By George V. Chilingar, Harold J. Bissell and Rhodes W. Fairbridge (Eds.)
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Extra resources for Carbonate Rocks Origin, Occurrence and Classification
4: 28-74. Chapter 2 MODERN CARBONATE SEDIMENTS WILLIAM H. TAFT Department of Geology, University of South Florida, Tampa, Fla. ) SUMMARY Modern carbonate sediments are accumulating in almost all depositional environments except for the very deep oceans. Chemical and physical conditions, however, govern preservation and abundance of carbonate relative to non-carbonate material. Most modern marine carbonate sediments owe their origin to accumulation of bioclastic debris. Rarely can inorganic precipitation be actually proven.
Factors affecting the aragonite/calcite ratios in carbonate-secreting organisms. J . , 62: 284-322. LOWENSTAM, H. , 1961. Mineralogy, 180/160 ratios, and strontium and magnesium contents of recent and fossil brachiopods and their bearing on the history of the oceans. J. , 69: 241-260. LOWENSTAM, H. , 1963. Biologic problems relating to the composition and diagenesis of sediments. In: T. W. D ~ N N E L(Editor), LY The Earth Sciences: Problems and Progress in Current Research. Univ. 137-195. LOWENSTAM, H.
Organisms, permanently attached to the sea bottom and possessing only slight tolerances to changes in chemical and physical environment, provide ideal working material for determination of isotopic composition in order to arrive at the temperature of depositional environment. Although there are a number of problems associated with interpreting stable isotope ratios of carbonate skeletons, nevertheless this technique is in its infancy and already a number of worth-while applications have been found.