By George V. Chilingar, Harold J. Bissell and Rhodes W. Fairbridge (Eds.)
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Extra info for Carbonate Rocks: Physical and Chemical Aspects
10-4 3 . 9. 9. 10-4 8 * 10-5; (microplankton): SUGAWARA et al. (1961) 7. I . 4. 10-3 30 (Peridiniaceae, Cyanophyceae) 11-25 (Diatomaceae) . 54 K. H. WOLF, G. V. CHlLlNGAR AND F. W. BEALES amounts larger than are concentrated by organisms 10-100 times that amount. Some of the elements present in the ocean in quantities less than are also organically utilized. Radioactivity of lake plankton reaches 100 times the radioactivity of the water in Quirke Lake, Ontario. (1937) and gave MASON(1958) discussed the work of WEBBand FEARON updated information on the elements found in biological material which can be classified as structural elements (C, H, N, 0, P, S, C1, Na, K, F, Mg, Si, Ca) and biocatalysts (Fe, Cu, B, Mn, I).
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Some invertebrates, upon adaptation to fresh-water conditions, lose Mg first of all from their marine “blood”. CHAW(1954a) found that, with the exception of a few cold-water calcitic forms, aragonitic skeletons are lower in Mg than the calcitic types, and that in all groups of calcitic organisms there is a linear or near linear relationship between the Mg content and the temperature (see also CHILINGAR, 1953, 1962a). CHAVE (1954a) also found that the total amount of Mg in skeletons decreases with an increase in phylogenetic level of the organisms.