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- W967580135 abstract "Publisher Summary This chapter discusses Upper Eocene and Lower Oligocene section of Southwestern Alabama in United States of America. The Upper Eocene and Lower Oligocene section of Southwestern Alabama has been of particular interest to stratigraphers over the years because these strata represent one of the most complete exposed marine Eocene–Oligocene sections in North America. The Eocene–Oligocene contact is preserved in a limestone quarry. At St. Stephens Quarry and Little Stave Creek, the Eocene–Oligocene boundary, as recognized because of planktonic foraminifera, occurs at or near the top of the Shubuta Clay Member of the Yazoo Clay. The Eocene–Oligocene boundary is defined worldwide because of the change in planktonic foraminiferal assemblages across this datum. As recognized because of calcareous nannoplankton, the Eocene-Oligocene boundary at St. Stephens Quarry could be placed at the disconformity in the Pachuta Marl Member and at the top of the Pachuta Marl Member of the Yazoo Clay at Little Stave Creek." @default.
- W967580135 created "2016-06-24" @default.
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- W967580135 date "1986-01-01" @default.
- W967580135 modified "2023-09-24" @default.
- W967580135 title "Upper Eocene and Lower Oligocene Strata in Southwestern Alabama, U.S.A." @default.
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- W967580135 doi "https://doi.org/10.1016/s0920-5446(08)70118-3" @default.
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