Bedoukian   RussellIPM   RussellIPM   Piezoelectric Micro-Sprayer


Home
Animal Taxa
Plant Taxa
Semiochemicals
Floral Compounds
Semiochemical Detail
Semiochemicals & Taxa
Synthesis
Control
Invasive spp.
References

Abstract

Guide

Alphascents
Pherobio
InsectScience
E-Econex
Counterpart-Semiochemicals
Print
Email to a Friend
Kindly Donate for The Pherobase

« Previous AbstractThe contribution of cometary volatiles to the primitive Earth    Next AbstractComets and the formation of biochemical compounds on the primitive Earth--a review »

Adv Space Res


Title:The cometary contribution to prebiotic chemistry
Author(s):Oro J; Mills T; Lazcano A;
Address:"Department of Biochemical and Biophysical Sciences, The University of Houston, TX 77204, USA"
Journal Title:Adv Space Res
Year:1992
Volume:12
Issue:4
Page Number:33 - 41
DOI: 10.1016/0273-1177(92)90150-v
ISSN/ISBN:0273-1177 (Print) 0273-1177 (Linking)
Abstract:"Different estimates based on dynamical considerations, lunar cratering rates, Solar System chemical abundances, and the single-impact theory on the origin of the Earth-Moon system suggest that comets and other related small, volatile-rich primitive minor bodies captured by the Earth during the early Archean must have been a major source of volatiles on our planet. It is likely that a substantial fraction of the organic molecules present in the colliding cometary nuclei, which may have included nitrogen bases and the precursors of amino acids, were destroyed due to the high temperatures and shock wave energy associated with the collision. However, the presence of H2O, CN, CH, CO, CO2 and other carbon-bearing molecules and radicals in the atmosphere of the Sun and in circumstellar shells around carbon-rich stars suggests that at least simple carbon species could have survived the cometary collisions. Under the anoxic conditions thought to prevail in the prebiotic terrestrial paleoatmosphere, the post-collisional formation of a large number of excited molecules and radicals, and the rapid quenching of the expanding gaseous ball may have led, upon rapid cooling, to the formation of molecules of biogenic elements and to their eventual deposition in localized environments where complex organic compounds of biochemical significance may have been produced and accumulated"
Keywords:"Carbon Chemical Phenomena Chemistry *Earth, Planet Hydrogen *Meteoroids *Moon Nitrogen Oxygen *Solar System Sulfur Temperature NASA Discipline Exobiology NASA Discipline Number 52-20 NASA Program Exobiology Non-NASA Center;"
Notes:"MedlineOro, J Mills, T Lazcano, A eng Research Support, U.S. Gov't, Non-P.H.S. Research Support, U.S. Gov't, P.H.S. England 1992/01/01 Adv Space Res. 1992; 12(4):33-41. doi: 10.1016/0273-1177(92)90150-v"

 
Back to top
 
Citation: El-Sayed AM 2024. The Pherobase: Database of Pheromones and Semiochemicals. <http://www.pherobase.com>.
© 2003-2024 The Pherobase - Extensive Database of Pheromones and Semiochemicals. Ashraf M. El-Sayed.
Page created on 06-11-2024