Corrections and Clarifications

Oxygen Isotope Fractionation in the System Dolomite-Calcite-Corbon Dioxide

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Science  13 May 1966:
Vol. 152, Issue 3724, pp. 997
DOI: 10.1126/science.152.3724.997

Abstract

In the report "Oxygen isotope fractionation in the system dolomite-calcite-carbon dioxide" by J. R. O'Neil and S. Epstein (8 April, p. 198), the last part of the first sentence should have read ". . . the oxygen isotopic compositions of each mineral of a pair are essentially the same (over a 7 per mil range)."