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    AGU (American Geophysical Union)
    In:  Paleoceanography, 6 (1). pp. 1-20.
    Publication Date: 2016-09-02
    Description: Benthic δ18O data from 95 core sites are used to infer possible temperature-salinity (T-S) fields of the Atlantic and Pacific oceans at the Last Glacial Maximum (LGM). A constraint of stable density stratification yields logically consistent scenarios for both T and S. The solutions are not unique but are useful as a thinking tool. To better constrain the inferences drawn from the spatial distribution of benthic δ18O, we must reduce scatter in the δ18O data with more high-quality measurements in high sedimentation rate cores. Also, we must intercalibrate mass spectrometers at different isotope laboratories more accurately, to insure our isotope data are compatible.
    Type: Article , PeerReviewed
    Format: text
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