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Hydrothermally Associated Organic Microspheres from S. W. Africa and Elsewhere

  • George Mueller

Abstract

The bulk of the organic matter constituting the terrestrial carbosphere is present in a more or less finely divided state within water-deposited sediments. The oldest known sedimentary rocks, of some 3. 1 to 3.5 Bi. Y. Radiogenic Age, are from the Swaziland System of South Africa. Some structures in these sedimentary shales and cherts have been interpreted as possible micro-fossils (1), although the possibility that the particles in question may be inorganic microconcretions or organic artifices cannot be excluded. The small quantities of amino acids detected in the rocks (1) may be of ultimate pre-biological or biological origins, or they may be more recent contaminants.

Keywords

Organic Substance Quartz Crystal Prolate Spheroid Hydrothermal Deposit Hydrothermal Mineral 
These keywords were added by machine and not by the authors. This process is experimental and the keywords may be updated as the learning algorithm improves.

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Copyright information

© Plenum Press 1972

Authors and Affiliations

  • George Mueller
    • 1
  1. 1.Institute for Molecular and Cellular EvolutionUniversity of MiamiCoral GablesUSA

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