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By George V. Chilingar, Harold J. Bissell and Rhodes W. Fairbridge (Eds.)

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8: 137-148. PILKEY,0. H. and GOODELL, H. , 1964. Comparison of the composition of fossil and Recent mollusk shells. Bull. Geol. Soc. , 75: 217-228. PILKEY,0. H. , 1960. The effect of environment on the concentration of skeletal magnesium and strontium in Dendraster. J. , 68: 203-214. PURDY,E. , 1963a. Recent calcium carbonate facies of the Great Bahama Bank. 1. Petrography and reaction groups. J. , 71: 334-355. PURDY,E. , 1963b. Recent calcium carbonate facies of the Great Bahama Bank. 2. Sedimentary facies.

KRINSLEY, D. , 1959. Changes in the chemical composition of pteropod shells after deposition on the sea floor. J. , 33: 682-684. MODERN CARBONATE SEDIMENTS 49 LOWENSTAM, H. , 1954a. Environmental relations of modification compositions of certain carbonate secreting marine invertebrates. Proc. Natl. Acad. Sci. ,40: 3948. LOWENSTAM, H. , 1954b. 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.

ISOTOPIC COMPOSITION The relative abundance in sea water of the two stable isotopes of carbon (13C and W)and two of the three stable isotopes of oxygen (lSOand160) has been shown to be fairly constant in open-ocean environments. Nearshore environments, on the other hand, ai-e known to be deficient in I3C relative to I2C and in 1 8 0 relative to 1 6 0 , as compared to mean ocean water. These differences are attributed to: ( I ) higher degree of volatility of 12C and 1 6 0 during evaporation, and (2) dilution by freshwater runoff deficient in 1 8 0 and enriched in IZC.

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