Abstract
The partition of elements between seawater and the marine solid phases (organisms and pelagic clays) is basically controlled by the same surface adsorption mechanisms as between soil pore water and the land solid phases (plants and soils). However, the elements in living organisms are separated into ‘biophile’ and ‘biophobe’ groups.
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Li, YH. Why are the chemical compositions of living organisms so similar?. Schweiz. Z. Hydrologie 46, 177–184 (1984). https://doi.org/10.1007/BF02538059
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DOI: https://doi.org/10.1007/BF02538059