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- W1987922182 abstract "In California, faunal parameters of planktonic foraminiferal assemblages change dramatically at the Lower-Middle Eocene boundary. By analogy with modern distributional data, these changes are interpreted to reflect alteration of the prevailing water-mass character from warm-temperate to temperate. The change from warm-temperate to temperate planktonic foraminiferal assemblages occurring over the California continental borderland is reconcilable with a minimum southward displacement of 15° latitude in water-mass boundaries and lends support to the concept of a bipolar Middle Eocene refrigeration." @default.
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- W1987922182 date "1971-04-01" @default.
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- W1987922182 title "MIDDLE EOCENE REFRIGERATION — NEW EVIDENCE FROM CALIFORNIA PLANKTONIC FORAMINIFERAL ASSEMBLAGES" @default.
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- W1987922182 doi "https://doi.org/10.1111/j.1502-3931.1971.tb01284.x" @default.
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