The fundamental nature of life as a chemical system: the part played by inorganic elements.
In this article we show why inorganic metal elements from the environment were an essential part of the origin of living aqueous systems of chemicals in flow. Unavoidably such systems have many closely fixed parameters, related to thermodynamic binding constants, for the interaction of the essential exchangeable inorganic metal elements with both inorganic and organic non-metal materials. The binding constants give rise to fixed free metal ion concentration profiles for different metal ions and ligands in the cytoplasm of all cells closely related to the Irving-Williams series. The amounts of bound elements depend on the organic molecules present as well as these free ion concentrations. This system must have predated coding which is probably only essential for reproductive life. Later evolution in changing chemical environments became based on the development of extra cytoplasmic compartments containing quite different energised free (and bound) element contents but in feed-back communication with the central primitive cytoplasm which changed little. Hence species multiplied late in evolution in large part due to the coupling with the altered inorganic environment.
Williams
Robert J P
RJ
Inorganic Chemistry Laboratory, University of Oxford, South Parks Road, Oxford OX1 3QR, UK. bob.williams@chemistry.oxford.uk
D019418:Evolution, Chemical; D007287:Inorganic Chemicals / Q000737:chemistry / Q000378:metabolism*; D000069497:Origin of Life; D010084:Oxidation-Reduction; D013816:Thermodynamics
D007287:Inorganic Chemicals