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- W2022196197 abstract "Worthington (1968, Meteorological Monographs, 8, 63–67) hypothesized that the salinity of the upper waters of the ocean was markedly lowered during deglaciation by the influx of meltwater. This hypothesis receives support by a critical evaluation of published δ18O data on planktonic foraminifera from deep-sea cores. At least one such core, from the equatorial Atlantic, has a signal that is entirely comparable to the Gulf of Mexico results of Kennett and Shackleton (1975, Science, 188, 147–150). This similarity becomes apparent after an “unmixing” procedure is applied to the deep-sea core. There are important oceanographic and climatological consequences if a Worthington-type meltwater lid did indeed develop." @default.
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- W2022196197 title "Oxygen-18 stratigraphy in deep-sea sediments: additional evidence for the deglacial meltwater effect" @default.
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