Literature DB >> 11536607

Submarine hot springs and the origin of life.

S L Miller1, J L Bada.   

Abstract

The discovery of hydrothermal vents at oceanic ridge crests and the appreciation of their importance in the element balance of the oceans is one of the main recent advances in marine geochemistry. It is likely that vents were present in the oceans of the primitive Earth because the process of hydrothermal circulation probably began early in the Earth's history. Here we examine the popular hypothesis that life arose in these vents. This proposal, however, is based on a number of misunderstandings concerning the organic chemistry involved. An example is the suggestion that organic compounds were destroyed on the surface of the early Earth by the impact of asteroids and comets, but at the same time assuming that organic syntheses can occur in hydrothermal vents. The high temperatures in the vents would not allow synthesis of organic compounds, but would decompose them, unless the exposure time at vent temperatures was short. Even if the essential organic molecules were available in the hot hydrothermal waters, the subsequent steps of polymerization and the conversion of these polymers into the first organisms would not occur as the vent waters were quenched to the colder temperatures of the primitive oceans.

Entities:  

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

Mesh:

Substances:

Year:  1988        PMID: 11536607     DOI: 10.1038/334609a0

Source DB:  PubMed          Journal:  Nature        ISSN: 0028-0836            Impact factor:   49.962


  55 in total

1.  The stability of some selected amino acids under attempted redox constrained hydrothermal conditions.

Authors:  E Andersson; N G Holm
Journal:  Orig Life Evol Biosph       Date:  2000-02       Impact factor: 1.950

2.  The stability of amino acids at submarine hydrothermal vent temperatures.

Authors:  J L Bada; S L Miller; M Zhao
Journal:  Orig Life Evol Biosph       Date:  1995-06       Impact factor: 1.950

3.  Mixed-valence hydroxides as bioorganic host minerals.

Authors:  K Kuma; W Paplawsky; B Gedulin; G Arrhenius
Journal:  Orig Life Evol Biosph       Date:  1989       Impact factor: 1.950

4.  Speculations on the origin of life and thermophily: review of available information on reverse gyrase suggests that hyperthermophilic procaryotes are not so primitive.

Authors:  P Forterre; F Confalonieri; F Charbonnier; M Duguet
Journal:  Orig Life Evol Biosph       Date:  1995-06       Impact factor: 1.950

5.  The origin of life--did it occur at high temperatures?

Authors:  S L Miller; A Lazcano
Journal:  J Mol Evol       Date:  1995       Impact factor: 2.395

6.  Impact constraints on the environment for chemical evolution and the continuity of life.

Authors:  V R Oberbeck; G Fogleman
Journal:  Orig Life Evol Biosph       Date:  1990       Impact factor: 1.950

7.  How long did it take for life to begin and evolve to cyanobacteria?

Authors:  A Lazcano; S L Miller
Journal:  J Mol Evol       Date:  1994-12       Impact factor: 2.395

8.  Hydrothermal and oceanic pH conditions of possible relevance to the origin of life.

Authors:  G MacLeod; C McKeown; A J Hall; M J Russell
Journal:  Orig Life Evol Biosph       Date:  1994-02       Impact factor: 1.950

Review 9.  Estimates of the maximum time required to originate life.

Authors:  V R Oberbeck; G Fogleman
Journal:  Orig Life Evol Biosph       Date:  1989       Impact factor: 1.950

10.  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

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