Literature DB >> 11536666

Evidence for organic synthesis in high temperature aqueous media--facts and prognosis.

B R Simoneit1.   

Abstract

Hydrothermal systems are common along the active tectonic areas of the earth. Potential sites being studied for organic matter alteration and possible organic synthesis are spreading ridges, off-axis systems, back-arc activity, hot spots, volcanism, and subduction. Organic matter alteration, primarily reductive and generally from immature organic detritus, occurs in these high temperature and rapid fluid flow hydrothermal regimes. Hot circulating water (temperature range - warm to >400 degrees C) is responsible for these molecular alterations, expulsion and migration. Compounds that are obviously synthesized are minor components because they are generally masked by the pyrolysis products formed from contemporary natural organic precursors. Heterocyclic sulfur compounds have been identified in high temperature zones and hydrothermal petroleums of the Guaymas Basin vent systems. They can be interpreted as being synthesized from formaldehyde and sulfur or HS kappa- in the hydrothermal fluids. Other products from potential synthesis reactions have not yet been found in the natural systems but are expected based on known industrial processes and inferences from experimental simulation data. Various industrial processes have been reviewed and are of relevance to hydrothermal synthesis of organic compounds. The reactivity of organic compounds in hot water (200-350 degrees C) has been studied in autoclaves, and supercritical water as a medium for chemistry has also been evaluated. This high temperature aqueous organic chemistry and the strong reducing conditions of the natural systems suggest this as an important route to produce organic compounds on the primitive earth. Thus a better understanding of the potential syntheses of organic compounds in hydrothermal systems will require investigations of the chemistry of condensation, autocatalysis, catalysis and hydrolysis reactions in aqueous mineral buffered systems over a range of temperatures from warm to >400 degrees C.

Entities:  

Keywords:  NASA Discipline Exobiology; NASA Discipline Number 52-20; NASA Program Exobiology; Non-NASA Center

Mesh:

Substances:

Year:  1995        PMID: 11536666     DOI: 10.1007/bf01581578

Source DB:  PubMed          Journal:  Orig Life Evol Biosph        ISSN: 0169-6149            Impact factor:   1.950


  17 in total

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Journal:  Geochim Cosmochim Acta       Date:  1993       Impact factor: 5.010

Review 3.  Chemical markers of prebiotic chemistry in hydrothermal systems.

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4.  Abiotic synthesis of amino acids under hydrothermal conditions and the origin of life: a perpetual phenomenon?

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5.  Supercritical fluids.

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Journal:  Geochim Cosmochim Acta       Date:  1993-07       Impact factor: 5.010

8.  Purification and characterization of an alpha-glucosidase from a hyperthermophilic archaebacterium, Pyrococcus furiosus, exhibiting a temperature optimum of 105 to 115 degrees C.

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9.  Oregon subduction zone: venting, fauna, and carbonates.

Authors:  L D Kulm; E Suess; J C Moore; B Carson; B T Lewis; S D Ritger; D C Kadko; T M Thornburg; R W Embley; W D Rugh; G J Massoth; M G Langseth; G R Cochrane; R L Scamman
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10.  Venting of carbon dioxide-rich fluid and hydrate formation in mid-okinawa trough backarc basin.

Authors:  H Sakai; T Gamo; E S Kim; M Tsutsumi; T Tanaka; J Ishibashi; H Wakita; M Yamano; T Oomori
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  12 in total

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Authors:  T M McCollom; B R Simoneit
Journal:  Orig Life Evol Biosph       Date:  1999-03       Impact factor: 1.950

2.  Lipid synthesis under hydrothermal conditions by Fischer-Tropsch-type reactions.

Authors:  T M McCollom; G Ritter; B R Simoneit
Journal:  Orig Life Evol Biosph       Date:  1999-03       Impact factor: 1.950

3.  Metabolism and motility in prebiotic structures.

Authors:  Martin M Hanczyc
Journal:  Philos Trans R Soc Lond B Biol Sci       Date:  2011-10-27       Impact factor: 6.237

4.  Amplification of diverse catalytic properties of evolving molecules in a simulated hydrothermal environment.

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Journal:  Orig Life Evol Biosph       Date:  2003-12       Impact factor: 1.950

5.  The asymmetry of organic aerosol fission and prebiotic chemistry.

Authors:  D J Donaldson; A F Tuck; V Vaida
Journal:  Orig Life Evol Biosph       Date:  2002-06       Impact factor: 1.950

6.  Chemical evolution and meteorites: an update.

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7.  Organic aerosols and the origin of life: an hypothesis.

Authors:  D J Donaldson; H Tervahattu; A F Tuck; V Vaida
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8.  The role of submarine hydrothermal systems in the synthesis of amino acids.

Authors:  A D Aubrey; H J Cleaves; Jeffrey L Bada
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9.  Biomarkers as tracers for life on early earth and Mars.

Authors:  B R Simoneit; R E Summons; L L Jahnke
Journal:  Orig Life Evol Biosph       Date:  1998-10       Impact factor: 1.950

Review 10.  The first living systems: a bioenergetic perspective.

Authors:  D W Deamer
Journal:  Microbiol Mol Biol Rev       Date:  1997-06       Impact factor: 11.056

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