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Literature DB >> 600509

Chemical evolution and the evolution of the earth's crust.

Abstract

It is hypothesized that there is a close relationship between the geologic evolution of the global plates of the Earth's crust and the chemical evolution of life on the Earth. Characteristics of the axes of plate spreading are discussed in relation to postulated environments conductive to the synthesis of chemical compounds thought to be important biological precursors. Likely locations for in situ measurements to test the hypothesis are identified.

Mesh：

Year: 1977 PMID： 600509 DOI： 10.1007/bf00930683

Source DB: PubMed Journal: Orig Life ISSN： 0302-1688

5 in total

1. A production of amino acids under possible primitive earth conditions.

Authors: S L MILLER
Journal: Science Date: 1953-05-15 Impact factor: 47.728

2. Precambrian geologic history.

Authors: R B Hargraves
Journal: Science Date: 1976-07-30 Impact factor: 47.728

3. Evidence for compounds hydrolyzable to amino acids in aqueous extracts of apollo 11 and apollo 12 lunar fines.

Authors: K Harada; P E Hare; C R Windsor; S W Fox
Journal: Science Date: 1971-07-30 Impact factor: 47.728

4. Red sea hot brine area: revisited.

Authors: D A Ross
Journal: Science Date: 1972-03-31 Impact factor: 47.728

5. Evidence for extraterrestrial amino-acids and hydrocarbons in the Murchison meteorite.

Authors: K Kvenvolden; J Lawless; K Pering; E Peterson; J Flores; C Ponnamperuma; I R Kaplan; C Moore
Journal: Nature Date: 1970-12-05 Impact factor: 49.962

5 in total

4 in total

Chemical evolution and the evolution of the earth's crust.

1. A production of amino acids under possible primitive earth conditions.

2. Precambrian geologic history.

3. Evidence for compounds hydrolyzable to amino acids in aqueous extracts of apollo 11 and apollo 12 lunar fines.

4. Red sea hot brine area: revisited.

5. Evidence for extraterrestrial amino-acids and hydrocarbons in the Murchison meteorite.

1. Oligomerization of glycine and alanine catalyzed by iron oxides: implications for prebiotic chemistry.

Review 2. A possible energetic role of mineral surfaces in chemical evolution.

3. The synthesis of primitive 'living' forms: definitions, goals, strategies and evolution synthesizers.

4. Modelling of the prebiotic synthesis of oligopeptides: silicate catalysts help to overcome the critical stage.