducted biological material, but has yet to be exploited for the Hadean record.
authors.affiliation: Department of Geophysics, Stanford University, Stanford, CA 94305, USA. norm@stanford.edu
authors.forename: Norman H
authors.initials: NH
authors.lastname: Sleep
authors.forename: Dennis K
authors.initials: DK
authors.lastname: Bird
authors.forename: Emily C
authors.initials: EC
authors.lastname: Pope
mesh_terms: D001105:Archaea / Q000737:chemistry* / Q000254:growth & development; D017632:Asbestos, Serpentine / Q000737:chemistry*; D001419:Bacteria / Q000737:chemistry* / Q000254:growth & development; D005075:Biological Evolution; D002247:Carbon Isotopes / Q000737:chemistry; D018534:Earth, Planet; D005290:Ferric Compounds / Q000737:chemistry; D019015:Geologic Sediments / Q000737:chemistry / Q000382:microbiology; D006859:Hydrogen / Q000737:chemistry; D006863:Hydrogen-Ion Concentration; D060086:Hydrothermal Vents / Q000737:chemistry; D009792:Oceans and Seas; D000069497:Origin of Life; D010710:Phosphates / Q000737:chemistry; D010788:Photosynthesis; D012313:RNA / Q000737:chemistry; D017640:Silicates / Q000737:chemistry
chemical_list: D017632:Asbestos, Serpentine; D002247:Carbon Isotopes; D005290:Ferric Compounds; D010710:Phosphates; D017640:Silicates; C060346:basalt; D012313:RNA; D006859:Hydrogen