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Revised Paleogene planktonic foraminiferal biozonation for the Austral Realm

机译:修订后的古近纪浮游有孔虫生物区带

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摘要

A major revision to the Antarctic Paleogene planktonic foraminifer biozonation is presented using the latest species concepts and biostratigraphic studies of Ocean Drilling Program (ODP) sites located between 52 degrees S and 65 degrees S paleolatitude in the southern South Atlantic and southern Indian Oceans. Shorthand prefixes for the Antarctic Paleogene zones are designated as "AP" zones for the "Antarctic Paleocene", "AE" zones for the "Antarctic Eocene", and "AO" zones for the "Antarctic Oligocene". New numerical ages for Paleogene planktonic foraminiferal and calcareous nannofossil first- and last-occurrence events are estimated using new age-depth curves constructed for ODP Sites 738 and 744 in the southern Indian Ocean. The order and timing of these events are compared with bio-, magneto- and chemostratigraphic datums that have been recently published, reinterpreted, or observed in the present study. The revised zonal framework and age models will improve correlation of Paleogene planktonic foraminifer pelagic and hemipelagic carbonate sequences within and outside the Austral Realm.
机译:利用南大西洋南部和印度洋南部古纬度介于52至65度之间的海洋钻探计划(ODP)站点的最新物种概念和生物地层研究,对南极古近纪浮游有孔虫生物区带进行了重大修订。将南极古近纪带的简写前缀指定为“南极古新世”的“ AP”带,“南极始新世”的“ AE”带和“南极渐新世”的“ AO”带。使用为印度洋南部ODP站点738和744构建的新的年龄-深度曲线,估算了古近纪浮游有孔虫和钙质纳米化石首次和最后发生的新的数字年龄。将这些事件的顺序和时间与最近在本研究中已发表,重新解释或观察到的生物,磁和化学地层学数据进行比较。修订后的区域框架和年龄模型将改善南界内外的古近纪浮游有孔虫浮游和半浮游碳酸盐序列的相关性。

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