Abstract
Nature 331, 513-516 (1988) IN this letter, Fig. 1 as printed is too small to allow the symbols to be properly differentiated. The figure is reprinted here with enlarged symbols. In addition, line 13 in the left-hand column on page 515 has become garbled by an error in a line correction. The first sentence in that paragraph should read: "Isotopic results obtained from residual clays (collected in situ from regolith profiles) of post-mid Tertiary age have 618O values between 17.
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