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- W151239025 abstract "Benthic foraminiferal paleoenvironmental indices demonstrate that from late Eocene into earliest Oligocene time the Atlantic Ocean gradually became more corrosive and less fertile, from abyssal depths up to the slope. Development of glacial conditions in the early Oligocene (early in Anomaly 13 time) reversed the process; the CCD dropped, fertility increased, and higher levels of residual organic carbon were distributed from the slope to the lower bathyal zone." @default.
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- W151239025 date "1986-01-01" @default.
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- W151239025 title "Eocene/Oligocene Atlantic Paleo-Oceanography Using Benthic Foraminifera" @default.
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- W151239025 doi "https://doi.org/10.1016/s0920-5446(08)70125-0" @default.
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