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Oxygen isotopic ratios of some evaporites from Precambrian to Recent ages
Authors:H Sakai
Institution:Institute for Thermal Spring Research, Okayama University, Misasa, Tottori-Pref., Japan
Abstract:The δ18O values of eighteen marine evaporites of Precambrian to Recent ages were found to vary from +8 to 25‰ relative to SMOW, while the δ34S values previously measured by Thode and Monster 2] vary from +10 to +38‰ relative to meteoritic sulfur. The results strongly suggest that the δ18O value of ocean sulfate varied with geologic age with a minimum at the Permian age.
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