. Bulletins of American paleontology. •• • tj^"?/* •• :•/ '^ • • •• . ••.V •• • 10 20 30 40 Inner FB 50 0. 10 20 30 40 Outer FB 50 0 10 20 30 40 White Water Bay SALINITY 10 20 30 40 50 0 Eastern Middle FB 10 20 30 40 Western Middle FB 50 0 10 20 30 40 Ten Thousand Islands Text-tigure 8.—Comparison of the linear relationship between carbon isotopic composition (DIC) and salinity for the six major areas designated in Text-figure 1. +, respectively, as compared to — and — for the precipitation. Florida Bay exhibits a wide range of 8"*0 values related to evaporation, pr


. Bulletins of American paleontology. •• • tj^"?/* •• :•/ '^ • • •• . ••.V •• • 10 20 30 40 Inner FB 50 0. 10 20 30 40 Outer FB 50 0 10 20 30 40 White Water Bay SALINITY 10 20 30 40 50 0 Eastern Middle FB 10 20 30 40 Western Middle FB 50 0 10 20 30 40 Ten Thousand Islands Text-tigure 8.—Comparison of the linear relationship between carbon isotopic composition (DIC) and salinity for the six major areas designated in Text-figure 1. +, respectively, as compared to — and — for the precipitation. Florida Bay exhibits a wide range of 8"*0 values related to evaporation, precipitation, and mixing with water derived from the Everglades, the Gulf of Mex- ico, and the Florida Reef Tract. The wide range of 8'*0 values was noted by Lloyd (1964) who was unable to exhibit any relationship between salinity and 8'^0. In contrast to the study of Lloyd (1964), the data in this study were collected within a temporal and spatial framework and consequently the apparent poor coitc- lation between salinity and 6'^0 noted by Lloyd can be explained by mixing between different end-mem- P CO -5 00 -^. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original Paleontological Research Institution (Ithaca, N. Y. ); Columbia University. Ithaca, N. Y. , Paleontological Research Institution [etc. ]


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